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| − | [[Image:RobinsonWhopisgohifdohiwfEOHEFHatWarmsTheEarth.gif|right|frame]] | + | :''See also [[Counterexamples to Global Warming|Counterexamples to global warming]]'' |
| | + | [[File:UAH LT 1979 thru July 2023 v6 20x9-1.jpg|thumb|Global temperatures peaked in 2016, according to the UAH satellite temperature record for 1979-2023]] |
| | + | '''Anthropogenic global warming''' (AGW) is an unproven theory that insists human activity is causing the [[Earth]] to warm to catastrophic levels over time. The theory posits that [[greenhouse gas]]es, including [[carbon dioxide]], methane, nitrous oxide, and water vapor, trap solar warmth on the planet. Computer models suggest that industrial and vehicular emissions could lead to catastrophic warming. [[Leftist]]s use this theory as a basis to require cuts in energy production and consumption and to promote de-industrialization. |
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| − | '''Global Warming''' is any increase in average air temperature at the [[Earth]]'s surface over a period of decades or more. Since 1989, advocates have clashed on the issue of whether human beings are more responsible than nature for modern periods of global warming; see "[[greenhouse warming]]" and [[global warming theory]].<ref>Some people predicted Global warming is the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.
| + | The rate of warming predicted by AGW is far higher than what has been observed so far. Based on an average of 102 climate models, the UN's Intergovernment Panel of Climate Change (IPCC) predicts that the lower troposphere should be warming at a rate of 3.1 degrees per century.<ref name="SpencerCSP2">"[https://www.newcriterion.com//cm/images/THE%20CLIMATE%20SURPRISE%20PAMPHLET.pdf The Climate Surprise Pamphlet]", ''The New Criterion'', 2016. Taken from chart "All 3 Global Temperature Dataset Types Disagree with the Climate Model During the Period of Greatest Greenhouse Concentration."</ref> Satellite data shows that the lower troposphere warmed at a rate of 1.4 degrees per century between 1978 and 2021.<ref name="SpencerCSP">"[https://www.newcriterion.com//cm/images/THE%20CLIMATE%20SURPRISE%20PAMPHLET.pdf The Climate Surprise Pamphlet]", ''The New Criterion'', 2016.</ref><ref name=SpencerUAH>Spencer, Roy, "[https://www.drroyspencer.com/2021/ Archive for 2021]", 2019. This is data from the University of Alabama in Huntsville.</ref> Weather balloon data shows a warming trend of 1.6 degrees per century between 1958 and 2018.<ref>"[https://www1.ncdc.noaa.gov/pub/data/ratpac/ratpac-a/ RATPAC-A-annual-levels.txt.zip]", NOAA, National Centers for Environmental Information. Based on data for 850-300 mb.</ref> |
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| − | The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 year period ending in 2005, which is higher than the earlier estimate of 0.6 ± 0.2 °C for the period ending in 2000.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations"[1] via the greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3] These basic conclusions have been endorsed by at least 30 scientific societies and academies of science, including all of the national academies of science of the major industrialized countries. While individual scientists have voiced disagreement with the conclusions of the IPCC, the overwhelming majority of scientists working on climate change are in agreement with the conclusions.[4]
| + | An analysis of weather station data by U.S. climate researcher [[Roy Spencer]] shows no significant warming since 1943. Unlike the official weather station record, Spencer's data includes only those stations that recorded temperature at a consistent time of day.<ref name="Spencer" /> The heating predicted by AGW but not detected in the temperature record is sometimes said to be accumulating in the oceans. But a study by the Scripps Institution of Oceanography found that ocean temperature has risen by only 0.1 degree Celsius in the last fifty years.<ref>"[https://dailycaller.com/2018/01/05/new-study-shows-past-research-on-rising-ocean-temps-built-on-faulty-science/ New Study Shows Past Research On Rising Ocean Temps Built On Faulty Science]," ''The Daily Caller'', 01/05/2018.</ref>[[File:May, Andy, Climate history.png|thumb|right|The last 4,000 years of climate history, 2000 BC to AD 1992, by Andy May. Based on the GISP2 ice cores from central Greenland.]] |
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| − | Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[1] The range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a millennium even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]
| + | The theory that "greenhouse gases" have a greater warming effect than other gases goes back to the 19th century. The idea that carbon dioxide emissions might lead to catastrophic warming was introduced by Carl Sagan in the 1960s. He was inspired by research on the atmosphere of Venus. Around 1978, the environmental movement decided to promote Sagan's theory. The movement was already advocating energy conservation and renewables as a response to the "energy crisis." That is to say, a desired political outcome was agreed upon and then a "scientific" justification was developed. |
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| − | Increasing global temperature will cause sea level to rise, and is expected to increase the intensity of extreme weather events and to change the amount and pattern of precipitation. Other effects of global warming include changes in agricultural yields, trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.
| + | Proponents of the global warming theory advocate for conversion to electric vehicles without expanding the electric power grid, which can only be powered by coal-burning power plants, fossil fuel, or nuclear energy. So-called renewable energy sources, solar and wind, cannot provide enough capacity to recharge hundreds of millions of electric vehicles. |
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| − | Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. There is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences. Most national governments have signed and ratified the Kyoto Protocol, aimed at reducing greenhouse gas emissions.
| + | ==Difficulties with the theory== |
| − | Contents
| + | *'''Carbon dioxide is insignificant as a greenhouse gas.''' The level of CO<sub>2</sub> in the Earth's atmosphere is only 400 parts per million. Ninety to 95 percent of the greenhouse effect is due to water vapor.<ref>Friedenreich and Ramaswamy, "Solar Radiation Absorption by Carbon Dioxide, Overlap with Water, and a Parameterization for General Circulation Models," Journal of Geophysical Research 98 (1993):7255-7264</ref> The IPCC claims that water vapor acts as a "positive feedback," i.e. warming creates more humidity, which leads to additional warming. There are humidity measurements going back to 1948, and they show no upward trend.<ref>"[https://wattsupwiththat.com/global-climate/ global climate]," ''Watt's Up with That''</ref> More humidity could lead to more clouds and therefore to cooling and to negative feedback. So why assume positive feedback? AGW works only if water vapor is a positive feedback, so that is what the IPCC must claim.<br/>Although Obama has denounced elevated carbon dioxide levels as "carbon pollution," greenhouse operators commonly increase the level of CO<sub>2</sub> to 1,000 ppm or more to enhance plant growth.<ref>"[https://www.sciencedaily.com/releases/2015/12/151210101819.htm Plant growth enhanced by increased carbon dioxide, but food webs give rise to significant variations]", ''Science News'', December 10, 2015.<br/>Harrison H. Schmitt and William Happer, "[http://arizonaskywatch.com/article/articles/In%20defense%20of%20carbon%20dioxide.pdf In Defense of Carbon Dioxide]," ''Wall Street Journal'', May 8, 2013.</ref> |
| − | [hide] | + | [[Image:NASA-1024x933.jpg|thumb|right|A composite map of [[Antarctica]] showing areas of greatest warming in red. The Wilkins Ice Shelf lies off the peninsula in the top left corner, and shows extensive warming. Overall, Antarctica shows little warming, and many areas to the East (right) are almost cooling.<ref>Roberts, Greg (April 18, 2009). [http://www.news.com.au/antarctic-ice-is-growing-not-melting-away/story-0-1225700043191 "Antarctic ice is growing, not melting away."] News.com.au. Retrieved on September 25, 2014.</ref>]] |
| | + | *'''The Earth has warmed or cooled many times. Historically, warm periods are associated with favorable climate.''' The [[Roman Warm Period]] (250 BC to 180 AD) featured temperatures comparable to those of modern times. This was followed by the Dark Ages Cold Period (450-950 AD).<ref>"[http://www.co2science.org/subject/d/summaries/dacpeurope.php Dark Ages Cold Period (Europe) - Summary]", ''CO<sub>2</sub> Science'', 1 June 2005.</ref> The Medieval Warm Period was even warmer than the Roman period and lasted from 950 to 1300.<ref>John P. Rafferty, "[https://global.britannica.com/science/medieval-warm-period Medieval warm period (MWP)]", ''Britannica''</ref> From the 14th century to the early 19th century, there was a Little Ice Age.<ref>John P. Rafferty, Stephen T. Jackson, "[https://global.britannica.com/science/Little-Ice-Age Little Ice Age (LIA)]", ''Britannica''.</ref><ref>See the graphs at "[http://www.climate4you.com/ Global temperatures]," Climate4you.</ref><ref>Bastasch, Michael, "[https://dailycaller.com/2013/12/13/study-earth-was-warmer-in-roman-medieval-times/ Study: Earth was warmer in Roman, Medieval times]", ''The Daily Caller''. For a peer-reviewed paper, see Moberg, A., et al. 2005 "[ftp://ftp.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/moberg2005/nhtemp-moberg2005.txt 2,000-Year Northern Hemisphere Temperature Reconstruction]", ''World Data Center for Paleoclimatology''. The Moberg data set is charted [https://i0.wp.com/i90.photobucket.com/albums/k247/dhm1353/Moberg-1.png here].</ref> |
| | + | *'''Carbon dioxide can be absorbed by promoting plant growth, an angle overlooked by the mainstream media.''' In fact, the increase in carbon dioxide in the atmosphere has already resulted in an increase in plant growth. If that's not enough, iron filings can be dumped at sea to encourage the growth of marine plants.<ref>Carrington, Damian, "[https://www.theguardian.com/environment/2012/jul/18/iron-sea-carbon Dumping iron at sea can bury carbon for centuries, study shows]" ''The Guardian'', 18 July 2012.</ref> Freeman Dyson, America's top physicist, has suggested genetically engineering trees to absorb more carbon.<ref>"[https://www.youtube.com/watch?v=BiKfWdXXfIs Freeman Dyson on the Global Warming Hysteria April, 2015]." Dyson recommends ''Cool It'' (2007) by Bjorn Lomborg as the best summary of the AGW issue.</ref> |
| | + | *'''If the science were in fact settled, we would see less outrage at "deniers" and greater concern for scientific integrity.''' One climate science scandal after another has been exposed. The Climategate emails show hoaxers scurrying to "hide the decline."<ref name=MISH>"[http://globaleconomicanalysis.blogspot.com/2009/11/hackers-prove-global-warming-is-scam.html#quEdWPhB8b6cs07f.99 Beware The Ice Age Cometh: Hackers Prove Global Warming Is A Scam]", ''MISH'S Global Economic Trend Analysis''</ref> The "hockey stick" view of climate history, which holds that global temperature was constant for 2,000 years and then surged in the last century, has been repeatedly debunked.<ref>Muller, Richard A., "[http://www.technologyreview.com/Energy/13830/ A Global Warming Bombshell]", ''Technology Review'' , Oct. 2004; calls into question famous graph by Michael Mann.</ref> No one's reputation is tarnished by these bloopers, no one pays any price. The first response of AGW backers is name calling and attempts to shut down the discussion. Argument is a last resort.<ref>Phil Plait, columnist for ''Discover'', is a good example. Plait has only contempt for those who express concerns about scientific integrity in climate research: "yawn," "non-event," etc. With no sense of irony, he can write, "these denialist claims are largely ad hominems." If you fail to show "the scientists" enough respect, then you are a "global warming denier." This name-calling-as-argument strategy is typical of AGW hacks. (Phil Plait, "[http://blogs.discovermagazine.com/badastronomy/2009/11/30/the-global-warming-emails-non-event/#.WHMkC9J97cs The global warming emails non-event]," ''Discover'', November 30, 2009.)</ref> The logical explanation is that they already know AGW is a hoax, and they don't care. |
| | + | *'''For leftists, the attraction of the theory is that it supports their agenda.''' The environmentalist agenda of renewables, solar energy, conservation, and world government was put together in the 1970s in response to the energy crisis and to the overpopulation scare. At that time, most scientists thought the Earth was cooling.<ref>"[http://realclimatescience.com/the-corrupt-history-of-nasa-temperature-history/ The corrupt history of NASA temperature history]", ''Real Climate Science''.</ref><ref name="Time" /> When AGW came along, it was treated as an additional justification for this agenda.<br/>Steven Schneider, founding father of the AGW movement, was a global cooling believer in the early 1970s. "We have to offer up scary scenarios, make simplified, dramatic statements, and make little mention of any doubts we might have," he explained.<ref>This is from an article Schneider wrote for ''Discover'' magazine in 1989.[http://www.creationworldview.org/articles_view.asp?id=67]</ref> To Schneider, global cooling and global warming were just two "scary scenarios." He could offer up whichever one was expedient. |
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| − | * 1 Terminology
| + | == How accurate are weather forecasts and climate forecasts? == |
| − | * 2 Causes
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| − | o 2.1 Greenhouse gases in the atmosphere
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| − | o 2.2 Feedbacks
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| − | o 2.3 Solar variation
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| − | * 3 Temperature changes
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| − | o 3.1 Recent
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| − | o 3.2 Pre-human climate variations
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| − | * 4 Climate models
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| − | * 5 Attributed and expected effects
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| − | o 5.1 Economic
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| − | o 5.2 Security
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| − | * 6 Adaptation and mitigation
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| − | * 7 Social and political debate
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| − | * 8 Related climatic issues
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| − | * 9 See also
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| − | * 10 References
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| − | * 11 Further reading
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| − | * 12 External links
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| − | Terminology
| + | In 2013, ''Scientific American'' published an article entitled ''Why Are Weather Forecasts Often Wrong?''<ref>[https://www.scientificamerican.com/article/why-are-weather-forecasts-often-wrong/ ''Why Are Weather Forecasts Often Wrong?''] By Lee Falin PhD on January 9, 2013, ''Scientific American''</ref> |
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| − | The term "global warming" is a specific example of the broader term climate change, which can also refer to global cooling. In common usage, the term refers to recent warming and implies a human influence.[5] The United Nations Framework Convention on Climate Change (UNFCCC) uses the term "climate change" for human-caused change, and "climate variability" for other changes.[6] The term "anthropogenic global warming" is sometimes used when focusing on human-induced changes.
| + | In 2020, data from the National Oceanic and Atmospheric Administration suggests a seven-day weather forecast by a [[meteorology|meteorologist]] could accurately predict the weather about 80 percent of the time.<ref>[https://www.mprnews.org/story/2020/01/02/forecast-models-keep-hinting-at-subzero-air-ahead How accurate are forecast models 1 to 2 weeks ahead?]</ref><ref>[https://www.wral.com/how-accurate-are-weather-forecasts/19645159/#:~:text=Longer%2Drange%20forecasts%20are%20less,90%20percent%20of%20the%20time. How accurate are weather forecasts?], WRAL</ref> However, beyond 10 days, a weather forecast is only right about half the time.<ref>[https://www.wral.com/how-accurate-are-weather-forecasts/19645159/#:~:text=Longer%2Drange%20forecasts%20are%20less,90%20percent%20of%20the%20time. How accurate are weather forecasts?], WRAL</ref> |
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| − | Causes
| + | The accuracy of the long-range forecasts of climate scientists' that are 10 years or decades ahead of time are of dubious value (See: [[Limitations of science]]). In addition, environmentalists have a history of making alarmist statements that do not come to fruition (see: [https://www.aei.org/carpe-diem/50-years-of-failed-doomsday-eco-pocalyptic-predictions-the-so-called-experts-are-0-50/ 50 years of failed doomsday, eco-pocalyptic predictions; the so-called ‘experts’ are 0-50], American Enterprise Institute). |
| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Main articles: Attribution of recent climate change and scientific opinion on climate change
| + | == A significant resistance to global warming alarmism is developing in Europe == |
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| − | The Earth's climate changes in response to external forcing, including variations in its orbit around the sun (orbital forcing),[7][8][9] volcanic eruptions, and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[10][11] identifies elevated levels of greenhouse gases due to human activity as the main influence. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain the observed increase in mean global temperature. One such hypothesis proposes that warming may be the result of variations in solar activity.[12][13][14]
| + | News reports of Europeans becoming increasingly resistant to global warming alarmism: |
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| − | None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[15]
| + | *The Daily Telegraph (Ross Clark): “[https://archive.md/XbVaC The EU's Net Zero plan is in tatters - and not a moment too soon]” (29 March 2023) |
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| − | Greenhouse gases in the atmosphere
| + | *Reuters (Riham Alkousaa): “[https://www.reuters.com/business/environment/berlin-votes-tighter-climate-goals-test-germans-commitment-change-2023-03-26/ Berliners vote down referendum on tighter climate goals]” (26 March 2023) |
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| − | Main article: Greenhouse effect
| + | *Politico (Nicolas Camut): “[https://www.politico.eu/article/dutch-farmers-party-bbb-mark-rutte-netherlands-big-winner-in-provincial-elections/ Dutch pro-farmers party wins big in provincial elections]” (16 March 2023) |
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| − | The greenhouse effect was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. It is the process by which absorption and emission of infrared radiation by atmospheric gases warm a planet's atmosphere and surface.
| + | *Express (Natalie Crookham): “[https://www.express.co.uk/life-style/cars/1752831/petrol-diesel-car-ban-poll-result-spt Staggering poll shows 93 percent oppose 2030 petrol and diesel car ban] [UK]” (30 March 2023) |
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| − | Existence of the greenhouse effect as such is not disputed. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F), without which Earth would be uninhabitable.[16][17] Rather, the issue is how the strength of the greenhouse effect is changed when human activity increases the atmospheric concentrations of some greenhouse gases.
| + | ''Forbes'' reported in 2023: |
| | + | {{Cquote|The editors of one leading paper put it like this: “The implausibility of a net-zero carbon energy future is becoming so obvious that even Europeans are starting to notice.” The shock news of Germany’s decision to block the EU-wide agreement on the combustion engine ban by 2035 is “threatening to unravel Germany’s three-party governing alliance, after the Green party accused its liberal coalition partners of gambling away the country’s [green] reputation…” The German government wants to replace this ban and permit combustion engine cars running on synthetic “e-fuels”. E-fuels are yet another unproven technology but, if somehow viable in the future, would at least preserve the country’s vaunted position in automobile combustion engines. That Western Europe’s reigning green ideologues could be blocked by the German car manufacturers’ lobby – one of the country’s industrial pillars and a major employer – seems to signal the victory of economic rationality over climate ideology in this instance at least. |
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| − | On Earth, the major greenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect (not including clouds); carbon dioxide (CO2), which causes 9–26%; methane (CH4), which causes 4–9%; and ozone, which causes 3–7%.[18][19] Some other naturally occurring gases contribute very small fractions of the greenhouse effect; one of these, nitrous oxide (N2O), is increasing in concentration owing to human activity such as agriculture. The atmospheric concentrations of CO2 and CH4 have increased by 31% and 149% respectively above pre-industrial levels since 1750. Molecule for molecule, methane is a more effective greenhouse gas than carbon dioxide, but its concentration is much smaller so that its total radiative forcing is only about a fourth of that from carbon dioxide. These levels are considerably higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores. From less direct geological evidence it is believed that CO2 values this high were last attained 20 million years ago.[20] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, in particular deforestation.[21]
| + | The country’s green advocates received further bad news as voters in the Berlin referendum for a climate-neutral city by 2030 failed resoundingly as “yes” votes failed to achieve the 25% quorum of all eligible voters needed to make the referendum valid. According to critics interviewed by [[Bild]], the radical climate project pushed in the referendum is “factually impossible” and “out of the question”, noting that “even the original 2045 target timetable [is] almost impossible to meet.” Even Berlin’s uber-green elites could not swing the vote against the average city-dweller sick of hot water rationing, dimmed street lights at night and shuttered swimming pools.<ref>[https://www.forbes.com/sites/tilakdoshi/2023/04/08/climate-hysteria-in-the-dark-age-are-we-seeing-glimmers-of-light/?sh=3e1b70c14c09 Climate Hysteria In The Dark Age: Are We Seeing Glimmers Of Light?], Forbes, April 2023</ref>}} |
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| − | The present atmospheric concentration of CO2 is about 383 parts per million (ppm) by volume.[22] Future CO2 levels are expected to rise due to ongoing burning of fossil fuels and land-use change. The rate of rise will depend on uncertain economic, sociological, technological, and natural developments, but may be ultimately limited by the availability of fossil fuels. The IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[23] Fossil fuel reserves are sufficient to reach this level and continue emissions past 2100, if coal, tar sands or methane clathrates are extensively used.[24] | + | == The Surprising Truth: Extremely Small, Almost Statistically Insignificant, Temperature Rises per Decade == |
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| − | Feedbacks
| + | Even mainstream sites admit the empirical fact: "For the last 50 years, global temperature rose at an average rate of about 0.13°C (around one-quarter degree Fahrenheit) per decade-almost twice as fast as the 0.07°C per decade increase observed over the previous half-century. In the next 20 years, scientists project that global average temperature will rise by around 0.2°C (about one-third of a degree Fahrenheit) per decade." <ref>https://www.climate.gov/news-features/videos/history-earths-temperature-1880</ref> This means, even at the allegedly "high" rate of temperature rise of "around 0.2°C", Global Temperatures will only rise by around 1°C in the next 50 years! Hardly a cause for Alarmism on this issue, especially in light of numerous well documented alarmist false predictions of Climate Change Hoaxers. |
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| − | Main article: Effects of global warming#Further global warming (positive feedback)
| + | == 5 of 18 Ridiculous and Spectacularly Wrong Alarmist Global Warming Predictions around 1970 that never came to pass == |
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| − | The effects of forcing agents on the climate are complicated by various feedback processes.
| + | When the Holy Bible warns us to beware of False Prophets (Deut 18:17-22, [[Matthew, Chapter 7#15|Matthew 7:15-20]]), that divine injunction certainly includes the False Prophets of Global Warming. |
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| − | One of the most pronounced feedback effects relates to the evaporation of water. In the case of warming by the addition of long-lived greenhouse gases such as CO2, the initial warming will cause more water to be evaporated into the atmosphere. Since water vapor itself acts as a greenhouse gas, this causes still more warming; the warming causes more water vapor to be evaporated, and so forth until a new dynamic equilibrium concentration of water vapor is reached with a much larger greenhouse effect than that due to CO2 alone. Although this feedback process involves an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[25] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.
| + | "1. Harvard biologist George Wald estimated that “civilization will end within 15 or 30 years [by 1985 or 2000] unless immediate action is taken against problems facing mankind.” |
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| − | Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models. Nevertheless, cloud feedback is second only to water vapor feedback and is positive in all the models that were used in the IPCC Fourth Assessment Report.[25]
| + | 2. “We are in an environmental crisis that threatens the survival of this nation, and of the world as a suitable place of human habitation,” wrote Washington University biologist Barry Commoner in the Earth Day issue of the scholarly journal Environment. |
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| − | Another important feedback process is ice-albedo feedback.[26] When global temperatures increase, ice near the poles melts at an increasing rate. As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.
| + | 3. The day after the first Earth Day, the New York Times editorial page warned, “Man must stop pollution and conserve his resources, not merely to enhance existence but to save the race from intolerable deterioration and possible extinction.” |
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| − | Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism contributing to warming.[27] A massive release of CH4 from methane clathrates could cause rapid warming, according to the clathrate gun hypothesis.
| + | 4. “Population will inevitably and completely outstrip whatever small increases in food supplies we make,” Paul Ehrlich confidently declared in the April 1970 issue of Mademoiselle. “The death rate will increase until at least 100-200 million people per year will be starving to death during the next ten years [by 1980].” |
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| − | The ocean's ability to sequester carbon is expected to decline as it warms, because the resulting low nutrient levels of the mesopelagic zone limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[28]
| + | 5. “Most of the people who are going to die in the greatest cataclysm in the history of man have already been born,” wrote Paul Ehrlich in a 1969 essay titled “Eco-Catastrophe! “By…[1975] some experts feel that food shortages will have escalated the present level of world hunger and starvation into famines of unbelievable proportions. Other experts, more optimistic, think the ultimate food-population collision will not occur until the decade of the 1980s.”<ref>https://www.aei.org/carpe-diem/18-spectacularly-wrong-predictions-were-made-around-the-time-of-the-first-earth-day-in-1970-expect-more-this-year/</ref> |
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| − | Solar variation
| + | == Who is behind the Global Warming Agenda? Communist China and [[Comsymp]]s at the UN == |
| − | Solar variation over the last 30 years.
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| − | Solar variation over the last 30 years.
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| − | Main article: Solar variation
| + | A careful analysis of the Evil Agenda behind the attempt to promote Global Warming Narratives suggests Communist Countries want to use this as a means to reduce the energy production of the Christian and Western World or to make them dependent on Communist Countries: "As evidence discredits global warming, resistance to such facts by green elites reveals their real aim is bringing socialism in through the back door. But don't take our word for it. Listen to the climate change boss at the U.N. |
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| − | A few papers suggest that the Sun's contribution may have been underestimated. Two researchers at Duke University, Bruce West and Nicola Scafetta, have estimated that the Sun may have contributed about 45–50% of the increase in the average global surface temperature over the period 1900–2000, and about 25–35% between 1980 and 2000.[29] A paper by Peter Stott and other researchers suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.[30] They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases.
| + | Christiana Figueres, with the lumpy title of executive secretary of the United Nations Framework Convention on Climate Change (UNFCCC), came right out and said it: Democracy is a poor political system for fighting global warming. The really good model is communist China."<ref>https://www.investors.com/politics/editorials/climate-change-a-back-door-to-communism-and-the-united-nations-admits-it/</ref> |
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| − | A different hypothesis is that variations in solar output, possibly amplified by cloud seeding via galactic cosmic rays, may have contributed to recent warming.[31] It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.[32]
| + | ==History== |
| | + | The greenhouse effect was proposed by [[Joseph Fourier]] in 1827. Swedish scientist Svante Arrhenius is sometimes considered the father of global warming theory because of a paper he published in 1896 on the effect of carbon dioxide emissions. Arrhenius thought of global warming as a positive thing. The idea that carbon dioxide emissions might lead to catastrophe comes from research on the Venusian atmosphere in the 1960s by Karl Sagan and other NASA scientists. In the 1970s, global cooling theories were more prominent than global warming theories. Even Steven Schneider, later a promoter of global warming, published a paper on global cooling. As a result of the energy crisis of the 1970s, the environmentalist movement adopted an agenda of conservation and renewable energy. With global warming as its flagship theory, the movement could continue promoting its 1970s agenda long after the original justifications for it had disappeared. Schneider offered up "scary scenarios," as he called them, to promote the theory. |
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| − | One predicted effect of an increase in solar activity would be a warming of the stratosphere; however, the observed effect since at least 1960 has been a cooling of the lower stratosphere, which is one of the predicted results of greenhouse gas warming.[33] Reduction of stratospheric ozone also has a cooling influence, although substantial ozone depletion did not occur until the late 1970s. Solar variation combined with changes in volcanic activity probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.[1] In 2006, Peter Foukal and other researchers from the United States, Germany, and Switzerland found no net increase of solar brightness over the last thousand years. Solar cycles led to a small increase of 0.07% in brightness over the last 30 years. This effect is far too small to contribute significantly to global warming.[34][35] A paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in cosmic rays.[36] Henrik Svensmark and Eigil Friis-Christensen, the main proponents of cloud seeding by galactic cosmic rays, disputed the findings of Lockwood and Fröhlich.[37] Another recent study speculates that other bodies within the Solar System may influence the climate in a complex manner.[38]
| + | ===Origin=== |
| | + | In 1827, French scientist Joseph Fourier suggested that although the atmosphere allowed sunlight to pass through to warm the Earth, it blocked "dark heat" (infrared radiation) from the Earth and thus prevented energy from being transferred back into space.<ref name=Fourier>Fourier, Jean Baptist Joseph, "On the Temperatures of the Terrestrial Sphere in Interplanetary Space", Translated in ''The Warming Papers: The Scientific Foundation for Climate Change Forecast''. The relevant section is pp. 12-13.</ref> Fourier did make an unfortunate analogy between the Earth's atmosphere and a space enclosed by glass. All the same, it may not be fair to blame Fourier for the greenhouse effect meme. He also discussed convection as an alternative explanation and, as a good scientist, recommended an experiment to resolve the issue. |
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| − | Temperature changes
| + | In 1861, Irish scientist John Tyndall measured the absorption of radiant energy by various gases in the atmosphere. He concluded that water vapor was the gas primarily responsible. It could therefore be considered the warming agent that Fourier hypothesized. Tyndall suggested that changes in humidity could bring about climate change. |
| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Main article: Temperature record
| + | The AGW theory was first presented in 1896 in an article by Swedish scientist Svante Arrhenius. Arrhenius predicted that a doubling of CO<sub>2</sub> in the atmosphere due to fossil fuel burning would lead to a temperature increase of 3 to 4 °C (about 5 to 7 °F) after 500 years. Arrhenius attributes his misunderstanding of the science to Fourier: "Fourier maintained that the atmosphere acts like the glass of a hothouse."<ref>Arrhenius, Svante, "On the Influence of Carbonic Acid in the Air on the Temperature on the Ground", ''London, Edinburgh, and Dublin Philosophical Magazine and Journal of Science,'' April 1896. Reprinted in ''The Warming Papers'', pp. 56-77.</ref> |
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| − | Recent
| + | The use of the Swedish word ''drivbänk'' (hothouse) by Arrhenius and his colleagues is likely to be the origin of the phrase "greenhouse effect." This phrase is first recorded in English in 1907.<ref>"[http://www.easterbrook.ca/steve/2015/08/who-first-coined-the-term-greenhouse-effect/ Who first coined the term “Greenhouse Effect”?]," ''Serendipity,'' August 2015</ref> |
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| − | Global temperatures on both land and sea have increased by 0.75 °C (1.35 °F) relative to the period 1860–1900, according to the instrumental temperature record. This measured temperature increase is not significantly affected by the urban heat island effect.[39] Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[40] Temperatures in the lower troposphere have increased between 0.12 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with possibly regional fluctuations such as the Medieval Warm Period or the Little Ice Age.
| + | ===The skeptics strike back=== |
| | + | Arrhenius ignored water vapor in his calculations, leading him to overestimate the effect of CO<sub>2</sub> by 96 percent, as Knut Ångström observed in 1901.<ref>"[https://realclimatescience.com/2016/12/climate-scientists-celebrating-115-years-of-debunked-science/ Climate Scientists Celebrating 115 Years Of Debunked Junk Science]"</ref> More controversially, Ångström questioned whether CO<sub>2</sub> could act as a greenhouse gas at all. He took a tube of carbon dioxide, shined black-body radiation on it, and varied the pressure on the gas. Increasing the pressure led to only a slight increase in absorption. He concluded that radiation absorption by CO<sub>2</sub> is already nearly saturated, so the emission of additional gas into the atmosphere would have little effect. Ångström thus became "the first denier." |
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| − | Sea temperatures increase more slowly than those on land both because of the larger effective heat capacity of the oceans and because the ocean can lose heat by evaporation more readily than the land.[41] Since the Northern Hemisphere has more land mass than the Southern Hemisphere it warms faster; also there are extensive areas of seasonal snow cover subject to the snow-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the asymmetry of warming as the major gases are essentially well-mixed between hemispheres.
| + | Nils Ekholm, an associate of Arrhenius, had an answer to Ångström's point about saturation.<ref>Ekholm, Nils, "On the Variations of the Geological and Historical Past their Causes, ''Quarterly Journal of the Royal Meteorological Society,'' January 1901. DOI: 10.1002/qj.49702711702.</ref> Ångström's tube was saturated because it was at ground level. High enough in the atmosphere, there must be an unsaturated layer of carbon dioxide capable of absorbing radiation. The greater the density of carbon dioxide in the atmosphere, the lower this layer would be. A lower layer would retransmit more radiation to the lower atmosphere and would therefore be responsible for greater warming. Ekholm's insight was lost on his fellow scientists. It was not rediscovered until the 1960s.<ref>"The Surface budget fallacy," ''The Warming Papers'', pp. 79-80.</ref> |
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| − | Based on estimates by NASA's Goddard Institute for Space Studies, 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[42] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit concluded that 2005 was the second warmest year, behind 1998.[43][44]
| + | As for Ångström's point concerning water vapor, Arrhenius insisted that CO<sub>2</sub> rose higher in the atmosphere than water vapor could, so water vapor was not relevant. This argument never caught on. The idea that adding CO<sub>2</sub> would change the climate, "was never widely accepted and was abandoned when it was found that all the long-wave radiation [that would be] absorbed by CO<sub>2</sub> is [already] absorbed by water vapor," the American Meteorological Society concluded in 1951.<ref>American Meteorological Society, ''[https://www.questia.com/read/97549786/compendium-of-meteorology 1951 Compendium of Meteorology]'', p. 1016.</ref> Despite Ångström's debunking of his theory, Arrhenius won the Nobel prize for chemistry in 1903 for unrelated research. The Ångströms, meanwhile, are remembered for a miniscule unit of length named after Anders Ångström, Knut's dad. |
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| − | Anthropogenic emissions of other pollutants—notably sulfate aerosols—can exert a cooling effect by increasing the reflection of incoming sunlight. This partially accounts for the cooling seen in the temperature record in the middle of the twentieth century,[45] though the cooling may also be due in part to natural variability. James Hansen and colleagues have proposed that the effects of the products of fossil fuel combustion—CO2 and aerosols—have largely offset one another, so that warming in recent decades has been driven mainly by non-CO2 greenhouse gases.[46]
| + | ===Disproving the greenhouse effect=== |
| | + | Finally performing the experiment Fourier had recommended a century earlier, Robert Wood showed in 1909 that energy is transferred from the Earth's surface to the atmosphere primarily through convection currents. In Wood's experiment, the temperature in a glass box was compared to that in a box with a top made of halite (rock salt). Halite allows sunlight to enter, but blocks infrared. Infrared re-radiation and the greenhouse effect play "a very small part," both in the atmosphere and in literal greenhouses, Wood concluded.<ref>Wood, Robert, "[http://www.tech-know-group.com/papers/Note_on_the_Theory_of_the_Greenhouse.pdf Note on the Theory of the Greenhouse]", ''Philosphical Magazine'', January—June 1909.<br/>"[http://hockeyschtick.blogspot.jp/2010/06/greenhouse-theory-disproven-in-1909.html Greenhouse Theory disproven in 1909, 1963, 1966, 1973...but still refuses to die]," June 28, 2010.<br/>Gerhard Gerlich and Ralf D. Tscheuschner, "[https://arxiv.org/PS_cache/arxiv/pdf/0707/0707.1161v4.pdf Falsification Of The Atmospheric CO<sub>2</sub> Greenhouse Effects Within The Frame Of Physics]"</ref> A greenhouse is warmer than the air outside because the roof limits convection and the walls restrict wind. "The acquired heat is concentrated, because it is not dissipated immediately by renewing the air," as Fourier himself explained.<ref name="Fourier" /> |
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| − | Paleoclimatologist William Ruddiman has argued that human influence on the global climate began around 8,000 years ago with the start of forest clearing to provide land for agriculture and 5,000 years ago with the start of Asian rice irrigation.[47] Ruddiman's interpretation of the historical record, with respect to the methane data, has been disputed.[48]
| + | From 1909 until the 1960s, only a few additional papers on AGW were published. Research went forward as the lonely project of English scientist Guy Callendar. Callendar collected historical temperature readings and CO<sub>2</sub> measurements and published the results in 1938.<ref>Callendar, G.S. (1938). "The Artificial Production of Carbon Dioxide and Its Influence on Climate." ''Quarterly J. Royal Meteorological Society'' 64: 223-40. Reprinted in ''The Warming Papers'', pp. 261-273.</ref> |
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| − | Pre-human climate variations
| + | ===Sagan and Venus=== |
| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
| + | In 1932, Venus was shown to have an atmosphere of carbon dioxide.<ref>"Carbon Dioxide Discovered in Atmosphere of Venus", Astronautics, Vol. 2, No. 21 (1932), pp. 6-7. https://dx.doi.org/10.2514/8.11921</ref> This finding prompted astronomer Rupert Wildt to propose in 1940 that a greenhouse effect operated on the planet. Radio telescope observations in 1958 showed that the temperature of Venus was even higher than Wildt's theory could explain. Astronomer Carl Sagan proposed in 1960 that the planet had a “very efficient greenhouse effect,” or runaway greenhouse as it later came to be called.<ref>Weart, Spencer, "[http://history.aip.org/history/climate/pdf/venus.pdf Venus & Mars]", June 2011.</ref><ref>Sagan, Carl, "[http://science.sciencemag.org/content/133/3456/849 The Planet Venus]", ''Science'', 24 March 1961.</ref> The Mariner 2 mission in 1962 measured the temperature of Venus as 500 degrees Celsius. The planet that had been considered "Earth's twin" just a few years earlier was revealed as a sulfurous vision of hell. |
| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Further information: Paleoclimatology
| + | Mariner's findings were sensational because they had been predicted by Immanuel Velikovsky in ''Worlds in Collision'' (1950), which argues that Venus was ejected from Jupiter in mythological times. The scientific community had denounced Velikovsky and his theory in the strongest terms, and Sagan emerged as its champion. Sagan and Velikovsky faced off at a dramatic conference in San Francisco in 1974.<ref>AAAS Symposium: "Velikovsky's Challenge to Science" held on February 25, 1974.</ref> |
| − | See also: Snowball Earth
| |
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| − | Earth has experienced warming and cooling many times in the past. The recent Antarctic EPICA ice core spans 800,000 years, including eight glacial cycles timed by orbital variations with interglacial warm periods comparable to present temperatures.[49]
| + | By portraying carbon dioxide as a doomsday chemical, Sagan put a radically new spin on the issue. Both Arrhenius and Callendar had assumed that greenhouse warming would be beneficial. With Rachel Carson's ''Silent Spring'' (1962), Paul R. Ehrlich's ''The Population Bomb'' (1968), and the Club of Rome's ''The Limits to Growth'' (1972), this was an era when the reading public had an enormous appetite for spurious theories concerning human-initiated global catastrophe. |
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| − | A rapid buildup of greenhouse gases caused warming in the early Jurassic period (about 180 million years ago), with average temperatures rising by 5 °C (9 °F). Research by the Open University indicates that the warming caused the rate of rock weathering to increase by 400%. As such weathering locks away carbon in calcite and dolomite, CO2 levels dropped back to normal over roughly the next 150,000 years.[50][51]
| + | While the Venus discoveries ignited a burst of interest in AGW, they did nothing to shore up its scientific merits. In 1971, Russian climatologist Mikhail Budyko gave a speech to a large international conference in Leningrad in which he presented an alarmist AGW scenario. Reaction was strongly negative. It was clear that AGW was very much a minority opinion among scientists at this time. A quick look at Venus reveals that the atmosphere is opaque due to globe-spanning sulfur dioxide clouds. These clouds are 30 to 40 km thick. No sunlight reaches the surface.<ref>NASA's "[http://nssdc.gsfc.nasa.gov/planetary/factsheet/venusfact.html Venus Fact Sheet]" gives the planet's diurnal temperature range as zero, i.e. no difference between night and day on the surface.</ref> It follows that the planet has no greenhouse effect whatsoever. |
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| − | Sudden releases of methane from clathrate compounds (the clathrate gun hypothesis) have been hypothesized as a cause for other warming events in the distant past, including the Permian-Triassic extinction event (about 251 million years ago) and the Paleocene-Eocene Thermal Maximum (about 55 million years ago).
| + | In a runaway greenhouse, the greenhouse effect vaporizes additional water, which in turn increases the greenhouse effect. This leads to even more water vaporization and so on in a cycle of positive feedback. Venus has very little water of any kind, so Sagan's runaway greenhouse is not possible.<ref name=pierre>*Raymond T. Pierrehumbert, ''[https://books.google.ca/books?id=bO_U8f5pVR8C&source=gbs_navlinks_s Principles of Planetary Climate]'', pp. 14-15.<br />*Anthony Watts explains why Sagan's theory is "beyond absurd" in "[https://wattsupwiththat.com/2010/05/06/hyperventilating-on-venus/ Hyperventilating on Venus]," May 6, 2010.</ref> Whatever the chemistry of the Venusian atmosphere, water vapor absorbs a wider spectrum of radiation than carbon dioxide does and remains the primary greenhouse gas in the terrestrial atmosphere, as Tyndall showed long ago. |
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| − | Climate models
| + | Venus research proved to be an incubator for AGW showboaters. James “Boiling Oceans” Hansen, who emerged as the public face of AGW in the late 1980s, was a NASA Venus researcher in the 1960s. Overlooking Hansen's history of following one kook theory after another, the mainstream media treated his talk of "runaway greenhouse" and "Venus syndrome" as serious science.<ref>Sullivan, John, "[https://johnosullivan.wordpress.com/2012/05/20/top-scientists-vent-on-nasas-sub-prime-greenhouse-gas-hoaxere-optional/ Top Scientists Vent on NASA’s Sub Prime Greenhouse Gas Hoaxer]", May 20, 2012. "The oceans will begin to boil," Hansen announces in [https://wattsupwiththat.com/2012/01/12/quote-of-the-week-dr-james-hansen-of-nasa-giss-unhinged/ this video]. In his book, ''Storms of my Grandchildren'', Hansen writes: "[I]f we burn all reserves of oil, gas, and coal, there is a substantial chance we will initiate the runaway greenhouse. If we also burn the tar sands and tar shale, I believe the Venus syndrome is a dead certainty."</ref> |
| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
| |
| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
| |
| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
| |
| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F). | |
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| − | Main article: Global climate model
| + | Hansen's claim that continued CO<sub>2</sub> emissions will trigger a runaway greenhouse on Earth is unlikely in view of the Earth's recovery after the Paleocene-Eocene Thermal Maximum (PETM), a huge natural spike in CO<sub>2</sub> that occurred 55.5 million years ago.<ref>Kunzig, Robert, "[http://news.nationalgeographic.com/news/2013/13/130729-runaway-greenhouse-global-warming-venus-ocean-climate-science/ Will Earth's Ocean Boil Away?]", ''National Geographic'', July 30, 2013.</ref> During PETM, the carbon dioxide level in the atmosphere increased by about 700 ppm over 20,000 years and the planet warmed by 5–8 degrees Celsius.<ref>McInherney, F.A..; Wing, S. (2011). "A perturbation of carbon cycle, climate, and biosphere with implications for the future". Annual Review of Earth and Planetary Sciences. 39: 489–516. Bibcode:2011AREPS..39..489M. doi:10.1146/annurev-earth-040610-133431</ref> Plant growth accelerated and there was a return to pre-PETM conditions after 200,000 years.<ref>Gabriel J. Bowen & James C. Zachos, "Rapid carbon sequestration at the termination of the Palaeocene–Eocene Thermal Maximum", ''Nature'' Geoscience 3, 866–869 (2010) doi:10.1038/ngeo1014</ref> Although this event is sometimes presented as confirmation of the greenhouse concept, warming preceded the CO<sub>2</sub> spike by about 3,000 years<ref>Sluijs, A.; Brinkhuis, H.; Schouten, S.; Bohaty, S.M.; John, C.M.; Zachos, J.C.; Reichart, G.J.; Sinninghe Damste, J.S.; Crouch, E.M.; Dickens, G.R. (2007). "Environmental precursors to rapid light carbon injection at the Palaeocene/Eocene boundary". Nature. 450 (7173): 1218–21. Bibcode:2007Natur.450.1218S. doi:10.1038/nature06400. PMID 18097406.</ref> and may have been initiated by a comet impact.<ref>[https://wattsupwiththat.com/tag/petm/ Study: Extraterrestrial impact preceded ancient global warming event]", October 13, 2016.<br/>Morgan F. Schaller, Megan K. Fung, James D. Wright, Miriam E. Katz, Dennis V. Kent, "[http://science.sciencemag.org/content/354/6309/225.full Impact ejecta at the Paleocene-Eocene boundary]", ''Science'', 14 Oct 2016: |
| | + | Vol. 354, Issue 6309, pp. 225-229 DOI: 10.1126/science.aaf5466.</ref> |
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| − | Scientists have studied global warming with computer models of the climate. These models are based on physical principles of fluid dynamics, radiative transfer, and other processes, with simplifications being necessary because of limitations in computer power and the complexity of the underlying system (climate). These models predict that the effect of adding greenhouse gases is to produce a warmer climate.[52] However, even when the same assumptions of future greenhouse gas levels are used, there still remains a considerable range of climate sensitivity.
| + | ===From cooling to warming=== |
| | + | Despite Venus-related attention, AGW was overshadowed by a cooling scare in the 1970s. Steven Schneider, who later emerged as a key player in AGW politics, confidently predicted more cooling in 1971: |
| | + | {{cquote|[I]t is projected that man's potential to pollute will increase six- to eightfold in the next 50 years. If this increased rate of injection of particulate matter in the atmosphere should raise the present background opacity by a factor of 4, our calculations suggest a decrease in global temperature by as much as 3.5 ''°K''. Such a large decrease in the average temperature of Earth, sustained over a period of few years, is '''believed to be sufficient to trigger an ice age.''' However, by that time, nuclear power may have largely replaced fossil fuels as a means of energy production.<ref>{{cite journal |author=Rasool SI, Schneider SH |title=Atmospheric carbon dioxide and aerosols: effects of large increases on global climate |journal=Science |volume=173 |issue=3992 |pages=138–41 |date=July 1971 |pmid=17739641 |doi=10.1126/science.173.3992.138 |url= }}</ref>}} |
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| − | Including uncertainties in future greenhouse gas concentrations and climate modeling, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999.[1] Models have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes.
| + | By the late 1970s, the cooling scare had tapered off and Schneider was actively promoting AGW. The energy crisis, which began in 1973, put energy policy in the center of the political debate. In response, the left adopted a platform of conservation, renewables, and solar energy. Schneider and others noticed that AGW provided an additional justification for this platform. |
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| − | Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.[53] These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.
| + | By the late 1980s, Schneider and his fellow activists had transformed global warming from a fringe concern to a central political issue. He explained how in a 1989 interview: |
| | + | {{cquote|And like most people we’d like to see the world a better place, which in this context translates into our working to reduce the risk of potentially disastrous climate change. To do that we need to get some broad based support, to capture the public’s imagination. '''That, of course, means getting loads of media coverage. So we have to offer up scary scenarios,''' make simplified, dramatic statements, '''and make little mention of any doubts we might have'''. This “double ethical bind” we frequently find ourselves in cannot be solved by any formula. Each of us has to decide what the right balance is between being effective and being honest. I hope that means being both.<ref>The quote is from ''Discover'', pp. 45–48, October 1989. See [https://www.weeklystandard.com/climategate-part-ii/article/610926 this link].</ref>}} |
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| − | Most global climate models, when run to project future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.[54][55][56]
| + | After Schneider abandoned his global cooling hobbyhorse and got on the global warming [[argumentum ad populum|bandwagon]], he never looked back. He was all about offering up "scary scenarios" in order to get "loads of media coverage." He had hoped to be honest, but, let's face it, nobody's perfect. Since he presents himself here as the high priest of climate science, it should be noted that Schneider's Ph.D. is in mechanical engineering. |
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| − | The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem.[57] There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability. | + | According to Oxfam, "climate-related disasters has tripled in the last 30 years", and "more than 20 million people a year are forced from their homes".<ref>[https://www.oxfam.org/en/5-natural-disasters-beg-climate-action Oxfam]</ref> |
| | + | |
| | + | ===The IPCC=== |
| | + | The Intergovernmental Panel on Climate Change, a UN agency that reports on climate science, was founded in 1988. IPCC reports are often cited as the gold standard of science in this field, proof that AGW is "settled science." But few journalists read the report itself. Instead, they rely on the "Executive Summary" or "Summary for Policymakers." This document is written, not by scientists, but by UN bureaucrats under the supervision of Rajendra Pachauri, the Indian railway economist who heads the IPCC. The Climategate II emails reveal that the summary is written first then material is added to the various chapters to support it.<ref>Hayward, Steven F., "[https://www.weeklystandard.com/climategate-part-ii/article/610926 Climategate (Part II)]," ''Weekly Standard'', Dec. 12, 2011</ref> This procedure makes a farce of the IPCC's stated mission, which is to review the published literature so as to determine the scientific consensus. |
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| − | Attributed and expected effects
| + | As for the main report, this is put together carelessly, according George Filippo: "I feel rather uncomfortable about using not only unpublished but also unreviewed material as the backbone of our conclusions (or any conclusions)....IPCC is not any more an assessment of published science (which is its proclaimed goal) but production of results....I feel that at this point there are very little rules and almost anything goes." Filippo was a vice chair of the group from 2002 to 2008 and has contributed to all five IPCC reports.<ref>"[http://tomnelson.blogspot.jp/2012/01/don-miss-this-devastating-criticism-of.html Don't miss this devastating criticism of the IPCC]," January 02, 2012</ref> |
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| − | Main article: Effects of global warming
| + | ===Climategate=== |
| | + | The AGW industry was exposed as a hoax by the release of the "[[Climategate]]" emails in 2009. The Climate Research Unit of East Anglia University in Britain prepared 156 megaybytes of email by their researchers for release under the Freedom of Information Act. This database was somehow leaked, either prematurely or by a whistleblower after the institution had second thoughts. |
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
| + | In the most notorious message, Phil Jones, director of the unit, wrote, "I've just completed '''Mike's ''Nature'' trick''' of adding in the real temps to each series for the last 20 years (ie from 1981 onwards) amd from 1961 for Keith's to '''hide the decline'''."<ref name=MISH /> This should not be understood to mean that real temperature was declining, but rather that the researchers were attempting to cover up flaws in their tree-ring based data set. The graph in question was a version of the famous "hockey stick" that shows global temperature constant for 2,000 years, followed by a dramatic warming in the last century. ''Nature'' is considered one of the most authoritative science journals. So this quote suggests that a chart prepared for the magazine was faked with the approval of Jones as supervisor. An email by CRU researcher Tim Osborn clarifies what the ''Nature'' trick was: "Also we have applied a completely artificial adjustment to the data after 1960, so they look closer to observed temperatures than the tree-ring data actually were."<ref>"[http://tomnelson.blogspot.jp/2011/12/in-case-you-missed-it-damning.html In case you missed it, damning ClimateGate emails from Tim Osborne]", Tom Nelson, Dec. 06, 2011.</ref> |
| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Although it is difficult to connect specific weather events to global warming, an increase in global temperatures may in turn cause broader changes, including glacial retreat, Arctic shrinkage, and worldwide sea level rise. Changes in the amount and pattern of precipitation may result in flooding and drought. There may also be changes in the frequency and intensity of extreme weather events. Other effects may include changes in agricultural yields, addition of new trade routes,[58] reduced summer streamflows, species extinctions, and increases in the range of disease vectors.
| + | What's wrong with using tree ring data to created a climate record? The CRU researchers assumed that a tree grows faster when it's warmer. But rainfall has a stronger influence on tree growth than temperature does. Temperature is correlated to tree growth only in the sense that it tends to rain more in warm eras. Critics call the CRU's approach the "tree-o-meter" theory.<ref>"[http://tomnelson.blogspot.jp/2012/02/email-3826-feb-2001-in-email-copied-to.html Email 3826, Feb 2001]," Tom Nelson, Feb. 04, 2012. "In one go, they tossed aside dozens of studies which confirmed the existence of the MWE [Medieval Warm Era] and LIA [Little Ice Age] as global events, and all on the basis of tree rings - a proxy which has all the deficiencies I have stated above."</ref> |
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| − | Some effects on both the natural environment and human life are, at least in part, already being attributed to global warming. A 2001 report by the IPCC suggests that glacier retreat, ice shelf disruption such as that of the Larsen Ice Shelf, sea level rise, changes in rainfall patterns, and increased intensity and frequency of extreme weather events, are being attributed in part to global warming.[59] While changes are expected for overall patterns, intensity, and frequencies, it is difficult to attribute specific events to global warming. Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.[60]
| + | In another Climategate email, Jones enthusiastically demands that the IPCC review process be rigged: "I can't see either of these papers being in the next IPCC report. Kevin and I will keep them out somehow - even if we have to redefine what the peer-review literature is!" Jones also admitted that the reason he claims the Earth is warming is political: "The scientific community would come down on me in no uncertain terms if I said the world had cooled from 1998. Okay it has but it is only seven years of data and it isn't statistically significant."<ref name=steyn14>Steyn, Mark, "[http://www.steynonline.com/2697/how-the-science-got-settled How the Science Got Settled]", December 6, 2014.</ref> Jones is ignoring the fact that 1998 was an unusually warm year due to an El Niño event. All the same, it's clear that he runs the CRU to produce made-to-order results rather than as a scientist. |
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| − | Increasing deaths, displacements, and economic losses projected due to extreme weather attributed to global warming may be exacerbated by growing population densities in affected areas, although temperate regions are projected to experience some minor benefits, such as fewer deaths due to cold exposure.[61] A summary of probable effects and recent understanding can be found in the report made for the IPCC Third Assessment Report by Working Group II.[59] The newer IPCC Fourth Assessment Report summary reports that there is observational evidence for an increase in intense tropical cyclone activity in the North Atlantic Ocean since about 1970, in correlation with the increase in sea surface temperature, but that the detection of long-term trends is complicated by the quality of records prior to routine satellite observations. The summary also states that there is no clear trend in the annual worldwide number of tropical cyclones.[1]
| + | ==The temperature record== |
| | + | Global temperatures are tracked by three methods: satellites, weather balloons, and weather stations. All three methods confirm a modest amount of warming in recent decades. Satellite data shows a warming trend of 0.11 K/decade for 1978 to 2015.<ref>Roy W. Spencer, John R. Christy, and William D. Braswell, "[http://www.drroyspencer.com/wp-content/uploads/Version-61.pdf Version 6.0 of the UAH Temperature Dataset Released]", 28 April 2015.</ref> Weather balloon data shows a warming trend of 0.18 K/decade for 1970 to 2015.<ref>The figure given is for RATPAC-A, surface to 700 mb. See "[https://wattsupwiththat.com/2015/12/14/gavins-admission-about-the-satellite-record-versus-the-surface-temperature-record/ Gavin’s admission about the satellite record versus the surface temperature record]," ''Watt's Up With That''. You can find a collection of global climate charts [https://wattsupwiththat.com/global-climate/ here].</ref> |
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| − | Additional anticipated effects include sea level rise of 110 to 770 millimeters (0.36 to 2.5 ft) between 1990 and 2100,[62] repercussions to agriculture, possible slowing of the thermohaline circulation, reductions in the ozone layer, increased intensity of hurricanes and extreme weather events, lowering of ocean pH, and the spread of diseases such as malaria and dengue fever. One study predicts 18% to 35% of a sample of 1,103 animal and plant species would be extinct by 2050, based on future climate projections.[63] However, few mechanistic studies have documented extinctions due to recent climate change[64] and one study suggests that projected rates of extinction are uncertain.[65]
| + | A reanalysis of weather station data for 1943 to 2012 by Roy Spencer shows that after a cooler period in the 1960s and 1970s, U.S. temperatures returned to their earlier level. Unlike CRU, NASA, and NOAA, Spencer corrects for the fact that at most stations measurement time of day has changed over the years.<ref name=Spencer>Spencer, Roy, "[http://www.drroyspencer.com/2012/08/a-new-analysis-of-u-s-temperature-trends-since-1943/ A New Analysis of U.S. Temperature Trends Since 1943]," August 6th, 2012.</ref> So Spencer's analysis implies that the warmest year on record was 1934, the warmest year of the 1930s, not 2016 as the climate establishment maintains. Spencer is a prominent skeptic and a professor at the University of Alabama in Huntsville. He maintains the UAH record, one of the two major satellite temperature records. As an active researcher at the center of the climate science community, Spencer is a standing rebuke to the claim that AGW represents the scientific consensus.<ref>Spencer, Roy, "[http://www.drroyspencer.com/my-global-warming-skepticism-for-dummies/ My Global Warming Skepticism, for Dummies]"</ref> While the cause is debatable, worldwide, 2016 was the warmest year on record, 2020 was the second-warmest, and 2011–2020 was the warmest decade on record since thermometer-based observations began. Eight of the top 10 warmest years on record for the contiguous 48 states have occurred since 1998, and 2012 and 2016 were the two warmest years on record.<ref>[https://www.epa.gov/climate-indicators/climate-change-indicators-us-and-global-temperature US and global temperatures]</ref> |
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| − | Economic
| + | The temperature records preferred by the climate establishment were built up over many years and include numerous gaps, bugs, incompatible coding, and other errors. The problems of the CRU data set are memorably documented in the "Harry read me" file, part of the Climategate trove. According to this file, the premier global temperature record contains, "botch after botch after botch."<ref name=Brownlow>Brownlow, Andie, "[https://pjmedia.com/blog/climategates-harry_read_me-txt-we-all-really-should/?singlepage=true Climategate's Harry_Read_Me.txt: We All Really Should]", Dec. 11, 2009.</ref> |
| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4. | |
| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
| |
| | | | |
| − | Main articles: Economics of global warming and Low-carbon economy
| + | AGW is hardly the only explanation that has been proposed for recent warming. There are also explanations involving natural cycles such as the 11-year-sunspot cycle, the Pacific decadal oscillation,<ref>Bratcher and Giese, "Tropical Pacific decadal variability and global warming", ''Geophysical Research Letters''.</ref> and the El Niño-Southern Oscillation (ENSO).<ref>*72 percent of global temperature variation since 1958 reflects the influence of a Pacific Ocean weather cycle called the El Niño-Southern Oscillation (McLean, J. D., C. R. de Freitas, and R. M. Carter--2009-07-23). "Influence of the Southern Oscillation on tropospheric temperature". ''Journal of Geophysical Research''<br/>*Spencer, R.W. & Braswell, W.D., "[http://link.springer.com/article/10.1007/s13143-014-0011-z The role of ENSO in global ocean temperature changes during 1955–2011 simulated with a 1D climate model]", Asia-Pacific J Atmos Sci (2014) 50: 229. doi:10.1007/s13143-014-0011-z</ref> |
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| − | Some economists have tried to estimate the aggregate net economic costs of damages from climate change across the globe. Such estimates have so far failed to reach conclusive findings; in a survey of 100 estimates, the values ran from US$-10 per tonne of carbon (tC) (US$-3 per tonne of carbon dioxide) up to US$350/tC (US$95 per tonne of carbon dioxide), with a mean of US$43 per tonne of carbon (US$12 per tonne of carbon dioxide).[61] One widely publicized report on potential economic impact is the Stern Review; it suggests that extreme weather might reduce global gross domestic product by up to 1%, and that in a worst-case scenario global per capita consumption could fall 20%.[66] The report's methodology, advocacy and conclusions have been criticized by many economists, primarily around the Review's assumptions of discounting and its choices of scenarios,[67] while others have supported the general attempt to quantify economic risk, even if not the specific numbers.[68][69]
| + | ==Summary of arguments against anthropogenic global warming== |
| | + | Natural periods of global warming and global cooling are expected to occur regardless of human activity, and not long ago liberals were demanding more government control to combat an alleged cooling in temperatures, with some scientists warning of a possible ice age.<ref name="Time">"Science: Another Ice Age?" (June 24, 1974). ''Time'' magazine. Retrieved on September 25, 2014.</ref> [[Global cooling]], a theory that predates global warming, obviously occurs naturally many times throughout [[Earth|Earth's]] geological history.<ref name="dissidents">"After any given warming phase begins, thousands of years later the cyclical [[Milankovitch]] decrease in the sun's heat kicks in. The warming stops, reverses and an [[ice age]] ensues." Cockburn, Alexander (June 9–11, 2007). [http://www.counterpunch.org/cockburn06092007.html "Dissidents against dogma"]. Counterpunch. Retrieved on September 25, 2014.</ref> The ease of refutation of anthropogenic global cooling claims foretells the eventual fate of the current global warming hysteria. |
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| − | In a summary of economic cost associated with climate change, the United Nations Environment Programme emphasizes the risks to insurers, reinsurers, and banks of increasingly traumatic and costly weather events. Other economic sectors likely to face difficulties related to climate change include agriculture and transport. Developing countries, rather than the developed world, are at greatest economic risk.[70]
| + | Many political activists use the term "global warming" to refer to [[anthropogenic global warming theory]] (AGW), which asserts that human activity such as spewing "[[greenhouse gases]]" is causing an increase in temperature and is more significant than natural causes. The AGW theory is supported by left-leaning political parties, as well as a majority of sovereign states, national agencies, and an intergovernmental panel (see [[IPCC]]). The reality is that there is no immediate global crisis, and even dire warnings by the UN's [[Intergovernmental Panel on Climate Change]] (IPCC) admit that significant effects will not be manifested for at least 100 years. Predictions made by [[climate model]]s publicized by the IPCC have not come to pass in recent years. Many scientists, such as Hal Lewis, have decried global warming as a conspiracy for the purpose of securing trillions of dollars in grant money. |
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| − | Security
| + | In November 2009, emails were disclosed that implicated a wrongful manipulation and concealment of data by scientists who have insisted that there is dangerous man-made global warming. Prior to [[ClimateGate]], both the Republican and Democratic party Platforms in 2008 suggested that global warming is happening, that it is caused by human activity, and that it should be counteracted. For example, in 2007, the Republican presidential candidate Senator [[John McCain]] called global warming "an issue we can no longer afford to ignore".<ref>"Issues" (September 1, 2007). www.JohnMcCain.com [2008 senate campaign website] quoted in [http://www.ontheissues.org/domestic/John_McCain_Environment.htm "John McCain on environment"] OnTheIssues.org. Retrieved on September 25, 2014.</ref> In 2010, an independent analysis cleared the scientists involved of any wrongdoing ''as scientists'', but remarked upon their omissions as data-presenters. Accordingly, the effects of the scandal still linger.<ref>Whiteman, Hilary (July 7, 2010). [https://www.cnn.com/2010/WORLD/europe/07/07/climategate.email.review/?hpt=Sbin "'Climategate' review clears scientists of dishonesty"]. CNN World. Retrieved on September 26, 2014.</ref> |
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| − | In November 2007, the Center for Strategic and International Studies and the Center for a New American Security published a report highlighting the national security effects of climate change.[71] These security effects include increased competition for resources between countries, mass migration from the worst affected areas, challenges to the cohesion of major states threatened by the rise in sea levels, and, as a consequence of these factors, an increased risk of armed conflict, including even nuclear conflicts.
| + | Former Vice President [[Al Gore]] won a [[Nobel Prize]] in 2007 for claiming that there is a dangerous man-made global warming that threatens the world. However, it has since been revealed that he convinced many people through inaccurate information in his "documentary," i.e., he only won the Nobel Prize by lying. [See [[#Al_Gore.27s_Claims|Al Gore's claims]] below.] |
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| | + | The following facts can help dissuade even the most illogical of liberals from believing in the flawed theory of anthropogenic global warming. |
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| − | Adaptation and mitigation
| + | === Temperature flat === |
| | + | The overall temperature has been flat for about 16 years.<ref name="Rose">Rose, David (October 13, 2012). [https://www.dailymail.co.uk/sciencetech/article-2217286/Global-warming-stopped-16-years-ago-reveals-Met-Office-report-quietly-released--chart-prove-it.html "Global warming stopped 16 years ago, reveals Met Office report quietly released...and here is the chart to prove it"]. MailOnline. Retrieved on September 26, 2014.</ref> |
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| − | Main articles: Adaptation to global warming, Mitigation of global warming, and Kyoto Protocol
| + | === Data manipulation === |
| | + | Climate data stating otherwise has been proven to be manipulated.<ref>Multiple references: |
| | + | *KUSI-TV (January 14, 2010). [http://www.spaceref.com/news/viewpr.html?pid=30000 "NASA caught in climate data manipulation; new revelations headlined on KUSI-TV climate special"]. SpaceRef. Retrieved on September 26, 2014. |
| | + | *[https://www.youtube.com/watch?v=2jasZcNQqsw "Climategate 2-US Government involved in data manipulation"] (January 16, 2010). YouTube video, 10:00, posted by Bigone5555J. Retrieved on September 26, 2014.</ref> |
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| − | The broad agreement among climate scientists that global temperatures will continue to increase has led some nations, states, corporations and individuals to implement actions to try to curtail global warming or adjust to it. Many environmental groups encourage action against global warming, often by the consumer, but also by community and regional organizations. Others have suggested a quota on worldwide fossil fuel production, citing a direct link between fossil fuel production and CO2 emissions.[72][73]
| + | === Alternate causation === |
| | + | Even if global warming did actually exist, the overall effect of human activities on global warming are minimal, if not nonexistent.<ref>Byrne, Dennis (August 30, 2011). [http://articles.chicagotribune.com/2011-08-30/news/ct-oped-0830-byrne-20110830_1_cosmic-rays-aerosols-magnetic-field "The real science trashers"]. ChicagoTribune. Retrieved on September 26, 2014.</ref> |
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| − | There has also been business action on climate change, including efforts at increased energy efficiency and limited moves towards use of alternative fuels. One important innovation has been the development of greenhouse gas emissions trading through which companies, in conjunction with government, agree to cap their emissions or to purchase credits from those below their allowances.
| + | ==Science of global warming== |
| | + | ===Presence of CO<sub>2</sub>=== |
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| − | The world's primary international agreement on combating global warming is the Kyoto Protocol, an amendment to the United Nations Framework Convention on Climate Change (UNFCCC) negotiated in 1997. The Protocol now covers more than 160 countries globally and over 55% of global greenhouse gas emissions.[74] Only the United States and Kazakhstan have not ratified the treaty, with the United States historically being the world's largest emitter of greenhouse gas. This treaty expires in 2012, and international talks began in May 2007 on a future treaty to succeed the current one.[75]
| + | One of the primary concerns of Global Warming research is the increased presence of carbon dioxide (CO<sub>2</sub>) in the atmosphere. Original claims stated that the increase in carbon dioxide—which is a greenhouse gas—were caused primarily through the burning of [[fossil fuels]], and that such increases were the foremost cause of global temperatures rising. Historically, Global temperature changes precede changes in carbon dioxide in the atmosphere.<ref>[http://www.skepticalscience.com/co2-lags-temperature.htm "CO2 lags temperature-what does it mean?"] (2007). SkepticalScience. Retrieved on September 26, 2014.</ref> |
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| − | Claiming "serious harm" to the United States economy and the exemption of "80 percent of the world, including major population centers" like China and India, from the treaty, George W. Bush contends that the Kyoto Protocol is an unfair and ineffective means of addressing global climate change concerns.[76] Still, various state, local, and regional governments within the United States have begun their own initiatives to indicate support and compliance with the Kyoto Protocol on a local basis. For example, the Regional Greenhouse Gas Initiative is a state-level emissions capping and trading program involving eight Northeastern U.S. states, which was founded on December 20, 2005.[77]
| + | The most obvious way that this would occur would be through the heating of ocean water. The oceans are the single largest storage unit for carbon dioxide gas on the planet, containing about 93% of the Earth's carbon dioxide.<ref>[http://www.waterencyclopedia.com/Bi-Ca/Carbon-Dioxide-in-the-Ocean-and-Atmosphere.html "Carbon dioxide in the ocean and atmosphere"] (2007). Water Encyclopedia. Retrieved on September 26, 2014</ref> As the temperature rises, the [[solubility]] of carbon dioxide in ocean water is reduced,<ref>[https://science.nasa.gov/earth-science/oceanography/ocean-earth-system/ocean-carbon-cycle/ "Carbon cycle"] (2010). NASA Science. Retrieved on September 26, 2014.</ref> causing the dissolved carbon dioxide gas to enter the atmosphere, and begin trapping radiation from the sun. Scientists now believe that this cycle causes a sort of chain effect, where increased temperature causes more carbon dioxide to enter the atmosphere, which in turn causes more temperature rise. |
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| − | China and India, though exempt from its provisions as developing countries, have ratified the Kyoto Protocol. China may have passed the U.S. in total annual greenhouse gas emissions according to some recent studies. Chinese Premier Wen Jiabao has called on the nation to redouble its efforts to tackle pollution and global warming.[78]
| + | It is also noteworthy to point out that carbon dioxide, while not as abundant in the atmosphere, has a more significant effect on global warming than water vapor does. Carbon dioxide cannot form clouds, as water vapor does. When water vapor forms clouds, those clouds actually block some of the sun's radiation from reaching the Earth, causing water vapor to both contribute positively and negatively to global temperature rise. Carbon dioxide can only act as a greenhouse gas, causing the above-mentioned cyclic effect. According to the IPCC and others, the current concentration of carbon dioxide in the Earth's atmosphere is about 392 ppm, which is the highest it has been in at about 800,000 years.<ref>Tans, Pieter and Keeling, Ralph (2010). [http://www.esrl.noaa.gov/gmd/ccgg/trends/mlo.html "Trends in atmospheric carbon dioxide"]. NOAA/Earth System Research Laboratory Global Monitoring Division. Retrieved on September 26, 2014.</ref> |
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| − | The IPCC's Working Group III is responsible for crafting reports that deal with the mitigation of global warming and analyzing the costs and benefits of different approaches. In the 2007 IPCC Fourth Assessment Report, they conclude that no one technology or sector can be completely responsible for mitigating future warming. They find there are key practices and technologies in various sectors, such as energy supply, transportation, industry, and agriculture, that should be implemented to reduced global emissions. They estimate that stabilization of carbon dioxide equivalent between 445 and 710 ppm by 2030 will result in between a 0.6% increase and 3% decrease in global gross domestic product.[79]
| + | But other scientists have disputed this claim of modern-day record-high carbon dioxide readings:<ref name="dissidents"/> |
| | + | <blockquote>Take Warsaw-based Professor Zbigniew Jaworowski, famous for his critiques of ice-core data. He’s devastating on the IPCC rallying cry that CO<sub>2</sub> is higher now than it has ever been over the past 650,000 years. In his 1997 paper in the Spring ''21st Century Science and Technology'', he demolishes this proposition. In particular, he’s very good on pointing out the enormous inaccuracies in the ice-core data and the ease with which a CO<sub>2</sub> reading from any given year is contaminated by the CO<sub>2</sub> from entirely different eras. He also points out that from 1985 on there’s been some highly suspect editing of the CO<sub>2</sub> data, presumably to reinforce the case for the "unprecedented levels" of modern CO<sub>2</sub>. In fact, in numerous papers prior to 1985, there were plenty of instances of CO<sub>2</sub> levels much higher than current CO<sub>2</sub> measurements, some even six times higher. He also points out that it is highly unscientific to merge ice-core temperature measurements with modern temperature measurements.</blockquote> |
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| − | Social and political debate
| + | ===The Modern Warm Period=== |
| | + | According to temperature reconstruction made within an [[Old Earth]] paradigm, there have been many cycles of naturally-caused global warming and cooling over many millions of years (see [[climate cycles]]). Some scientists, including [[Richard Lindzen]] of [[MIT]], [[Sallie Baliunas]] of [[Harvard]] and [[Fred Singer]] (independent), say that the recent warming could be part of another natural cycle or random fluctuations in the atmosphere. |
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| − | Main articles: Global warming controversy, Politics of global warming, and Economics of global warming
| + | Recent studies of the Milankovitch Cycles, which predict Earth's climate by studying changes in its orbit and axial tilt, suggest that we are currently 18,000 years into a 150,000 year period between ice ages. This would imply that we should expect the temperature to be rising anyway. A 2002 study by Berger and Loutre suggests 50,000 years of warmer weather before Earth begins to cool again, but that model incorporated anthropogenic forces and concluded: |
| − | See also: Climate change denial
| + | <blockquote>While combinations of natural forcings produce a gradual warming up to about 1960, none of them leads to a warming over the last 30 years (this period containing three major volcanic eruptions). In contrast, simulations incorporating only anthropogenic forcings reproduce the warming over the last three decades at a rate consistent with that observed, but underestimate the early 20th century warming. As a consequence, only the use of both natural and anthropogenic forcings allows to reproduce much of the observed decadal scale variations of the annual mean hemispheric temperature over the last 150 years.<ref>Bertrand, Cédric, Loutre, Marie-France et al. (May 2002). [http://onlinelibrary.wiley.com/doi/10.1034/j.1600-0870.2002.00287.x/full "Climate of the last millennium: a sensitivity study"]. ''Tellus'' [Stockholm], vol. 54, iss. 3, pp. 221-244. Retrieved from Wiley Online Library on September 26, 2014.</ref></blockquote> |
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| − | Per capita greenhouse gas emissions in 2000
| + | It should be noted, however, that computer simulated climate models are often tweaked so they agree with the historical temperature record. There is no way to completely simulate all of the Earth's climate with a computer program. |
| − | Per capita greenhouse gas emissions in 2000
| |
| − | Per country greenhouse gas emissions in 2000
| |
| − | Per country greenhouse gas emissions in 2000
| |
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| − | Over the past several years, public perceptions and attitudes concerning the causes and importance of global warming have changed.[80] Increased awareness of the scientific findings surrounding global warming has resulted in political and economic debate. Poor regions, particularly Africa, appear at greatest risk from the suggested effects of global warming, while their actual emissions have been small compared to the developed world.[81] At the same time, developing country exemptions from provisions of the Kyoto Protocol have been criticized by the United States and Australia, and have been used as part of the rationale for continued non-ratification by the U.S.[82] In the Western world, the idea of human influence on climate has gained wider acceptance in Europe than in the United States.[83][84]
| + | After a major set of temperature readings was found to be an incompatible mix of older and recent data (in the Climategate II scandal) in 2010, Judith Curry, chair of the School of Earth and Atmospheric Science at America's Georgia Tech university examined new data causing her to state (as quoted by MailOnline):<ref name="Rose"/> |
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| − | The issue of climate change has sparked debate weighing the benefits of limiting industrial emissions of greenhouse gases against the costs that such changes would entail. There has been discussion in several countries about the cost and benefits of adopting alternative energy sources in order to reduce carbon emissions.[85] Organizations and companies such as the Competitive Enterprise Institute and ExxonMobil have emphasized more conservative climate change scenarios while highlighting the potential economic cost of stricter controls.[86][87][88][89] Likewise, various environmental lobbies and a number of public figures have launched campaigns to emphasize the potential risks of climate change and promote the implementation of stricter controls. Some fossil fuel companies have scaled back their efforts in recent years,[90] or called for policies to reduce global warming.[91]
| + | <blockquote>'Natural variability [the impact of factors such as long-term temperature cycles in the oceans and the output of the sun] has been shown over the past two decades to have a magnitude that dominates the greenhouse warming effect.</blockquote> |
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| − | Another point of debate is the degree to which newly developed economies such as India and China should be expected to constrain their emissions. China's gross national CO2 emissions are expected to exceed those of the U.S. within the next few years, and may have already done so according to a 2006 report.[92] China has contended that it has less of an obligation to reduce emissions since its per capita emissions are roughly one-fifth that of the United States.[93] India, also exempt from Kyoto restrictions and another of the biggest sources of industrial emissions, has made similar assertions.[94] However, the U.S. contends that if they must bear the cost of reducing emissions, then China should do the same.[95]
| + | <blockquote>'It is becoming increasingly apparent that our attribution of warming since 1980 and future projections of climate change needs to consider natural internal variability as a factor of fundamental importance.'</blockquote> |
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| − | Related climatic issues
| + | The MailOnline article continued: |
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| − | Main articles: Ocean acidification, global dimming, and ozone depletion
| + | <blockquote>Professor Phil Jones, director of the Climate Research Unit at the University of East Anglia, who found himself at the centre of the ‘Climategate’ scandal over leaked emails three years ago, would not normally be expected to agree with her.... Prof Jones also admitted that the climate models were imperfect: ‘We don’t fully understand how to input things like changes in the oceans, and because we don’t fully understand it you could say that natural variability is now working to suppress the warming. We don’t know what natural variability is doing.’</blockquote> |
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| − | A variety of issues are often raised in relation to global warming. One is ocean acidification. Increased atmospheric CO2 increases the amount of CO2 dissolved in the oceans.[96] CO2 dissolved in the ocean reacts with water to form carbonic acid, resulting in acidification. Ocean surface pH is estimated to have decreased from 8.25 near the beginning of the industrial era to 8.14 by 2004,[97] and is projected to decrease by a further 0.14 to 0.5 units by 2100 as the ocean absorbs more CO2.[1][98] Since organisms and ecosystems are adapted to a narrow range of pH, this raises extinction concerns, directly driven by increased atmospheric CO2, that could disrupt food webs and impact human societies that depend on marine ecosystem services.[99]
| + | ==Polar bears== |
| | + | It was announced on the news that polar bears risk going extinct by the end of the twenty-first century if current carbon emissions continue. |
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| − | Global dimming, the gradual reduction in the amount of global direct irradiance at the Earth's surface, may have partially mitigated global warming in the late twentieth century. From 1960 to 1990 human-caused aerosols likely precipitated this effect. Scientists have stated with 66–90% confidence that the effects of human-caused aerosols, along with volcanic activity, have offset some of the global warming, and that greenhouse gases would have resulted in more warming than observed if not for these dimming agents.[1]
| + | ===Sunspots=== |
| | + | Sunspot activity is a factor in climate fluctuations, however, little details were known about how much of an impact these fluctuations had on the Earth's climate. During the deepest solar minimum ever recorded, from 2005 to 2010, NASA measured the Earth's energy balance, i.e. the amount of energy absorbed by the sun subtract the amount of energy lost to radiation into space. They concluded: |
| | + | <blockquote>If the Sun were the only climate forcing or the dominant climate forcing, then the planet would gain energy during the solar maxima, but lose energy during solar minima. The fact that Earth gained energy at a rate 0.58 W/m<sup>2</sup> during a deep prolonged solar minimum reveals that there is a strong positive forcing overwhelming the negative forcing by below-average solar irradiance. That result is not a surprise, given knowledge of other forcings, but it provides unequivocal refutation of assertions that the Sun is the dominant climate forcing.<ref>Hansen, James, Sato, Makiko et al. (January 2012). [http://www.giss.nasa.gov/research/briefs/hansen_16/ "Earth's energy imbalance"] nasa.gov/Goddard Institute for Space Studies. Retrieved on September 26, 2014.</ref></blockquote> |
| | + | But heat energy is not the only force of the Sun affecting the Earth. The Sun also produces magnetic activity, the effect of which was not measured in this study, and which could affect the Earth's climate in little-understood ways. British astrophysicist Piers Corbyn, speaking in May 2017, claimed that low sunspot activity heralds a mini ice age which could last for 20 years.<ref>https://abruptearthchanges.com/2017/06/14/mini-ice-age-is-here-to-stay-says-astrophysicist/</ref> |
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| − | Ozone depletion, the steady decline in the total amount of ozone in Earth's stratosphere, is frequently cited in relation to global warming. Although there are areas of linkage, the relationship between the two is not strong.
| + | ==Economics of global warming== |
| | + | While the marriage of anti-capitalists and alleged climate science is nothing new, Rep. [[Alexandria Ocasio-Cortez]] has introduced legislation as part of her [[Green New Deal]], [[reparations]] for minorities, a basic income, and [[Medicare for All]] as part of her "[[climate justice]]" program.<ref>https://news.grabien.com/story-ocasio-cortezs-green-new-deal-radical-mandate-government-con</ref> |
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| − | See also
| + | ===Unnecessary expansion of government=== |
| | + | The idea of dangerous anthropogenic (man-made) global warming (AGW) is promoted by liberals and socialists seeking greater government control over the production and use of energy, which is a substantial percentage of the economy. In economic terms, they would like to 'internalize' the 'externality,' which is to say that they think that producers of emissions should be directly connected to the consequences of those emissions, leading syndicated columnist [[Charles Krauthammer]] to warn of an impending "environmental shakedown".<ref>Krauthammer, Charles (December 11, 2009). [http://www.realclearpolitics.com/articles/2009/12/11/copenhagen_shakedown.html "The environmental shakedown"]. Real Clear Politics. Retrieved on September 27, 2014.</ref> |
| | | | |
| − | * Glossary of climate change
| + | ==Public stances on global warming== |
| | + | In 2021 72% of American believed that global warming is real and 14# believed that was not.<ref>[https://climatecommunication.yale.edu/visualizations-data/ycom-us/]</ref> However, the ''Daily Mail'' gives a figure of 63% of Americans who believe in climate change. Another survey in March 2021 conducted in the United States, some 70 percent of the respondents said they believed that global warming was happening. A much smaller share, 15 percent, believed global warming was not happening.<ref>[https://www.statista.com/statistics/663247/belief-of-global-warming-according-to-us-adults/]</ref> In the UK, according to a ''Daily Mail'' poll, "the public strongly supportsc [Conservative] [[Boris Johnson]]’s bid to curb climate change – but they are not prepared to pay more than £5 extra a week in tax to fund his trillion-pound green energy plans".<ref>[https://www.dailymail.co.uk/news/article-10146089/Daily-Mail-poll-shows-strong-support-PMs-bid-curb-climate-change-public-fears-Cop26-flop.html]></ref> While little is known about public opinion in Russia, the Russian government is beginning to take climate change seriously. Vladimir Putin, who was for long a sceptic, said in 2021 that "climate change is one of the greatest challenges facing humanity. He reiterated this in connection with the climate summit in Glasgow in November this year".<ref>[https://sciencenorway.no/climate-policy-russia-society-and-culture/have-russian,-climate-scientists-convinced-vladimir-putin-that-climate-change-is-real/1956249]</ref> |
| | | | |
| − | References
| + | ===Climate change as a cult=== |
| | + | The zeal of climate-change advocates and lack of objectivity has led some observers to see it as a core belief in a new eco-theology, using themes of traditional Judeo-Christian beliefs. Columnist Deon Feder warns,<ref>Feder, Don (July 31, 2007). [http://archive.frontpagemag.com/readArticle.aspx?ARTID=27579 "The cult of global warming"]. GrassTopsUSA.com. Retrieved from archive at FrontPageMag.com on September 27, 2014.</ref> that following other attempts such as Marxism, overpopulation, ''[[Silent Spring]]'', |
| | + | <blockquote>now we have the Church of Global Warming, under the leadership of Pope Albert I and his college of cardinals (the [[Natural Resources Defense Council]], [[Sierra Club]] and editorial board of ''The New York Times'').</blockquote> |
| | | | |
| − | 1. ^ a b c d e f g h i Summary for Policymakers (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change (2007-02-05). Retrieved on 2007-02-02. “The updated 100-year linear trend (1906 to 2005) of 0.74°C [0.56°C to 0.92°C] is therefore larger than the corresponding trend for 1901 to 2000 given in the TAR of 0.6°C [0.4°C to 0.8°C].”
| + | <blockquote>Its Office for the Propagation of the Faith works overtime, churning out books, movies (from the fictional “The Day After Tomorrow” to the fictional [[An Inconvenient Truth|“An Inconvenient Truth”]]), textbooks, concerts, congressional hearings, media pleading and inquisitions.</blockquote> |
| − | 2. ^ Hegerl, Gabriele C.; et al. (2007-05-07). Understanding and Attributing Climate Change (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 690. Intergovernmental Panel on Climate Change. Retrieved on 2007-05-20. “Recent estimates (Figure 9.9) indicate a relatively small combined effect of natural forcings on the global mean temperature evolution of the seconds half of the 20th century, with a small net cooling from the combined effects of solar and volcanic forcings”
| |
| − | 3. ^ Ammann, Caspar; et al. (2007-04-06). "Solar influence on climate during the past millennium: Results from ransient simulations with the NCAR Climate Simulation Model" (PDF). Proceedings of the National Academy of Sciences of the United States of America 104 (10): 3713–3718. “However, because of a lack of interactive ozone, the model cannot fully simulate features discussed in (44)." "While the NH temperatures of the high-scaled experiment are often colder than the lower bound from proxy data, the modeled decadal-scale NH surface temperature for the medium-scaled case falls within the uncertainty range of the available temperature reconstructions. The medium-scaled simulation also broadly reproduces the main features seen in the proxy records." "Without anthropogenic forcing, the 20th century warming is small. The simulations with only natural forcing components included yield an early 20th century peak warming of ≈0.2 °C (≈1950 AD), which is reduced to about half by the end of the century because of increased volcanism.”
| |
| − | 4. ^ A guide to facts and fictions about climate change. Royal Society (March 2005). Retrieved on 2007-11-18. “"However, the overwhelming majority of scientists who work on climate change agree on the main points"”
| |
| − | 5. ^ Climate Change: Basic Information. United States Environmental Protection Agency (2006-12-14). Retrieved on 2007-02-09. “In common usage, 'global warming' often refers to the warming that can occur as a result of increased emissions of greenhouse gases from human activities.”
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| − | 6. ^ United Nations Framework Convention on Climate Change, Article I. United Nations Framework Convention on Climate Change. Retrieved on 2007-01-15.
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| − | 10. ^ Joint science academies' statement: The science of climate change (ASP). Royal Society (2001-05-17). Retrieved on 2007-04-01. “The work of the Intergovernmental Panel on Climate Change (IPCC) represents the consensus of the international scientific community on climate change science”
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| − | 13. ^ Forster, Piers; et al. (2007-02-05). Changes in Atmospheric Constituents and in Radiative Forcing (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 188-193. Intergovernmental Panel on Climate Change. Retrieved on 2007-09-17.
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| − | 16. ^ IPCC WG1 AR4 Report — Chapter 1: Historical Overview of Climate Change Science (PDF). IPCC WG1 AR4 Report p97 (pdf page 5 of 36). IPCC (2007). Retrieved on 2007-10-07. “To emit 240 W m–2, a surface would have to have a temperature of around –19 °C. This is much colder than the conditions that actually exist at the Earth’s surface (the global mean surface temperature is about 14 °C). Instead, the necessary –19 °C is found at an altitude about 5 km above the surface.”
| |
| − | 17. ^ Note that the Greenhouse Effect produces a temperature increase of about 33 °C (59 °F) with respect to black body predictions and not a surface temperature of 33 °C (91 °F) which is 32 °F higher. The average surface temperature is about 14 °C (57 °F). Also note that both the Celsius and Fahrenheit temperatures are expressed to 2 significant figures even though the conversion formula produces 3.
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| − | 93. ^ China: US should take lead on climate, by Michael Casey, Associated Press, 12/7/07.
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| | | | |
| − | Global warming is the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.
| + | Commenting on the tendency to hastily issue dire warnings of Climate Change, seen in the coming [[Ice Age]] scare of the 70's, Maurizio Morabito<ref>Morabito, Maurizio (December 5, 2009). [http://www.spectator.co.uk/features/5592803/the-cias-global-cooling-files/ "The CIA’s ‘global cooling’ file"]. ''[[The Spectator]]''. Retrieved from The Spectator website on September 27, 2014.</ref> asked, "Is the problem with the general public, who cannot talk about climate except in doom-laden terms, and for whom the sky is the last animist god?" |
| | | | |
| − | The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 year period ending in 2005, which is higher than the earlier estimate of 0.6 ± 0.2 °C for the period ending in 2000.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations"[1] via the greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3] These basic conclusions have been endorsed by at least 30 scientific societies and academies of science, including all of the national academies of science of the major industrialized countries. While individual scientists have voiced disagreement with the conclusions of the IPCC, the overwhelming majority of scientists working on climate change are in agreement with the conclusions.[4]
| + | Mark Steyn writes in ''Macleans'',<ref name="hot">Steyn, Mark (December 24, 2009). [http://www2.macleans.ca/2009/12/24/why-climate-change-is-hot-hot-hot/2/ "Why climate change is hot hot hot"]. Macleans. Retrieved on September 27, 2014.</ref> |
| | + | <blockquote> |
| | + | Forty years ago conventional religious belief was certainly in decline in what we once knew as Christendom, but the hole was not yet ozone-layer sized. Once the sea of faith had receded far from shore, the post-Christian West looked at what remained and found “Gaia.”</blockquote> |
| | | | |
| − | Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[1] The range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a millennium even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]
| + | And while, "When man was made in the image of God, he was fallen but redeemable", among these devotees of [[Gaia]], |
| | + | <blockquote>Anti-humanism is everywhere, not least in the barely concealed admiration for China’s (demographically disastrous) “One Child” policy advanced by everyone from the ''National Post''’s Diane Francis to Sir David Attenborough, the world’s leading telly naturalist but also a BBC exec who once long ago commissioned the great series ''The Ascent of Man''. If Sir David’s any guide, the great thing about man’s ascent is it gives him a higher cliff to nosedive off.</blockquote> |
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| − | Increasing global temperature will cause sea level to rise, and is expected to increase the intensity of extreme weather events and to change the amount and pattern of precipitation. Other effects of global warming include changes in agricultural yields, trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.
| + | ===Politics of global warming and dissent=== |
| | + | {{main|Politics of global warming}} |
| | + | [[File:Global carbon emissions.PNG|right|300px|thumb|The [[Peoples Republic of China]] is responsible for 27% of global carbon emissions, more than all other developed nations combined.]] |
| | + | Christine Stewart—Canadian Environment Ministry, "'''No matter if the science is all phony''', there are collateral environmental benefits.... [C]limate change [provides] the greatest chance to bring about justice and equality in the world." <ref>Stewart, Christine (December 14, 1998). ''Calgary Herald''. Reprinted at "Match these quotes" (December 2004). ''Resource Roundup'', p. 8. Reprinted at [http://www.aim.org/wls/use-environmentalism-to-change-the-world/ "Use environmentalism to change the world"]. Accuracy in Media, "What liberals say" series. Retrieved on September 27, 2014.</ref> |
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| − | Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. There is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences. Most national governments have signed and ratified the Kyoto Protocol, aimed at reducing greenhouse gas emissions.
| + | 'Global Warming Now World's Most Boring Topic' <ref>Sheppard, Noel (July 17, 2007). [http://newsbusters.org/node/14467 "Hysterical satire: 'Global warming now world's most boring topic'"]. MRC NewsBusters. Retrieved on September 27, 2014.</ref> |
| − | Contents
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| − | [hide]
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| | | | |
| − | * 1 Terminology
| + | The need to fight "global warming" has become part of the dogma of the liberal conscience.<ref name="cato">Lindzen, Richard (Spring 1992). [http://www.cato.org/regulation/spring-1992 "Global warming: The origin and nature of the alleged scientific consensus"]. ''Regulation'', vol. 15, no. 2. Retrieved from Cato Institute website on September 29, 2014.</ref> |
| − | * 2 Causes
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| − | o 2.1 Greenhouse gases in the atmosphere
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| − | o 2.2 Feedbacks
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| − | o 2.3 Solar variation
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| − | * 3 Temperature changes
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| − | o 3.1 Recent
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| − | o 3.2 Pre-human climate variations
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| − | * 4 Climate models
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| − | * 5 Attributed and expected effects
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| − | o 5.1 Economic
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| − | o 5.2 Security
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| − | * 6 Adaptation and mitigation
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| − | * 7 Social and political debate
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| − | * 8 Related climatic issues
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| − | * 9 See also
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| − | * 10 References
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| − | * 11 Further reading
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| − | * 12 External links
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| | | | |
| − | Terminology
| + | Clearly, "global warming" is a tempting issue for many very important groups to exploit. |
| | + | ... dealing with the threat of warming fits in with a great variety of preexisting agendas [like] dissatisfaction with industrial society (neopastoralism), ... governmental desires for enhanced revenues (carbon taxes), and bureaucratic desires for enhanced power.<ref name="cato"/> |
| | | | |
| − | The term "global warming" is a specific example of the broader term climate change, which can also refer to global cooling. In common usage, the term refers to recent warming and implies a human influence.[5] The United Nations Framework Convention on Climate Change (UNFCCC) uses the term "climate change" for human-caused change, and "climate variability" for other changes.[6] The term "anthropogenic global warming" is sometimes used when focusing on human-induced changes.
| + | Mark Steyn writes in "Why climate change is hot hot hot",<ref name="hot"/> |
| | + | <blockquote> |
| | + | What’s also changed since the seventies is the nature of the UN and the transnational bureaucracies...“Aid” is a discredited word these days and comes with too many strings attached. But eco-credits sluiced through an oil-for-food program on steroids offers splendid new opportunities for bulking up an ambitious dictator’s Swiss bank accounts.</blockquote> |
| | | | |
| − | Causes
| + | The IPCC is desperate to claim the 20th century—the warmest on record. Thus, tying the progress of modern mankind to our supposed planet imbalance problem. Unfortunately for the IPCC, that point is disputed as well. In 2008, it was discovered that tree rings in Finland were more accurate record of the warmest century. The current era was not the warmest period—it was the period between 931 and 1180.<ref>Birdnow, Timothy (June 24, 2008). [http://tbirdnow.mee.nu/archive/2008/6?page=2 "The trees of Finland; temperature readings and historical reconstruction"]. Birdnow's Aviary blog. Retrieved on September 29, 2014. With links to actual data sources.</ref> |
| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| | | | |
| − | Main articles: Attribution of recent climate change and scientific opinion on climate change
| + | Assessments of climate science by the [[United Nations]] (see [[IPCC]] — ''Intergovernmental Panel on Climate Change'') have claimed that scientists are 90% sure that over 50% of the observed global warming in recent decades is human-caused, and that continued global warming should be expected over at least the next century. |
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| − | The Earth's climate changes in response to external forcing, including variations in its orbit around the sun (orbital forcing),[7][8][9] volcanic eruptions, and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[10][11] identifies elevated levels of greenhouse gases due to human activity as the main influence. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain the observed increase in mean global temperature. One such hypothesis proposes that warming may be the result of variations in solar activity.[12][13][14]
| + | Several prominent scientists have pointed out the [[politicized science]] of the UN's assessment methods. The scientific reports are submitted to a panel of representatives appointed by each country in the IPCC. Several scientists whose research demonstrates that climate change is taking place have complained about their work being misrepresented by the U.N. |
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| − | None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[15]
| + | In addition, a number of the participants have testified to the pressures placed on them to emphasize results supportive of the current scenario and to suppress other results. That pressure has frequently been effective, and a survey of participants reveals substantial disagreement with the final report.<ref name="cato" /> |
| | | | |
| − | Greenhouse gases in the atmosphere
| + | Richard Lindzen wrote: |
| − | | + | :Perhaps more important are the pressures being brought to bear on scientists to get the "right" results. Such pressures are inevitable, given how far out on a limb much of the scientific community has gone. The situation is compounded by the fact that some of the strongest proponents of "global warming" in Congress are also among the major supporters of science (Sen. Gore is notable among those).<ref name="cato"/> |
| − | Main article: Greenhouse effect
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| − | | |
| − | The greenhouse effect was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. It is the process by which absorption and emission of infrared radiation by atmospheric gases warm a planet's atmosphere and surface.
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| − | | |
| − | Existence of the greenhouse effect as such is not disputed. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F), without which Earth would be uninhabitable.[16][17] Rather, the issue is how the strength of the greenhouse effect is changed when human activity increases the atmospheric concentrations of some greenhouse gases.
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| − | On Earth, the major greenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect (not including clouds); carbon dioxide (CO2), which causes 9–26%; methane (CH4), which causes 4–9%; and ozone, which causes 3–7%.[18][19] Some other naturally occurring gases contribute very small fractions of the greenhouse effect; one of these, nitrous oxide (N2O), is increasing in concentration owing to human activity such as agriculture. The atmospheric concentrations of CO2 and CH4 have increased by 31% and 149% respectively above pre-industrial levels since 1750. Molecule for molecule, methane is a more effective greenhouse gas than carbon dioxide, but its concentration is much smaller so that its total radiative forcing is only about a fourth of that from carbon dioxide. These levels are considerably higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores. From less direct geological evidence it is believed that CO2 values this high were last attained 20 million years ago.[20] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, in particular deforestation.[21]
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| − | | |
| − | The present atmospheric concentration of CO2 is about 383 parts per million (ppm) by volume.[22] Future CO2 levels are expected to rise due to ongoing burning of fossil fuels and land-use change. The rate of rise will depend on uncertain economic, sociological, technological, and natural developments, but may be ultimately limited by the availability of fossil fuels. The IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[23] Fossil fuel reserves are sufficient to reach this level and continue emissions past 2100, if coal, tar sands or methane clathrates are extensively used.[24]
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| − | | |
| − | Feedbacks
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| − | | |
| − | Main article: Effects of global warming#Further global warming (positive feedback)
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| − | | |
| − | The effects of forcing agents on the climate are complicated by various feedback processes.
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| − | One of the most pronounced feedback effects relates to the evaporation of water. In the case of warming by the addition of long-lived greenhouse gases such as CO2, the initial warming will cause more water to be evaporated into the atmosphere. Since water vapor itself acts as a greenhouse gas, this causes still more warming; the warming causes more water vapor to be evaporated, and so forth until a new dynamic equilibrium concentration of water vapor is reached with a much larger greenhouse effect than that due to CO2 alone. Although this feedback process involves an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[25] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.
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| − | | |
| − | Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models. Nevertheless, cloud feedback is second only to water vapor feedback and is positive in all the models that were used in the IPCC Fourth Assessment Report.[25]
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| − | | |
| − | Another important feedback process is ice-albedo feedback.[26] When global temperatures increase, ice near the poles melts at an increasing rate. As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.
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| − | | |
| − | Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism contributing to warming.[27] A massive release of CH4 from methane clathrates could cause rapid warming, according to the clathrate gun hypothesis.
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| − | The ocean's ability to sequester carbon is expected to decline as it warms, because the resulting low nutrient levels of the mesopelagic zone limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[28]
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| − | | |
| − | Solar variation
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| − | Solar variation over the last 30 years.
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| − | Solar variation over the last 30 years.
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| − | Main article: Solar variation
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| − | A few papers suggest that the Sun's contribution may have been underestimated. Two researchers at Duke University, Bruce West and Nicola Scafetta, have estimated that the Sun may have contributed about 45–50% of the increase in the average global surface temperature over the period 1900–2000, and about 25–35% between 1980 and 2000.[29] A paper by Peter Stott and other researchers suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.[30] They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases.
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| − | | |
| − | A different hypothesis is that variations in solar output, possibly amplified by cloud seeding via galactic cosmic rays, may have contributed to recent warming.[31] It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.[32]
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| − | One predicted effect of an increase in solar activity would be a warming of the stratosphere; however, the observed effect since at least 1960 has been a cooling of the lower stratosphere, which is one of the predicted results of greenhouse gas warming.[33] Reduction of stratospheric ozone also has a cooling influence, although substantial ozone depletion did not occur until the late 1970s. Solar variation combined with changes in volcanic activity probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.[1] In 2006, Peter Foukal and other researchers from the United States, Germany, and Switzerland found no net increase of solar brightness over the last thousand years. Solar cycles led to a small increase of 0.07% in brightness over the last 30 years. This effect is far too small to contribute significantly to global warming.[34][35] A paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in cosmic rays.[36] Henrik Svensmark and Eigil Friis-Christensen, the main proponents of cloud seeding by galactic cosmic rays, disputed the findings of Lockwood and Fröhlich.[37] Another recent study speculates that other bodies within the Solar System may influence the climate in a complex manner.[38]
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| − | Temperature changes
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | | |
| − | Main article: Temperature record
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| − | | |
| − | Recent
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| − | | |
| − | Global temperatures on both land and sea have increased by 0.75 °C (1.35 °F) relative to the period 1860–1900, according to the instrumental temperature record. This measured temperature increase is not significantly affected by the urban heat island effect.[39] Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[40] Temperatures in the lower troposphere have increased between 0.12 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with possibly regional fluctuations such as the Medieval Warm Period or the Little Ice Age.
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| − | Sea temperatures increase more slowly than those on land both because of the larger effective heat capacity of the oceans and because the ocean can lose heat by evaporation more readily than the land.[41] Since the Northern Hemisphere has more land mass than the Southern Hemisphere it warms faster; also there are extensive areas of seasonal snow cover subject to the snow-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the asymmetry of warming as the major gases are essentially well-mixed between hemispheres.
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| − | Based on estimates by NASA's Goddard Institute for Space Studies, 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[42] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit concluded that 2005 was the second warmest year, behind 1998.[43][44]
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| − | Anthropogenic emissions of other pollutants—notably sulfate aerosols—can exert a cooling effect by increasing the reflection of incoming sunlight. This partially accounts for the cooling seen in the temperature record in the middle of the twentieth century,[45] though the cooling may also be due in part to natural variability. James Hansen and colleagues have proposed that the effects of the products of fossil fuel combustion—CO2 and aerosols—have largely offset one another, so that warming in recent decades has been driven mainly by non-CO2 greenhouse gases.[46]
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| − | Paleoclimatologist William Ruddiman has argued that human influence on the global climate began around 8,000 years ago with the start of forest clearing to provide land for agriculture and 5,000 years ago with the start of Asian rice irrigation.[47] Ruddiman's interpretation of the historical record, with respect to the methane data, has been disputed.[48]
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| − | Pre-human climate variations
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | | |
| − | Further information: Paleoclimatology
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| − | See also: Snowball Earth
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| − | | |
| − | Earth has experienced warming and cooling many times in the past. The recent Antarctic EPICA ice core spans 800,000 years, including eight glacial cycles timed by orbital variations with interglacial warm periods comparable to present temperatures.[49]
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| − | A rapid buildup of greenhouse gases caused warming in the early Jurassic period (about 180 million years ago), with average temperatures rising by 5 °C (9 °F). Research by the Open University indicates that the warming caused the rate of rock weathering to increase by 400%. As such weathering locks away carbon in calcite and dolomite, CO2 levels dropped back to normal over roughly the next 150,000 years.[50][51]
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| − | Sudden releases of methane from clathrate compounds (the clathrate gun hypothesis) have been hypothesized as a cause for other warming events in the distant past, including the Permian-Triassic extinction event (about 251 million years ago) and the Paleocene-Eocene Thermal Maximum (about 55 million years ago).
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| − | Climate models
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | Main article: Global climate model
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| − | | |
| − | Scientists have studied global warming with computer models of the climate. These models are based on physical principles of fluid dynamics, radiative transfer, and other processes, with simplifications being necessary because of limitations in computer power and the complexity of the underlying system (climate). These models predict that the effect of adding greenhouse gases is to produce a warmer climate.[52] However, even when the same assumptions of future greenhouse gas levels are used, there still remains a considerable range of climate sensitivity.
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| − | Including uncertainties in future greenhouse gas concentrations and climate modeling, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999.[1] Models have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes.
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| − | Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.[53] These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.
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| − | Most global climate models, when run to project future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.[54][55][56]
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| − | The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem.[57] There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability.
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| − | | |
| − | Attributed and expected effects
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| − | | |
| − | Main article: Effects of global warming
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| − | | |
| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Although it is difficult to connect specific weather events to global warming, an increase in global temperatures may in turn cause broader changes, including glacial retreat, Arctic shrinkage, and worldwide sea level rise. Changes in the amount and pattern of precipitation may result in flooding and drought. There may also be changes in the frequency and intensity of extreme weather events. Other effects may include changes in agricultural yields, addition of new trade routes,[58] reduced summer streamflows, species extinctions, and increases in the range of disease vectors.
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| − | Some effects on both the natural environment and human life are, at least in part, already being attributed to global warming. A 2001 report by the IPCC suggests that glacier retreat, ice shelf disruption such as that of the Larsen Ice Shelf, sea level rise, changes in rainfall patterns, and increased intensity and frequency of extreme weather events, are being attributed in part to global warming.[59] While changes are expected for overall patterns, intensity, and frequencies, it is difficult to attribute specific events to global warming. Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.[60]
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| − | Increasing deaths, displacements, and economic losses projected due to extreme weather attributed to global warming may be exacerbated by growing population densities in affected areas, although temperate regions are projected to experience some minor benefits, such as fewer deaths due to cold exposure.[61] A summary of probable effects and recent understanding can be found in the report made for the IPCC Third Assessment Report by Working Group II.[59] The newer IPCC Fourth Assessment Report summary reports that there is observational evidence for an increase in intense tropical cyclone activity in the North Atlantic Ocean since about 1970, in correlation with the increase in sea surface temperature, but that the detection of long-term trends is complicated by the quality of records prior to routine satellite observations. The summary also states that there is no clear trend in the annual worldwide number of tropical cyclones.[1]
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| − | Additional anticipated effects include sea level rise of 110 to 770 millimeters (0.36 to 2.5 ft) between 1990 and 2100,[62] repercussions to agriculture, possible slowing of the thermohaline circulation, reductions in the ozone layer, increased intensity of hurricanes and extreme weather events, lowering of ocean pH, and the spread of diseases such as malaria and dengue fever. One study predicts 18% to 35% of a sample of 1,103 animal and plant species would be extinct by 2050, based on future climate projections.[63] However, few mechanistic studies have documented extinctions due to recent climate change[64] and one study suggests that projected rates of extinction are uncertain.[65]
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| − | Economic
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | Main articles: Economics of global warming and Low-carbon economy
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| − | Some economists have tried to estimate the aggregate net economic costs of damages from climate change across the globe. Such estimates have so far failed to reach conclusive findings; in a survey of 100 estimates, the values ran from US$-10 per tonne of carbon (tC) (US$-3 per tonne of carbon dioxide) up to US$350/tC (US$95 per tonne of carbon dioxide), with a mean of US$43 per tonne of carbon (US$12 per tonne of carbon dioxide).[61] One widely publicized report on potential economic impact is the Stern Review; it suggests that extreme weather might reduce global gross domestic product by up to 1%, and that in a worst-case scenario global per capita consumption could fall 20%.[66] The report's methodology, advocacy and conclusions have been criticized by many economists, primarily around the Review's assumptions of discounting and its choices of scenarios,[67] while others have supported the general attempt to quantify economic risk, even if not the specific numbers.[68][69]
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| − | In a summary of economic cost associated with climate change, the United Nations Environment Programme emphasizes the risks to insurers, reinsurers, and banks of increasingly traumatic and costly weather events. Other economic sectors likely to face difficulties related to climate change include agriculture and transport. Developing countries, rather than the developed world, are at greatest economic risk.[70]
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| − | Security
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| − | In November 2007, the Center for Strategic and International Studies and the Center for a New American Security published a report highlighting the national security effects of climate change.[71] These security effects include increased competition for resources between countries, mass migration from the worst affected areas, challenges to the cohesion of major states threatened by the rise in sea levels, and, as a consequence of these factors, an increased risk of armed conflict, including even nuclear conflicts.
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| − | Adaptation and mitigation
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| − | | |
| − | Main articles: Adaptation to global warming, Mitigation of global warming, and Kyoto Protocol
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| − | | |
| − | The broad agreement among climate scientists that global temperatures will continue to increase has led some nations, states, corporations and individuals to implement actions to try to curtail global warming or adjust to it. Many environmental groups encourage action against global warming, often by the consumer, but also by community and regional organizations. Others have suggested a quota on worldwide fossil fuel production, citing a direct link between fossil fuel production and CO2 emissions.[72][73]
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| − | There has also been business action on climate change, including efforts at increased energy efficiency and limited moves towards use of alternative fuels. One important innovation has been the development of greenhouse gas emissions trading through which companies, in conjunction with government, agree to cap their emissions or to purchase credits from those below their allowances.
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| − | The world's primary international agreement on combating global warming is the Kyoto Protocol, an amendment to the United Nations Framework Convention on Climate Change (UNFCCC) negotiated in 1997. The Protocol now covers more than 160 countries globally and over 55% of global greenhouse gas emissions.[74] Only the United States and Kazakhstan have not ratified the treaty, with the United States historically being the world's largest emitter of greenhouse gas. This treaty expires in 2012, and international talks began in May 2007 on a future treaty to succeed the current one.[75]
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| − | Claiming "serious harm" to the United States economy and the exemption of "80 percent of the world, including major population centers" like China and India, from the treaty, George W. Bush contends that the Kyoto Protocol is an unfair and ineffective means of addressing global climate change concerns.[76] Still, various state, local, and regional governments within the United States have begun their own initiatives to indicate support and compliance with the Kyoto Protocol on a local basis. For example, the Regional Greenhouse Gas Initiative is a state-level emissions capping and trading program involving eight Northeastern U.S. states, which was founded on December 20, 2005.[77]
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| − | China and India, though exempt from its provisions as developing countries, have ratified the Kyoto Protocol. China may have passed the U.S. in total annual greenhouse gas emissions according to some recent studies. Chinese Premier Wen Jiabao has called on the nation to redouble its efforts to tackle pollution and global warming.[78]
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| − | | |
| − | The IPCC's Working Group III is responsible for crafting reports that deal with the mitigation of global warming and analyzing the costs and benefits of different approaches. In the 2007 IPCC Fourth Assessment Report, they conclude that no one technology or sector can be completely responsible for mitigating future warming. They find there are key practices and technologies in various sectors, such as energy supply, transportation, industry, and agriculture, that should be implemented to reduced global emissions. They estimate that stabilization of carbon dioxide equivalent between 445 and 710 ppm by 2030 will result in between a 0.6% increase and 3% decrease in global gross domestic product.[79]
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| − | | |
| − | Social and political debate
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| − | | |
| − | Main articles: Global warming controversy, Politics of global warming, and Economics of global warming
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| − | See also: Climate change denial
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| − | | |
| − | Per capita greenhouse gas emissions in 2000
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | | |
| − | Over the past several years, public perceptions and attitudes concerning the causes and importance of global warming have changed.[80] Increased awareness of the scientific findings surrounding global warming has resulted in political and economic debate. Poor regions, particularly Africa, appear at greatest risk from the suggested effects of global warming, while their actual emissions have been small compared to the developed world.[81] At the same time, developing country exemptions from provisions of the Kyoto Protocol have been criticized by the United States and Australia, and have been used as part of the rationale for continued non-ratification by the U.S.[82] In the Western world, the idea of human influence on climate has gained wider acceptance in Europe than in the United States.[83][84]
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| − | | |
| − | The issue of climate change has sparked debate weighing the benefits of limiting industrial emissions of greenhouse gases against the costs that such changes would entail. There has been discussion in several countries about the cost and benefits of adopting alternative energy sources in order to reduce carbon emissions.[85] Organizations and companies such as the Competitive Enterprise Institute and ExxonMobil have emphasized more conservative climate change scenarios while highlighting the potential economic cost of stricter controls.[86][87][88][89] Likewise, various environmental lobbies and a number of public figures have launched campaigns to emphasize the potential risks of climate change and promote the implementation of stricter controls. Some fossil fuel companies have scaled back their efforts in recent years,[90] or called for policies to reduce global warming.[91]
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| − | | |
| − | Another point of debate is the degree to which newly developed economies such as India and China should be expected to constrain their emissions. China's gross national CO2 emissions are expected to exceed those of the U.S. within the next few years, and may have already done so according to a 2006 report.[92] China has contended that it has less of an obligation to reduce emissions since its per capita emissions are roughly one-fifth that of the United States.[93] India, also exempt from Kyoto restrictions and another of the biggest sources of industrial emissions, has made similar assertions.[94] However, the U.S. contends that if they must bear the cost of reducing emissions, then China should do the same.[95]
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| − | | |
| − | Related climatic issues
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| − | | |
| − | Main articles: Ocean acidification, global dimming, and ozone depletion
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| − | | |
| − | A variety of issues are often raised in relation to global warming. One is ocean acidification. Increased atmospheric CO2 increases the amount of CO2 dissolved in the oceans.[96] CO2 dissolved in the ocean reacts with water to form carbonic acid, resulting in acidification. Ocean surface pH is estimated to have decreased from 8.25 near the beginning of the industrial era to 8.14 by 2004,[97] and is projected to decrease by a further 0.14 to 0.5 units by 2100 as the ocean absorbs more CO2.[1][98] Since organisms and ecosystems are adapted to a narrow range of pH, this raises extinction concerns, directly driven by increased atmospheric CO2, that could disrupt food webs and impact human societies that depend on marine ecosystem services.[99]
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| − | Global dimming, the gradual reduction in the amount of global direct irradiance at the Earth's surface, may have partially mitigated global warming in the late twentieth century. From 1960 to 1990 human-caused aerosols likely precipitated this effect. Scientists have stated with 66–90% confidence that the effects of human-caused aerosols, along with volcanic activity, have offset some of the global warming, and that greenhouse gases would have resulted in more warming than observed if not for these dimming agents.[1]
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| − | | |
| − | Ozone depletion, the steady decline in the total amount of ozone in Earth's stratosphere, is frequently cited in relation to global warming. Although there are areas of linkage, the relationship between the two is not strong.
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| − | | |
| − | See also
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| − | | |
| − | * Glossary of climate change
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| − | | |
| − | References
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| − | | |
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| − | 2. ^ Hegerl, Gabriele C.; et al. (2007-05-07). Understanding and Attributing Climate Change (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 690. Intergovernmental Panel on Climate Change. Retrieved on 2007-05-20. “Recent estimates (Figure 9.9) indicate a relatively small combined effect of natural forcings on the global mean temperature evolution of the seconds half of the 20th century, with a small net cooling from the combined effects of solar and volcanic forcings”
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| − | | |
| − | Global warming is the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.
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| − | | |
| − | The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 year period ending in 2005, which is higher than the earlier estimate of 0.6 ± 0.2 °C for the period ending in 2000.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations"[1] via the greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3] These basic conclusions have been endorsed by at least 30 scientific societies and academies of science, including all of the national academies of science of the major industrialized countries. While individual scientists have voiced disagreement with the conclusions of the IPCC, the overwhelming majority of scientists working on climate change are in agreement with the conclusions.[4]
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| − | Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[1] The range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a millennium even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]
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| − | Increasing global temperature will cause sea level to rise, and is expected to increase the intensity of extreme weather events and to change the amount and pattern of precipitation. Other effects of global warming include changes in agricultural yields, trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.
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| − | Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. There is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences. Most national governments have signed and ratified the Kyoto Protocol, aimed at reducing greenhouse gas emissions.
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| − | Contents
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| − | [hide]
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| − | * 1 Terminology
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| − | * 2 Causes
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| − | o 2.1 Greenhouse gases in the atmosphere
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| − | o 2.2 Feedbacks
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| − | o 2.3 Solar variation
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| − | * 3 Temperature changes
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| − | o 3.1 Recent
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| − | o 3.2 Pre-human climate variations
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| − | * 4 Climate models
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| − | * 5 Attributed and expected effects
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| − | o 5.1 Economic
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| − | o 5.2 Security
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| − | * 6 Adaptation and mitigation
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| − | * 7 Social and political debate
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| − | * 8 Related climatic issues
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| − | * 9 See also
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| − | * 10 References
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| − | * 11 Further reading
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| − | * 12 External links
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| − | | |
| − | Terminology
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| − | The term "global warming" is a specific example of the broader term climate change, which can also refer to global cooling. In common usage, the term refers to recent warming and implies a human influence.[5] The United Nations Framework Convention on Climate Change (UNFCCC) uses the term "climate change" for human-caused change, and "climate variability" for other changes.[6] The term "anthropogenic global warming" is sometimes used when focusing on human-induced changes.
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| − | Causes
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Main articles: Attribution of recent climate change and scientific opinion on climate change
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| − | | |
| − | The Earth's climate changes in response to external forcing, including variations in its orbit around the sun (orbital forcing),[7][8][9] volcanic eruptions, and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[10][11] identifies elevated levels of greenhouse gases due to human activity as the main influence. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain the observed increase in mean global temperature. One such hypothesis proposes that warming may be the result of variations in solar activity.[12][13][14]
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| − | None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[15]
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| − | Greenhouse gases in the atmosphere
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| − | Main article: Greenhouse effect
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| − | The greenhouse effect was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. It is the process by which absorption and emission of infrared radiation by atmospheric gases warm a planet's atmosphere and surface.
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| − | Existence of the greenhouse effect as such is not disputed. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F), without which Earth would be uninhabitable.[16][17] Rather, the issue is how the strength of the greenhouse effect is changed when human activity increases the atmospheric concentrations of some greenhouse gases.
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| − | On Earth, the major greenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect (not including clouds); carbon dioxide (CO2), which causes 9–26%; methane (CH4), which causes 4–9%; and ozone, which causes 3–7%.[18][19] Some other naturally occurring gases contribute very small fractions of the greenhouse effect; one of these, nitrous oxide (N2O), is increasing in concentration owing to human activity such as agriculture. The atmospheric concentrations of CO2 and CH4 have increased by 31% and 149% respectively above pre-industrial levels since 1750. Molecule for molecule, methane is a more effective greenhouse gas than carbon dioxide, but its concentration is much smaller so that its total radiative forcing is only about a fourth of that from carbon dioxide. These levels are considerably higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores. From less direct geological evidence it is believed that CO2 values this high were last attained 20 million years ago.[20] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, in particular deforestation.[21]
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| − | The present atmospheric concentration of CO2 is about 383 parts per million (ppm) by volume.[22] Future CO2 levels are expected to rise due to ongoing burning of fossil fuels and land-use change. The rate of rise will depend on uncertain economic, sociological, technological, and natural developments, but may be ultimately limited by the availability of fossil fuels. The IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[23] Fossil fuel reserves are sufficient to reach this level and continue emissions past 2100, if coal, tar sands or methane clathrates are extensively used.[24]
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| − | Feedbacks
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| − | Main article: Effects of global warming#Further global warming (positive feedback)
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| − | The effects of forcing agents on the climate are complicated by various feedback processes.
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| − | One of the most pronounced feedback effects relates to the evaporation of water. In the case of warming by the addition of long-lived greenhouse gases such as CO2, the initial warming will cause more water to be evaporated into the atmosphere. Since water vapor itself acts as a greenhouse gas, this causes still more warming; the warming causes more water vapor to be evaporated, and so forth until a new dynamic equilibrium concentration of water vapor is reached with a much larger greenhouse effect than that due to CO2 alone. Although this feedback process involves an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[25] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.
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| − | Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models. Nevertheless, cloud feedback is second only to water vapor feedback and is positive in all the models that were used in the IPCC Fourth Assessment Report.[25]
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| − | Another important feedback process is ice-albedo feedback.[26] When global temperatures increase, ice near the poles melts at an increasing rate. As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.
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| − | | |
| − | Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism contributing to warming.[27] A massive release of CH4 from methane clathrates could cause rapid warming, according to the clathrate gun hypothesis.
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| − | The ocean's ability to sequester carbon is expected to decline as it warms, because the resulting low nutrient levels of the mesopelagic zone limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[28] | |
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| − | Solar variation
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| − | Solar variation over the last 30 years.
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| − | Solar variation over the last 30 years.
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| − | Main article: Solar variation
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| − | A few papers suggest that the Sun's contribution may have been underestimated. Two researchers at Duke University, Bruce West and Nicola Scafetta, have estimated that the Sun may have contributed about 45–50% of the increase in the average global surface temperature over the period 1900–2000, and about 25–35% between 1980 and 2000.[29] A paper by Peter Stott and other researchers suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.[30] They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases.
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| − | A different hypothesis is that variations in solar output, possibly amplified by cloud seeding via galactic cosmic rays, may have contributed to recent warming.[31] It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.[32]
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| − | One predicted effect of an increase in solar activity would be a warming of the stratosphere; however, the observed effect since at least 1960 has been a cooling of the lower stratosphere, which is one of the predicted results of greenhouse gas warming.[33] Reduction of stratospheric ozone also has a cooling influence, although substantial ozone depletion did not occur until the late 1970s. Solar variation combined with changes in volcanic activity probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.[1] In 2006, Peter Foukal and other researchers from the United States, Germany, and Switzerland found no net increase of solar brightness over the last thousand years. Solar cycles led to a small increase of 0.07% in brightness over the last 30 years. This effect is far too small to contribute significantly to global warming.[34][35] A paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in cosmic rays.[36] Henrik Svensmark and Eigil Friis-Christensen, the main proponents of cloud seeding by galactic cosmic rays, disputed the findings of Lockwood and Fröhlich.[37] Another recent study speculates that other bodies within the Solar System may influence the climate in a complex manner.[38]
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| − | Temperature changes
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Main article: Temperature record
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| − | Recent
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| − | Global temperatures on both land and sea have increased by 0.75 °C (1.35 °F) relative to the period 1860–1900, according to the instrumental temperature record. This measured temperature increase is not significantly affected by the urban heat island effect.[39] Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[40] Temperatures in the lower troposphere have increased between 0.12 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with possibly regional fluctuations such as the Medieval Warm Period or the Little Ice Age.
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| − | Sea temperatures increase more slowly than those on land both because of the larger effective heat capacity of the oceans and because the ocean can lose heat by evaporation more readily than the land.[41] Since the Northern Hemisphere has more land mass than the Southern Hemisphere it warms faster; also there are extensive areas of seasonal snow cover subject to the snow-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the asymmetry of warming as the major gases are essentially well-mixed between hemispheres.
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| − | Based on estimates by NASA's Goddard Institute for Space Studies, 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[42] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit concluded that 2005 was the second warmest year, behind 1998.[43][44]
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| − | Anthropogenic emissions of other pollutants—notably sulfate aerosols—can exert a cooling effect by increasing the reflection of incoming sunlight. This partially accounts for the cooling seen in the temperature record in the middle of the twentieth century,[45] though the cooling may also be due in part to natural variability. James Hansen and colleagues have proposed that the effects of the products of fossil fuel combustion—CO2 and aerosols—have largely offset one another, so that warming in recent decades has been driven mainly by non-CO2 greenhouse gases.[46]
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| − | Paleoclimatologist William Ruddiman has argued that human influence on the global climate began around 8,000 years ago with the start of forest clearing to provide land for agriculture and 5,000 years ago with the start of Asian rice irrigation.[47] Ruddiman's interpretation of the historical record, with respect to the methane data, has been disputed.[48]
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| − | Pre-human climate variations
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Further information: Paleoclimatology
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| − | See also: Snowball Earth
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| − | Earth has experienced warming and cooling many times in the past. The recent Antarctic EPICA ice core spans 800,000 years, including eight glacial cycles timed by orbital variations with interglacial warm periods comparable to present temperatures.[49]
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| − | A rapid buildup of greenhouse gases caused warming in the early Jurassic period (about 180 million years ago), with average temperatures rising by 5 °C (9 °F). Research by the Open University indicates that the warming caused the rate of rock weathering to increase by 400%. As such weathering locks away carbon in calcite and dolomite, CO2 levels dropped back to normal over roughly the next 150,000 years.[50][51]
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| − | Sudden releases of methane from clathrate compounds (the clathrate gun hypothesis) have been hypothesized as a cause for other warming events in the distant past, including the Permian-Triassic extinction event (about 251 million years ago) and the Paleocene-Eocene Thermal Maximum (about 55 million years ago).
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| − | Climate models
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | Main article: Global climate model
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| − | Scientists have studied global warming with computer models of the climate. These models are based on physical principles of fluid dynamics, radiative transfer, and other processes, with simplifications being necessary because of limitations in computer power and the complexity of the underlying system (climate). These models predict that the effect of adding greenhouse gases is to produce a warmer climate.[52] However, even when the same assumptions of future greenhouse gas levels are used, there still remains a considerable range of climate sensitivity.
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| − | Including uncertainties in future greenhouse gas concentrations and climate modeling, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999.[1] Models have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes.
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| − | Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.[53] These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.
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| − | Most global climate models, when run to project future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.[54][55][56]
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| − | The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem.[57] There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability.
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| − | Attributed and expected effects
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| − | Main article: Effects of global warming
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Although it is difficult to connect specific weather events to global warming, an increase in global temperatures may in turn cause broader changes, including glacial retreat, Arctic shrinkage, and worldwide sea level rise. Changes in the amount and pattern of precipitation may result in flooding and drought. There may also be changes in the frequency and intensity of extreme weather events. Other effects may include changes in agricultural yields, addition of new trade routes,[58] reduced summer streamflows, species extinctions, and increases in the range of disease vectors.
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| − | Some effects on both the natural environment and human life are, at least in part, already being attributed to global warming. A 2001 report by the IPCC suggests that glacier retreat, ice shelf disruption such as that of the Larsen Ice Shelf, sea level rise, changes in rainfall patterns, and increased intensity and frequency of extreme weather events, are being attributed in part to global warming.[59] While changes are expected for overall patterns, intensity, and frequencies, it is difficult to attribute specific events to global warming. Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.[60]
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| − | Increasing deaths, displacements, and economic losses projected due to extreme weather attributed to global warming may be exacerbated by growing population densities in affected areas, although temperate regions are projected to experience some minor benefits, such as fewer deaths due to cold exposure.[61] A summary of probable effects and recent understanding can be found in the report made for the IPCC Third Assessment Report by Working Group II.[59] The newer IPCC Fourth Assessment Report summary reports that there is observational evidence for an increase in intense tropical cyclone activity in the North Atlantic Ocean since about 1970, in correlation with the increase in sea surface temperature, but that the detection of long-term trends is complicated by the quality of records prior to routine satellite observations. The summary also states that there is no clear trend in the annual worldwide number of tropical cyclones.[1]
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| − | Additional anticipated effects include sea level rise of 110 to 770 millimeters (0.36 to 2.5 ft) between 1990 and 2100,[62] repercussions to agriculture, possible slowing of the thermohaline circulation, reductions in the ozone layer, increased intensity of hurricanes and extreme weather events, lowering of ocean pH, and the spread of diseases such as malaria and dengue fever. One study predicts 18% to 35% of a sample of 1,103 animal and plant species would be extinct by 2050, based on future climate projections.[63] However, few mechanistic studies have documented extinctions due to recent climate change[64] and one study suggests that projected rates of extinction are uncertain.[65]
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| − | Economic
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | Main articles: Economics of global warming and Low-carbon economy
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| − | Some economists have tried to estimate the aggregate net economic costs of damages from climate change across the globe. Such estimates have so far failed to reach conclusive findings; in a survey of 100 estimates, the values ran from US$-10 per tonne of carbon (tC) (US$-3 per tonne of carbon dioxide) up to US$350/tC (US$95 per tonne of carbon dioxide), with a mean of US$43 per tonne of carbon (US$12 per tonne of carbon dioxide).[61] One widely publicized report on potential economic impact is the Stern Review; it suggests that extreme weather might reduce global gross domestic product by up to 1%, and that in a worst-case scenario global per capita consumption could fall 20%.[66] The report's methodology, advocacy and conclusions have been criticized by many economists, primarily around the Review's assumptions of discounting and its choices of scenarios,[67] while others have supported the general attempt to quantify economic risk, even if not the specific numbers.[68][69]
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| − | In a summary of economic cost associated with climate change, the United Nations Environment Programme emphasizes the risks to insurers, reinsurers, and banks of increasingly traumatic and costly weather events. Other economic sectors likely to face difficulties related to climate change include agriculture and transport. Developing countries, rather than the developed world, are at greatest economic risk.[70]
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| − | Security
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| − | In November 2007, the Center for Strategic and International Studies and the Center for a New American Security published a report highlighting the national security effects of climate change.[71] These security effects include increased competition for resources between countries, mass migration from the worst affected areas, challenges to the cohesion of major states threatened by the rise in sea levels, and, as a consequence of these factors, an increased risk of armed conflict, including even nuclear conflicts.
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| − | Adaptation and mitigation
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| − | Main articles: Adaptation to global warming, Mitigation of global warming, and Kyoto Protocol
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| − | The broad agreement among climate scientists that global temperatures will continue to increase has led some nations, states, corporations and individuals to implement actions to try to curtail global warming or adjust to it. Many environmental groups encourage action against global warming, often by the consumer, but also by community and regional organizations. Others have suggested a quota on worldwide fossil fuel production, citing a direct link between fossil fuel production and CO2 emissions.[72][73]
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| − | There has also been business action on climate change, including efforts at increased energy efficiency and limited moves towards use of alternative fuels. One important innovation has been the development of greenhouse gas emissions trading through which companies, in conjunction with government, agree to cap their emissions or to purchase credits from those below their allowances.
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| − | The world's primary international agreement on combating global warming is the Kyoto Protocol, an amendment to the United Nations Framework Convention on Climate Change (UNFCCC) negotiated in 1997. The Protocol now covers more than 160 countries globally and over 55% of global greenhouse gas emissions.[74] Only the United States and Kazakhstan have not ratified the treaty, with the United States historically being the world's largest emitter of greenhouse gas. This treaty expires in 2012, and international talks began in May 2007 on a future treaty to succeed the current one.[75]
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| − | Claiming "serious harm" to the United States economy and the exemption of "80 percent of the world, including major population centers" like China and India, from the treaty, George W. Bush contends that the Kyoto Protocol is an unfair and ineffective means of addressing global climate change concerns.[76] Still, various state, local, and regional governments within the United States have begun their own initiatives to indicate support and compliance with the Kyoto Protocol on a local basis. For example, the Regional Greenhouse Gas Initiative is a state-level emissions capping and trading program involving eight Northeastern U.S. states, which was founded on December 20, 2005.[77]
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| − | China and India, though exempt from its provisions as developing countries, have ratified the Kyoto Protocol. China may have passed the U.S. in total annual greenhouse gas emissions according to some recent studies. Chinese Premier Wen Jiabao has called on the nation to redouble its efforts to tackle pollution and global warming.[78]
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| − | The IPCC's Working Group III is responsible for crafting reports that deal with the mitigation of global warming and analyzing the costs and benefits of different approaches. In the 2007 IPCC Fourth Assessment Report, they conclude that no one technology or sector can be completely responsible for mitigating future warming. They find there are key practices and technologies in various sectors, such as energy supply, transportation, industry, and agriculture, that should be implemented to reduced global emissions. They estimate that stabilization of carbon dioxide equivalent between 445 and 710 ppm by 2030 will result in between a 0.6% increase and 3% decrease in global gross domestic product.[79]
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| − | Social and political debate
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| − | | |
| − | Main articles: Global warming controversy, Politics of global warming, and Economics of global warming
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| − | See also: Climate change denial
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Over the past several years, public perceptions and attitudes concerning the causes and importance of global warming have changed.[80] Increased awareness of the scientific findings surrounding global warming has resulted in political and economic debate. Poor regions, particularly Africa, appear at greatest risk from the suggested effects of global warming, while their actual emissions have been small compared to the developed world.[81] At the same time, developing country exemptions from provisions of the Kyoto Protocol have been criticized by the United States and Australia, and have been used as part of the rationale for continued non-ratification by the U.S.[82] In the Western world, the idea of human influence on climate has gained wider acceptance in Europe than in the United States.[83][84]
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| − | The issue of climate change has sparked debate weighing the benefits of limiting industrial emissions of greenhouse gases against the costs that such changes would entail. There has been discussion in several countries about the cost and benefits of adopting alternative energy sources in order to reduce carbon emissions.[85] Organizations and companies such as the Competitive Enterprise Institute and ExxonMobil have emphasized more conservative climate change scenarios while highlighting the potential economic cost of stricter controls.[86][87][88][89] Likewise, various environmental lobbies and a number of public figures have launched campaigns to emphasize the potential risks of climate change and promote the implementation of stricter controls. Some fossil fuel companies have scaled back their efforts in recent years,[90] or called for policies to reduce global warming.[91]
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| − | Another point of debate is the degree to which newly developed economies such as India and China should be expected to constrain their emissions. China's gross national CO2 emissions are expected to exceed those of the U.S. within the next few years, and may have already done so according to a 2006 report.[92] China has contended that it has less of an obligation to reduce emissions since its per capita emissions are roughly one-fifth that of the United States.[93] India, also exempt from Kyoto restrictions and another of the biggest sources of industrial emissions, has made similar assertions.[94] However, the U.S. contends that if they must bear the cost of reducing emissions, then China should do the same.[95]
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| − | Related climatic issues
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| − | Main articles: Ocean acidification, global dimming, and ozone depletion
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| − | A variety of issues are often raised in relation to global warming. One is ocean acidification. Increased atmospheric CO2 increases the amount of CO2 dissolved in the oceans.[96] CO2 dissolved in the ocean reacts with water to form carbonic acid, resulting in acidification. Ocean surface pH is estimated to have decreased from 8.25 near the beginning of the industrial era to 8.14 by 2004,[97] and is projected to decrease by a further 0.14 to 0.5 units by 2100 as the ocean absorbs more CO2.[1][98] Since organisms and ecosystems are adapted to a narrow range of pH, this raises extinction concerns, directly driven by increased atmospheric CO2, that could disrupt food webs and impact human societies that depend on marine ecosystem services.[99]
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| − | Global dimming, the gradual reduction in the amount of global direct irradiance at the Earth's surface, may have partially mitigated global warming in the late twentieth century. From 1960 to 1990 human-caused aerosols likely precipitated this effect. Scientists have stated with 66–90% confidence that the effects of human-caused aerosols, along with volcanic activity, have offset some of the global warming, and that greenhouse gases would have resulted in more warming than observed if not for these dimming agents.[1]
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| − | Ozone depletion, the steady decline in the total amount of ozone in Earth's stratosphere, is frequently cited in relation to global warming. Although there are areas of linkage, the relationship between the two is not strong.
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| − | See also
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| − | * Glossary of climate change
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| − | References
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| − | 1. ^ a b c d e f g h i Summary for Policymakers (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change (2007-02-05). Retrieved on 2007-02-02. “The updated 100-year linear trend (1906 to 2005) of 0.74°C [0.56°C to 0.92°C] is therefore larger than the corresponding trend for 1901 to 2000 given in the TAR of 0.6°C [0.4°C to 0.8°C].”
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| − | 2. ^ Hegerl, Gabriele C.; et al. (2007-05-07). Understanding and Attributing Climate Change (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 690. Intergovernmental Panel on Climate Change. Retrieved on 2007-05-20. “Recent estimates (Figure 9.9) indicate a relatively small combined effect of natural forcings on the global mean temperature evolution of the seconds half of the 20th century, with a small net cooling from the combined effects of solar and volcanic forcings”
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| − | 3. ^ Ammann, Caspar; et al. (2007-04-06). "Solar influence on climate during the past millennium: Results from ransient simulations with the NCAR Climate Simulation Model" (PDF). Proceedings of the National Academy of Sciences of the United States of America 104 (10): 3713–3718. “However, because of a lack of interactive ozone, the model cannot fully simulate features discussed in (44)." "While the NH temperatures of the high-scaled experiment are often colder than the lower bound from proxy data, the modeled decadal-scale NH surface temperature for the medium-scaled case falls within the uncertainty range of the available temperature reconstructions. The medium-scaled simulation also broadly reproduces the main features seen in the proxy records." "Without anthropogenic forcing, the 20th century warming is small. The simulations with only natural forcing components included yield an early 20th century peak warming of ≈0.2 °C (≈1950 AD), which is reduced to about half by the end of the century because of increased volcanism.”
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| − | 4. ^ A guide to facts and fictions about climate change. Royal Society (March 2005). Retrieved on 2007-11-18. “"However, the overwhelming majority of scientists who work on climate change agree on the main points"”
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| − | 5. ^ Climate Change: Basic Information. United States Environmental Protection Agency (2006-12-14). Retrieved on 2007-02-09. “In common usage, 'global warming' often refers to the warming that can occur as a result of increased emissions of greenhouse gases from human activities.”
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| − | 6. ^ United Nations Framework Convention on Climate Change, Article I. United Nations Framework Convention on Climate Change. Retrieved on 2007-01-15.
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| − | 17. ^ Note that the Greenhouse Effect produces a temperature increase of about 33 °C (59 °F) with respect to black body predictions and not a surface temperature of 33 °C (91 °F) which is 32 °F higher. The average surface temperature is about 14 °C (57 °F). Also note that both the Celsius and Fahrenheit temperatures are expressed to 2 significant figures even though the conversion formula produces 3.
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| − | 66. ^ At-a-glance: The Stern Review. BBC (2006-10-30). Retrieved on 2007-04-29.
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| − | 67. ^ Tol and Yohe (2006) "A Review of the Stern Review" World Economics 7(4): 233-50. See also other critiques in World Economics 7(4).
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| − | 68. ^ Brad DeLong. Do unto others....
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| − | 69. ^ John Quiggin. Stern and the critics on discounting.
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| − | 73. ^ Monbiot, George. Rigged - The climate talks are a stitch-up, as no one is talking about supply. (HTML). Retrieved on 2007-12-22.
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| − | 75. ^ Climate talks face international hurdles, by Arthur Max, Associated press, 5/14/07.
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| − | 81. ^ Revkin, Andrew. "Poor Nations to Bear Brunt as World Warms", The New York Times, 2007-04-01. Retrieved on 2007-05-02.
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| − | 84. ^ Summary of Findings. Little Consensus on Global Warming. Partisanship Drives Opinion. Pew Research Center (2006-07-12). Retrieved on 2007-04-14.
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| − | 85. ^ "EU agrees on carbon dioxide cuts", BCC, 2007-03-09. Retrieved on 2007-05-04.
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| − | 88. ^ "Exxon cuts ties to global warming skeptics", MSNBC, 2007-01-12. Retrieved on 2007-05-02.
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| − | 89. ^ Sandell, Clayton. "Report: Big Money Confusing Public on Global Warming", ABC, 2007-01-03. Retrieved on 2007-04-27.
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| − | 93. ^ China: US should take lead on climate, by Michael Casey, Associated Press, 12/7/07.
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| − | 94. ^ India's glaciers give grim message on warming, by Somni Sengupta, 7/17/07, New York Times via oregonlive.com.
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| − | 95. ^ Chinese object to climate draft, BBC, 5/1/07; In Battle for U.S. Carbon Caps, Eyes and Efforts Focus on China,by Steven Mufson, Washington Post, 6/6/07.
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| − | 97. ^ Jacobson, Mark Z. (2005-04-02). "Studying ocean acidification with conservative, stable numerical schemes for nonequilibrium air-ocean exchange and ocean equilibrium chemistry" (PDF). Journal of Geophysical Research 110 (D7). doi:10.1029/2004JD005220. D07302. Retrieved on 2007-04-28.
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| − | | |
| − | Global warming is the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.
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| − | | |
| − | The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 year period ending in 2005, which is higher than the earlier estimate of 0.6 ± 0.2 °C for the period ending in 2000.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations"[1] via the greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3] These basic conclusions have been endorsed by at least 30 scientific societies and academies of science, including all of the national academies of science of the major industrialized countries. While individual scientists have voiced disagreement with the conclusions of the IPCC, the overwhelming majority of scientists working on climate change are in agreement with the conclusions.[4]
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| − | | |
| − | Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[1] The range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a millennium even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]
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| − | | |
| − | Increasing global temperature will cause sea level to rise, and is expected to increase the intensity of extreme weather events and to change the amount and pattern of precipitation. Other effects of global warming include changes in agricultural yields, trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.
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| − | | |
| − | Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. There is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences. Most national governments have signed and ratified the Kyoto Protocol, aimed at reducing greenhouse gas emissions.
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| − | Contents
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| − | [hide]
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| − | | |
| − | * 1 Terminology
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| − | * 2 Causes
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| − | o 2.1 Greenhouse gases in the atmosphere
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| − | o 2.2 Feedbacks
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| − | o 2.3 Solar variation
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| − | * 3 Temperature changes
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| − | o 3.1 Recent
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| − | o 3.2 Pre-human climate variations
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| − | * 4 Climate models
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| − | * 5 Attributed and expected effects
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| − | o 5.1 Economic
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| − | o 5.2 Security
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| − | * 6 Adaptation and mitigation
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| − | * 7 Social and political debate
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| − | * 8 Related climatic issues
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| − | * 9 See also
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| − | * 10 References
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| − | * 11 Further reading
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| − | * 12 External links
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| − | | |
| − | Terminology
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| − | | |
| − | The term "global warming" is a specific example of the broader term climate change, which can also refer to global cooling. In common usage, the term refers to recent warming and implies a human influence.[5] The United Nations Framework Convention on Climate Change (UNFCCC) uses the term "climate change" for human-caused change, and "climate variability" for other changes.[6] The term "anthropogenic global warming" is sometimes used when focusing on human-induced changes.
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| − | | |
| − | Causes
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Main articles: Attribution of recent climate change and scientific opinion on climate change
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| − | The Earth's climate changes in response to external forcing, including variations in its orbit around the sun (orbital forcing),[7][8][9] volcanic eruptions, and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[10][11] identifies elevated levels of greenhouse gases due to human activity as the main influence. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain the observed increase in mean global temperature. One such hypothesis proposes that warming may be the result of variations in solar activity.[12][13][14]
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| − | None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[15]
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| − | Greenhouse gases in the atmosphere
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| − | Main article: Greenhouse effect
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| − | The greenhouse effect was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. It is the process by which absorption and emission of infrared radiation by atmospheric gases warm a planet's atmosphere and surface.
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| − | Existence of the greenhouse effect as such is not disputed. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F), without which Earth would be uninhabitable.[16][17] Rather, the issue is how the strength of the greenhouse effect is changed when human activity increases the atmospheric concentrations of some greenhouse gases.
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| − | On Earth, the major greenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect (not including clouds); carbon dioxide (CO2), which causes 9–26%; methane (CH4), which causes 4–9%; and ozone, which causes 3–7%.[18][19] Some other naturally occurring gases contribute very small fractions of the greenhouse effect; one of these, nitrous oxide (N2O), is increasing in concentration owing to human activity such as agriculture. The atmospheric concentrations of CO2 and CH4 have increased by 31% and 149% respectively above pre-industrial levels since 1750. Molecule for molecule, methane is a more effective greenhouse gas than carbon dioxide, but its concentration is much smaller so that its total radiative forcing is only about a fourth of that from carbon dioxide. These levels are considerably higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores. From less direct geological evidence it is believed that CO2 values this high were last attained 20 million years ago.[20] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, in particular deforestation.[21]
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| − | The present atmospheric concentration of CO2 is about 383 parts per million (ppm) by volume.[22] Future CO2 levels are expected to rise due to ongoing burning of fossil fuels and land-use change. The rate of rise will depend on uncertain economic, sociological, technological, and natural developments, but may be ultimately limited by the availability of fossil fuels. The IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[23] Fossil fuel reserves are sufficient to reach this level and continue emissions past 2100, if coal, tar sands or methane clathrates are extensively used.[24]
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| − | Feedbacks
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| − | Main article: Effects of global warming#Further global warming (positive feedback)
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| − | The effects of forcing agents on the climate are complicated by various feedback processes.
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| − | One of the most pronounced feedback effects relates to the evaporation of water. In the case of warming by the addition of long-lived greenhouse gases such as CO2, the initial warming will cause more water to be evaporated into the atmosphere. Since water vapor itself acts as a greenhouse gas, this causes still more warming; the warming causes more water vapor to be evaporated, and so forth until a new dynamic equilibrium concentration of water vapor is reached with a much larger greenhouse effect than that due to CO2 alone. Although this feedback process involves an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[25] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.
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| − | Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models. Nevertheless, cloud feedback is second only to water vapor feedback and is positive in all the models that were used in the IPCC Fourth Assessment Report.[25]
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| − | Another important feedback process is ice-albedo feedback.[26] When global temperatures increase, ice near the poles melts at an increasing rate. As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.
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| − | Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism contributing to warming.[27] A massive release of CH4 from methane clathrates could cause rapid warming, according to the clathrate gun hypothesis.
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| − | The ocean's ability to sequester carbon is expected to decline as it warms, because the resulting low nutrient levels of the mesopelagic zone limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[28]
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| − | Solar variation
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| − | Solar variation over the last 30 years.
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| − | Solar variation over the last 30 years.
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| − | Main article: Solar variation
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| − | A few papers suggest that the Sun's contribution may have been underestimated. Two researchers at Duke University, Bruce West and Nicola Scafetta, have estimated that the Sun may have contributed about 45–50% of the increase in the average global surface temperature over the period 1900–2000, and about 25–35% between 1980 and 2000.[29] A paper by Peter Stott and other researchers suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.[30] They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases.
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| − | A different hypothesis is that variations in solar output, possibly amplified by cloud seeding via galactic cosmic rays, may have contributed to recent warming.[31] It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.[32]
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| − | One predicted effect of an increase in solar activity would be a warming of the stratosphere; however, the observed effect since at least 1960 has been a cooling of the lower stratosphere, which is one of the predicted results of greenhouse gas warming.[33] Reduction of stratospheric ozone also has a cooling influence, although substantial ozone depletion did not occur until the late 1970s. Solar variation combined with changes in volcanic activity probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.[1] In 2006, Peter Foukal and other researchers from the United States, Germany, and Switzerland found no net increase of solar brightness over the last thousand years. Solar cycles led to a small increase of 0.07% in brightness over the last 30 years. This effect is far too small to contribute significantly to global warming.[34][35] A paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in cosmic rays.[36] Henrik Svensmark and Eigil Friis-Christensen, the main proponents of cloud seeding by galactic cosmic rays, disputed the findings of Lockwood and Fröhlich.[37] Another recent study speculates that other bodies within the Solar System may influence the climate in a complex manner.[38]
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| − | Temperature changes
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | | |
| − | Main article: Temperature record
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| − | Recent
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| − | Global temperatures on both land and sea have increased by 0.75 °C (1.35 °F) relative to the period 1860–1900, according to the instrumental temperature record. This measured temperature increase is not significantly affected by the urban heat island effect.[39] Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[40] Temperatures in the lower troposphere have increased between 0.12 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with possibly regional fluctuations such as the Medieval Warm Period or the Little Ice Age.
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| − | Sea temperatures increase more slowly than those on land both because of the larger effective heat capacity of the oceans and because the ocean can lose heat by evaporation more readily than the land.[41] Since the Northern Hemisphere has more land mass than the Southern Hemisphere it warms faster; also there are extensive areas of seasonal snow cover subject to the snow-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the asymmetry of warming as the major gases are essentially well-mixed between hemispheres.
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| − | Based on estimates by NASA's Goddard Institute for Space Studies, 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[42] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit concluded that 2005 was the second warmest year, behind 1998.[43][44]
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| − | Anthropogenic emissions of other pollutants—notably sulfate aerosols—can exert a cooling effect by increasing the reflection of incoming sunlight. This partially accounts for the cooling seen in the temperature record in the middle of the twentieth century,[45] though the cooling may also be due in part to natural variability. James Hansen and colleagues have proposed that the effects of the products of fossil fuel combustion—CO2 and aerosols—have largely offset one another, so that warming in recent decades has been driven mainly by non-CO2 greenhouse gases.[46]
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| − | Paleoclimatologist William Ruddiman has argued that human influence on the global climate began around 8,000 years ago with the start of forest clearing to provide land for agriculture and 5,000 years ago with the start of Asian rice irrigation.[47] Ruddiman's interpretation of the historical record, with respect to the methane data, has been disputed.[48]
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| − | Pre-human climate variations
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Further information: Paleoclimatology
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| − | See also: Snowball Earth
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| − | | |
| − | Earth has experienced warming and cooling many times in the past. The recent Antarctic EPICA ice core spans 800,000 years, including eight glacial cycles timed by orbital variations with interglacial warm periods comparable to present temperatures.[49]
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| − | A rapid buildup of greenhouse gases caused warming in the early Jurassic period (about 180 million years ago), with average temperatures rising by 5 °C (9 °F). Research by the Open University indicates that the warming caused the rate of rock weathering to increase by 400%. As such weathering locks away carbon in calcite and dolomite, CO2 levels dropped back to normal over roughly the next 150,000 years.[50][51]
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| − | Sudden releases of methane from clathrate compounds (the clathrate gun hypothesis) have been hypothesized as a cause for other warming events in the distant past, including the Permian-Triassic extinction event (about 251 million years ago) and the Paleocene-Eocene Thermal Maximum (about 55 million years ago).
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| − | Climate models
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | Main article: Global climate model
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| − | | |
| − | Scientists have studied global warming with computer models of the climate. These models are based on physical principles of fluid dynamics, radiative transfer, and other processes, with simplifications being necessary because of limitations in computer power and the complexity of the underlying system (climate). These models predict that the effect of adding greenhouse gases is to produce a warmer climate.[52] However, even when the same assumptions of future greenhouse gas levels are used, there still remains a considerable range of climate sensitivity.
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| − | Including uncertainties in future greenhouse gas concentrations and climate modeling, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999.[1] Models have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes.
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| − | Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.[53] These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.
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| − | Most global climate models, when run to project future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.[54][55][56]
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| − | The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem.[57] There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability.
| + | [[Christopher Monckton]] wrote an article entitled "Climate sensitivity reconsidered" which states that the Intergovernmental Panel on Climate Change studies are flawed.<ref>Monckton, Christopher (July 2008). [http://www.aps.org/units/fps/newsletters/200807/monckton.cfm "Climate sensitivity reconsidered"]. ''Physics & Society'' newsletter. Retrieved from American Physical Society/Forum on Physics and Society website on September 29, 2014.</ref> |
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| − | Attributed and expected effects
| + | :The present analysis suggests that the failure of the IPCC's models to predict this and many other climatic phenomena arises from defects in its evaluation of the three factors whose product is climate sensitivity: |
| | | | |
| − | Main article: Effects of global warming
| + | ::Radiative forcing ΔF; |
| | + | ::The no-feedbacks climate sensitivity parameter κ; and |
| | + | ::The feedback multiplier ƒ. |
| | | | |
| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
| + | :Some reasons why the IPCC’s estimates may be excessive and unsafe are explained. More importantly, the conclusion is that, perhaps, there is no “climate crisis”, and that currently-fashionable efforts by governments to reduce anthropogenic CO<sub>2</sub> emissions are pointless, may be ill-conceived, and could even be harmful. |
| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Although it is difficult to connect specific weather events to global warming, an increase in global temperatures may in turn cause broader changes, including glacial retreat, Arctic shrinkage, and worldwide sea level rise. Changes in the amount and pattern of precipitation may result in flooding and drought. There may also be changes in the frequency and intensity of extreme weather events. Other effects may include changes in agricultural yields, addition of new trade routes,[58] reduced summer streamflows, species extinctions, and increases in the range of disease vectors.
| + | This was published on a forum of the American Physical Society with the following disclaimers: "The article has not undergone any scientific peer review" and "the APS disagrees with the article's conclusions". In fact, the APS disagrees with the article without ever reviewing it. |
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| − | Some effects on both the natural environment and human life are, at least in part, already being attributed to global warming. A 2001 report by the IPCC suggests that glacier retreat, ice shelf disruption such as that of the Larsen Ice Shelf, sea level rise, changes in rainfall patterns, and increased intensity and frequency of extreme weather events, are being attributed in part to global warming.[59] While changes are expected for overall patterns, intensity, and frequencies, it is difficult to attribute specific events to global warming. Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.[60]
| + | Ryan N. Maue: |
| | + | :A doctoral student at the Department of Meteorology at Florida State University did a study of global tropical cyclone activity. Its conclusions state that global warming might be greatly overblown.<ref>Tribune-Review, The (March 21, 2009). [http://www.pittsburghlive.com/x/pittsburghtrib/opinion/s_617111.html# "Global warming? More doubts"]. TribLive [''Pittsburgh Tribune'' website]. Retrieved on September 29, 2014.</ref> Mr. Maue found that tropical cyclone activity worldwide "has completely and utterly collapsed" during the past two to three years with energy levels sinking to those of the late 1970s. |
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| − | Increasing deaths, displacements, and economic losses projected due to extreme weather attributed to global warming may be exacerbated by growing population densities in affected areas, although temperate regions are projected to experience some minor benefits, such as fewer deaths due to cold exposure.[61] A summary of probable effects and recent understanding can be found in the report made for the IPCC Third Assessment Report by Working Group II.[59] The newer IPCC Fourth Assessment Report summary reports that there is observational evidence for an increase in intense tropical cyclone activity in the North Atlantic Ocean since about 1970, in correlation with the increase in sea surface temperature, but that the detection of long-term trends is complicated by the quality of records prior to routine satellite observations. The summary also states that there is no clear trend in the annual worldwide number of tropical cyclones.[1]
| + | Dr. Vincent Gray: |
| | + | :A member of the IPCC’s expert reviewers’ panel asserts, "There is no relationship between warming and the level of gases in the atmosphere," and "there is no serious threat to the climate" <ref>Hendrickson, Mark W. (May 25, 2009). [https://townhall.com/columnists/markwhendrickson/2009/05/25/a_closer_look_at_climate_change "A closer look at climate change"]. Townhall.com. Retrieved on September 29, 2014. "The panic over global warming is totally unjustified" says Vice Chair, IPCC.</ref> |
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| − | Additional anticipated effects include sea level rise of 110 to 770 millimeters (0.36 to 2.5 ft) between 1990 and 2100,[62] repercussions to agriculture, possible slowing of the thermohaline circulation, reductions in the ozone layer, increased intensity of hurricanes and extreme weather events, lowering of ocean pH, and the spread of diseases such as malaria and dengue fever. One study predicts 18% to 35% of a sample of 1,103 animal and plant species would be extinct by 2050, based on future climate projections.[63] However, few mechanistic studies have documented extinctions due to recent climate change[64] and one study suggests that projected rates of extinction are uncertain.[65]
| + | Joe D’Aleo: Climatologist: |
| | + | :The International Climate and Environmental Change Assessment Project says new data "show that in five of the last seven decades since World War II, including this one, global temperatures have cooled while carbon dioxide has continued to rise," and "'''The data suggest cooling''', not warming, in Earth's future." <ref>[https://www.wnd.com/index.php?fa=PAGE.view&pageId=92557 "Shocker: 'Global warming' simply no longer happening"] (March 22, 2009). WND. Retrieved on September 29, 2014.</ref> |
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| − | Economic
| + | Dr. John S. Theon: |
| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
| + | :Retired senior NASA atmospheric [[scientist]], Dr. John S. Theon, the former boss of global warming alarmist James Hansen of [[NASA]], rebukes him declaring “climate models are useless.” “My own belief concerning anthropogenic climate change is that the models do not realistically simulate the climate system because there are many very important sub-grid scale processes that the models either replicate poorly or completely omit,” “Furthermore, some scientists have manipulated the observed data to justify their model results." <ref>Blumer, Tom (January 28, 2009). [http://newsbusters.org/blogs/tom-blumer/2009/01/28/former-boss-rebukes-nasa-global-warming-alarmist-hansen-agw-skeptic "Former boss rebukes NASA global warming alarmist Hansen, is AGW skeptic"]. MRC NewsBusters. Retrieved on September 29, 2014.</ref> |
| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| | | | |
| − | Main articles: Economics of global warming and Low-carbon economy
| + | Sammy Wilson—Ireland's environment minister |
| | + | :He argues that global weather patterns are naturally cooling, not warming. He calls television ads that promote global warming as "an insidious propaganda campaign" peddling "patent nonsense." <ref>Pogatchnik, Shawn (February 9, 2009). [http://cnsnews.com/news/article/belfast-environment-chief-bans-climate-change-ads "Belfast environment chief bans climate change ads"]. Associated Press. Retrieved from CNSNews.com on September 29, 2014.</ref> |
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| − | Some economists have tried to estimate the aggregate net economic costs of damages from climate change across the globe. Such estimates have so far failed to reach conclusive findings; in a survey of 100 estimates, the values ran from US$-10 per tonne of carbon (tC) (US$-3 per tonne of carbon dioxide) up to US$350/tC (US$95 per tonne of carbon dioxide), with a mean of US$43 per tonne of carbon (US$12 per tonne of carbon dioxide).[61] One widely publicized report on potential economic impact is the Stern Review; it suggests that extreme weather might reduce global gross domestic product by up to 1%, and that in a worst-case scenario global per capita consumption could fall 20%.[66] The report's methodology, advocacy and conclusions have been criticized by many economists, primarily around the Review's assumptions of discounting and its choices of scenarios,[67] while others have supported the general attempt to quantify economic risk, even if not the specific numbers.[68][69]
| + | After the broadcast of his movie '[[The Great Global Warming Swindle]]', filmmaker Martin Durkin's statements read <ref>Goodenough, Patrick (July 22, 2008). [http://cnsnews.com/news/article/uk-broadcaster-scolded-film-global-warming-swindle "UK broadcaster scolded for film on global warming"]. CNSNews. Retrieved on September 29, 2014.</ref> |
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| − | In a summary of economic cost associated with climate change, the United Nations Environment Programme emphasizes the risks to insurers, reinsurers, and banks of increasingly traumatic and costly weather events. Other economic sectors likely to face difficulties related to climate change include agriculture and transport. Developing countries, rather than the developed world, are at greatest economic risk.[70]
| + | *“Everywhere you are told that man-made [[climate change]] is proved beyond doubt,” “But you are being told lies.” |
| | + | *“This is a story of how a theory about climate turned into a political [[ideology]] ... it is the story of the distortion of a whole area of [[science]].” |
| | + | *“as the frenzy over man-made global warming grows shriller, many senior scientists say the actual scientific basis for the [[theory]] is crumbling.” |
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| − | Security
| + | In late 2008, the [[AP]] published an article by its Science Writer Seth Borenstein, which is seen by skeptics as another example of one-sided, uncritical reporting on the issue by [[liberal media]]. The report stated that global warming was "a ticking time bomb that President-elect Barack Obama can't avoid", and that "We're out of time", with Al Gore calling the situation "the equivalent of a five-alarm fire that has to be addressed immediately."<ref>Borenstein, Seth (December 14, 2008). [https://web.archive.org/web/20081215162025/https://www.breitbart.com/article.php?id=D952LKOO1&show_article=1 "Obama left with little time to curb global warming"]. Associated Press. Reprinted at Breitbart.com. Retrieved from December 15, 2008 archive at Internet Archive on September 29, 2014.</ref> In response, Fox News (December 16, 2008) reported that scientists skeptical of anthropogenic global warming criticized the report as "irrational hysteria," "horrifically bad" and "incredibly biased", containing sweeping scientific errors and being a one-sided portrayal of a complicated issue. Geology professor [[David Deming]] stated, "If the issues weren't so serious and the ramifications so profound, I would have to laugh at it", and accused Borenstein of "writing a polemic and reporting it as fact." Deming noted that "the mean global temperature, at least as measured by satellite, is now the same as it was in the year 1980. In the last couple of years sea level has stopped rising. Hurricane and cyclone activity in the northern hemisphere is at a 24-year low and sea ice globally is also the same as it was in 1980." The AP responded to criticism by stating that, "It’s a news story, based on fact and the clearly expressed views of President-elect Barack Obama and others."<ref>[https://www.foxnews.com/story/0,2933,468084,00.html "Scientists call AP Report on global warming 'hysteria'"] (December 16, 2008). Fox News website. Retrieved on September 29, 2014.</ref> |
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| − | In November 2007, the Center for Strategic and International Studies and the Center for a New American Security published a report highlighting the national security effects of climate change.[71] These security effects include increased competition for resources between countries, mass migration from the worst affected areas, challenges to the cohesion of major states threatened by the rise in sea levels, and, as a consequence of these factors, an increased risk of armed conflict, including even nuclear conflicts.
| + | Also in the discussion of the biased AP report, Michael R. Fox, a retired nuclear scientist and chemistry professor from the University of Idaho stated, "There is little evidence to believe that man-made carbon dioxide is causing temperature fluctuation. Other factors, including sun spots, solar winds, variations in the solar magnetic field and solar irradiation, could all be affecting temperature changes." |
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| − | Adaptation and mitigation
| + | The year 2008 turned out to be the coolest year since 2000, yet the seventh to tenth warmest year on record, according to the NASA Goddard Institute for Space Studies.<ref>[https://web.archive.org/web/20110725075133/http://news.eoportal.org/research/090127_res3.html "2008 global temperature"] (January 21, 2009). EO [Earth Observation]. Retrieved from July 25, 2011 archive at Internet Archive on September 29, 2014.</ref> According to a preliminary analysis by NOAA's National Climatic Data Center, the average June–August 2009 summer temperature for the contiguous United States was below average—the 34th coolest on record.<ref>[http://www.noaanews.noaa.gov/stories2009/20090910_summerstats.html "NOAA: Summer temperature below average for U.S."] (September 10, 2009). NOAA. Retrieved on September 29, 2014.</ref> |
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| − | Main articles: Adaptation to global warming, Mitigation of global warming, and Kyoto Protocol
| + | Richard S. Courtney, a U.N. Intergovernmental Panel on Climate Change (IPCC) expert reviewer and a U.K.-based climate and atmospheric science consultant says "Rubbish! Global warming is not 'accelerating," and "...that anybody who proclaims that 'Global warming is accelerating' is a liar, a fool, or both."<ref>Brennan, Phil (December 16, 2008). [https://www.newsmax.com/brennan/global-warming-debunked/2009/12/12/id/341719/ "Global warming’s last gasp"]. NewsMax. Retrieved on September 29, 2014.</ref> |
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| − | The broad agreement among climate scientists that global temperatures will continue to increase has led some nations, states, corporations and individuals to implement actions to try to curtail global warming or adjust to it. Many environmental groups encourage action against global warming, often by the consumer, but also by community and regional organizations. Others have suggested a quota on worldwide fossil fuel production, citing a direct link between fossil fuel production and CO2 emissions.[72][73]
| + | Don J. Easterbrook, Ph.D., emeritus professor of geology at Western Washington University, asked, "What does it take to ignore 10 years of global cooling....? The answer is really quite simple—just follow the money!" |
| | + | ==== Belief in global warming and political and religious views ==== |
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| − | There has also been business action on climate change, including efforts at increased energy efficiency and limited moves towards use of alternative fuels. One important innovation has been the development of greenhouse gas emissions trading through which companies, in conjunction with government, agree to cap their emissions or to purchase credits from those below their allowances.
| + | The more religious an individual is, the more likely they are to disbelieve in global warming. In 2014, whereas 80% of American [[Atheism|atheists]] believed in climate change, only 56% of all very religious Americans did.<ref name="randalolson.com">[http://www.randalolson.com/2014/09/13/who-are-the-climate-change-deniers/ Statistics on belief in climate change], Randal S. Olson</ref> |
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| − | The world's primary international agreement on combating global warming is the Kyoto Protocol, an amendment to the United Nations Framework Convention on Climate Change (UNFCCC) negotiated in 1997. The Protocol now covers more than 160 countries globally and over 55% of global greenhouse gas emissions.[74] Only the United States and Kazakhstan have not ratified the treaty, with the United States historically being the world's largest emitter of greenhouse gas. This treaty expires in 2012, and international talks began in May 2007 on a future treaty to succeed the current one.[75]
| + | In 2014, 86% of [[Democrats]] accepted climate change, whereas half of all [[Republican]]s disbelieve in global warming.<ref name="randalolson.com"/> |
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| − | Claiming "serious harm" to the United States economy and the exemption of "80 percent of the world, including major population centers" like China and India, from the treaty, George W. Bush contends that the Kyoto Protocol is an unfair and ineffective means of addressing global climate change concerns.[76] Still, various state, local, and regional governments within the United States have begun their own initiatives to indicate support and compliance with the Kyoto Protocol on a local basis. For example, the Regional Greenhouse Gas Initiative is a state-level emissions capping and trading program involving eight Northeastern U.S. states, which was founded on December 20, 2005.[77]
| + | ===== Evangelicals ===== |
| | + | In 2008 86 evangelical pastors, including Rev. Dr.[[Rick Warren]] signed a statement titled "Climate Change: An Evangelical Call to Action", which called on Christians to acknowledge the moral importance of action to counteract man-made climate change. the statement includes specific support for market-based CO<sub>2</sub> reductions such as a cap-and-trade program.<ref>Evangelical Climate Initiative (2006). [https://web.archive.org/web/20140201232519/http://christiansandclimate.org/statement/ "ECI Statement"]. Climate Change: An Evangelical Call to Action. Retrieved from February 1, 2014 archive at Internet Archive on September 29, 2014.</ref> In contrast, a group of evangelical scholars, comprised of scientists, economists and theologians, contend that the liberal view of pending catastrophe caused by climate change is misleading and/or exaggerated.<ref>Vu, Michelle A. (December 4, 2009). [http://www.christianpost.com/article/20091204/evangelicals-push-back-against-climate-change-hoax/pageall.html "Evangelicals push back against global warming doom"] The Christian Post website. Retrieved on September 29, 2014.</ref> |
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| − | China and India, though exempt from its provisions as developing countries, have ratified the Kyoto Protocol. China may have passed the U.S. in total annual greenhouse gas emissions according to some recent studies. Chinese Premier Wen Jiabao has called on the nation to redouble its efforts to tackle pollution and global warming.[78]
| + | ===The Bill Nye challenge=== |
| | | | |
| − | The IPCC's Working Group III is responsible for crafting reports that deal with the mitigation of global warming and analyzing the costs and benefits of different approaches. In the 2007 IPCC Fourth Assessment Report, they conclude that no one technology or sector can be completely responsible for mitigating future warming. They find there are key practices and technologies in various sectors, such as energy supply, transportation, industry, and agriculture, that should be implemented to reduced global emissions. They estimate that stabilization of carbon dioxide equivalent between 445 and 710 ppm by 2030 will result in between a 0.6% increase and 3% decrease in global gross domestic product.[79]
| + | In April 2016 science popularizer "[[Bill Nye|Bill Nye the Science Guy]]" took the debate up to the "put your money where your mouth is" level. He issued two bets, of $10,000 each, with Joe Bastardi, a "climate change contrarian" and frequent critic of Nye. One bet was that "2016 will be in the top 10 of hottest years on record", and that "this current decade will be the warmest ever recorded".<ref>[http://time.com/4301258/bill-nye-sarah-palin-climate-change-bet/ The Bill Nye climate change bet].</ref> As of late May Mr. Bastardi has not taken up the offer. |
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| − | Social and political debate
| + | ==Inaccuracies of global warming evidence== |
| | + | ===Climate "science" fraud=== |
| | + | {{main|Climategate}} |
| | | | |
| − | Main articles: Global warming controversy, Politics of global warming, and Economics of global warming
| + | The [[Climategate#Climategate scandal|Climategate scandal]] revealed how liberal scientists appeared to be deceiving the public with the use of fraudulent data for use as climate science. The [[liberal media]] has attempted to bury the story and discount it as the work of computer hackers illegally stealing data. However, [[FOIA|Freedom of Information]] requests is likely what led to the data being leaked — intentionally.<ref>[https://web.archive.org/web/20091212190817/http://www.junkscience.com/ JunkScience.com] (December 12, 2009). Retrieved from December 12, 2009 archive at Internet Archive on September 29, 2014.</ref> Dr. Willie Soon, a [[physicist]], [[astronomer]] and climate researcher at the solar and stellar physics division of the [[Harvard University]]-Smithsonian Center for Astrophysics, said in an interview, "[The Climatic Research Unit climate scientists] are making scientific progress more difficult now. This is a shameful, dark day for science." Dr. Soon also suggested that there has been systemic suppression of dissenting opinion among scientists in the climate change community, ranging from social snubs to e-mail stalking and even threats of harm.<ref>Koprowski, Gene J. (December 1, 2009). [https://www.foxnews.com/story/0,2933,578368,00.html "Global warming scandal makes scientific progress more difficult, experts say"]. Fox News website. Retrieved on September 30, 2014. See [[Fox News]].</ref> |
| − | See also: Climate change denial
| |
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| − | Per capita greenhouse gas emissions in 2000
| + | [[Image:GoreFireBreathing.jpg|thumb|left|250px|Al Gore's [[Schlockumentary]] under fire; ''[[An Inconvenient Truth]]'' found to be an inconvenient [[lie]] based on [[junk science]] and digitally enhanced, totally faked scenes of polar icecaps melting.]] |
| − | Per capita greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Over the past several years, public perceptions and attitudes concerning the causes and importance of global warming have changed.[80] Increased awareness of the scientific findings surrounding global warming has resulted in political and economic debate. Poor regions, particularly Africa, appear at greatest risk from the suggested effects of global warming, while their actual emissions have been small compared to the developed world.[81] At the same time, developing country exemptions from provisions of the Kyoto Protocol have been criticized by the United States and Australia, and have been used as part of the rationale for continued non-ratification by the U.S.[82] In the Western world, the idea of human influence on climate has gained wider acceptance in Europe than in the United States.[83][84]
| + | ===Liberal claims of "consensus"=== |
| | + | Reports of a scientific "consensus" among scientists are similar to their one-sided support of other [[liberal]] policies and beliefs. For example, nearly 100% of political donations from professors are to [[Democrats]] rather than Republicans. Similarly, according to NASA, 97% of climate scientists believe that climate-warming trends over the past century are very likely due to human activities.<ref>NASA's Jet Propulsion Laboratory-California Institute of Technology Earth Science Communications Team (2013). [http://climate.nasa.gov/scientific-consensus "Consensus"]. NASA website/Global Climate Change. Retrieved on September 30, 2014.</ref> These liberal scientists believe, or say they believe, that the Earth is warming overall, and that this warming, as well as other changes in climate patterns, is largely caused by human activities.<ref>Multiple references: |
| | + | *Anderegg, William R. L., Prall, James W. et al. (July 6, 2010). [http://www.pnas.org/content/early/2010/06/04/1003187107.full.pdf+html "Expert credibility in climate change."] ''Proceedings of the National Academy of Sciences'', vol. 107, no. 27, pp. 12107-12109. Retrieved from PNAS.org on September 30, 2014. |
| | + | *[http://www.ipcc.ch/publications_and_data/ar4/wg1/en/spmsspm-understanding-and.html "Working group I: The physical science basis/Summary for policy makers/Understanding and attributing climate change"] (2007). ''IPCC Fourth Assessment Report: Climate Change 2007.'' Retrieved from Intergovernmental Panel on Climate Change website on September 30, 2014.</ref> These allegations do not necessarily make the consensus true, as discussed throughout the referenced citation. Numerous scientists, especially those outside of university faculties, have been critical of anthropogenic global warming. However, according to some researchers, scientists who do not support the anthropogenic global warming theory offer a general lack of comparative credentials; proponents of man-made global warming argue that this has led to agreement that, among authorities in scientific disciplines, there is a "[[scientific consensus]]" supporting the theory for greater government control. Scientists skeptical of the theory question whether there is a financial incentive for supporting research.<ref>Chesser, Paul (October 25, 2007). [http://www.seattlepi.com/local/opinion/article/Be-wary-of-climate-policy-development-1253536.php "Be wary of climate policy development"]. Seattle Post-Intelligencer website. Retrieved on September 30, 2014.</ref> It has also been documented that on most college campuses criticism of the global warming theory is silenced or censored; evidence shows that scientists skeptical of AGW are being suppressed.<ref>Multiple references: |
| | + | *O'Neill, Brendan (October 6, 2006). [http://www.spiked-online.com/index.php?/site/article/1782/ "Global warming: The chilling effect on free speech"]. Sp!ked. Retrieved on September 30, 2014. |
| | + | *Schilling, Chelsea (June 24, 2009). [https://www.wnd.com/index.php?fa=PAGE.view&pageId=102031 "EPA's own research expert 'shut up' on climate change"]. WND. Retrieved on September 30, 2014.</ref> |
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| − | The issue of climate change has sparked debate weighing the benefits of limiting industrial emissions of greenhouse gases against the costs that such changes would entail. There has been discussion in several countries about the cost and benefits of adopting alternative energy sources in order to reduce carbon emissions.[85] Organizations and companies such as the Competitive Enterprise Institute and ExxonMobil have emphasized more conservative climate change scenarios while highlighting the potential economic cost of stricter controls.[86][87][88][89] Likewise, various environmental lobbies and a number of public figures have launched campaigns to emphasize the potential risks of climate change and promote the implementation of stricter controls. Some fossil fuel companies have scaled back their efforts in recent years,[90] or called for policies to reduce global warming.[91]
| + | It is well understood that most media companies do not offer balanced reporting. Many politicians have bought into the liberal claim of consensus, for example Barack Obama's views, "Few challenges facing America and the world are more urgent than fighting climate change. The science is beyond dispute and the facts are clear." <ref>[https://web.archive.org/web/20090331121618/http://www.cato.org/special/climatechange/ "Climate change reality"] (March 2009). Cato Institute website. Retrieved on September 30, 2014.</ref> In fact, many scientists disagree with the "facts," their certainty, and their interpretation. Over 100 of them have signed the statement that appears in the Cato Institute's newspaper ad. Liberals have failed to back up their claims with any scientific facts. |
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| − | Another point of debate is the degree to which newly developed economies such as India and China should be expected to constrain their emissions. China's gross national CO2 emissions are expected to exceed those of the U.S. within the next few years, and may have already done so according to a 2006 report.[92] China has contended that it has less of an obligation to reduce emissions since its per capita emissions are roughly one-fifth that of the United States.[93] India, also exempt from Kyoto restrictions and another of the biggest sources of industrial emissions, has made similar assertions.[94] However, the U.S. contends that if they must bear the cost of reducing emissions, then China should do the same.[95]
| + | [[File:ad.jpg|center]] |
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| − | Related climatic issues
| + | According to 80 graphs published in 58 peer-reviewed scientific papers in the first five months of 2017 alone, catastrophic anthropogenic global warming does not exist.<ref>Delingpole, James (June 6, 2017). [https://www.breitbart.com/big-government/2017/06/06/delingpole-global-warming-is-myth-58-scientific-papers-2017/ DELINGPOLE: ‘Global Warming’ Is a Myth, Say 58 Scientific Papers in 2017]. ''Breitbart News''. Retrieved June 7, 2017.</ref> By October 2017, the number of peer-reviewed papers rejecting global warming had increased to 400.<ref>Delingpole, James (October 24, 2017). [https://www.breitbart.com/big-government/2017/10/24/delingpole-now-400-scientific-papers-in-2017-say-global-warming-is-a-myth/ Delingpole: Now 400 Scientific Papers in 2017 Say ‘Global Warming’ Is a Myth]. ''Breitbart News''. Retrieved October 24, 2017.</ref> |
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| − | Main articles: Ocean acidification, global dimming, and ozone depletion
| + | ===Past speculation=== |
| | | | |
| − | A variety of issues are often raised in relation to global warming. One is ocean acidification. Increased atmospheric CO2 increases the amount of CO2 dissolved in the oceans.[96] CO2 dissolved in the ocean reacts with water to form carbonic acid, resulting in acidification. Ocean surface pH is estimated to have decreased from 8.25 near the beginning of the industrial era to 8.14 by 2004,[97] and is projected to decrease by a further 0.14 to 0.5 units by 2100 as the ocean absorbs more CO2.[1][98] Since organisms and ecosystems are adapted to a narrow range of pH, this raises extinction concerns, directly driven by increased atmospheric CO2, that could disrupt food webs and impact human societies that depend on marine ecosystem services.[99]
| + | Speculation and warnings of catastrophic climate change are not unprecedented. In 2001 the ''Guardian'' noted that some 70s headlines shouted, "Brace yourself for another ice age". In 1971 the journal ''Science'' reported that the subsequent cooling effect resulting from a possible eightfold increased from atmospheric aerosol concentrations, "if sustained over a period of several years—is believed to be sufficient to trigger an ice age." <ref>George, Alison (June 28, 2001). [https://www.theguardian.com/science/2001/jun/28/physicalsciences.highereducation "Breaking the ice"]. The Guardian website. Retrieved on September 30, 2014. See [[Guardian (UK)]].</ref> |
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| − | Global dimming, the gradual reduction in the amount of global direct irradiance at the Earth's surface, may have partially mitigated global warming in the late twentieth century. From 1960 to 1990 human-caused aerosols likely precipitated this effect. Scientists have stated with 66–90% confidence that the effects of human-caused aerosols, along with volcanic activity, have offset some of the global warming, and that greenhouse gases would have resulted in more warming than observed if not for these dimming agents.[1]
| + | [[Richard Lindzen]] wrote in 1992 on the doubtfulness of man-caused warming on Earth. |
| | + | {{Cquote|Indeed, a recent Gallup poll of climate scientists in the American Meteorological Society and in the American Geophysical Union shows that a vast majority doubts that there has been any identifiable man-caused warming to date (49 percent asserted no, 33 percent did not know, 18 percent thought some has occurred; however, among those actively involved in research and publishing frequently in peer-reviewed research journals, none believes that any man-caused global warming has been identified so far).<ref name="cato"/>}} |
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| − | Ozone depletion, the steady decline in the total amount of ozone in Earth's stratosphere, is frequently cited in relation to global warming. Although there are areas of linkage, the relationship between the two is not strong.
| + | Oddly enough, even though 82% of US climate scientists refused to support the global warming theory then, [[liberal]] activists were already claiming a scientific consensus for [[anthropogenic global warming]]. (It's hard to understand how 18 percent credence in ''any'' global warming translates into "consensus" support for ''human-caused'' global warming.) |
| | | | |
| − | See also
| + | The campaign to convince the public (and their elected representatives) that the "science is settled" began in 1988 or 1989. |
| | | | |
| − | * Glossary of climate change
| + | By the 2008 elections both candidates for the Presidency of the United States were proposing plans to mitigate climate change. |
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| − | References
| + | Over 31,000 American scientists have signed the petition rejecting global warming.<ref>[http://www.petitionproject.org/ "Global warming petition project"] (2008). Global Warming Petition Project. Retrieved on September 30, 2014.</ref> |
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| + | [[Image:Teller_Card_100dpi.jpg|600px|center|thumb| Global Warming Petition]] |
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| − | 54. ^ Torn, Margaret; Harte, John (2006-05-26). "Missing feedbacks, asymmetric uncertainties, and the underestimation of future warming". Geophysical Research Letters 33 (10). L10703. Retrieved on 2007-03-04.
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| − | 57. ^ Stocker, Thomas F.; et al. (2001-01-20). 7.2.2 Cloud Processes and Feedbacks. Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change. Retrieved on 2007-03-04.
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| − | 63. ^ Thomas, Chris D.; et al. (2004-01-08). "Extinction risk from climate change" (PDF). Nature 427 (6970): 145-138. doi:10.1038/nature02121. Retrieved on 2007-03-18.
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| − | 64. ^ McLaughlin, John F.; et al. (2002-04-30). "Climate change hastens population extinctions" (PDF). PNAS 99 (9): 6070–6074. doi:10.1073/pnas.052131199. Retrieved on 2007-03-29.
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| − | 65. ^ Botkin, Daniel B.; et al. (March 2007). "Forecasting the Effects of Global Warming on Biodiversity". BioScience 57 (3): 227–236. doi:10.1641/B570306. Retrieved on 2007-11-30.
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| − | 66. ^ At-a-glance: The Stern Review. BBC (2006-10-30). Retrieved on 2007-04-29.
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| − | 67. ^ Tol and Yohe (2006) "A Review of the Stern Review" World Economics 7(4): 233-50. See also other critiques in World Economics 7(4).
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| − | 68. ^ Brad DeLong. Do unto others....
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| − | 69. ^ John Quiggin. Stern and the critics on discounting.
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| − | 70. ^ Dlugolecki, Andrew; et al. (2002). Climate Risk to Global Economy (PDF). CEO Briefing: UNEP FI Climate Change Working Group. United Nations Environment Programme. Retrieved on 2007-04-29.
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| − | 71. ^ Kurt M. Campbell, Jay Gulledge, J.R. McNeill, John Podesta, Peter Ogden, Leon Fuerth, R. James Woolsey, Alexander T.J. Lennon, Julianne Smith, Richard Weitz, Derek Mix (Oktober 2007). The Age of Consequences: The Foreign Policy and National Security Implications of Global Climate Change (PDF). Retrieved on 2007-11-06.
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| − | 72. ^ Climate Control: a proposal for controlling global greenhouse gas emissions (PDF). Sustento Institute. Retrieved on 2007-12-10.
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| − | 73. ^ Monbiot, George. Rigged - The climate talks are a stitch-up, as no one is talking about supply. (HTML). Retrieved on 2007-12-22.
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| − | 74. ^ Kyoto Protocol Status of Ratification (PDF). United Nations Framework Convention on Climate Change (2006-07-10). Retrieved on 2007-04-27.
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| − | 75. ^ Climate talks face international hurdles, by Arthur Max, Associated press, 5/14/07.
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| − | 76. ^ George W. Bush (March 13, 2001). Text of a Letter from the President to Senators Hagel, Helms, Craig, and Roberts. Office of the Press Secretary. Retrieved on 2007-11-21.
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| − | 77. ^ Regional Greenhouse Gas Initiative. Retrieved on 2006-11-07.
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| − | 78. ^ www.planetark.com/dailynewsstory.cfm/newsid/43027/story.htm. Retrieved on 2007-07-27.
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| − | 80. ^ Weart, Spencer (2006), "The Public and Climate Change", in Weart, Spencer, The Discovery of Global Warming, American Institute of Physics, <http://www.aip.org/history/climate/Public.htm>. Retrieved on 2007-04-14
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| − | 81. ^ Revkin, Andrew. "Poor Nations to Bear Brunt as World Warms", The New York Times, 2007-04-01. Retrieved on 2007-05-02.
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| − | 82. ^ Brahic, Catherine (2006-04-25). China's emissions may surpass the US in 2007. New Scientist. Retrieved on 2007-05-02.
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| − | 83. ^ Crampton, Thomas. "More in Europe worry about climate than in U.S., poll shows", International Herald Tribune, 2007-01-04. Retrieved on 2007-04-14.
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| − | 84. ^ Summary of Findings. Little Consensus on Global Warming. Partisanship Drives Opinion. Pew Research Center (2006-07-12). Retrieved on 2007-04-14.
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| − | 85. ^ "EU agrees on carbon dioxide cuts", BCC, 2007-03-09. Retrieved on 2007-05-04.
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| − | 86. ^ Begley, Sharon. "The Truth About Denial", Newsweek, 2007-08-13. Retrieved on 2007-08-13.
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| − | 87. ^ Adams, David (2006-09-20). Royal Society tells Exxon: stop funding climate change denial. The Guardian. Retrieved on 2007-08-09.
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| − | 88. ^ "Exxon cuts ties to global warming skeptics", MSNBC, 2007-01-12. Retrieved on 2007-05-02.
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| − | 89. ^ Sandell, Clayton. "Report: Big Money Confusing Public on Global Warming", ABC, 2007-01-03. Retrieved on 2007-04-27.
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| − | 90. ^ "Greenpeace: Exxon still funding climate skeptics", USA TODAY, 2007-05-18. Retrieved on 2007-07-09.
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| − | 91. ^ Ceres (April 28, 2004). "Global Warming Resolutions at U.S. Oil Companies Bring Policy Commitments from Leaders, and Record High Votes at Laggards". Press release. Retrieved on 2007-07-27.
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| − | 92. ^ "Group: China tops world in CO2 emissions", Associated Press, 2007-06-20. Retrieved on 2007-10-16. ; "Group: China surpassed US in carbon emissions in 2006: Dutch report", Reuters, 2007-06-20. Retrieved on 2007-10-16.
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| − | 93. ^ China: US should take lead on climate, by Michael Casey, Associated Press, 12/7/07.
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| − | 94. ^ India's glaciers give grim message on warming, by Somni Sengupta, 7/17/07, New York Times via oregonlive.com.
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| − | 95. ^ Chinese object to climate draft, BBC, 5/1/07; In Battle for U.S. Carbon Caps, Eyes and Efforts Focus on China,by Steven Mufson, Washington Post, 6/6/07.
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| − | 96. ^ The Ocean and the Carbon Cycle. NASA (2005-06-21). Retrieved on 2007-03-04.
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| − | 97. ^ Jacobson, Mark Z. (2005-04-02). "Studying ocean acidification with conservative, stable numerical schemes for nonequilibrium air-ocean exchange and ocean equilibrium chemistry" (PDF). Journal of Geophysical Research 110 (D7). doi:10.1029/2004JD005220. D07302. Retrieved on 2007-04-28.
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| | | | |
| − | Global warming is the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.
| + | In June, 1974, ''[[Time]]'' magazine published its front-page article, ''Science: Another Ice Age?'',<ref name="Time"/> while a report by the [[CIA]] in the same year stated that, "The western world's leading climatologists have confirmed recent reports of a detrimental global climatic change”, noting such things as that the "world's snow and ice cover had increased by at least 10 to 15 percent", and in the "Canadian area of [[Arctic]] Greenland, below normal temperatures were recorded for 19 consecutive months", which was unique during the last 100 years. A "major climatic shift" was speculated, which would threaten the "the stability of most nations.” It further warned that "Scientists are confident that unless man is able to effectively modify the climate, the northern regions, such as Canada" to "major areas in northern China, will again be covered with 100 to 200 feet of ice and snow", within the next 2500 years—or sooner.<ref>Central Intelligence Agency (August 1974). [http://www.climatemonitor.it/wp-content/uploads/2009/12/1974.pdf ''A Study of Climatological Research as it Pertains to Intelligence Problems''], pp. 1, 5, 7, 16. Retrieved from Climatemonitor [Italy] on September 30, 2014.</ref> |
| | | | |
| − | The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 year period ending in 2005, which is higher than the earlier estimate of 0.6 ± 0.2 °C for the period ending in 2000.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations"[1] via the greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3] These basic conclusions have been endorsed by at least 30 scientific societies and academies of science, including all of the national academies of science of the major industrialized countries. While individual scientists have voiced disagreement with the conclusions of the IPCC, the overwhelming majority of scientists working on climate change are in agreement with the conclusions.[4]
| + | Also in 1974, Nigel Calder, former editor of ''New Scientist'' and atmospheric researcher wrote in his book ''The Weather Machine'', "One might argue that there is a virtual certainty of the next ice age starting some time in the next 2000 years. Then the odds are only about 20-to-1 against it beginning in the next 100 years." |
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| − | Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[1] The range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a millennium even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]
| + | In 1975 the liberal magazine ''[[Newsweek]]'' reported that "Meteorologists disagree about the cause and extent of the cooling trend,...but they are almost unanimous in the view that the trend will reduce agricultural productivity for the rest of the century." These authorities were skeptical that political leaders would take any positive action to compensate for the [[climate change]], and they conceded that the more dramatic solutions, such as melting the arctic ice cap, might create worse problems than that which they were designed to solve.<ref>Gwynne, Peter (April 28, 1975). [http://denisdutton.com/newsweek_coolingworld.pdf "The cooling world"]. ''Newsweek''. Retrieved from DenisDutton.com on September 30, 2014. Caution: Copyrighted material; for fair educational use only.</ref> |
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| − | Increasing global temperature will cause sea level to rise, and is expected to increase the intensity of extreme weather events and to change the amount and pattern of precipitation. Other effects of global warming include changes in agricultural yields, trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.
| + | ===Natural variability of the climate system=== |
| | + | It is virtually universally accepted amongst secular climatologists that the earth has experienced numerous [[Ice Age|ice age]]s over two million years, during which global temperatures fluctuated created glacial and inter-glacial periods. The frigid temperatures allowed ice sheets to expand southward, covering much of [[Asia]], [[Europe]], and [[North America]]. The cooling associated with ice ages is gradual, while the terminations are relatively rapid. However, even the rapid terminations of ice ages take centuries to millennia. |
| | | | |
| − | Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. There is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences. Most national governments have signed and ratified the Kyoto Protocol, aimed at reducing greenhouse gas emissions.
| + | ===Natural climate change on other planets=== |
| − | Contents
| |
| − | [hide]
| |
| | | | |
| − | * 1 Terminology
| + | Since the [[Viking spacecraft]] reached [[Mars]] in the 1970s until recent readings were taken, the average temperature on Mars has risen {{temperature|0.6|1.1}} just as the average temperature on the earth has risen. Since human industrialization is clearly not to blame for the change on Mars, other causes are being considered. One possibility is that dust storms are changing the albedo of the planet, allowing it to warm, while another possibility is that solar variations from the sun are causing the warming.<ref>Multiple references: |
| − | * 2 Causes
| + | *Than, Ker (April 4, 2007). [http://www.space.com/scienceastronomy/070404_gw_mars.html "Dust storms fuel global warming on Mars"]. Space.com. Retrieved on September 30, 2014. |
| − | o 2.1 Greenhouse gases in the atmosphere
| + | *Taylor, James M. (November 1, 2005). [http://www.heartland.org/Article.cfm?artId=17977 "Mars is warming, NASA scientists report"]. Heartlander Magazine. Retrieved on September 30, 2014.</ref> |
| − | o 2.2 Feedbacks
| |
| − | o 2.3 Solar variation
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| − | * 3 Temperature changes
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| − | o 3.1 Recent
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| − | o 3.2 Pre-human climate variations
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| − | * 4 Climate models
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| − | * 5 Attributed and expected effects
| |
| − | o 5.1 Economic
| |
| − | o 5.2 Security
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| − | * 6 Adaptation and mitigation
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| − | * 7 Social and political debate
| |
| − | * 8 Related climatic issues
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| − | * 9 See also
| |
| − | * 10 References
| |
| − | * 11 Further reading
| |
| − | * 12 External links
| |
| | | | |
| − | Terminology
| + | Recently, it has also been found that similar to the Earth and Mars, [[Neptune]] is also undergoing global warming. Measurements taken at the Lowell observatory in [[Arizona]] have shown an increase in Neptune's brightness and temperature since 1980 following the same pattern seen on Earth and Mars. The researchers who discovered this warming suggest there may be a correlation between the warming and solar variations.<ref>Hammel, H. B. and Lockwood, G. W. (April 8, 2007). [http://www.agu.org/pubs/crossref/2007.../2006GL028764.shtml "Suggestive correlations between the brightness of Neptune, solar variability, and Earth's temperature"]. ''Geophysical Research Letters''. Retrieved from Wiley Online Library on September 30, 2014.</ref> |
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| − | The term "global warming" is a specific example of the broader term climate change, which can also refer to global cooling. In common usage, the term refers to recent warming and implies a human influence.[5] The United Nations Framework Convention on Climate Change (UNFCCC) uses the term "climate change" for human-caused change, and "climate variability" for other changes.[6] The term "anthropogenic global warming" is sometimes used when focusing on human-induced changes.
| + | [[Pluto]] has also been found to be undergoing global warming. The overall temperature increase on Pluto has been greater than that on the earth.<ref>Britt, Robert Roy (October 9, 2002). [http://www.space.com/scienceastronomy/pluto_warming_021009.html "Global warming on Pluto puzzles scientists"]. Space.com. Retrieved on September 30, 2014.</ref> |
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| − | Causes
| + | On the other hand, [[Uranus]] has had no net change in temperature since 1977. A rapid increase in temperature reversed itself. The reasons for this are not understood.<ref>Young, Leslie A., Bosh, Amanda S. et al. (October 2001). [http://www.boulder.swri.edu/~layoung/eprint/ur149/Young2001Uranus.pdf "Uranus after solstice: Results from the 1998 November 6 occultation"]. ''Icarus'', vol. 153, iss. 2, pp. 236-247. Retrieved from Southwest Research Institute [Boulder, CO] website on September 30, 2014.</ref> |
| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
| |
| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
| |
| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
| |
| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
| |
| | | | |
| − | Main articles: Attribution of recent climate change and scientific opinion on climate change
| + | Global temperatures change on other planets even when there is no life, something which strongly supports the idea that humans are not necessarily the cause of earth's global warming. Moreover, the temperature on Uranus has fluctuated back and forth. There is no reason that fluctuations cannot occur on earth, too. |
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| − | The Earth's climate changes in response to external forcing, including variations in its orbit around the sun (orbital forcing),[7][8][9] volcanic eruptions, and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[10][11] identifies elevated levels of greenhouse gases due to human activity as the main influence. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain the observed increase in mean global temperature. One such hypothesis proposes that warming may be the result of variations in solar activity.[12][13][14]
| + | Although measurements have been made of the temperatures of other planets these are by no means thorough or comparable with the measurements used for earth. The short space of time over which measurements have been taken and the very limited spatial coverage means that reliable average figures have not been obtained. They have certainly not been taken extensively enough to produce a five-year average temperature, which is the standard when determining temperature trends on earth. |
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| − | None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[15]
| + | However, if accurate measurements could be made, and their accuracy and reliability is improving over time, then they may prove useful to climate science. Their different atmospheres and distances from the sun provide natural laboratories to study climatic changes without human influences. Though of course they will not be directly comparable due to the vast differences. |
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| − | Greenhouse gases in the atmosphere
| + | ===Al Gore's claims=== |
| | + | [[File:Gore GlobalWarming.jpg|right|200px]] |
| | + | The decision by the government to distribute Al Gore's film, ''An Inconvenient Truth'', became the subject of a legal challenge by [[New Party]] member Stewart Dimmock. A school governor from Dover and father of two, Dimmock charged the Government with brainwashing children with propaganda by presenting Gore's sci-fi film as science. In October 2007, Mr Justice Burton of London's High Court found that while the film was "broadly accurate", it contained nine significant errors,“in which statements were made that were not supported by the current mainstream scientific consensus”, some of which had arisen in “the context of alarmism and exaggeration”. He also found the Guidance Notes drafted by the Education Secretary's advisers only worked to exacerbate the political propaganda in the film.<ref>Multiple references: |
| | + | *Sheppard, Marc (July 14, 2009). [https://www.americanthinker.com/blog/2009/07/clearly_its_al_gore_whos_in_de.html "Clearly it's Al Gore who's in denial"]. American Thinker. Retrieved on October 1, 2014. |
| | + | *Smith, Lewis (October 11, 2007). [https://www.thetimes.co.uk/tto/law/article2210175.ece "Al Gore’s inconvenient judgment"]. The Times website. Retrieved on October 1, 2014. Fee required to see article. |
| | + | *Smith, Lewis (October 11, 2007). [http://www.uio.no/studier/emner/matnat/ifi/MNSES9100/h11/undervisningsmateriale/literature/Al%20Gore%E2%80%99s%20inconvenient%20judgement%20times%202007.pdf "Al Gore’s inconvenient judgment"]. The Times website. Retrieved from University of Oslo/Faculty of Mathematics and Natural Science website on October 1, 2014. Caution: Copyrighted; for fair educational use only.</ref> |
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| − | Main article: Greenhouse effect
| + | Taken from the official transcript,<ref>Burton, Mr Justice Michael (October 10, 2007). [http://noteviljustwrong.com/images/nejw/docs/22161.pdf "Stuart Dimmock and Secretary of State for Education and Skills"]. United Kingdom of Great Britain's High Court of Justice/Queen's Bench Division/Administrative Court. Retrieved from Not Evil Just Wrong on October 1, 2014.</ref> the nine errors the judge found were: |
| | | | |
| − | The greenhouse effect was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. It is the process by which absorption and emission of infrared radiation by atmospheric gases warm a planet's atmosphere and surface.
| + | *1. Sea level rise of up to 20 feet (7 metres) will be caused by melting of either West Antarctica or Greenland in the near future. This is distinctly alarmist, and part of Mr Gore's 'wake-up call'. It is common ground that if indeed Greenland melted, it would release this amount of water, but only after, and over, millennia, so that the Armageddon scenario he predicts, insofar as it suggests that sea level rises of 7 metres might occur in the immediate future, is not in line with the scientific consensus. |
| | | | |
| − | Existence of the greenhouse effect as such is not disputed. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F), without which Earth would be uninhabitable.[16][17] Rather, the issue is how the strength of the greenhouse effect is changed when human activity increases the atmospheric concentrations of some greenhouse gases.
| + | *2. Low lying inhabited Pacific atolls are being inundated because of anthropogenic global warming. In scene 20, Mr Gore states "that's why the citizens of these Pacific nations have all had to evacuate to New Zealand". There is no evidence of any such evacuation having yet happened. |
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| − | On Earth, the major greenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect (not including clouds); carbon dioxide (CO2), which causes 9–26%; methane (CH4), which causes 4–9%; and ozone, which causes 3–7%.[18][19] Some other naturally occurring gases contribute very small fractions of the greenhouse effect; one of these, nitrous oxide (N2O), is increasing in concentration owing to human activity such as agriculture. The atmospheric concentrations of CO2 and CH4 have increased by 31% and 149% respectively above pre-industrial levels since 1750. Molecule for molecule, methane is a more effective greenhouse gas than carbon dioxide, but its concentration is much smaller so that its total radiative forcing is only about a fourth of that from carbon dioxide. These levels are considerably higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores. From less direct geological evidence it is believed that CO2 values this high were last attained 20 million years ago.[20] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, in particular deforestation.[21]
| + | *3. Shutting down of the "Ocean Conveyor". According to the IPCC, it is very unlikely that the Ocean Conveyor (known technically as the Meridional Overturning Circulation or thermohaline circulation) will shut down in the future, though it is considered likely that thermohaline circulation may slow down. |
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| − | The present atmospheric concentration of CO2 is about 383 parts per million (ppm) by volume.[22] Future CO2 levels are expected to rise due to ongoing burning of fossil fuels and land-use change. The rate of rise will depend on uncertain economic, sociological, technological, and natural developments, but may be ultimately limited by the availability of fossil fuels. The IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[23] Fossil fuel reserves are sufficient to reach this level and continue emissions past 2100, if coal, tar sands or methane clathrates are extensively used.[24]
| + | *4. Direct coincidence between rise in CO<sub>2</sub> in the atmosphere and in temperature, by reference to two graphs. In scenes 8 and 9, Mr Gore shows two graphs relating to a period of 650,000 years, one showing rise in CO<sub>2</sub> and one showing rise in temperature, and asserts (by ridiculing the opposite view) that they show an exact fit. Although there is general scientific agreement that there is a connection, the two graphs do not establish what Mr Gore asserts. |
| | | | |
| − | Feedbacks
| + | *5. The snows of Kilimanjaro. The film asserted that melting snows on Mount Kilimanjaro evidenced global warming. The Government's expert was had to admit that this is not correct. Mr Gore asserts in scene 7 that the disappearance of snow on Mt Kilimanjaro is expressly attributable to global warming. It is noteworthy that this is a point that specifically impressed Mr Milliband (see the press release quoted at paragraph 6 above). However, it is common ground that, the scientific consensus is that it cannot be established that the recession of snows on Mt Kilimanjaro is mainly attributable to human-induced climate change. |
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| − | Main article: Effects of global warming#Further global warming (positive feedback)
| + | *6. Lake Chad etc. The drying up of Lake Chad is used as a prime example of a catastrophic result of global warming. However, it is generally accepted that the evidence remains insufficient to establish such an attribution. It is apparently considered to be far more likely to result from other factors, such as population increase and over-grazing, and regional climate variability. |
| | | | |
| − | The effects of forcing agents on the climate are complicated by various feedback processes.
| + | *7. Hurricane Katrina. In scene 12 Hurricane Katrina and the consequent devastation in New Orleans is ascribed to global warming. It is common ground that there is insufficient evidence to show that. |
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| − | One of the most pronounced feedback effects relates to the evaporation of water. In the case of warming by the addition of long-lived greenhouse gases such as CO2, the initial warming will cause more water to be evaporated into the atmosphere. Since water vapor itself acts as a greenhouse gas, this causes still more warming; the warming causes more water vapor to be evaporated, and so forth until a new dynamic equilibrium concentration of water vapor is reached with a much larger greenhouse effect than that due to CO2 alone. Although this feedback process involves an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[25] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.
| + | *8. Death of polar bears. In scene 16, by reference to a dramatic graphic of a polar bear desperately swimming through the water looking for ice, Mr Gore says: "A new scientific study shows that for the first time they are finding polar bears that have actually drowned swimming long distances up to 60 miles to find the ice. They did not find that before." The only scientific study that either side before me can find is one which indicates that four polar bears have recently been found drowned because of a storm. |
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| − | Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models. Nevertheless, cloud feedback is second only to water vapor feedback and is positive in all the models that were used in the IPCC Fourth Assessment Report.[25]
| + | *9. Coral reefs. In scene 19, Mr Gore says: "Coral reefs all over the world because of global warming and other factors are bleaching and they end up like this. All the fish species that depend on the coral reef are also in jeopardy as a result. Overall specie loss is now occurring at a rate 1000 times greater than the natural background rate." The actual scientific view, as recorded in the IPCC report, is that, if the temperature were to rise by 1-3 degrees Centigrade, there would be increased coral bleaching and widespread coral mortality, unless corals could adapt or climatize, but that separating the impacts of climate change-related stresses from other stresses, such as over-fishing and polluting, is difficult. |
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| | + | Dimmock's lawyer, Mr. Downes, argued that by schools making available such film to its teachers, and if teachers then showed such film to their pupils, then this would inevitably result "in the promotion of partisan political views in the teaching of any subject in the school, which is thus not only not being forbidden by the local education authority (and the DES), but being positively facilitated by them." |
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| − | Another important feedback process is ice-albedo feedback.[26] When global temperatures increase, ice near the poles melts at an increasing rate. As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.
| + | Mr Justice Barton stressed that the “apocalyptic vision” presented in the film was politically partisan and not an impartial analysis of the science of climate change. “It is now common ground that it is not simply a science film—although it is clear that it is based substantially on scientific research and opinion—but that it is a political film. |
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| − | Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism contributing to warming.[27] A massive release of CH4 from methane clathrates could cause rapid warming, according to the clathrate gun hypothesis.
| + | Justice Barton also stated that, “I conclude that the claimant substantially won this case by virtue of my finding that, but for the new guidance note, the film would have been distributed in breach of sections 406 and 407 of the 1996 Education Act.”<ref>[http://news.bbc.co.uk/2/hi/7037671.stm "Gore climate film's nine 'errors'"] (October 11, 2007). BBC News website. Retrieved on October 1, 2014.</ref> |
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| − | The ocean's ability to sequester carbon is expected to decline as it warms, because the resulting low nutrient levels of the mesopelagic zone limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[28]
| + | In order for the film to be shown, the Government must first amend their Guidance Notes to Teachers to make clear that |
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| − | Solar variation
| + | *1. The Film is a political work and promotes only one side of the argument. |
| − | Solar variation over the last 30 years.
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| − | Solar variation over the last 30 years.
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| − | Main article: Solar variation
| + | *2. If teachers present the Film without making this plain they may be in breach of section 406 of the Education Act 1996 and guilty of political indoctrination. |
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| − | A few papers suggest that the Sun's contribution may have been underestimated. Two researchers at Duke University, Bruce West and Nicola Scafetta, have estimated that the Sun may have contributed about 45–50% of the increase in the average global surface temperature over the period 1900–2000, and about 25–35% between 1980 and 2000.[29] A paper by Peter Stott and other researchers suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.[30] They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases.
| + | *3. Nine inaccuracies have to be specifically drawn to the attention of school children.<ref>[http://www.newparty.co.uk/articles/inaccuracies-gore.html "Inaccuracies in Al Gore's 'An Inconvenient Truth'"] (October 2007). The New Party [U.K.]. Retrieved on October 1, 2014.</ref> |
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| − | A different hypothesis is that variations in solar output, possibly amplified by cloud seeding via galactic cosmic rays, may have contributed to recent warming.[31] It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.[32]
| + | Science and Public Policy took issue with the response to the ruling by Al Gore's spokesman and environment adviser, and asserted that his film contains ''35 Inconvenient Truths''.<ref>Monckton, Christopher (October 19, 2007). [https://web.archive.org/web/20140915002809/http://scienceandpublicpolicy.org/monckton/goreerrors.html "35 inconvenient truths: The errors in Al Gore's movie"]. The Science and Public Policy Institute website. Retrieved from September 15, 2014 archive at Internet Archive on October 1, 2014.</ref> |
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| − | One predicted effect of an increase in solar activity would be a warming of the stratosphere; however, the observed effect since at least 1960 has been a cooling of the lower stratosphere, which is one of the predicted results of greenhouse gas warming.[33] Reduction of stratospheric ozone also has a cooling influence, although substantial ozone depletion did not occur until the late 1970s. Solar variation combined with changes in volcanic activity probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.[1] In 2006, Peter Foukal and other researchers from the United States, Germany, and Switzerland found no net increase of solar brightness over the last thousand years. Solar cycles led to a small increase of 0.07% in brightness over the last 30 years. This effect is far too small to contribute significantly to global warming.[34][35] A paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in cosmic rays.[36] Henrik Svensmark and Eigil Friis-Christensen, the main proponents of cloud seeding by galactic cosmic rays, disputed the findings of Lockwood and Fröhlich.[37] Another recent study speculates that other bodies within the Solar System may influence the climate in a complex manner.[38]
| + | Regarding his claims that the snow cap atop Africa's Mt. Kilimanjaro is shrinking and that global warming is to blame, the November 23, 2003, issue of ''Nature'' magazine stated, |
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| − | Temperature changes
| + | :Although it's tempting to blame the ice loss on global warming, researchers think that deforestation of the mountain's foothills is the more likely culprit. Without the forests' humidity, previously moisture-laden winds blew dry. No longer replenished with water, the ice is evaporating in the strong equatorial sunshine." |
| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Main article: Temperature record
| + | Many conservatives see Al Gore as an example of [[liberals]] using [[deceit]]ful tactics in important debates, in order to make a position seem more solid than it is. |
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| − | Recent
| + | ===Scientists=== |
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| − | Global temperatures on both land and sea have increased by 0.75 °C (1.35 °F) relative to the period 1860–1900, according to the instrumental temperature record. This measured temperature increase is not significantly affected by the urban heat island effect.[39] Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[40] Temperatures in the lower troposphere have increased between 0.12 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with possibly regional fluctuations such as the Medieval Warm Period or the Little Ice Age.
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| − | Sea temperatures increase more slowly than those on land both because of the larger effective heat capacity of the oceans and because the ocean can lose heat by evaporation more readily than the land.[41] Since the Northern Hemisphere has more land mass than the Southern Hemisphere it warms faster; also there are extensive areas of seasonal snow cover subject to the snow-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the asymmetry of warming as the major gases are essentially well-mixed between hemispheres.
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| − | Based on estimates by NASA's Goddard Institute for Space Studies, 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[42] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit concluded that 2005 was the second warmest year, behind 1998.[43][44]
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| − | Anthropogenic emissions of other pollutants—notably sulfate aerosols—can exert a cooling effect by increasing the reflection of incoming sunlight. This partially accounts for the cooling seen in the temperature record in the middle of the twentieth century,[45] though the cooling may also be due in part to natural variability. James Hansen and colleagues have proposed that the effects of the products of fossil fuel combustion—CO2 and aerosols—have largely offset one another, so that warming in recent decades has been driven mainly by non-CO2 greenhouse gases.[46]
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| − | Paleoclimatologist William Ruddiman has argued that human influence on the global climate began around 8,000 years ago with the start of forest clearing to provide land for agriculture and 5,000 years ago with the start of Asian rice irrigation.[47] Ruddiman's interpretation of the historical record, with respect to the methane data, has been disputed.[48]
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| − | Pre-human climate variations
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Further information: Paleoclimatology
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| − | See also: Snowball Earth
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| − | | |
| − | Earth has experienced warming and cooling many times in the past. The recent Antarctic EPICA ice core spans 800,000 years, including eight glacial cycles timed by orbital variations with interglacial warm periods comparable to present temperatures.[49]
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| − | A rapid buildup of greenhouse gases caused warming in the early Jurassic period (about 180 million years ago), with average temperatures rising by 5 °C (9 °F). Research by the Open University indicates that the warming caused the rate of rock weathering to increase by 400%. As such weathering locks away carbon in calcite and dolomite, CO2 levels dropped back to normal over roughly the next 150,000 years.[50][51]
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| − | Sudden releases of methane from clathrate compounds (the clathrate gun hypothesis) have been hypothesized as a cause for other warming events in the distant past, including the Permian-Triassic extinction event (about 251 million years ago) and the Paleocene-Eocene Thermal Maximum (about 55 million years ago).
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| − | Climate models
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | | |
| − | Main article: Global climate model
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| − | | |
| − | Scientists have studied global warming with computer models of the climate. These models are based on physical principles of fluid dynamics, radiative transfer, and other processes, with simplifications being necessary because of limitations in computer power and the complexity of the underlying system (climate). These models predict that the effect of adding greenhouse gases is to produce a warmer climate.[52] However, even when the same assumptions of future greenhouse gas levels are used, there still remains a considerable range of climate sensitivity.
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| − | Including uncertainties in future greenhouse gas concentrations and climate modeling, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999.[1] Models have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes.
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| − | Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.[53] These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.
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| − | Most global climate models, when run to project future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.[54][55][56]
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| − | The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem.[57] There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability.
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| − | Attributed and expected effects
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| − | | |
| − | Main article: Effects of global warming
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| − | | |
| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Although it is difficult to connect specific weather events to global warming, an increase in global temperatures may in turn cause broader changes, including glacial retreat, Arctic shrinkage, and worldwide sea level rise. Changes in the amount and pattern of precipitation may result in flooding and drought. There may also be changes in the frequency and intensity of extreme weather events. Other effects may include changes in agricultural yields, addition of new trade routes,[58] reduced summer streamflows, species extinctions, and increases in the range of disease vectors.
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| − | Some effects on both the natural environment and human life are, at least in part, already being attributed to global warming. A 2001 report by the IPCC suggests that glacier retreat, ice shelf disruption such as that of the Larsen Ice Shelf, sea level rise, changes in rainfall patterns, and increased intensity and frequency of extreme weather events, are being attributed in part to global warming.[59] While changes are expected for overall patterns, intensity, and frequencies, it is difficult to attribute specific events to global warming. Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.[60]
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| − | Increasing deaths, displacements, and economic losses projected due to extreme weather attributed to global warming may be exacerbated by growing population densities in affected areas, although temperate regions are projected to experience some minor benefits, such as fewer deaths due to cold exposure.[61] A summary of probable effects and recent understanding can be found in the report made for the IPCC Third Assessment Report by Working Group II.[59] The newer IPCC Fourth Assessment Report summary reports that there is observational evidence for an increase in intense tropical cyclone activity in the North Atlantic Ocean since about 1970, in correlation with the increase in sea surface temperature, but that the detection of long-term trends is complicated by the quality of records prior to routine satellite observations. The summary also states that there is no clear trend in the annual worldwide number of tropical cyclones.[1]
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| − | Additional anticipated effects include sea level rise of 110 to 770 millimeters (0.36 to 2.5 ft) between 1990 and 2100,[62] repercussions to agriculture, possible slowing of the thermohaline circulation, reductions in the ozone layer, increased intensity of hurricanes and extreme weather events, lowering of ocean pH, and the spread of diseases such as malaria and dengue fever. One study predicts 18% to 35% of a sample of 1,103 animal and plant species would be extinct by 2050, based on future climate projections.[63] However, few mechanistic studies have documented extinctions due to recent climate change[64] and one study suggests that projected rates of extinction are uncertain.[65]
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| − | Economic
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | Main articles: Economics of global warming and Low-carbon economy
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| − | Some economists have tried to estimate the aggregate net economic costs of damages from climate change across the globe. Such estimates have so far failed to reach conclusive findings; in a survey of 100 estimates, the values ran from US$-10 per tonne of carbon (tC) (US$-3 per tonne of carbon dioxide) up to US$350/tC (US$95 per tonne of carbon dioxide), with a mean of US$43 per tonne of carbon (US$12 per tonne of carbon dioxide).[61] One widely publicized report on potential economic impact is the Stern Review; it suggests that extreme weather might reduce global gross domestic product by up to 1%, and that in a worst-case scenario global per capita consumption could fall 20%.[66] The report's methodology, advocacy and conclusions have been criticized by many economists, primarily around the Review's assumptions of discounting and its choices of scenarios,[67] while others have supported the general attempt to quantify economic risk, even if not the specific numbers.[68][69]
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| − | In a summary of economic cost associated with climate change, the United Nations Environment Programme emphasizes the risks to insurers, reinsurers, and banks of increasingly traumatic and costly weather events. Other economic sectors likely to face difficulties related to climate change include agriculture and transport. Developing countries, rather than the developed world, are at greatest economic risk.[70]
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| − | Security
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| − | In November 2007, the Center for Strategic and International Studies and the Center for a New American Security published a report highlighting the national security effects of climate change.[71] These security effects include increased competition for resources between countries, mass migration from the worst affected areas, challenges to the cohesion of major states threatened by the rise in sea levels, and, as a consequence of these factors, an increased risk of armed conflict, including even nuclear conflicts.
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| − | Adaptation and mitigation
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| − | | |
| − | Main articles: Adaptation to global warming, Mitigation of global warming, and Kyoto Protocol
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| − | The broad agreement among climate scientists that global temperatures will continue to increase has led some nations, states, corporations and individuals to implement actions to try to curtail global warming or adjust to it. Many environmental groups encourage action against global warming, often by the consumer, but also by community and regional organizations. Others have suggested a quota on worldwide fossil fuel production, citing a direct link between fossil fuel production and CO2 emissions.[72][73]
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| − | There has also been business action on climate change, including efforts at increased energy efficiency and limited moves towards use of alternative fuels. One important innovation has been the development of greenhouse gas emissions trading through which companies, in conjunction with government, agree to cap their emissions or to purchase credits from those below their allowances.
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| − | The world's primary international agreement on combating global warming is the Kyoto Protocol, an amendment to the United Nations Framework Convention on Climate Change (UNFCCC) negotiated in 1997. The Protocol now covers more than 160 countries globally and over 55% of global greenhouse gas emissions.[74] Only the United States and Kazakhstan have not ratified the treaty, with the United States historically being the world's largest emitter of greenhouse gas. This treaty expires in 2012, and international talks began in May 2007 on a future treaty to succeed the current one.[75]
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| − | Claiming "serious harm" to the United States economy and the exemption of "80 percent of the world, including major population centers" like China and India, from the treaty, George W. Bush contends that the Kyoto Protocol is an unfair and ineffective means of addressing global climate change concerns.[76] Still, various state, local, and regional governments within the United States have begun their own initiatives to indicate support and compliance with the Kyoto Protocol on a local basis. For example, the Regional Greenhouse Gas Initiative is a state-level emissions capping and trading program involving eight Northeastern U.S. states, which was founded on December 20, 2005.[77]
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| − | China and India, though exempt from its provisions as developing countries, have ratified the Kyoto Protocol. China may have passed the U.S. in total annual greenhouse gas emissions according to some recent studies. Chinese Premier Wen Jiabao has called on the nation to redouble its efforts to tackle pollution and global warming.[78]
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| − | The IPCC's Working Group III is responsible for crafting reports that deal with the mitigation of global warming and analyzing the costs and benefits of different approaches. In the 2007 IPCC Fourth Assessment Report, they conclude that no one technology or sector can be completely responsible for mitigating future warming. They find there are key practices and technologies in various sectors, such as energy supply, transportation, industry, and agriculture, that should be implemented to reduced global emissions. They estimate that stabilization of carbon dioxide equivalent between 445 and 710 ppm by 2030 will result in between a 0.6% increase and 3% decrease in global gross domestic product.[79]
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| − | Social and political debate
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| − | | |
| − | Main articles: Global warming controversy, Politics of global warming, and Economics of global warming
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| − | See also: Climate change denial
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Over the past several years, public perceptions and attitudes concerning the causes and importance of global warming have changed.[80] Increased awareness of the scientific findings surrounding global warming has resulted in political and economic debate. Poor regions, particularly Africa, appear at greatest risk from the suggested effects of global warming, while their actual emissions have been small compared to the developed world.[81] At the same time, developing country exemptions from provisions of the Kyoto Protocol have been criticized by the United States and Australia, and have been used as part of the rationale for continued non-ratification by the U.S.[82] In the Western world, the idea of human influence on climate has gained wider acceptance in Europe than in the United States.[83][84]
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| − | The issue of climate change has sparked debate weighing the benefits of limiting industrial emissions of greenhouse gases against the costs that such changes would entail. There has been discussion in several countries about the cost and benefits of adopting alternative energy sources in order to reduce carbon emissions.[85] Organizations and companies such as the Competitive Enterprise Institute and ExxonMobil have emphasized more conservative climate change scenarios while highlighting the potential economic cost of stricter controls.[86][87][88][89] Likewise, various environmental lobbies and a number of public figures have launched campaigns to emphasize the potential risks of climate change and promote the implementation of stricter controls. Some fossil fuel companies have scaled back their efforts in recent years,[90] or called for policies to reduce global warming.[91]
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| − | Another point of debate is the degree to which newly developed economies such as India and China should be expected to constrain their emissions. China's gross national CO2 emissions are expected to exceed those of the U.S. within the next few years, and may have already done so according to a 2006 report.[92] China has contended that it has less of an obligation to reduce emissions since its per capita emissions are roughly one-fifth that of the United States.[93] India, also exempt from Kyoto restrictions and another of the biggest sources of industrial emissions, has made similar assertions.[94] However, the U.S. contends that if they must bear the cost of reducing emissions, then China should do the same.[95]
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| − | Related climatic issues
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| − | Main articles: Ocean acidification, global dimming, and ozone depletion
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| − | | |
| − | A variety of issues are often raised in relation to global warming. One is ocean acidification. Increased atmospheric CO2 increases the amount of CO2 dissolved in the oceans.[96] CO2 dissolved in the ocean reacts with water to form carbonic acid, resulting in acidification. Ocean surface pH is estimated to have decreased from 8.25 near the beginning of the industrial era to 8.14 by 2004,[97] and is projected to decrease by a further 0.14 to 0.5 units by 2100 as the ocean absorbs more CO2.[1][98] Since organisms and ecosystems are adapted to a narrow range of pH, this raises extinction concerns, directly driven by increased atmospheric CO2, that could disrupt food webs and impact human societies that depend on marine ecosystem services.[99]
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| − | Global dimming, the gradual reduction in the amount of global direct irradiance at the Earth's surface, may have partially mitigated global warming in the late twentieth century. From 1960 to 1990 human-caused aerosols likely precipitated this effect. Scientists have stated with 66–90% confidence that the effects of human-caused aerosols, along with volcanic activity, have offset some of the global warming, and that greenhouse gases would have resulted in more warming than observed if not for these dimming agents.[1]
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| − | Ozone depletion, the steady decline in the total amount of ozone in Earth's stratosphere, is frequently cited in relation to global warming. Although there are areas of linkage, the relationship between the two is not strong.
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| − | See also
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| − | * Glossary of climate change
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| − | | |
| − | References
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| − | | |
| − | 1. ^ a b c d e f g h i Summary for Policymakers (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change (2007-02-05). Retrieved on 2007-02-02. “The updated 100-year linear trend (1906 to 2005) of 0.74°C [0.56°C to 0.92°C] is therefore larger than the corresponding trend for 1901 to 2000 given in the TAR of 0.6°C [0.4°C to 0.8°C].”
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| − | 2. ^ Hegerl, Gabriele C.; et al. (2007-05-07). Understanding and Attributing Climate Change (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 690. Intergovernmental Panel on Climate Change. Retrieved on 2007-05-20. “Recent estimates (Figure 9.9) indicate a relatively small combined effect of natural forcings on the global mean temperature evolution of the seconds half of the 20th century, with a small net cooling from the combined effects of solar and volcanic forcings”
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| − | 3. ^ Ammann, Caspar; et al. (2007-04-06). "Solar influence on climate during the past millennium: Results from ransient simulations with the NCAR Climate Simulation Model" (PDF). Proceedings of the National Academy of Sciences of the United States of America 104 (10): 3713–3718. “However, because of a lack of interactive ozone, the model cannot fully simulate features discussed in (44)." "While the NH temperatures of the high-scaled experiment are often colder than the lower bound from proxy data, the modeled decadal-scale NH surface temperature for the medium-scaled case falls within the uncertainty range of the available temperature reconstructions. The medium-scaled simulation also broadly reproduces the main features seen in the proxy records." "Without anthropogenic forcing, the 20th century warming is small. The simulations with only natural forcing components included yield an early 20th century peak warming of ≈0.2 °C (≈1950 AD), which is reduced to about half by the end of the century because of increased volcanism.”
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| − | 4. ^ A guide to facts and fictions about climate change. Royal Society (March 2005). Retrieved on 2007-11-18. “"However, the overwhelming majority of scientists who work on climate change agree on the main points"”
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| − | 5. ^ Climate Change: Basic Information. United States Environmental Protection Agency (2006-12-14). Retrieved on 2007-02-09. “In common usage, 'global warming' often refers to the warming that can occur as a result of increased emissions of greenhouse gases from human activities.”
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| − | 6. ^ United Nations Framework Convention on Climate Change, Article I. United Nations Framework Convention on Climate Change. Retrieved on 2007-01-15.
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| − | 7. ^ Berger, A.; et al. (2005-12-10). "On the origin of the 100-kyr cycles in the astronomical forcing". Paleoceanography 20 (4). PA4019. Retrieved on 2007-11-05.
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| − | 8. ^ Genthon, C.; et al. (1987-10-01). "Vostok Ice Core - Climatic response to CO2 and orbital forcing changes over the last climatic cycle". Nature 329 (6138): 414–418. Retrieved on 2007-11-05.
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| − | 9. ^ Alley, Richard B.; et al. (January 2002). "A northern lead in the orbital band: north-south phasing of Ice-Age events". Quaternary Science Reviews 21 (1-3): 431–441. Retrieved on 2007-11-05.
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| − | 10. ^ Joint science academies' statement: The science of climate change (ASP). Royal Society (2001-05-17). Retrieved on 2007-04-01. “The work of the Intergovernmental Panel on Climate Change (IPCC) represents the consensus of the international scientific community on climate change science”
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| − | 11. ^ (2007-10-18) "Rising to the climate challenge". Nature 449 (7164). Retrieved on 2007-11-06.
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| − | 12. ^ Svensmark, Henrik (February 2007). "Cosmoclimatology: a new theory emerges". Astronomy & Geophysics 48 (1): 18-24. doi:10.1111/j.1468-4004.2007.48118.x.
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| − | 13. ^ Forster, Piers; et al. (2007-02-05). Changes in Atmospheric Constituents and in Radiative Forcing (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 188-193. Intergovernmental Panel on Climate Change. Retrieved on 2007-09-17.
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| − | 14. ^ Bard, Edouard; Frank, Martin (2006-06-09). "Climate change and solar variability: What's new under the sun?". Earth and Planetary Science Letters 248 (1-2): 1-14. Retrieved on 2007-09-17.
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| − | 15. ^ Meehl, Gerald A.; et al. (2005-03-18). "How Much More Global Warming and Sea Level Rise" (PDF). Science 307 (5716): 1769–1772. doi:10.1126/science.1106663. Retrieved on 2007-02-11.
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| − | 16. ^ IPCC WG1 AR4 Report — Chapter 1: Historical Overview of Climate Change Science (PDF). IPCC WG1 AR4 Report p97 (pdf page 5 of 36). IPCC (2007). Retrieved on 2007-10-07. “To emit 240 W m–2, a surface would have to have a temperature of around –19 °C. This is much colder than the conditions that actually exist at the Earth’s surface (the global mean surface temperature is about 14 °C). Instead, the necessary –19 °C is found at an altitude about 5 km above the surface.”
| |
| − | 17. ^ Note that the Greenhouse Effect produces a temperature increase of about 33 °C (59 °F) with respect to black body predictions and not a surface temperature of 33 °C (91 °F) which is 32 °F higher. The average surface temperature is about 14 °C (57 °F). Also note that both the Celsius and Fahrenheit temperatures are expressed to 2 significant figures even though the conversion formula produces 3.
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| − | 18. ^ Kiehl, J. T.; Kevin E. Trenberth (February 1997). "Earth’s Annual Global Mean Energy Budget" (PDF). Bulletin of the American Meteorological Society 78 (2): 197-208. Retrieved on 2006-05-01.
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| − | 19. ^ Water vapour: feedback or forcing?. RealClimate (6 Apr 2005). Retrieved on 2006-05-01.
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| − | 22. ^ Tans, Pieter. Trends in Atmospheric Carbon Dioxide – Mauna Loa. National Oceanic and Atmospheric Administration. Retrieved on 2007-04-28.
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| − | 24. ^ 4.4.6. Resource Availability. IPCC Special Report on Emissions Scenarios. Intergovernmental Panel on Climate Change. Retrieved on 2007-04-28.
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| − | 25. ^ a b Soden, Brian J.; Held, Isacc M. (2005-11-01). "An Assessment of Climate Feedbacks in Coupled Ocean–Atmosphere Models" (PDF). Journal of Climate 19 (14). Retrieved on 2007-04-21. “Interestingly, the true feedback is consistently weaker than the constant relative humidity value, implying a small but robust reduction in relative humidity in all models on average" "clouds appear to provide a positive feedback in all models”
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| − | 26. ^ Stocker, Thomas F.; et al. (2001-01-20). 7.5.2 Sea Ice. Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change. Retrieved on 2007-02-11.
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| − | 67. ^ Tol and Yohe (2006) "A Review of the Stern Review" World Economics 7(4): 233-50. See also other critiques in World Economics 7(4).
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| − | 68. ^ Brad DeLong. Do unto others....
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| − | 88. ^ "Exxon cuts ties to global warming skeptics", MSNBC, 2007-01-12. Retrieved on 2007-05-02.
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| − | 93. ^ China: US should take lead on climate, by Michael Casey, Associated Press, 12/7/07.
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| − | 94. ^ India's glaciers give grim message on warming, by Somni Sengupta, 7/17/07, New York Times via oregonlive.com.
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| − | 95. ^ Chinese object to climate draft, BBC, 5/1/07; In Battle for U.S. Carbon Caps, Eyes and Efforts Focus on China,by Steven Mufson, Washington Post, 6/6/07.
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| − | | |
| − | "global warming," which has come to mean extreme [[greenhouse warming]] of the atmosphere leading to catastrophic environmental consequences. [http://www.junkscience.com/news/robinson.htm]</ref>
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| − | | |
| − | As an issue, it is a political battle over the science of climate change and is mainly used to justify support for the [[Kyoto Protocol]], which seeks to restrict [[carbon dioxide]] production on the grounds that it accelerates the "[[greenhouse effect]]".
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| − | | |
| − | Most non-scientific support for the global warming theory rests on popular accounts such as Al Gore's ''[[An Inconvenient Truth]]'' or on reports issued by the UN's [[IPCC]]. However, Keston Green of Monash University and Scott Armstrong of the Wharton School wrote that:
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| − | | |
| − | *Because the forecasting processes examined in Chapter 8 overlook scientific evidence on forecasting, the IPCC forecasts of climate change are not scientific. <ref>http://www.forecastingprinciples.com/Public_Policy/WarmAudit31.pdf</ref>
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| − | | |
| − | Politician [[Al Gore]] calls it a [[moral issue]], while scientist [[Richard Lindzen]] says, "It is probably the most immoral thing you could do to restrain energy so that the billions in the earth who don’t have access to electricity won't conveniently get it." <ref>http://www.americaabroadmedia.org/media/On%20line%20extra%20materials/Climate%20change%20-%20lindzen%20interview.doc</ref>
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| − | However, it is to be noted that many proponents of the theory propose energy conservation only until 'green' energy generation becomes predominant.{{Fact}}
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| − | | |
| − | In the general, the term ''global warming'' can be used for any upward trend in the [[global mean temperature]], but it is mostly used to refer to the 1° F warming since 1850.
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| − | | |
| − | The two sides are divided on whether this warming is a natural recovery from the [[Little Ice Age]] or a man-made environmental phenomenon. There are also debates regarding the potential positive or negative effects of a warming.
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| − | | |
| − | Republicans and Democrats in the U.S. are evenly split on the issue. ''Boston Globe'' writer [[Ellen Goodman]] wrote:
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| − | * 23 percent of college-educated Republicans believe [[anthropogenic global warming theory|the warming is due to humans]], while 75 percent of college-educated Democrats believe it. <ref> [http://www.boston.com/news/globe/editorial_opinion/oped/articles/2007/02/09/no_change_in_political_climate/] </ref>
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| − | | |
| − | As we learn more about climate, the "settled" conclusions of global warming [[alarmist]]s, appear more and more ridiculous.
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| − | "Clinging to alarmist scenarios for which there is no evidence, is simply exploitation of public gullibility." <ref>http://64.233.169.104/search?q=cache:A0llnpZ71lMJ:www.physics.harvard.edu/~motl/lindzen-nature-of-arguments.pdf+warming&hl=en&ct=clnk&cd=1&gl=us</ref>
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| − | | |
| − | | |
| − | ==The Modern Warm Period==
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| − | [[Image:Artic 1979.jpg|left|thumb|275px|A computer projection comparing the Polar Ice Mass in 1979 (left) and 2000 (right).]]
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| − | Average [[Earth]] surface air temperature has risen about 1° F since 1850.
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| − | <ref>Hansen's group at the Goddard Institute wrote, "Global warming is now 0.6 °C [1.0 °F] in the past three decades and 0.8 °C [1.4 °F] in the past century." http://data.giss.nasa.gov/gistemp/2005/</ref> How much of this is due to contamination of the temperature record from the [[urban heat island]] effect is hard to assess. Efforts are currently underway to detect and remove this bias. Spurious warming trends that might be considered as global warming can occur almost anywhere. <ref>http://climatesci.colorado.edu/2006/01/29/do-urban-areas-have-larger-long-term-temperature-trends-than-other-locations/feed/</ref>
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| − | Nonetheless, controversy has persisted over the influence of urban warming on reported large-scale surface-air temperature trends. <ref>http://climatesci.colorado.edu/2006/01/29/do-urban-areas-have-larger-long-term-temperature-trends-than-other-locations/feed/</ref>
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| − | | |
| − | According to temperature reconstruction made within an [[Old Earth]] paradigm, there have been many cycles of naturally-caused global warming and cooling over many millions of years (see [[climate cycles]]). Some scientists, including [[Richard Lindzen]] of [[MIT]], [[Sallie Baliunas]] of [[Harvard]] and [[Fred Singer]] (independent), say that the recent warming could be part of another natural cycle or random fluctuations in the atmosphere. However, many scientists also think that human activities were most likely the cause of the the planet's recent warming.
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| − | | |
| − | A [[United Nations]] panel ([[IPCC]]) asserts that most of the warming since around 1850 is human-caused. Global warming alarmists call this panel "authoritative". Others question its objectivity, and a handful of scientists have resigned from the panel in protest over unauthorized changes in scientific reports.
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| − | | |
| − | In February, 2007, the [[IPCC|Intergovernmental Panel on Climate Change]], whose members were appointed by their governments, released their fourth assessment report on climate change. That report concluded that most of recent global warming was "very likely" caused by human activity<ref>http://news.bbc.co.uk/2/hi/science/nature/6321351.stm</ref>. It says that increases in atmospheric concentrations of [[greenhouse gas]]es cause warming. Several members of this panel later complained their contributions were misrepresented in the final report.
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| − | | |
| − | ===IPCC controversy===
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| − | A reporter for the ''Chicago Tribune'' called the IPCC "the top body of climate change scientists in the world". <ref>http://www.chicagotribune.com/news/nationworld/chi-0704280477apr29,1,4275902.story?coll=chi-newsnationworld-hed</ref>
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| − | | |
| − | Fred Singer and other scientists dispute this view. <!-- I need to supply some quotes from Singer and Lindzen. The IPCC is not just scientists, in fact not even mostly climatologists. It supports a pre-ordained conclusion. It ignores contrary data. -->
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| − | <!-- Backing evidence for this claim? -->
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| − | | |
| − | ==False Claims of "Consensus"==
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| − | | |
| − | [[Richard Lindzen]] wrote in 1992,
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| − | | |
| − | :Indeed, a recent Gallup poll of climate scientists in the American Meteorological Society and in the American Geophysical Union shows that a vast majority doubts that there has been any idenGlobal warming is the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.
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| − | | |
| − | The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 year period ending in 2005, which is higher than the earlier estimate of 0.6 ± 0.2 °C for the period ending in 2000.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations"[1] via the greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3] These basic conclusions have been endorsed by at least 30 scientific societies and academies of science, including all of the national academies of science of the major industrialized countries. While individual scientists have voiced disagreement with the conclusions of the IPCC, the overwhelming majority of scientists working on climate change are in agreement with the conclusions.[4]
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| − | | |
| − | Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[1] The range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a millennium even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]
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| − | | |
| − | Increasing global temperature will cause sea level to rise, and is expected to increase the intensity of extreme weather events and to change the amount and pattern of precipitation. Other effects of global warming include changes in agricultural yields, trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.
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| − | | |
| − | Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. There is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences. Most national governments have signed and ratified the Kyoto Protocol, aimed at reducing greenhouse gas emissions.
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| − | Contents
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| − | [hide]
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| − | | |
| − | * 1 Terminology
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| − | * 2 Causes
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| − | o 2.1 Greenhouse gases in the atmosphere
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| − | o 2.2 Feedbacks
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| − | o 2.3 Solar variation
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| − | * 3 Temperature changes
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| − | o 3.1 Recent
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| − | o 3.2 Pre-human climate variations
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| − | * 4 Climate models
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| − | * 5 Attributed and expected effects
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| − | o 5.1 Economic
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| − | o 5.2 Security
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| − | * 6 Adaptation and mitigation
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| − | * 7 Social and political debate
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| − | * 8 Related climatic issues
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| − | * 9 See also
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| − | * 10 References
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| − | * 11 Further reading
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| − | * 12 External links
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| − | | |
| − | Terminology
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| − | The term "global warming" is a specific example of the broader term climate change, which can also refer to global cooling. In common usage, the term refers to recent warming and implies a human influence.[5] The United Nations Framework Convention on Climate Change (UNFCCC) uses the term "climate change" for human-caused change, and "climate variability" for other changes.[6] The term "anthropogenic global warming" is sometimes used when focusing on human-induced changes.
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| − | Causes
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Main articles: Attribution of recent climate change and scientific opinion on climate change
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| − | The Earth's climate changes in response to external forcing, including variations in its orbit around the sun (orbital forcing),[7][8][9] volcanic eruptions, and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[10][11] identifies elevated levels of greenhouse gases due to human activity as the main influence. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain the observed increase in mean global temperature. One such hypothesis proposes that warming may be the result of variations in solar activity.[12][13][14]
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| − | None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[15]
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| − | Greenhouse gases in the atmosphere
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| − | Main article: Greenhouse effect
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| − | The greenhouse effect was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. It is the process by which absorption and emission of infrared radiation by atmospheric gases warm a planet's atmosphere and surface.
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| − | Existence of the greenhouse effect as such is not disputed. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F), without which Earth would be uninhabitable.[16][17] Rather, the issue is how the strength of the greenhouse effect is changed when human activity increases the atmospheric concentrations of some greenhouse gases.
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| − | On Earth, the major greenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect (not including clouds); carbon dioxide (CO2), which causes 9–26%; methane (CH4), which causes 4–9%; and ozone, which causes 3–7%.[18][19] Some other naturally occurring gases contribute very small fractions of the greenhouse effect; one of these, nitrous oxide (N2O), is increasing in concentration owing to human activity such as agriculture. The atmospheric concentrations of CO2 and CH4 have increased by 31% and 149% respectively above pre-industrial levels since 1750. Molecule for molecule, methane is a more effective greenhouse gas than carbon dioxide, but its concentration is much smaller so that its total radiative forcing is only about a fourth of that from carbon dioxide. These levels are considerably higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores. From less direct geological evidence it is believed that CO2 values this high were last attained 20 million years ago.[20] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, in particular deforestation.[21]
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| − | The present atmospheric concentration of CO2 is about 383 parts per million (ppm) by volume.[22] Future CO2 levels are expected to rise due to ongoing burning of fossil fuels and land-use change. The rate of rise will depend on uncertain economic, sociological, technological, and natural developments, but may be ultimately limited by the availability of fossil fuels. The IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[23] Fossil fuel reserves are sufficient to reach this level and continue emissions past 2100, if coal, tar sands or methane clathrates are extensively used.[24]
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| − | Feedbacks
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| − | Main article: Effects of global warming#Further global warming (positive feedback)
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| − | The effects of forcing agents on the climate are complicated by various feedback processes.
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| − | One of the most pronounced feedback effects relates to the evaporation of water. In the case of warming by the addition of long-lived greenhouse gases such as CO2, the initial warming will cause more water to be evaporated into the atmosphere. Since water vapor itself acts as a greenhouse gas, this causes still more warming; the warming causes more water vapor to be evaporated, and so forth until a new dynamic equilibrium concentration of water vapor is reached with a much larger greenhouse effect than that due to CO2 alone. Although this feedback process involves an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[25] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.
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| − | Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models. Nevertheless, cloud feedback is second only to water vapor feedback and is positive in all the models that were used in the IPCC Fourth Assessment Report.[25]
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| − | Another important feedback process is ice-albedo feedback.[26] When global temperatures increase, ice near the poles melts at an increasing rate. As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.
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| − | Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism contributing to warming.[27] A massive release of CH4 from methane clathrates could cause rapid warming, according to the clathrate gun hypothesis.
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| − | The ocean's ability to sequester carbon is expected to decline as it warms, because the resulting low nutrient levels of the mesopelagic zone limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[28]
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| − | Solar variation
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| − | Solar variation over the last 30 years.
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| − | Solar variation over the last 30 years.
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| − | Main article: Solar variation
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| − | A few papers suggest that the Sun's contribution may have been underestimated. Two researchers at Duke University, Bruce West and Nicola Scafetta, have estimated that the Sun may have contributed about 45–50% of the increase in the average global surface temperature over the period 1900–2000, and about 25–35% between 1980 and 2000.[29] A paper by Peter Stott and other researchers suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.[30] They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases.
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| − | A different hypothesis is that variations in solar output, possibly amplified by cloud seeding via galactic cosmic rays, may have contributed to recent warming.[31] It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.[32]
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| − | One predicted effect of an increase in solar activity would be a warming of the stratosphere; however, the observed effect since at least 1960 has been a cooling of the lower stratosphere, which is one of the predicted results of greenhouse gas warming.[33] Reduction of stratospheric ozone also has a cooling influence, although substantial ozone depletion did not occur until the late 1970s. Solar variation combined with changes in volcanic activity probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.[1] In 2006, Peter Foukal and other researchers from the United States, Germany, and Switzerland found no net increase of solar brightness over the last thousand years. Solar cycles led to a small increase of 0.07% in brightness over the last 30 years. This effect is far too small to contribute significantly to global warming.[34][35] A paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in cosmic rays.[36] Henrik Svensmark and Eigil Friis-Christensen, the main proponents of cloud seeding by galactic cosmic rays, disputed the findings of Lockwood and Fröhlich.[37] Another recent study speculates that other bodies within the Solar System may influence the climate in a complex manner.[38]
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| − | Temperature changes
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Main article: Temperature record
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| − | Recent
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| − | Global temperatures on both land and sea have increased by 0.75 °C (1.35 °F) relative to the period 1860–1900, according to the instrumental temperature record. This measured temperature increase is not significantly affected by the urban heat island effect.[39] Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[40] Temperatures in the lower troposphere have increased between 0.12 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with possibly regional fluctuations such as the Medieval Warm Period or the Little Ice Age.
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| − | Sea temperatures increase more slowly than those on land both because of the larger effective heat capacity of the oceans and because the ocean can lose heat by evaporation more readily than the land.[41] Since the Northern Hemisphere has more land mass than the Southern Hemisphere it warms faster; also there are extensive areas of seasonal snow cover subject to the snow-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the asymmetry of warming as the major gases are essentially well-mixed between hemispheres.
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| − | Based on estimates by NASA's Goddard Institute for Space Studies, 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[42] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit concluded that 2005 was the second warmest year, behind 1998.[43][44]
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| − | Anthropogenic emissions of other pollutants—notably sulfate aerosols—can exert a cooling effect by increasing the reflection of incoming sunlight. This partially accounts for the cooling seen in the temperature record in the middle of the twentieth century,[45] though the cooling may also be due in part to natural variability. James Hansen and colleagues have proposed that the effects of the products of fossil fuel combustion—CO2 and aerosols—have largely offset one another, so that warming in recent decades has been driven mainly by non-CO2 greenhouse gases.[46]
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| − | Paleoclimatologist William Ruddiman has argued that human influence on the global climate began around 8,000 years ago with the start of forest clearing to provide land for agriculture and 5,000 years ago with the start of Asian rice irrigation.[47] Ruddiman's interpretation of the historical record, with respect to the methane data, has been disputed.[48]
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| − | Pre-human climate variations
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Further information: Paleoclimatology
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| − | See also: Snowball Earth
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| − | Earth has experienced warming and cooling many times in the past. The recent Antarctic EPICA ice core spans 800,000 years, including eight glacial cycles timed by orbital variations with interglacial warm periods comparable to present temperatures.[49]
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| − | A rapid buildup of greenhouse gases caused warming in the early Jurassic period (about 180 million years ago), with average temperatures rising by 5 °C (9 °F). Research by the Open University indicates that the warming caused the rate of rock weathering to increase by 400%. As such weathering locks away carbon in calcite and dolomite, CO2 levels dropped back to normal over roughly the next 150,000 years.[50][51]
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| − | Sudden releases of methane from clathrate compounds (the clathrate gun hypothesis) have been hypothesized as a cause for other warming events in the distant past, including the Permian-Triassic extinction event (about 251 million years ago) and the Paleocene-Eocene Thermal Maximum (about 55 million years ago).
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| − | Climate models
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | Main article: Global climate model
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| − | Scientists have studied global warming with computer models of the climate. These models are based on physical principles of fluid dynamics, radiative transfer, and other processes, with simplifications being necessary because of limitations in computer power and the complexity of the underlying system (climate). These models predict that the effect of adding greenhouse gases is to produce a warmer climate.[52] However, even when the same assumptions of future greenhouse gas levels are used, there still remains a considerable range of climate sensitivity. | |
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| − | Including uncertainties in future greenhouse gas concentrations and climate modeling, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999.[1] Models have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes.
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| − | Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.[53] These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.
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| − | Most global climate models, when run to project future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.[54][55][56]
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| − | The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem.[57] There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability.
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| − | Attributed and expected effects
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| − | Main article: Effects of global warming
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Although it is difficult to connect specific weather events to global warming, an increase in global temperatures may in turn cause broader changes, including glacial retreat, Arctic shrinkage, and worldwide sea level rise. Changes in the amount and pattern of precipitation may result in flooding and drought. There may also be changes in the frequency and intensity of extreme weather events. Other effects may include changes in agricultural yields, addition of new trade routes,[58] reduced summer streamflows, species extinctions, and increases in the range of disease vectors.
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| − | Some effects on both the natural environment and human life are, at least in part, already being attributed to global warming. A 2001 report by the IPCC suggests that glacier retreat, ice shelf disruption such as that of the Larsen Ice Shelf, sea level rise, changes in rainfall patterns, and increased intensity and frequency of extreme weather events, are being attributed in part to global warming.[59] While changes are expected for overall patterns, intensity, and frequencies, it is difficult to attribute specific events to global warming. Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.[60]
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| − | Increasing deaths, displacements, and economic losses projected due to extreme weather attributed to global warming may be exacerbated by growing population densities in affected areas, although temperate regions are projected to experience some minor benefits, such as fewer deaths due to cold exposure.[61] A summary of probable effects and recent understanding can be found in the report made for the IPCC Third Assessment Report by Working Group II.[59] The newer IPCC Fourth Assessment Report summary reports that there is observational evidence for an increase in intense tropical cyclone activity in the North Atlantic Ocean since about 1970, in correlation with the increase in sea surface temperature, but that the detection of long-term trends is complicated by the quality of records prior to routine satellite observations. The summary also states that there is no clear trend in the annual worldwide number of tropical cyclones.[1]
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| − | Additional anticipated effects include sea level rise of 110 to 770 millimeters (0.36 to 2.5 ft) between 1990 and 2100,[62] repercussions to agriculture, possible slowing of the thermohaline circulation, reductions in the ozone layer, increased intensity of hurricanes and extreme weather events, lowering of ocean pH, and the spread of diseases such as malaria and dengue fever. One study predicts 18% to 35% of a sample of 1,103 animal and plant species would be extinct by 2050, based on future climate projections.[63] However, few mechanistic studies have documented extinctions due to recent climate change[64] and one study suggests that projected rates of extinction are uncertain.[65]
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| − | Economic
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | Main articles: Economics of global warming and Low-carbon economy
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| − | Some economists have tried to estimate the aggregate net economic costs of damages from climate change across the globe. Such estimates have so far failed to reach conclusive findings; in a survey of 100 estimates, the values ran from US$-10 per tonne of carbon (tC) (US$-3 per tonne of carbon dioxide) up to US$350/tC (US$95 per tonne of carbon dioxide), with a mean of US$43 per tonne of carbon (US$12 per tonne of carbon dioxide).[61] One widely publicized report on potential economic impact is the Stern Review; it suggests that extreme weather might reduce global gross domestic product by up to 1%, and that in a worst-case scenario global per capita consumption could fall 20%.[66] The report's methodology, advocacy and conclusions have been criticized by many economists, primarily around the Review's assumptions of discounting and its choices of scenarios,[67] while others have supported the general attempt to quantify economic risk, even if not the specific numbers.[68][69]
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| − | In a summary of economic cost associated with climate change, the United Nations Environment Programme emphasizes the risks to insurers, reinsurers, and banks of increasingly traumatic and costly weather events. Other economic sectors likely to face difficulties related to climate change include agriculture and transport. Developing countries, rather than the developed world, are at greatest economic risk.[70]
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| − | Security
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| − | In November 2007, the Center for Strategic and International Studies and the Center for a New American Security published a report highlighting the national security effects of climate change.[71] These security effects include increased competition for resources between countries, mass migration from the worst affected areas, challenges to the cohesion of major states threatened by the rise in sea levels, and, as a consequence of these factors, an increased risk of armed conflict, including even nuclear conflicts.
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| − | Adaptation and mitigation
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| − | Main articles: Adaptation to global warming, Mitigation of global warming, and Kyoto Protocol
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| − | The broad agreement among climate scientists that global temperatures will continue to increase has led some nations, states, corporations and individuals to implement actions to try to curtail global warming or adjust to it. Many environmental groups encourage action against global warming, often by the consumer, but also by community and regional organizations. Others have suggested a quota on worldwide fossil fuel production, citing a direct link between fossil fuel production and CO2 emissions.[72][73]
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| − | There has also been business action on climate change, including efforts at increased energy efficiency and limited moves towards use of alternative fuels. One important innovation has been the development of greenhouse gas emissions trading through which companies, in conjunction with government, agree to cap their emissions or to purchase credits from those below their allowances.
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| − | The world's primary international agreement on combating global warming is the Kyoto Protocol, an amendment to the United Nations Framework Convention on Climate Change (UNFCCC) negotiated in 1997. The Protocol now covers more than 160 countries globally and over 55% of global greenhouse gas emissions.[74] Only the United States and Kazakhstan have not ratified the treaty, with the United States historically being the world's largest emitter of greenhouse gas. This treaty expires in 2012, and international talks began in May 2007 on a future treaty to succeed the current one.[75]
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| − | Claiming "serious harm" to the United States economy and the exemption of "80 percent of the world, including major population centers" like China and India, from the treaty, George W. Bush contends that the Kyoto Protocol is an unfair and ineffective means of addressing global climate change concerns.[76] Still, various state, local, and regional governments within the United States have begun their own initiatives to indicate support and compliance with the Kyoto Protocol on a local basis. For example, the Regional Greenhouse Gas Initiative is a state-level emissions capping and trading program involving eight Northeastern U.S. states, which was founded on December 20, 2005.[77]
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| − | China and India, though exempt from its provisions as developing countries, have ratified the Kyoto Protocol. China may have passed the U.S. in total annual greenhouse gas emissions according to some recent studies. Chinese Premier Wen Jiabao has called on the nation to redouble its efforts to tackle pollution and global warming.[78]
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| − | The IPCC's Working Group III is responsible for crafting reports that deal with the mitigation of global warming and analyzing the costs and benefits of different approaches. In the 2007 IPCC Fourth Assessment Report, they conclude that no one technology or sector can be completely responsible for mitigating future warming. They find there are key practices and technologies in various sectors, such as energy supply, transportation, industry, and agriculture, that should be implemented to reduced global emissions. They estimate that stabilization of carbon dioxide equivalent between 445 and 710 ppm by 2030 will result in between a 0.6% increase and 3% decrease in global gross domestic product.[79]
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| − | Social and political debate
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| − | Main articles: Global warming controversy, Politics of global warming, and Economics of global warming
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| − | See also: Climate change denial
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Over the past several years, public perceptions and attitudes concerning the causes and importance of global warming have changed.[80] Increased awareness of the scientific findings surrounding global warming has resulted in political and economic debate. Poor regions, particularly Africa, appear at greatest risk from the suggested effects of global warming, while their actual emissions have been small compared to the developed world.[81] At the same time, developing country exemptions from provisions of the Kyoto Protocol have been criticized by the United States and Australia, and have been used as part of the rationale for continued non-ratification by the U.S.[82] In the Western world, the idea of human influence on climate has gained wider acceptance in Europe than in the United States.[83][84]
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| − | The issue of climate change has sparked debate weighing the benefits of limiting industrial emissions of greenhouse gases against the costs that such changes would entail. There has been discussion in several countries about the cost and benefits of adopting alternative energy sources in order to reduce carbon emissions.[85] Organizations and companies such as the Competitive Enterprise Institute and ExxonMobil have emphasized more conservative climate change scenarios while highlighting the potential economic cost of stricter controls.[86][87][88][89] Likewise, various environmental lobbies and a number of public figures have launched campaigns to emphasize the potential risks of climate change and promote the implementation of stricter controls. Some fossil fuel companies have scaled back their efforts in recent years,[90] or called for policies to reduce global warming.[91]
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| − | Another point of debate is the degree to which newly developed economies such as India and China should be expected to constrain their emissions. China's gross national CO2 emissions are expected to exceed those of the U.S. within the next few years, and may have already done so according to a 2006 report.[92] China has contended that it has less of an obligation to reduce emissions since its per capita emissions are roughly one-fifth that of the United States.[93] India, also exempt from Kyoto restrictions and another of the biggest sources of industrial emissions, has made similar assertions.[94] However, the U.S. contends that if they must bear the cost of reducing emissions, then China should do the same.[95]
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| − | Related climatic issues
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| − | Main articles: Ocean acidification, global dimming, and ozone depletion
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| − | A variety of issues are often raised in relation to global warming. One is ocean acidification. Increased atmospheric CO2 increases the amount of CO2 dissolved in the oceans.[96] CO2 dissolved in the ocean reacts with water to form carbonic acid, resulting in acidification. Ocean surface pH is estimated to have decreased from 8.25 near the beginning of the industrial era to 8.14 by 2004,[97] and is projected to decrease by a further 0.14 to 0.5 units by 2100 as the ocean absorbs more CO2.[1][98] Since organisms and ecosystems are adapted to a narrow range of pH, this raises extinction concerns, directly driven by increased atmospheric CO2, that could disrupt food webs and impact human societies that depend on marine ecosystem services.[99]
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| − | Global dimming, the gradual reduction in the amount of global direct irradiance at the Earth's surface, may have partially mitigated global warming in the late twentieth century. From 1960 to 1990 human-caused aerosols likely precipitated this effect. Scientists have stated with 66–90% confidence that the effects of human-caused aerosols, along with volcanic activity, have offset some of the global warming, and that greenhouse gases would have resulted in more warming than observed if not for these dimming agents.[1]
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| − | Ozone depletion, the steady decline in the total amount of ozone in Earth's stratosphere, is frequently cited in relation to global warming. Although there are areas of linkage, the relationship between the two is not strong.
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| − | See also
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| − | * Glossary of climate change
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| − | References
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| − | 1. ^ a b c d e f g h i Summary for Policymakers (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change (2007-02-05). Retrieved on 2007-02-02. “The updated 100-year linear trend (1906 to 2005) of 0.74°C [0.56°C to 0.92°C] is therefore larger than the corresponding trend for 1901 to 2000 given in the TAR of 0.6°C [0.4°C to 0.8°C].”
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| − | 2. ^ Hegerl, Gabriele C.; et al. (2007-05-07). Understanding and Attributing Climate Change (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 690. Intergovernmental Panel on Climate Change. Retrieved on 2007-05-20. “Recent estimates (Figure 9.9) indicate a relatively small combined effect of natural forcings on the global mean temperature evolution of the seconds half of the 20th century, with a small net cooling from the combined effects of solar and volcanic forcings”
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| − | 3. ^ Ammann, Caspar; et al. (2007-04-06). "Solar influence on climate during the past millennium: Results from ransient simulations with the NCAR Climate Simulation Model" (PDF). Proceedings of the National Academy of Sciences of the United States of America 104 (10): 3713–3718. “However, because of a lack of interactive ozone, the model cannot fully simulate features discussed in (44)." "While the NH temperatures of the high-scaled experiment are often colder than the lower bound from proxy data, the modeled decadal-scale NH surface temperature for the medium-scaled case falls within the uncertainty range of the available temperature reconstructions. The medium-scaled simulation also broadly reproduces the main features seen in the proxy records." "Without anthropogenic forcing, the 20th century warming is small. The simulations with only natural forcing components included yield an early 20th century peak warming of ≈0.2 °C (≈1950 AD), which is reduced to about half by the end of the century because of increased volcanism.”
| |
| − | 4. ^ A guide to facts and fictions about climate change. Royal Society (March 2005). Retrieved on 2007-11-18. “"However, the overwhelming majority of scientists who work on climate change agree on the main points"”
| |
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| − | 17. ^ Note that the Greenhouse Effect produces a temperature increase of about 33 °C (59 °F) with respect to black body predictions and not a surface temperature of 33 °C (91 °F) which is 32 °F higher. The average surface temperature is about 14 °C (57 °F). Also note that both the Celsius and Fahrenheit temperatures are expressed to 2 significant figures even though the conversion formula produces 3.
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| − | | |
| − | tifiable man-caused warming to date (49 percent asserted no, 33 percent did not know, 18 percent thought some has occurred; however, among those actively involved in research and publishing frequently in peer-reviewed research journals, none believes that any man-caused global warming has been identified so far). <ref>http://www.cato.org/pubs/regulation/regv15n2/reg15n2g.html</ref>
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| − | | |
| − | Oddly enough, even though 82% of US climate scientists refused to support the global warming theory then, liberal activists were already claiming a scientific consensus for [[anthropogenic global warming]]. (It's hard to understand how 18 percent credence in ''any'' global warming translates into "consensus" support for ''human-caused'' global warming.)
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| − | | |
| − | The campaign to convince the public (and their elected representatives) that the "science is settled" began in 1988 or 1989, shortly after the communist nations lost the Cold War.
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| − | <!-- Irrelevant. Also lacking backing evidence. -->
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| − | | |
| − | ==The Hockey Stick Temperature Reconstruction== | |
| − | [[Image:Hockey stick chart ipcc.jpg|right|thumb|300px|The flawed Hockey Stick graph in a 2001 IPCC report shows blue proxy values along the "shaft" with red instrumental values superimposed as the "blade".]]
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| − | One of the main pieces of evidence for anthropogenic global warming presented during the 3rd IPCC report was a temperature reconstruction done by climatologist [[Michael Mann]]. The resulting graph of the Northern Hemisphere temperature is shaped like a hockey stick, and it is used as evidence for the unusualness of the earth's temperature in the past few decades.
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| − | | |
| − | While dramatic, the graph encountered serious questions from the beginning. It failed to reproduce two Northern Hemisphere climate episodes that were well documented in the literature, the Medieval Warm Period and The Little Ice Age (it should be noted that these were not global phenomenons, but were limited to Europe and Greenland; the Mann diagram concerned global average temperatures). Concerned about these discrepancies, [[Stephen McIntyre]] and [[Canada|Canadian]] economist Ross McKitrick attempted to reproduce the result and discovered a serious flaw in the statistical methods used to construct the hockey stick graph. Because of this, the 4th Assessment Report of the IPCC included several different temperature reconstruction methods instead of favoring just one hypothesis.
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| − | | |
| − | ==Natural Variability of the Climate System==
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| − | Evolutionary scientists who believe in global warming think that the Earth has experienced numerous [[Ice Age|ice age]]s over two million years, during which global temperatures dropped approximately 11° F and then returned to normal. The frigid temperatures allowed ice sheets to expand southward, covering much of [[Asia]], [[Europe]], and [[North America]]. The cooling associated with ice ages is gradual, while the terminations are relatively rapid. However, even the rapid terminations of ice ages take centuries to millennia.
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| − | | |
| − | ==Natural Climate Change on Other Planets==
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| − | | |
| − | Since the [[Viking spacecraft]] reached [[Mars]] in the 1970s until recent readings were taken, the average temperature on Mars has risen 1.1° F just as the average temperature on the earth has risen. Since human industrialization is clearly not to blame for the change on Mars, other causes are being considered. One possibility is that dust storms are changing the albedo of the planet, allowing it to warm, while another possibility is that solar variations from the sun are causing the warming.<ref>http://www.space.com/scienceastronomy/070404_gw_mars.html</ref><ref>http://www.heartland.org/Article.cfm?artId=17977</ref>
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| − | | |
| − | Recently, it has also been found that similar to the Earth and Mars, [[Neptune]] is also undergoing global warming. Measurements taken at the Lowell observatory in [[Arizona]] have shown an increase in Neptune's brightness and temperature since 1980 following the same pattern seen on Earth and Mars. The researchers who discovered this warming suggest there may be a correlation between the warming and solar variations.<ref>http://www.agu.org/pubs/crossref/2007.../2006GL028764.shtml</ref>
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| − | | |
| − | [[Pluto]] has also been found to be undergoing global warming. The overall temperature increase on Pluto has been greater than that on the earth.<ref>http://www.space.com/scienceastronomy/pluto_warming_021009.html</ref>
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| − | | |
| − | On the other hand, [[Uranus]] has been found to be undergoing rapid cooling, for reasons not entirely understood.<ref>http://www.boulder.swri.edu/~layoung/eprint/ur149/Young2001Uranus.pdf</ref>
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| − | | |
| − | ==Politics of Global Warming==
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| − | | |
| − | 'Global Warming Now World's Most Boring Topic’ <ref>http://newsbusters.org/node/14167</ref>
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| − | | |
| − | The need to fight "global warming" has become part of the dogma of the liberal conscience. <ref>http://www.cato.org/pubs/regulation/regv15n2/reg15n2g.html</ref>
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| − | | |
| − | Clearly, "global warming" is a tempting issue for many very important groups to exploit.
| |
| − | ... dealing with the threat of warming fits in with a great variety of preexisting agendas [like] dissatisfaction with industrial society (neopastoralism), ... governmental desires for enhanced revenues (carbon taxes), and bureaucratic desires for enhanced power. <ref>http://www.cato.org/pubs/regulation/regv15n2/reg15n2g.html</ref>
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| − | | |
| − | The global average surface temperature warmed about 0.9 °F over the second half of the 20th Century.
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| − | | |
| − | Assessments of climate science by the [[United Nations]] (see [[IPCC]] - ''Intergovernmental Panel on Climate Change'')
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| − | have claimed that scientists are 90% sure that over 50% of the observed global warming in recent decades is human-caused, and that continued global warming should be expected over at least the next century. ''Science'' published a literature search by Naomi Oreskes concluding that "scientific consensus" supports the IPCC reports. <ref>http://www.sciencemag.org/cgi/content/full/306/5702/1686]</ref>
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| − | | |
| − | Several prominent scientists have pointed out the [[politicized science]] of the UN's assessment methods. The scientific reports are submitted to a panel of representatives appointed by each country in the IPCC. Several scientists whose research demonstrates that climate change is taking place have complained about their work being misrepresented by the U.N.
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| − | | |
| − | *In addition, a number of the participants have testified to the pressures placed on them to emphasize results supportive of the current scenario and to suppress other results. That pressure has frequently been effective, and a survey of participants reveals substantial disagreement with the final report. <ref>http://www.cato.org/pubs/regulation/regv15n2/reg15n2g.html</ref>
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| − | | |
| − | | |
| − | Richard Lindzen wrote:
| |
| − | :Perhaps more important are the pressures being brought to bear on scientists to get the "right" results. Such pressures are inevitable, given how far out on a limb much of the scientific community has gone. The situation is compounded by the fact that some of the strongest proponents of "global warming" in Congress are also among the major supporters of science (Sen. Gore is notable among those). <ref>http://www.cato.org/pubs/regulation/regv15n2/reg15n2g.html</ref>
| |
| − | | |
| − | ==Al Gore's Assault on Science==
| |
| − | | |
| − | *Gore claims that Himalayan glaciers are shrinking and global warming is to blame. Yet the September 2006 issue of the American Meteorological Society's Journal of Climate reported, "Glaciers are growing in the Himalayan Mountains, confounding global warming alarmists who recently claimed the glaciers were shrinking and that global warming was to blame." <ref>http://www.suntimes.com/news/otherviews/450392,CST-EDT-REF30b.article</ref>
| |
| − | <!-- This is wrong. Read the paper and you will see that it never claimed anything which contradicted global warming theory; indeed, the anomalous growing of these particular glaciers was expected. -->
| |
| − | | |
| − | *Gore claims the snowcap atop Africa's Mt. Kilimanjaro is shrinking and that global warming is to blame. Yet according to the November 23, 2003, issue of Nature magazine, "Although it's tempting to blame the ice loss on global warming, researchers think that deforestation of the mountain's foothills is the more likely culprit. Without the forests' humidity, previously moisture-laden winds blew dry. No longer replenished with water, the ice is evaporating in the strong equatorial sunshine." <ref>http://www.suntimes.com/news/otherviews/450392,CST-EDT-REF30b.article</ref>
| |
| − | | |
| − | *Gore claims global warming is causing more tornadoes. Yet the United Nations Intergovernmental Panel on Climate Change stated in February that there has been no scientific link established between global warming and tornadoes. <ref>http://www.suntimes.com/news/otherviews/450392,CST-EDT-REF30b.article</ref>
| |
| − | | |
| − | == Scientists ==
| |
| | | | |
| | [[Image:Rogerrevelle.jpg|thumb|right|200px|Roger Revelle]] | | [[Image:Rogerrevelle.jpg|thumb|right|200px|Roger Revelle]] |
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| | |} | | |} |
| | | | |
| − | ==See Also== | + | ====Hal Lewis==== |
| − | *[[Anthropogenic global warming theory]]
| + | [[Liberal]] claims of global warming led to the resignation in October 2010 by Professor Hal Lewis from The American Physical Society because of "the global warming scam, with the (literally) trillions of dollars driving it, that has corrupted so many scientists, and has carried APS before it like a rogue wave. '''It is the greatest and most successful pseudoscientific fraud I have seen in my long life as a physicist'''."<ref>Lewis, Hal (October 8, 2010). [https://web.archive.org/web/20140212001321/http://www.thegwpf.org/hal-lewis-my-resignation-from-the-american-physical-society/ "Hal Lewis: My resignation from the American Physical Society"]. The Global Warming Policy Foundation website. Retrieved from February 12, 2014 archive at Internet Archive on October 1, 2014.</ref> |
| − | *[[Global Warming Controversy]] | + | |
| − | *[[Politics of global warming]] | + | ===Critique of the "Hockey Stick" reconstruction=== |
| − | *[[Liberal_Hysteria#Global_Warming_Derangement_Syndrome|Global Warming Derangement Syndrome]] | + | ::''See also : [[Climategate#Hockey Stick Graph|Climategate: hockey stick graph]]'' |
| | + | <small> |
| | + | *Shabecoff, Philip, [https://www.nytimes.com/1989/01/26/us/us-data-since-1895-fail-to-show-warming-trend.html U.S. Data Since 1895 Fail To Show Warming Trend]", ''New York Times'', January 26, 1989 |
| | + | *[http://blogs.nature.com/climatefeedback/2007/05/the_decay_of_the_hockey_stick.html The Decay of the Hockey Stick by Von Storch] published on the journal ''Nature'''s blog, May 3, 2007. |
| | + | *Stephen McIntyre and Ross McKitrick, "[http://climateaudit.files.wordpress.com/2005/09/mcintyre.mckitrick.2003.pdf Corrections To The Mann et. al. (1998) Proxy Data Base And Northern Hemispheric Average Temperature Series], ''Energy & Enviornment'' volume 14, 2003. |
| | + | *[http://www.technologyreview.com/Energy/13830/ A Global Warming Bombshell] by Richard A. Muller, ''Technology Review'' , Oct. 2004; calls into question famous graph by Michael Mann. |
| | + | *[http://www.sciencemag.org/cgi/content/abstract/306/5696/679 Reconstructing Past Climate from Noisy Data] by Hans von Storch, Eduardo Zorita, Julie M. Jones, Yegor Dimitriev, Fidel González-Rouco, Simon F. B. Tett, ''Science'' magazine, 22 October 2004. |
| | + | *[http://www.image.ucar.edu/~boli/manuscripts/2007-LNA-TeA.pdf The ‘hockey stick’ and the 1990s: a statistical perspective on reconstructing hemispheric temperatures] by Bo Li, Douglas W. Nychka and Casper M. Ammann, ''Institute for Mathmatics Applied to Geosciences''; (Manuscript received 22 March 2007; in final form 28 June 2007). |
| | + | *[http://www.21stcenturysciencetech.com/2006_articles/IceCoreSprg97.pdf Ice Core Data Show No Carbon Dioxide Increase] by Zbigniew Jaworowski, Ph.D., Spring 1997; this article examines one of the main pillars of the global warming thesis. |
| | + | *[http://climateaudit.files.wordpress.com/2005/09/mcintyre.ee.2005.pdf The M&M Critique of the MBH98 Northern Hemisphere Climate Index: Update and Implications] (''Energy & Environment'', vol. 16, no. 1, pp. 69–100, January 2005) - Stephen McIntyre, Ross McKitrick |
| | + | *[http://climateaudit.files.wordpress.com/2005/09/mcintyre.grl.2005.pdf Hockey sticks, principal components, and spurious significance] (''Geophysical Research Letters'', vol. 32, February 2005) - Stephen McIntyre, Ross McKitrick |
| | + | |
| | + | *Dalmia, Shikha (December 2, 2009). [https://www.forbes.com/2009/12/01/climategate-scandal-science-obama-opinions-columnists-shikha-dalmia.html "Cringing over Climategate"]. Forbes website. Retrieved on September 25, 2014. |
| | + | *Taylor, James (November 23, 2011). [https://www.forbes.com/sites/jamestaylor/2011/11/23/climategate-2-0-new-e-mails-rock-the-global-warming-debate/ "Climategate 2.0: New e-mails rock the global warming debate"]. Forbes website. Retrieved on September 25, 2014. |
| | + | *Bailey, Ronald (December 26, 2012). [http://reason.com/blog/2012/12/26/34-years-of-satellite-temperature-data-s "34 years of satellite temperature data show global warming is on a plateau"]. Hit & Run Blog/[[Reason.com]]. Retrieved on September 25, 2014. |
| | + | *Cole, Steve and McCarthy, Leslie (January 12, 2011). [https://www.nasa.gov/topics/earth/features/2010-warmest-year.html "NASA research finds 2010 tied for warmest year on record"]. NASA website. Retrieved on September 25, 2014. |
| | + | *Tisdale, Bob (August 10, 2012). [http://wattsupwiththat.com/2012/08/10/not-hot-ocean-sst-around-the-usa-not-anywhere-near-record-levels/ "Not so hot—ocean temperatures around the USA are not anywhere near record levels"]. Watts Up with That? Retrieved on September 25, 2014.</ref> |
| | + | </small> |
| | + | |
| | + | ==Effects of global warming== |
| | + | ===Beneficial effects of global warming=== |
| | + | [[File:Autumn foliage.jpg|thumb|Canoing on a Colorful Day, (NY).]] |
| | + | Some researchers point out that benefits of health global warming have been overlooked, or minimized. As far back as 1996, Thomas Gale Moore, Senior Fellow at Hoover Institution (Stanford University) contended that positive health and amenity effects would be a result of projected increases in temperature.<ref>Moore, Thomas Gale (May 30, 1996). [http://www.stanford.edu/~moore/health.html "Health and amenity effects of global warming"]. Stanford University/Thomas Gale Moore webpage. Retrieved on October 1, 2014.</ref> |
| | + | |
| | + | Another source notes,<ref>[https://web.archive.org/web/20081223011000/http://www.bionomicfuel.com/what-are-the-benefits-of-global-warming/ "What are the benefits of global warming?"] (November 3, 2008). Bionomicfuel.com. Retrieved from December 21, 2008 archive at Internet Archive on October 1, 2014.</ref> |
| | + | |
| | + | <blockquote>In areas that see extreme cold temperatures, deaths related to colder weather would drop significantly, leading to decreased health care costs, while areas that already have hot climates will see no increase. Warmer temperatures would also mean less energy use to heat homes and buildings, helping to conserve energy as cooling is much more energy efficient. With the changes brought about by global warming more land that is not lost to desert and/or rising sea levels would become available for uses like farming and living. Forests and plants would grow stronger, healthier, and more abundant because of the warmer weather, and this would mean more oxygen being released into the atmosphere.</blockquote> |
| | + | |
| | + | ===Reported effects of global warming=== |
| | + | |
| | + | Reported past or expected/possible future environmental and societal consequences of man-made global warming include global cooling,<ref>72Jag (August 25, 2014). [https://web.archive.org/web/20090827143311/http://www.nowpublic.com/environment/global-warming-causing-global-cooling "Is global warming causing global cooling?"] NowPublic. Retrieved on October 1, 2014.</ref> decreased food production,<ref>Fred Pearce (April 26, 2005). [http://www.newscientist.com/article/dn7310-climate-change-warning-over-food-production.html "Climate change warning over food production"] Newscientist website. Retrieved on October 1, 2014.</ref> increased food production,<ref>Booth, William (May 17, 1990). [http://www.highbeam.com/doc/1P2-1127111.html "Global heating could benefit U.S. farmers; prices seen rising as production falls"]. ''The Washington Post''. Retrieved from HighBeam Research website on October 1, 2014.</ref> shrinking forest.,<ref>Adam, David (March 11, 2009). [http://www.guardian.co.uk/environment/2009/mar/11/amazon-global-warming-trees/print "Amazon could shrink by 85% due to climate change"]. Theguardian [U. K.]. Retrieved on October 1, 2014. See [[The Guardian]].</ref> increased tree foliage,<ref>[http://www.greenfingers.com/articledisplay.asp?id=1734 "Global warming causes greening"] (2008). Greenfingers.com. Retrieved on October 1, 2014.</ref> increased productivity of high-elevation forests,<ref>Oregon State University (Oct. 20, 2009). [https://www.sciencedaily.com/releases/2009/10/091019163020.htm "Global warming may spur increased growth in Pacific northwest forests"]. ScienceDaily. Retrieved on October 1, 2014.</ref> melting glaciers.,<ref>Asian News International (June 6, 2007). [http://www.andhranews.net/Intl/2007/June/6/Global-warming-causing-3633.asp "Global warming causing hundreds of Antarctic Peninsula glaciers to melt"]. AndhraNews.net. Retrieved on October 1, 2014.</ref> growing glaciers,<ref>[http://www.cbc.ca/news/technology/global-warming-causing-california-glacier-to-grow-scientists-say-1.749761?ref=rss "Global warming causing California glacier to grow, scientists say"] (July 9, 2008). CBCnews. Retrieved on October 1, 2014. Located by Sub-Driver of [http://www.freerepublic.com/focus/news/2043047/posts?page=51 Free Republic].</ref> increasing landmass in Antarctica,<ref>[http://www.worldclimatereport.com/index.php/2005/05/27/antarctic-ice-a-global-warming-snow-job/ "Antarctic ice: A global warming snow job?"] (May 27, 2005). World Climate Report. Retrieved on October 2, 2014.</ref> colder winters,<ref>[http://www.cbc.ca/news/technology/climate-change-could-bring-colder-winters-1.363574 "Climate change could bring colder winters"] (March 13, 2003). CBCNews. Retrieved on October 2, 2014.</ref> a new ice age,<ref>McGuire, Bill (November 13, 2003). [http://www.guardian.co.uk/environment/2003/nov/13/comment.research "Will global warming trigger a new ice age?"] The Guardian website. Retrieved on October 2, 2014.</ref> prevention of an ice age,<ref>Thompson, Andrea (September 10, 2007). [https://www.foxnews.com/printer_friendly_story/0,3566,296060,00.html "Global warming may cancel next ice age"]. Fox News website. Retrieved on October 2, 2014.</ref> taller mountains.,<ref>Than, Ker (August 4, 2006). [http://www.livescience.com/938-taller-mountains-blamed-global-warming.html "Taller mountains blamed on global warming, too"]. LiveScience. Retrieved on October 2, 2014.</ref> a lop-sided planet,<ref>Britt, Robert Roy (June 29, 2005). [http://www.livescience.com/3884-global-warming-create-lopsided-planet.html "Global warming might create lopsided planet"]. LiveScience. Retrieved on October 2, 2014.</ref> stronger hurricanes,<ref>Florida State University (Sep. 4, 2008). [https://www.sciencedaily.com/releases/2008/09/080903134323.htm "Global warming: Warmer seas linked to strengthening hurricanes, according to new research"]. ScienceDaily. Retrieved on October 2, 2014.</ref> weaker hurricanes,<ref>Schmid, Randolph E., AP Science Writer (April 17, 2007). [http://usatoday30.usatoday.com/weather/research/2007-04-17-globalwarming-hurricanes_N.htm "Study: Global warming may diminish Atlantic hurricane activity"]. USA Today. Retrieved on October 2, 2014.</ref> shorter days,<ref>Atkins, William (April 11, 2007). [http://www.itwire.com/science-news/climate/11220-researchers-say-global-warming-should-cause-shorter-days "Researchers say global warming should cause shorter days"]. iTWire. Retrieved on October 2, 2014.</ref> earthquakes and volcanoes, and other geological disasters. Attempts to prevent climate change may do the same,<ref>Fisher, Richard. (September 23, 2009). [http://www.newscientist.com/article/mg20327273.800-climate-change-may-trigger-earthquakes-and-volcanoes.html "Climate change may trigger earthquakes and volcanoes" [preview]]. Newscientist website. Preview retrieved on October 2, 2014. Subscription required for full article.</ref> shrinking brains,<ref>[http://www.albany.edu/campusnews/releases_286.htm "Study: Global warming could be reversing a trend that led to bigger human brains"] (March 15, 2007). State University of New York at Albany. Retrieved on October 2, 2014.</ref> shrinking sheep,<ref>Connor, Steve (July 3, 2009). [http://www.independent.co.uk/news/science/how-global-warming-shrank-st-kildas-sheep-1729609.html "How global warming shrank St Kilda's sheep"]. The Independent [U. K.] website. Retrieved on October 2, 2014.</ref> tiger attacks.,<ref>Dhar, Sujoy (October 20, 2008). [http://southasia.oneworld.net/news/tiger-attacks-linked-to-global-warming "Tiger attacks linked to global warming"]. Reuters. Retrieved from OneWorld South Asia on October 2, 2014.</ref> shark attacks,<ref>Johnston, Bruce (August 31, 1998). [http://junksciencearchive.com/news3/shark.html "Shark attack on boat 'result of global warming'"]. Electronic Telegraph (U.K.) Retrieved from JunkScienceArchive on October 3, 2014.</ref> walrus stampede deaths,<ref>Associated Press (December 17, 2007). [https://web.archive.org/web/20141003042107/http://6abc.com/archive/5839622/ "Global warming is blamed for walrus stampede deaths"]. 6abc Action News website. Retrieved from October 3, 2014 archive at Internet Archive on October 3, 2014. Located by digger48 of [http://www.freerepublic.com/focus/f-news/1939754/posts Free Republic]</ref> imminent cannibalism,<ref>Baker, Brent (April 2, 2008). [http://newsbusters.org/blogs/brent-baker/2008/04/02/turner-iraqi-insurgents-patriots-inaction-warming-cannibalism "Turner: Global warming will cause mass cannibalism, insurgents are patriots"]. MRC NewsBusters. Retrieved on October 2, 2014.</ref> the need for a drastic reduction of the earth's population,<ref>[http://thisistheendoftheworldasweknowit.com/archives/one-less-child-environmental-extremists-warn-that-overpopulation-is-causing-climate-change-and-will-ultimately-destroy-the-earth "One less child? Environmental extremists warn that overpopulation is causing climate change and will ultimately destroy the Earth"] (November 17, 2009). The End of the World. Retrieved on October 2, 2014.</ref> a strong increase in people dying of [[AIDS]],<ref>McLean, Tamara (April 29, 2008). [https://web.archive.org/web/20110831093248/http://news.theage.com.au/national/global-warming-set-to-fan-the-hiv-fire-20080430-29eh.html "Global warming hoax set to fan the HIV fire"]. Theage.com.au. Retrieved from August 31, 2011 archive at Internet Archive on October 1, 2014. Located by |
| | + | [https://web.archive.org/web/20110725075338/http://www.skepticsglobalwarming.com/?p=608 Skeptics Global Warning].</ref> increased risk of civil war in Africa,<ref>[http://news.stanford.edu/news/2009/november23/climate-civil-wars-112309.html "Global warming increases risk of civil war in Africa"] (November 23, 2009). Stanford Report. Retrieved from Stanford News on October 1, 2014.</ref> child ''climate cops'',<ref>[https://www.wnd.com/index.php?fa=PAGE.view&pageId=70811 "Beware your children: They might be 'climate cops'"] (July 28, 2008). WND. Retrieved on October 1, 2014.</ref> increase in depression,<ref>Sohn, Emily (December 10, 2009). [http://www.google.com/search?q=%22Deadly+heat+waves%2C+home-wrecking+hurricanes%22&hl=en&gbv=2&oq=&gs_l= “Mental health to decline with climate change”]. Discovery.com News. Retrieved from Google Search on October 1, 2014.</ref> increase in psychiatric illness<ref>Press Trust of India (April 8, 2008). [http://www.sify.com/news/climate-change-leads-to-psychiatric-illness-news-national-jegnGhfjihasi.html "'Climate change leads to psychiatric illness'"]. Sify News. Retrieved on October 1, 2014.</ref> and increased anxiety and loss of sleep among many children.<ref>Jones, Alan (February 22, 2007). [http://www.scotsman.com/news/uk/children-losing-sleep-over-global-warming-1-683217 "Children losing sleep over global warming"]. The Scotsman website. Retrieved on September 30, 2014.</ref> |
| | + | |
| | + | ==References== |
| | + | {{Reflist|colwidth=35em}} |
| | + | |
| | + | == See also == |
| | + | *''[[Massachusetts v. EPA]]'' |
| | + | *[[Liberal hysteria#Global Warming Derangement Syndrome|Global Warming Derangement Syndrome]] |
| | *[[Socialist Environmental Disasters]] | | *[[Socialist Environmental Disasters]] |
| − | *[[An Inconvenient Truth]] | + | *[[Counterexamples to Global Warming]] |
| − | *[[Previous Breaking News/Global Warming|Articles about '''Global Warming''' from previous "Breaking News"]] | + | *[[Winter of 2010]] |
| − | *[[More News/Global Warming|Articles about '''Global Warming''' from "More News"]] | + | *[[Reducing carbon dioxide emissions]] |
| | + | *[[Essay:Global Warming]] |
| | + | *[[Essay:Parallels between evolution and global warming]] |
| | + | *[[Exaggeration of global warming]] |
| | + | *[[Global warming and polar bears]] |
| | + | *[[Global climate disruption]] |
| | + | *[[Global warming research]] |
| | + | *[[Global annual average temperature]] |
| | + | *[[Warm period]] |
| | + | *[[Liberal lies]] |
| | + | *[[War on Science]] |
| | + | *[[Lysenkoism]] |
| | + | *[[Failed climate change predictions]] |
| | | | |
| − | ==External Links== | + | ==External links== |
| − | <small>
| + | *[http://www.creationworldview.org/articles_view.asp?id=67 Global Warming? Absolutely No Truth To It!] |
| | + | *[http://www.aim.org/wls/category/global-warming/ What Liberals Say - Category: Global Warming], [[Accuracy In Media]] |
| | *[http://global-warming.accuweather.com/2007/12/attempting_to_stop_global_warm_1.html Attempting to Stop Global Warming is Futile and a Mistake, says letter to the UN] | | *[http://global-warming.accuweather.com/2007/12/attempting_to_stop_global_warm_1.html Attempting to Stop Global Warming is Futile and a Mistake, says letter to the UN] |
| − | *[http://www.nationalpost.com/news/story.html?id=164004 Signatories of an open letter on the UN climate-conference] | + | *[https://www.icr.org/creation-meteorology Clinate Change] by The Institute for Creation Research |
| − | *[http://schwinger.harvard.edu/~motl/global-temperature-not-exist.pdf Does a global temperature exist?], ''Journal of Non-Equilibrium Thermodynamics'', June 2007.
| |
| | *[http://environment.guardian.co.uk/climatechange/story/0,,2032821,00.html The appliance of science] by Mike Hulme. | | *[http://environment.guardian.co.uk/climatechange/story/0,,2032821,00.html The appliance of science] by Mike Hulme. |
| − | *[http://www.climatecrisis.net/ ''An Inconvenient Truth''], Film by [[Al Gore]]
| |
| − | *[http://video.google.com/videoplay?docid=2332531355859226455&q=great+global+warming+swindle ''The Great Global Warming Swindle'' - Documentary Film]
| |
| − | *[http://www.physics.harvard.edu/%7Emotl/iris-effect.pdf Climate Sensitivity and Observed Negative Feedbacks], lecture by Richard Lindzen and Roberto Rondanelli.
| |
| − | *[http://www.physics.harvard.edu/%7Emotl/lindzen-nature-of-arguments.pdf Nature of Arguments for Anthropogenic Global Warming], by Richard Lindzen
| |
| − | *[http://www.independent.org/store/book_detail.asp?bookID=42 ''Hot Talk, Cold Science: Global Warmings's Unfinished Debate'', by S. Fred Singer]
| |
| | *[http://www.cato.org/pubs/regulation/regv15n2/reg15n2g.html Global Warming: The Origin and Nature of the Alleged Scientific Consensus] - [[Richard S. Lindzen]], Alfred P. Sloan Professor of Meteorology at the [[Massachusetts Institute of Technology]] | | *[http://www.cato.org/pubs/regulation/regv15n2/reg15n2g.html Global Warming: The Origin and Nature of the Alleged Scientific Consensus] - [[Richard S. Lindzen]], Alfred P. Sloan Professor of Meteorology at the [[Massachusetts Institute of Technology]] |
| | *[http://www.independent.org/publications/tir/article.asp?issueID=47&articleID=604 "Should We Have Acted Thirty Years Ago to Prevent Climate Change?", by Randall G. Holcombe]. | | *[http://www.independent.org/publications/tir/article.asp?issueID=47&articleID=604 "Should We Have Acted Thirty Years Ago to Prevent Climate Change?", by Randall G. Holcombe]. |
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| | *[http://www.heartland.org/Article.cfm?artId=17181 Survey Shows Climatologists Are Split on Global Warming] | | *[http://www.heartland.org/Article.cfm?artId=17181 Survey Shows Climatologists Are Split on Global Warming] |
| | *[http://www.magma.ca/~hurleyp/FightingTheHoax.htm Fighting the Hoax] | | *[http://www.magma.ca/~hurleyp/FightingTheHoax.htm Fighting the Hoax] |
| | + | *[http://www.globalwarminghoax.com/news.php Refuting the Myth of Man-made Global Warming] |
| | *[http://www.climateaudit.org Climate Audit], Steve McIntyre's blog | | *[http://www.climateaudit.org Climate Audit], Steve McIntyre's blog |
| − | *[http://www.realclimate.org Real Climate], blog by a group of climatologists including Michael Mann</small> | + | *[http://www.realclimate.org Real Climate], blog by a group of climatologists including Michael Mann |
| − | | + | *[https://www.americanthinker.com/2009/01/co2_fairytales_in_global_warmi.html "CO<sub>2</sub> Fairytales in Global Warming"] |
| − | ==Critique of the Hockey Stick Reconstruction==
| + | *[http://www.numberwatch.co.uk/warmlist.htm A complete list of things caused by global warming] |
| − | <small>*[http://www.climateaudit.org/pdf/mcintyre.mckitrick.2003.pdf Corrections To The Mann et. al. (1998) Proxy Data Base And Northern Hemispheric AveraGlobal warming is the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.
| + | *[http://globaleconomicanalysis.blogspot.com/2009/11/hackers-prove-global-warming-is-scam.html Hackers Prove Global Warming Is A Scam] |
| − | | + | *[http://www.frontpagemag.com/fpm/266930/i-dont-believe-science-daniel-greenfield] |
| − | The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 year period ending in 2005, which is higher than the earlier estimate of 0.6 ± 0.2 °C for the period ending in 2000.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations"[1] via the greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3] These basic conclusions have been endorsed by at least 30 scientific societies and academies of science, including all of the national academies of science of the major industrialized countries. While individual scientists have voiced disagreement with the conclusions of the IPCC, the overwhelming majority of scientists working on climate change are in agreement with the conclusions.[4]
| |
| − | | |
| − | Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[1] The range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a millennium even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]
| |
| − | | |
| − | Increasing global temperature will cause sea level to rise, and is expected to increase the intensity of extreme weather events and to change the amount and pattern of precipitation. Other effects of global warming include changes in agricultural yields, trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.
| |
| − | | |
| − | Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. There is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences. Most national governments have signed and ratified the Kyoto Protocol, aimed at reducing greenhouse gas emissions.
| |
| − | Contents
| |
| − | [hide]
| |
| | | | |
| − | * 1 Terminology
| + | {{liberalism}} |
| − | * 2 Causes
| + | {{Climategate scandal}} |
| − | o 2.1 Greenhouse gases in the atmosphere
| |
| − | o 2.2 Feedbacks
| |
| − | o 2.3 Solar variation
| |
| − | * 3 Temperature changes
| |
| − | o 3.1 Recent
| |
| − | o 3.2 Pre-human climate variations
| |
| − | * 4 Climate models
| |
| − | * 5 Attributed and expected effects
| |
| − | o 5.1 Economic
| |
| − | o 5.2 Security
| |
| − | * 6 Adaptation and mitigation
| |
| − | * 7 Social and political debate
| |
| − | * 8 Related climatic issues
| |
| − | * 9 See also
| |
| − | * 10 References
| |
| − | * 11 Further reading
| |
| − | * 12 External links
| |
| − | | |
| − | Terminology
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| − | | |
| − | The term "global warming" is a specific example of the broader term climate change, which can also refer to global cooling. In common usage, the term refers to recent warming and implies a human influence.[5] The United Nations Framework Convention on Climate Change (UNFCCC) uses the term "climate change" for human-caused change, and "climate variability" for other changes.[6] The term "anthropogenic global warming" is sometimes used when focusing on human-induced changes.
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| − | Causes
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Main articles: Attribution of recent climate change and scientific opinion on climate change
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| − | The Earth's climate changes in response to external forcing, including variations in its orbit around the sun (orbital forcing),[7][8][9] volcanic eruptions, and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[10][11] identifies elevated levels of greenhouse gases due to human activity as the main influence. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain the observed increase in mean global temperature. One such hypothesis proposes that warming may be the result of variations in solar activity.[12][13][14]
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| − | None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[15]
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| − | Greenhouse gases in the atmosphere
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| − | Main article: Greenhouse effect
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| − | The greenhouse effect was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. It is the process by which absorption and emission of infrared radiation by atmospheric gases warm a planet's atmosphere and surface.
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| − | Existence of the greenhouse effect as such is not disputed. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F), without which Earth would be uninhabitable.[16][17] Rather, the issue is how the strength of the greenhouse effect is changed when human activity increases the atmospheric concentrations of some greenhouse gases.
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| − | On Earth, the major greenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect (not including clouds); carbon dioxide (CO2), which causes 9–26%; methane (CH4), which causes 4–9%; and ozone, which causes 3–7%.[18][19] Some other naturally occurring gases contribute very small fractions of the greenhouse effect; one of these, nitrous oxide (N2O), is increasing in concentration owing to human activity such as agriculture. The atmospheric concentrations of CO2 and CH4 have increased by 31% and 149% respectively above pre-industrial levels since 1750. Molecule for molecule, methane is a more effective greenhouse gas than carbon dioxide, but its concentration is much smaller so that its total radiative forcing is only about a fourth of that from carbon dioxide. These levels are considerably higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores. From less direct geological evidence it is believed that CO2 values this high were last attained 20 million years ago.[20] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, in particular deforestation.[21]
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| − | The present atmospheric concentration of CO2 is about 383 parts per million (ppm) by volume.[22] Future CO2 levels are expected to rise due to ongoing burning of fossil fuels and land-use change. The rate of rise will depend on uncertain economic, sociological, technological, and natural developments, but may be ultimately limited by the availability of fossil fuels. The IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[23] Fossil fuel reserves are sufficient to reach this level and continue emissions past 2100, if coal, tar sands or methane clathrates are extensively used.[24]
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| − | Feedbacks
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| − | Main article: Effects of global warming#Further global warming (positive feedback)
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| − | The effects of forcing agents on the climate are complicated by various feedback processes.
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| − | One of the most pronounced feedback effects relates to the evaporation of water. In the case of warming by the addition of long-lived greenhouse gases such as CO2, the initial warming will cause more water to be evaporated into the atmosphere. Since water vapor itself acts as a greenhouse gas, this causes still more warming; the warming causes more water vapor to be evaporated, and so forth until a new dynamic equilibrium concentration of water vapor is reached with a much larger greenhouse effect than that due to CO2 alone. Although this feedback process involves an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[25] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.
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| − | Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models. Nevertheless, cloud feedback is second only to water vapor feedback and is positive in all the models that were used in the IPCC Fourth Assessment Report.[25]
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| − | Another important feedback process is ice-albedo feedback.[26] When global temperatures increase, ice near the poles melts at an increasing rate. As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.
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| − | Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism contributing to warming.[27] A massive release of CH4 from methane clathrates could cause rapid warming, according to the clathrate gun hypothesis.
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| − | The ocean's ability to sequester carbon is expected to decline as it warms, because the resulting low nutrient levels of the mesopelagic zone limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[28]
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| − | Solar variation
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| − | Solar variation over the last 30 years.
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| − | Solar variation over the last 30 years.
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| − | Main article: Solar variation
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| − | A few papers suggest that the Sun's contribution may have been underestimated. Two researchers at Duke University, Bruce West and Nicola Scafetta, have estimated that the Sun may have contributed about 45–50% of the increase in the average global surface temperature over the period 1900–2000, and about 25–35% between 1980 and 2000.[29] A paper by Peter Stott and other researchers suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.[30] They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases.
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| − | A different hypothesis is that variations in solar output, possibly amplified by cloud seeding via galactic cosmic rays, may have contributed to recent warming.[31] It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.[32]
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| − | One predicted effect of an increase in solar activity would be a warming of the stratosphere; however, the observed effect since at least 1960 has been a cooling of the lower stratosphere, which is one of the predicted results of greenhouse gas warming.[33] Reduction of stratospheric ozone also has a cooling influence, although substantial ozone depletion did not occur until the late 1970s. Solar variation combined with changes in volcanic activity probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.[1] In 2006, Peter Foukal and other researchers from the United States, Germany, and Switzerland found no net increase of solar brightness over the last thousand years. Solar cycles led to a small increase of 0.07% in brightness over the last 30 years. This effect is far too small to contribute significantly to global warming.[34][35] A paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in cosmic rays.[36] Henrik Svensmark and Eigil Friis-Christensen, the main proponents of cloud seeding by galactic cosmic rays, disputed the findings of Lockwood and Fröhlich.[37] Another recent study speculates that other bodies within the Solar System may influence the climate in a complex manner.[38]
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| − | Temperature changes
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | | |
| − | Main article: Temperature record
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| − | Recent
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| − | Global temperatures on both land and sea have increased by 0.75 °C (1.35 °F) relative to the period 1860–1900, according to the instrumental temperature record. This measured temperature increase is not significantly affected by the urban heat island effect.[39] Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[40] Temperatures in the lower troposphere have increased between 0.12 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with possibly regional fluctuations such as the Medieval Warm Period or the Little Ice Age.
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| − | Sea temperatures increase more slowly than those on land both because of the larger effective heat capacity of the oceans and because the ocean can lose heat by evaporation more readily than the land.[41] Since the Northern Hemisphere has more land mass than the Southern Hemisphere it warms faster; also there are extensive areas of seasonal snow cover subject to the snow-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the asymmetry of warming as the major gases are essentially well-mixed between hemispheres.
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| − | Based on estimates by NASA's Goddard Institute for Space Studies, 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[42] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit concluded that 2005 was the second warmest year, behind 1998.[43][44]
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| − | Anthropogenic emissions of other pollutants—notably sulfate aerosols—can exert a cooling effect by increasing the reflection of incoming sunlight. This partially accounts for the cooling seen in the temperature record in the middle of the twentieth century,[45] though the cooling may also be due in part to natural variability. James Hansen and colleagues have proposed that the effects of the products of fossil fuel combustion—CO2 and aerosols—have largely offset one another, so that warming in recent decades has been driven mainly by non-CO2 greenhouse gases.[46]
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| − | Paleoclimatologist William Ruddiman has argued that human influence on the global climate began around 8,000 years ago with the start of forest clearing to provide land for agriculture and 5,000 years ago with the start of Asian rice irrigation.[47] Ruddiman's interpretation of the historical record, with respect to the methane data, has been disputed.[48]
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| − | Pre-human climate variations
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Further information: Paleoclimatology
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| − | See also: Snowball Earth
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| − | | |
| − | Earth has experienced warming and cooling many times in the past. The recent Antarctic EPICA ice core spans 800,000 years, including eight glacial cycles timed by orbital variations with interglacial warm periods comparable to present temperatures.[49]
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| − | A rapid buildup of greenhouse gases caused warming in the early Jurassic period (about 180 million years ago), with average temperatures rising by 5 °C (9 °F). Research by the Open University indicates that the warming caused the rate of rock weathering to increase by 400%. As such weathering locks away carbon in calcite and dolomite, CO2 levels dropped back to normal over roughly the next 150,000 years.[50][51]
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| − | Sudden releases of methane from clathrate compounds (the clathrate gun hypothesis) have been hypothesized as a cause for other warming events in the distant past, including the Permian-Triassic extinction event (about 251 million years ago) and the Paleocene-Eocene Thermal Maximum (about 55 million years ago).
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| − | Climate models
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | | |
| − | Main article: Global climate model
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| − | Scientists have studied global warming with computer models of the climate. These models are based on physical principles of fluid dynamics, radiative transfer, and other processes, with simplifications being necessary because of limitations in computer power and the complexity of the underlying system (climate). These models predict that the effect of adding greenhouse gases is to produce a warmer climate.[52] However, even when the same assumptions of future greenhouse gas levels are used, there still remains a considerable range of climate sensitivity.
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| − | Including uncertainties in future greenhouse gas concentrations and climate modeling, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999.[1] Models have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes.
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| − | Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.[53] These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.
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| − | Most global climate models, when run to project future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.[54][55][56]
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| − | The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem.[57] There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability.
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| − | Attributed and expected effects
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| − | | |
| − | Main article: Effects of global warming
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| − | | |
| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Although it is difficult to connect specific weather events to global warming, an increase in global temperatures may in turn cause broader changes, including glacial retreat, Arctic shrinkage, and worldwide sea level rise. Changes in the amount and pattern of precipitation may result in flooding and drought. There may also be changes in the frequency and intensity of extreme weather events. Other effects may include changes in agricultural yields, addition of new trade routes,[58] reduced summer streamflows, species extinctions, and increases in the range of disease vectors.
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| − | Some effects on both the natural environment and human life are, at least in part, already being attributed to global warming. A 2001 report by the IPCC suggests that glacier retreat, ice shelf disruption such as that of the Larsen Ice Shelf, sea level rise, changes in rainfall patterns, and increased intensity and frequency of extreme weather events, are being attributed in part to global warming.[59] While changes are expected for overall patterns, intensity, and frequencies, it is difficult to attribute specific events to global warming. Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.[60]
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| − | Increasing deaths, displacements, and economic losses projected due to extreme weather attributed to global warming may be exacerbated by growing population densities in affected areas, although temperate regions are projected to experience some minor benefits, such as fewer deaths due to cold exposure.[61] A summary of probable effects and recent understanding can be found in the report made for the IPCC Third Assessment Report by Working Group II.[59] The newer IPCC Fourth Assessment Report summary reports that there is observational evidence for an increase in intense tropical cyclone activity in the North Atlantic Ocean since about 1970, in correlation with the increase in sea surface temperature, but that the detection of long-term trends is complicated by the quality of records prior to routine satellite observations. The summary also states that there is no clear trend in the annual worldwide number of tropical cyclones.[1]
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| − | Additional anticipated effects include sea level rise of 110 to 770 millimeters (0.36 to 2.5 ft) between 1990 and 2100,[62] repercussions to agriculture, possible slowing of the thermohaline circulation, reductions in the ozone layer, increased intensity of hurricanes and extreme weather events, lowering of ocean pH, and the spread of diseases such as malaria and dengue fever. One study predicts 18% to 35% of a sample of 1,103 animal and plant species would be extinct by 2050, based on future climate projections.[63] However, few mechanistic studies have documented extinctions due to recent climate change[64] and one study suggests that projected rates of extinction are uncertain.[65]
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| − | Economic
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | Main articles: Economics of global warming and Low-carbon economy
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| − | Some economists have tried to estimate the aggregate net economic costs of damages from climate change across the globe. Such estimates have so far failed to reach conclusive findings; in a survey of 100 estimates, the values ran from US$-10 per tonne of carbon (tC) (US$-3 per tonne of carbon dioxide) up to US$350/tC (US$95 per tonne of carbon dioxide), with a mean of US$43 per tonne of carbon (US$12 per tonne of carbon dioxide).[61] One widely publicized report on potential economic impact is the Stern Review; it suggests that extreme weather might reduce global gross domestic product by up to 1%, and that in a worst-case scenario global per capita consumption could fall 20%.[66] The report's methodology, advocacy and conclusions have been criticized by many economists, primarily around the Review's assumptions of discounting and its choices of scenarios,[67] while others have supported the general attempt to quantify economic risk, even if not the specific numbers.[68][69]
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| − | In a summary of economic cost associated with climate change, the United Nations Environment Programme emphasizes the risks to insurers, reinsurers, and banks of increasingly traumatic and costly weather events. Other economic sectors likely to face difficulties related to climate change include agriculture and transport. Developing countries, rather than the developed world, are at greatest economic risk.[70]
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| − | Security
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| − | In November 2007, the Center for Strategic and International Studies and the Center for a New American Security published a report highlighting the national security effects of climate change.[71] These security effects include increased competition for resources between countries, mass migration from the worst affected areas, challenges to the cohesion of major states threatened by the rise in sea levels, and, as a consequence of these factors, an increased risk of armed conflict, including even nuclear conflicts.
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| − | Adaptation and mitigation
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| − | | |
| − | Main articles: Adaptation to global warming, Mitigation of global warming, and Kyoto Protocol
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| − | | |
| − | The broad agreement among climate scientists that global temperatures will continue to increase has led some nations, states, corporations and individuals to implement actions to try to curtail global warming or adjust to it. Many environmental groups encourage action against global warming, often by the consumer, but also by community and regional organizations. Others have suggested a quota on worldwide fossil fuel production, citing a direct link between fossil fuel production and CO2 emissions.[72][73]
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| − | There has also been business action on climate change, including efforts at increased energy efficiency and limited moves towards use of alternative fuels. One important innovation has been the development of greenhouse gas emissions trading through which companies, in conjunction with government, agree to cap their emissions or to purchase credits from those below their allowances.
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| − | The world's primary international agreement on combating global warming is the Kyoto Protocol, an amendment to the United Nations Framework Convention on Climate Change (UNFCCC) negotiated in 1997. The Protocol now covers more than 160 countries globally and over 55% of global greenhouse gas emissions.[74] Only the United States and Kazakhstan have not ratified the treaty, with the United States historically being the world's largest emitter of greenhouse gas. This treaty expires in 2012, and international talks began in May 2007 on a future treaty to succeed the current one.[75]
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| − | Claiming "serious harm" to the United States economy and the exemption of "80 percent of the world, including major population centers" like China and India, from the treaty, George W. Bush contends that the Kyoto Protocol is an unfair and ineffective means of addressing global climate change concerns.[76] Still, various state, local, and regional governments within the United States have begun their own initiatives to indicate support and compliance with the Kyoto Protocol on a local basis. For example, the Regional Greenhouse Gas Initiative is a state-level emissions capping and trading program involving eight Northeastern U.S. states, which was founded on December 20, 2005.[77]
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| − | China and India, though exempt from its provisions as developing countries, have ratified the Kyoto Protocol. China may have passed the U.S. in total annual greenhouse gas emissions according to some recent studies. Chinese Premier Wen Jiabao has called on the nation to redouble its efforts to tackle pollution and global warming.[78]
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| − | The IPCC's Working Group III is responsible for crafting reports that deal with the mitigation of global warming and analyzing the costs and benefits of different approaches. In the 2007 IPCC Fourth Assessment Report, they conclude that no one technology or sector can be completely responsible for mitigating future warming. They find there are key practices and technologies in various sectors, such as energy supply, transportation, industry, and agriculture, that should be implemented to reduced global emissions. They estimate that stabilization of carbon dioxide equivalent between 445 and 710 ppm by 2030 will result in between a 0.6% increase and 3% decrease in global gross domestic product.[79]
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| − | Social and political debate
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| − | | |
| − | Main articles: Global warming controversy, Politics of global warming, and Economics of global warming
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| − | See also: Climate change denial
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Over the past several years, public perceptions and attitudes concerning the causes and importance of global warming have changed.[80] Increased awareness of the scientific findings surrounding global warming has resulted in political and economic debate. Poor regions, particularly Africa, appear at greatest risk from the suggested effects of global warming, while their actual emissions have been small compared to the developed world.[81] At the same time, developing country exemptions from provisions of the Kyoto Protocol have been criticized by the United States and Australia, and have been used as part of the rationale for continued non-ratification by the U.S.[82] In the Western world, the idea of human influence on climate has gained wider acceptance in Europe than in the United States.[83][84]
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| − | The issue of climate change has sparked debate weighing the benefits of limiting industrial emissions of greenhouse gases against the costs that such changes would entail. There has been discussion in several countries about the cost and benefits of adopting alternative energy sources in order to reduce carbon emissions.[85] Organizations and companies such as the Competitive Enterprise Institute and ExxonMobil have emphasized more conservative climate change scenarios while highlighting the potential economic cost of stricter controls.[86][87][88][89] Likewise, various environmental lobbies and a number of public figures have launched campaigns to emphasize the potential risks of climate change and promote the implementation of stricter controls. Some fossil fuel companies have scaled back their efforts in recent years,[90] or called for policies to reduce global warming.[91]
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| − | Another point of debate is the degree to which newly developed economies such as India and China should be expected to constrain their emissions. China's gross national CO2 emissions are expected to exceed those of the U.S. within the next few years, and may have already done so according to a 2006 report.[92] China has contended that it has less of an obligation to reduce emissions since its per capita emissions are roughly one-fifth that of the United States.[93] India, also exempt from Kyoto restrictions and another of the biggest sources of industrial emissions, has made similar assertions.[94] However, the U.S. contends that if they must bear the cost of reducing emissions, then China should do the same.[95]
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| − | Related climatic issues
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| − | Main articles: Ocean acidification, global dimming, and ozone depletion
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| − | A variety of issues are often raised in relation to global warming. One is ocean acidification. Increased atmospheric CO2 increases the amount of CO2 dissolved in the oceans.[96] CO2 dissolved in the ocean reacts with water to form carbonic acid, resulting in acidification. Ocean surface pH is estimated to have decreased from 8.25 near the beginning of the industrial era to 8.14 by 2004,[97] and is projected to decrease by a further 0.14 to 0.5 units by 2100 as the ocean absorbs more CO2.[1][98] Since organisms and ecosystems are adapted to a narrow range of pH, this raises extinction concerns, directly driven by increased atmospheric CO2, that could disrupt food webs and impact human societies that depend on marine ecosystem services.[99]
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| − | Global dimming, the gradual reduction in the amount of global direct irradiance at the Earth's surface, may have partially mitigated global warming in the late twentieth century. From 1960 to 1990 human-caused aerosols likely precipitated this effect. Scientists have stated with 66–90% confidence that the effects of human-caused aerosols, along with volcanic activity, have offset some of the global warming, and that greenhouse gases would have resulted in more warming than observed if not for these dimming agents.[1]
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| − | Ozone depletion, the steady decline in the total amount of ozone in Earth's stratosphere, is frequently cited in relation to global warming. Although there are areas of linkage, the relationship between the two is not strong.
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| − | See also
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| − | * Glossary of climate change
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| − | References
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| − | 1. ^ a b c d e f g h i Summary for Policymakers (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change (2007-02-05). Retrieved on 2007-02-02. “The updated 100-year linear trend (1906 to 2005) of 0.74°C [0.56°C to 0.92°C] is therefore larger than the corresponding trend for 1901 to 2000 given in the TAR of 0.6°C [0.4°C to 0.8°C].”
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| − | 2. ^ Hegerl, Gabriele C.; et al. (2007-05-07). Understanding and Attributing Climate Change (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 690. Intergovernmental Panel on Climate Change. Retrieved on 2007-05-20. “Recent estimates (Figure 9.9) indicate a relatively small combined effect of natural forcings on the global mean temperature evolution of the seconds half of the 20th century, with a small net cooling from the combined effects of solar and volcanic forcings”
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| − | 3. ^ Ammann, Caspar; et al. (2007-04-06). "Solar influence on climate during the past millennium: Results from ransient simulations with the NCAR Climate Simulation Model" (PDF). Proceedings of the National Academy of Sciences of the United States of America 104 (10): 3713–3718. “However, because of a lack of interactive ozone, the model cannot fully simulate features discussed in (44)." "While the NH temperatures of the high-scaled experiment are often colder than the lower bound from proxy data, the modeled decadal-scale NH surface temperature for the medium-scaled case falls within the uncertainty range of the available temperature reconstructions. The medium-scaled simulation also broadly reproduces the main features seen in the proxy records." "Without anthropogenic forcing, the 20th century warming is small. The simulations with only natural forcing components included yield an early 20th century peak warming of ≈0.2 °C (≈1950 AD), which is reduced to about half by the end of the century because of increased volcanism.”
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| − | 17. ^ Note that the Greenhouse Effect produces a temperature increase of about 33 °C (59 °F) with respect to black body predictions and not a surface temperature of 33 °C (91 °F) which is 32 °F higher. The average surface temperature is about 14 °C (57 °F). Also note that both the Celsius and Fahrenheit temperatures are expressed to 2 significant figures even though the conversion formula produces 3.
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| − | | |
| − | Global warming is the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.
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| − | | |
| − | The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 year period ending in 2005, which is higher than the earlier estimate of 0.6 ± 0.2 °C for the period ending in 2000.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations"[1] via the greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3] These basic conclusions have been endorsed by at least 30 scientific societies and academies of science, including all of the national academies of science of the major industrialized countries. While individual scientists have voiced disagreement with the conclusions of the IPCC, the overwhelming majority of scientists working on climate change are in agreement with the conclusions.[4]
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| − | | |
| − | Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[1] The range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a millennium even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]
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| − | | |
| − | Increasing global temperature will cause sea level to rise, and is expected to increase the intensity of extreme weather events and to change the amount and pattern of precipitation. Other effects of global warming include changes in agricultural yields, trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.
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| − | | |
| − | Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. There is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences. Most national governments have signed and ratified the Kyoto Protocol, aimed at reducing greenhouse gas emissions.
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| − | Contents
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| − | [hide]
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| − | | |
| − | * 1 Terminology
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| − | * 2 Causes
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| − | o 2.1 Greenhouse gases in the atmosphere
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| − | o 2.2 Feedbacks
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| − | o 2.3 Solar variation
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| − | * 3 Temperature changes
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| − | o 3.1 Recent
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| − | o 3.2 Pre-human climate variations
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| − | * 4 Climate models
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| − | * 5 Attributed and expected effects
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| − | o 5.1 Economic
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| − | o 5.2 Security
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| − | * 6 Adaptation and mitigation
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| − | * 7 Social and political debate
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| − | * 8 Related climatic issues
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| − | * 9 See also
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| − | * 10 References
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| − | * 11 Further reading
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| − | * 12 External links
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| − | | |
| − | Terminology
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| − | | |
| − | The term "global warming" is a specific example of the broader term climate change, which can also refer to global cooling. In common usage, the term refers to recent warming and implies a human influence.[5] The United Nations Framework Convention on Climate Change (UNFCCC) uses the term "climate change" for human-caused change, and "climate variability" for other changes.[6] The term "anthropogenic global warming" is sometimes used when focusing on human-induced changes.
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| − | | |
| − | Causes
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | | |
| − | Main articles: Attribution of recent climate change and scientific opinion on climate change
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| − | | |
| − | The Earth's climate changes in response to external forcing, including variations in its orbit around the sun (orbital forcing),[7][8][9] volcanic eruptions, and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[10][11] identifies elevated levels of greenhouse gases due to human activity as the main influence. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain the observed increase in mean global temperature. One such hypothesis proposes that warming may be the result of variations in solar activity.[12][13][14]
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| − | | |
| − | None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[15]
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| − | | |
| − | Greenhouse gases in the atmosphere
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| − | | |
| − | Main article: Greenhouse effect
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| − | | |
| − | The greenhouse effect was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. It is the process by which absorption and emission of infrared radiation by atmospheric gases warm a planet's atmosphere and surface.
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| − | | |
| − | Existence of the greenhouse effect as such is not disputed. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F), without which Earth would be uninhabitable.[16][17] Rather, the issue is how the strength of the greenhouse effect is changed when human activity increases the atmospheric concentrations of some greenhouse gases.
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| − | | |
| − | On Earth, the major greenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect (not including clouds); carbon dioxide (CO2), which causes 9–26%; methane (CH4), which causes 4–9%; and ozone, which causes 3–7%.[18][19] Some other naturally occurring gases contribute very small fractions of the greenhouse effect; one of these, nitrous oxide (N2O), is increasing in concentration owing to human activity such as agriculture. The atmospheric concentrations of CO2 and CH4 have increased by 31% and 149% respectively above pre-industrial levels since 1750. Molecule for molecule, methane is a more effective greenhouse gas than carbon dioxide, but its concentration is much smaller so that its total radiative forcing is only about a fourth of that from carbon dioxide. These levels are considerably higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores. From less direct geological evidence it is believed that CO2 values this high were last attained 20 million years ago.[20] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, in particular deforestation.[21]
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| − | The present atmospheric concentration of CO2 is about 383 parts per million (ppm) by volume.[22] Future CO2 levels are expected to rise due to ongoing burning of fossil fuels and land-use change. The rate of rise will depend on uncertain economic, sociological, technological, and natural developments, but may be ultimately limited by the availability of fossil fuels. The IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[23] Fossil fuel reserves are sufficient to reach this level and continue emissions past 2100, if coal, tar sands or methane clathrates are extensively used.[24]
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| − | Feedbacks
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| − | | |
| − | Main article: Effects of global warming#Further global warming (positive feedback)
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| − | The effects of forcing agents on the climate are complicated by various feedback processes.
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| − | One of the most pronounced feedback effects relates to the evaporation of water. In the case of warming by the addition of long-lived greenhouse gases such as CO2, the initial warming will cause more water to be evaporated into the atmosphere. Since water vapor itself acts as a greenhouse gas, this causes still more warming; the warming causes more water vapor to be evaporated, and so forth until a new dynamic equilibrium concentration of water vapor is reached with a much larger greenhouse effect than that due to CO2 alone. Although this feedback process involves an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[25] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.
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| − | Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models. Nevertheless, cloud feedback is second only to water vapor feedback and is positive in all the models that were used in the IPCC Fourth Assessment Report.[25]
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| − | Another important feedback process is ice-albedo feedback.[26] When global temperatures increase, ice near the poles melts at an increasing rate. As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.
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| − | Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism contributing to warming.[27] A massive release of CH4 from methane clathrates could cause rapid warming, according to the clathrate gun hypothesis.
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| − | The ocean's ability to sequester carbon is expected to decline as it warms, because the resulting low nutrient levels of the mesopelagic zone limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[28]
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| − | Solar variation
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| − | Solar variation over the last 30 years.
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| − | Solar variation over the last 30 years.
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| − | Main article: Solar variation
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| − | | |
| − | A few papers suggest that the Sun's contribution may have been underestimated. Two researchers at Duke University, Bruce West and Nicola Scafetta, have estimated that the Sun may have contributed about 45–50% of the increase in the average global surface temperature over the period 1900–2000, and about 25–35% between 1980 and 2000.[29] A paper by Peter Stott and other researchers suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.[30] They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases.
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| − | A different hypothesis is that variations in solar output, possibly amplified by cloud seeding via galactic cosmic rays, may have contributed to recent warming.[31] It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.[32]
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| − | One predicted effect of an increase in solar activity would be a warming of the stratosphere; however, the observed effect since at least 1960 has been a cooling of the lower stratosphere, which is one of the predicted results of greenhouse gas warming.[33] Reduction of stratospheric ozone also has a cooling influence, although substantial ozone depletion did not occur until the late 1970s. Solar variation combined with changes in volcanic activity probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.[1] In 2006, Peter Foukal and other researchers from the United States, Germany, and Switzerland found no net increase of solar brightness over the last thousand years. Solar cycles led to a small increase of 0.07% in brightness over the last 30 years. This effect is far too small to contribute significantly to global warming.[34][35] A paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in cosmic rays.[36] Henrik Svensmark and Eigil Friis-Christensen, the main proponents of cloud seeding by galactic cosmic rays, disputed the findings of Lockwood and Fröhlich.[37] Another recent study speculates that other bodies within the Solar System may influence the climate in a complex manner.[38]
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| − | Temperature changes
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | | |
| − | Main article: Temperature record
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| − | | |
| − | Recent
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| − | Global temperatures on both land and sea have increased by 0.75 °C (1.35 °F) relative to the period 1860–1900, according to the instrumental temperature record. This measured temperature increase is not significantly affected by the urban heat island effect.[39] Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[40] Temperatures in the lower troposphere have increased between 0.12 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with possibly regional fluctuations such as the Medieval Warm Period or the Little Ice Age.
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| − | Sea temperatures increase more slowly than those on land both because of the larger effective heat capacity of the oceans and because the ocean can lose heat by evaporation more readily than the land.[41] Since the Northern Hemisphere has more land mass than the Southern Hemisphere it warms faster; also there are extensive areas of seasonal snow cover subject to the snow-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the asymmetry of warming as the major gases are essentially well-mixed between hemispheres.
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| − | Based on estimates by NASA's Goddard Institute for Space Studies, 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[42] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit concluded that 2005 was the second warmest year, behind 1998.[43][44]
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| − | Anthropogenic emissions of other pollutants—notably sulfate aerosols—can exert a cooling effect by increasing the reflection of incoming sunlight. This partially accounts for the cooling seen in the temperature record in the middle of the twentieth century,[45] though the cooling may also be due in part to natural variability. James Hansen and colleagues have proposed that the effects of the products of fossil fuel combustion—CO2 and aerosols—have largely offset one another, so that warming in recent decades has been driven mainly by non-CO2 greenhouse gases.[46]
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| − | | |
| − | Paleoclimatologist William Ruddiman has argued that human influence on the global climate began around 8,000 years ago with the start of forest clearing to provide land for agriculture and 5,000 years ago with the start of Asian rice irrigation.[47] Ruddiman's interpretation of the historical record, with respect to the methane data, has been disputed.[48]
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| − | | |
| − | Pre-human climate variations
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | | |
| − | Further information: Paleoclimatology
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| − | See also: Snowball Earth
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| − | | |
| − | Earth has experienced warming and cooling many times in the past. The recent Antarctic EPICA ice core spans 800,000 years, including eight glacial cycles timed by orbital variations with interglacial warm periods comparable to present temperatures.[49]
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| − | | |
| − | A rapid buildup of greenhouse gases caused warming in the early Jurassic period (about 180 million years ago), with average temperatures rising by 5 °C (9 °F). Research by the Open University indicates that the warming caused the rate of rock weathering to increase by 400%. As such weathering locks away carbon in calcite and dolomite, CO2 levels dropped back to normal over roughly the next 150,000 years.[50][51]
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| − | | |
| − | Sudden releases of methane from clathrate compounds (the clathrate gun hypothesis) have been hypothesized as a cause for other warming events in the distant past, including the Permian-Triassic extinction event (about 251 million years ago) and the Paleocene-Eocene Thermal Maximum (about 55 million years ago).
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| − | Climate models
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | | |
| − | Main article: Global climate model
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| − | | |
| − | Scientists have studied global warming with computer models of the climate. These models are based on physical principles of fluid dynamics, radiative transfer, and other processes, with simplifications being necessary because of limitations in computer power and the complexity of the underlying system (climate). These models predict that the effect of adding greenhouse gases is to produce a warmer climate.[52] However, even when the same assumptions of future greenhouse gas levels are used, there still remains a considerable range of climate sensitivity.
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| − | | |
| − | Including uncertainties in future greenhouse gas concentrations and climate modeling, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999.[1] Models have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes.
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| − | Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.[53] These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.
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| − | | |
| − | Most global climate models, when run to project future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.[54][55][56]
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| − | The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem.[57] There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability.
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| − | | |
| − | Attributed and expected effects
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| − | | |
| − | Main article: Effects of global warming
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| − | | |
| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Although it is difficult to connect specific weather events to global warming, an increase in global temperatures may in turn cause broader changes, including glacial retreat, Arctic shrinkage, and worldwide sea level rise. Changes in the amount and pattern of precipitation may result in flooding and drought. There may also be changes in the frequency and intensity of extreme weather events. Other effects may include changes in agricultural yields, addition of new trade routes,[58] reduced summer streamflows, species extinctions, and increases in the range of disease vectors.
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| − | | |
| − | Some effects on both the natural environment and human life are, at least in part, already being attributed to global warming. A 2001 report by the IPCC suggests that glacier retreat, ice shelf disruption such as that of the Larsen Ice Shelf, sea level rise, changes in rainfall patterns, and increased intensity and frequency of extreme weather events, are being attributed in part to global warming.[59] While changes are expected for overall patterns, intensity, and frequencies, it is difficult to attribute specific events to global warming. Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.[60]
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| − | Increasing deaths, displacements, and economic losses projected due to extreme weather attributed to global warming may be exacerbated by growing population densities in affected areas, although temperate regions are projected to experience some minor benefits, such as fewer deaths due to cold exposure.[61] A summary of probable effects and recent understanding can be found in the report made for the IPCC Third Assessment Report by Working Group II.[59] The newer IPCC Fourth Assessment Report summary reports that there is observational evidence for an increase in intense tropical cyclone activity in the North Atlantic Ocean since about 1970, in correlation with the increase in sea surface temperature, but that the detection of long-term trends is complicated by the quality of records prior to routine satellite observations. The summary also states that there is no clear trend in the annual worldwide number of tropical cyclones.[1]
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| − | | |
| − | Additional anticipated effects include sea level rise of 110 to 770 millimeters (0.36 to 2.5 ft) between 1990 and 2100,[62] repercussions to agriculture, possible slowing of the thermohaline circulation, reductions in the ozone layer, increased intensity of hurricanes and extreme weather events, lowering of ocean pH, and the spread of diseases such as malaria and dengue fever. One study predicts 18% to 35% of a sample of 1,103 animal and plant species would be extinct by 2050, based on future climate projections.[63] However, few mechanistic studies have documented extinctions due to recent climate change[64] and one study suggests that projected rates of extinction are uncertain.[65]
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| − | | |
| − | Economic
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | | |
| − | Main articles: Economics of global warming and Low-carbon economy
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| − | | |
| − | Some economists have tried to estimate the aggregate net economic costs of damages from climate change across the globe. Such estimates have so far failed to reach conclusive findings; in a survey of 100 estimates, the values ran from US$-10 per tonne of carbon (tC) (US$-3 per tonne of carbon dioxide) up to US$350/tC (US$95 per tonne of carbon dioxide), with a mean of US$43 per tonne of carbon (US$12 per tonne of carbon dioxide).[61] One widely publicized report on potential economic impact is the Stern Review; it suggests that extreme weather might reduce global gross domestic product by up to 1%, and that in a worst-case scenario global per capita consumption could fall 20%.[66] The report's methodology, advocacy and conclusions have been criticized by many economists, primarily around the Review's assumptions of discounting and its choices of scenarios,[67] while others have supported the general attempt to quantify economic risk, even if not the specific numbers.[68][69]
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| − | In a summary of economic cost associated with climate change, the United Nations Environment Programme emphasizes the risks to insurers, reinsurers, and banks of increasingly traumatic and costly weather events. Other economic sectors likely to face difficulties related to climate change include agriculture and transport. Developing countries, rather than the developed world, are at greatest economic risk.[70]
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| − | Security
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| − | In November 2007, the Center for Strategic and International Studies and the Center for a New American Security published a report highlighting the national security effects of climate change.[71] These security effects include increased competition for resources between countries, mass migration from the worst affected areas, challenges to the cohesion of major states threatened by the rise in sea levels, and, as a consequence of these factors, an increased risk of armed conflict, including even nuclear conflicts.
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| − | Adaptation and mitigation
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| − | | |
| − | Main articles: Adaptation to global warming, Mitigation of global warming, and Kyoto Protocol
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| − | | |
| − | The broad agreement among climate scientists that global temperatures will continue to increase has led some nations, states, corporations and individuals to implement actions to try to curtail global warming or adjust to it. Many environmental groups encourage action against global warming, often by the consumer, but also by community and regional organizations. Others have suggested a quota on worldwide fossil fuel production, citing a direct link between fossil fuel production and CO2 emissions.[72][73]
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| − | There has also been business action on climate change, including efforts at increased energy efficiency and limited moves towards use of alternative fuels. One important innovation has been the development of greenhouse gas emissions trading through which companies, in conjunction with government, agree to cap their emissions or to purchase credits from those below their allowances.
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| − | The world's primary international agreement on combating global warming is the Kyoto Protocol, an amendment to the United Nations Framework Convention on Climate Change (UNFCCC) negotiated in 1997. The Protocol now covers more than 160 countries globally and over 55% of global greenhouse gas emissions.[74] Only the United States and Kazakhstan have not ratified the treaty, with the United States historically being the world's largest emitter of greenhouse gas. This treaty expires in 2012, and international talks began in May 2007 on a future treaty to succeed the current one.[75]
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| − | Claiming "serious harm" to the United States economy and the exemption of "80 percent of the world, including major population centers" like China and India, from the treaty, George W. Bush contends that the Kyoto Protocol is an unfair and ineffective means of addressing global climate change concerns.[76] Still, various state, local, and regional governments within the United States have begun their own initiatives to indicate support and compliance with the Kyoto Protocol on a local basis. For example, the Regional Greenhouse Gas Initiative is a state-level emissions capping and trading program involving eight Northeastern U.S. states, which was founded on December 20, 2005.[77]
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| − | China and India, though exempt from its provisions as developing countries, have ratified the Kyoto Protocol. China may have passed the U.S. in total annual greenhouse gas emissions according to some recent studies. Chinese Premier Wen Jiabao has called on the nation to redouble its efforts to tackle pollution and global warming.[78]
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| − | | |
| − | The IPCC's Working Group III is responsible for crafting reports that deal with the mitigation of global warming and analyzing the costs and benefits of different approaches. In the 2007 IPCC Fourth Assessment Report, they conclude that no one technology or sector can be completely responsible for mitigating future warming. They find there are key practices and technologies in various sectors, such as energy supply, transportation, industry, and agriculture, that should be implemented to reduced global emissions. They estimate that stabilization of carbon dioxide equivalent between 445 and 710 ppm by 2030 will result in between a 0.6% increase and 3% decrease in global gross domestic product.[79]
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| − | | |
| − | Social and political debate
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| − | | |
| − | Main articles: Global warming controversy, Politics of global warming, and Economics of global warming
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| − | See also: Climate change denial
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | | |
| − | Over the past several years, public perceptions and attitudes concerning the causes and importance of global warming have changed.[80] Increased awareness of the scientific findings surrounding global warming has resulted in political and economic debate. Poor regions, particularly Africa, appear at greatest risk from the suggested effects of global warming, while their actual emissions have been small compared to the developed world.[81] At the same time, developing country exemptions from provisions of the Kyoto Protocol have been criticized by the United States and Australia, and have been used as part of the rationale for continued non-ratification by the U.S.[82] In the Western world, the idea of human influence on climate has gained wider acceptance in Europe than in the United States.[83][84]
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| − | The issue of climate change has sparked debate weighing the benefits of limiting industrial emissions of greenhouse gases against the costs that such changes would entail. There has been discussion in several countries about the cost and benefits of adopting alternative energy sources in order to reduce carbon emissions.[85] Organizations and companies such as the Competitive Enterprise Institute and ExxonMobil have emphasized more conservative climate change scenarios while highlighting the potential economic cost of stricter controls.[86][87][88][89] Likewise, various environmental lobbies and a number of public figures have launched campaigns to emphasize the potential risks of climate change and promote the implementation of stricter controls. Some fossil fuel companies have scaled back their efforts in recent years,[90] or called for policies to reduce global warming.[91]
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| − | Another point of debate is the degree to which newly developed economies such as India and China should be expected to constrain their emissions. China's gross national CO2 emissions are expected to exceed those of the U.S. within the next few years, and may have already done so according to a 2006 report.[92] China has contended that it has less of an obligation to reduce emissions since its per capita emissions are roughly one-fifth that of the United States.[93] India, also exempt from Kyoto restrictions and another of the biggest sources of industrial emissions, has made similar assertions.[94] However, the U.S. contends that if they must bear the cost of reducing emissions, then China should do the same.[95]
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| − | Related climatic issues
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| − | | |
| − | Main articles: Ocean acidification, global dimming, and ozone depletion
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| − | | |
| − | A variety of issues are often raised in relation to global warming. One is ocean acidification. Increased atmospheric CO2 increases the amount of CO2 dissolved in the oceans.[96] CO2 dissolved in the ocean reacts with water to form carbonic acid, resulting in acidification. Ocean surface pH is estimated to have decreased from 8.25 near the beginning of the industrial era to 8.14 by 2004,[97] and is projected to decrease by a further 0.14 to 0.5 units by 2100 as the ocean absorbs more CO2.[1][98] Since organisms and ecosystems are adapted to a narrow range of pH, this raises extinction concerns, directly driven by increased atmospheric CO2, that could disrupt food webs and impact human societies that depend on marine ecosystem services.[99]
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| − | Global dimming, the gradual reduction in the amount of global direct irradiance at the Earth's surface, may have partially mitigated global warming in the late twentieth century. From 1960 to 1990 human-caused aerosols likely precipitated this effect. Scientists have stated with 66–90% confidence that the effects of human-caused aerosols, along with volcanic activity, have offset some of the global warming, and that greenhouse gases would have resulted in more warming than observed if not for these dimming agents.[1]
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| − | | |
| − | Ozone depletion, the steady decline in the total amount of ozone in Earth's stratosphere, is frequently cited in relation to global warming. Although there are areas of linkage, the relationship between the two is not strong.
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| − | See also
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| − | | |
| − | * Glossary of climate change
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| − | | |
| − | References
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| − | | |
| − | 1. ^ a b c d e f g h i Summary for Policymakers (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change (2007-02-05). Retrieved on 2007-02-02. “The updated 100-year linear trend (1906 to 2005) of 0.74°C [0.56°C to 0.92°C] is therefore larger than the corresponding trend for 1901 to 2000 given in the TAR of 0.6°C [0.4°C to 0.8°C].”
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| − | 2. ^ Hegerl, Gabriele C.; et al. (2007-05-07). Understanding and Attributing Climate Change (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 690. Intergovernmental Panel on Climate Change. Retrieved on 2007-05-20. “Recent estimates (Figure 9.9) indicate a relatively small combined effect of natural forcings on the global mean temperature evolution of the seconds half of the 20th century, with a small net cooling from the combined effects of solar and volcanic forcings”
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| − | 3. ^ Ammann, Caspar; et al. (2007-04-06). "Solar influence on climate during the past millennium: Results from ransient simulations with the NCAR Climate Simulation Model" (PDF). Proceedings of the National Academy of Sciences of the United States of America 104 (10): 3713–3718. “However, because of a lack of interactive ozone, the model cannot fully simulate features discussed in (44)." "While the NH temperatures of the high-scaled experiment are often colder than the lower bound from proxy data, the modeled decadal-scale NH surface temperature for the medium-scaled case falls within the uncertainty range of the available temperature reconstructions. The medium-scaled simulation also broadly reproduces the main features seen in the proxy records." "Without anthropogenic forcing, the 20th century warming is small. The simulations with only natural forcing components included yield an early 20th century peak warming of ≈0.2 °C (≈1950 AD), which is reduced to about half by the end of the century because of increased volcanism.”
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| − | 4. ^ A guide to facts and fictions about climate change. Royal Society (March 2005). Retrieved on 2007-11-18. “"However, the overwhelming majority of scientists who work on climate change agree on the main points"”
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| − | 5. ^ Climate Change: Basic Information. United States Environmental Protection Agency (2006-12-14). Retrieved on 2007-02-09. “In common usage, 'global warming' often refers to the warming that can occur as a result of increased emissions of greenhouse gases from human activities.”
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| − | 6. ^ United Nations Framework Convention on Climate Change, Article I. United Nations Framework Convention on Climate Change. Retrieved on 2007-01-15.
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| − | 7. ^ Berger, A.; et al. (2005-12-10). "On the origin of the 100-kyr cycles in the astronomical forcing". Paleoceanography 20 (4). PA4019. Retrieved on 2007-11-05.
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| − | 8. ^ Genthon, C.; et al. (1987-10-01). "Vostok Ice Core - Climatic response to CO2 and orbital forcing changes over the last climatic cycle". Nature 329 (6138): 414–418. Retrieved on 2007-11-05.
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| − | 9. ^ Alley, Richard B.; et al. (January 2002). "A northern lead in the orbital band: north-south phasing of Ice-Age events". Quaternary Science Reviews 21 (1-3): 431–441. Retrieved on 2007-11-05.
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| − | 10. ^ Joint science academies' statement: The science of climate change (ASP). Royal Society (2001-05-17). Retrieved on 2007-04-01. “The work of the Intergovernmental Panel on Climate Change (IPCC) represents the consensus of the international scientific community on climate change science”
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| − | 11. ^ (2007-10-18) "Rising to the climate challenge". Nature 449 (7164). Retrieved on 2007-11-06.
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| − | 12. ^ Svensmark, Henrik (February 2007). "Cosmoclimatology: a new theory emerges". Astronomy & Geophysics 48 (1): 18-24. doi:10.1111/j.1468-4004.2007.48118.x.
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| − | 13. ^ Forster, Piers; et al. (2007-02-05). Changes in Atmospheric Constituents and in Radiative Forcing (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 188-193. Intergovernmental Panel on Climate Change. Retrieved on 2007-09-17.
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| − | 14. ^ Bard, Edouard; Frank, Martin (2006-06-09). "Climate change and solar variability: What's new under the sun?". Earth and Planetary Science Letters 248 (1-2): 1-14. Retrieved on 2007-09-17.
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| − | 15. ^ Meehl, Gerald A.; et al. (2005-03-18). "How Much More Global Warming and Sea Level Rise" (PDF). Science 307 (5716): 1769–1772. doi:10.1126/science.1106663. Retrieved on 2007-02-11.
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| |
| − | 17. ^ Note that the Greenhouse Effect produces a temperature increase of about 33 °C (59 °F) with respect to black body predictions and not a surface temperature of 33 °C (91 °F) which is 32 °F higher. The average surface temperature is about 14 °C (57 °F). Also note that both the Celsius and Fahrenheit temperatures are expressed to 2 significant figures even though the conversion formula produces 3.
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| − | | |
| − | Global warming is the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.
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| − | | |
| − | The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 year period ending in 2005, which is higher than the earlier estimate of 0.6 ± 0.2 °C for the period ending in 2000.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations"[1] via the greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3] These basic conclusions have been endorsed by at least 30 scientific societies and academies of science, including all of the national academies of science of the major industrialized countries. While individual scientists have voiced disagreement with the conclusions of the IPCC, the overwhelming majority of scientists working on climate change are in agreement with the conclusions.[4]
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| − | | |
| − | Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[1] The range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a millennium even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]
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| − | | |
| − | Increasing global temperature will cause sea level to rise, and is expected to increase the intensity of extreme weather events and to change the amount and pattern of precipitation. Other effects of global warming include changes in agricultural yields, trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.
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| − | | |
| − | Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. There is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences. Most national governments have signed and ratified the Kyoto Protocol, aimed at reducing greenhouse gas emissions.
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| − | Contents
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| − | [hide]
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| − | | |
| − | * 1 Terminology
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| − | * 2 Causes
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| − | o 2.1 Greenhouse gases in the atmosphere
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| − | o 2.2 Feedbacks
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| − | o 2.3 Solar variation
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| − | * 3 Temperature changes
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| − | o 3.1 Recent
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| − | o 3.2 Pre-human climate variations
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| − | * 4 Climate models
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| − | * 5 Attributed and expected effects
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| − | o 5.1 Economic
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| − | o 5.2 Security
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| − | * 6 Adaptation and mitigation
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| − | * 7 Social and political debate
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| − | * 8 Related climatic issues
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| − | * 9 See also
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| − | * 10 References
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| − | * 11 Further reading
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| − | * 12 External links
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| − | | |
| − | Terminology
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| − | | |
| − | The term "global warming" is a specific example of the broader term climate change, which can also refer to global cooling. In common usage, the term refers to recent warming and implies a human influence.[5] The United Nations Framework Convention on Climate Change (UNFCCC) uses the term "climate change" for human-caused change, and "climate variability" for other changes.[6] The term "anthropogenic global warming" is sometimes used when focusing on human-induced changes.
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| − | | |
| − | Causes
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | | |
| − | Main articles: Attribution of recent climate change and scientific opinion on climate change
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| − | | |
| − | The Earth's climate changes in response to external forcing, including variations in its orbit around the sun (orbital forcing),[7][8][9] volcanic eruptions, and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[10][11] identifies elevated levels of greenhouse gases due to human activity as the main influence. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain the observed increase in mean global temperature. One such hypothesis proposes that warming may be the result of variations in solar activity.[12][13][14]
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| − | | |
| − | None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[15]
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| − | | |
| − | Greenhouse gases in the atmosphere
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| − | | |
| − | Main article: Greenhouse effect
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| − | | |
| − | The greenhouse effect was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. It is the process by which absorption and emission of infrared radiation by atmospheric gases warm a planet's atmosphere and surface.
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| − | | |
| − | Existence of the greenhouse effect as such is not disputed. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F), without which Earth would be uninhabitable.[16][17] Rather, the issue is how the strength of the greenhouse effect is changed when human activity increases the atmospheric concentrations of some greenhouse gases.
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| − | | |
| − | On Earth, the major greenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect (not including clouds); carbon dioxide (CO2), which causes 9–26%; methane (CH4), which causes 4–9%; and ozone, which causes 3–7%.[18][19] Some other naturally occurring gases contribute very small fractions of the greenhouse effect; one of these, nitrous oxide (N2O), is increasing in concentration owing to human activity such as agriculture. The atmospheric concentrations of CO2 and CH4 have increased by 31% and 149% respectively above pre-industrial levels since 1750. Molecule for molecule, methane is a more effective greenhouse gas than carbon dioxide, but its concentration is much smaller so that its total radiative forcing is only about a fourth of that from carbon dioxide. These levels are considerably higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores. From less direct geological evidence it is believed that CO2 values this high were last attained 20 million years ago.[20] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, in particular deforestation.[21]
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| − | | |
| − | The present atmospheric concentration of CO2 is about 383 parts per million (ppm) by volume.[22] Future CO2 levels are expected to rise due to ongoing burning of fossil fuels and land-use change. The rate of rise will depend on uncertain economic, sociological, technological, and natural developments, but may be ultimately limited by the availability of fossil fuels. The IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[23] Fossil fuel reserves are sufficient to reach this level and continue emissions past 2100, if coal, tar sands or methane clathrates are extensively used.[24]
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| − | | |
| − | Feedbacks
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| − | | |
| − | Main article: Effects of global warming#Further global warming (positive feedback)
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| − | | |
| − | The effects of forcing agents on the climate are complicated by various feedback processes.
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| − | | |
| − | One of the most pronounced feedback effects relates to the evaporation of water. In the case of warming by the addition of long-lived greenhouse gases such as CO2, the initial warming will cause more water to be evaporated into the atmosphere. Since water vapor itself acts as a greenhouse gas, this causes still more warming; the warming causes more water vapor to be evaporated, and so forth until a new dynamic equilibrium concentration of water vapor is reached with a much larger greenhouse effect than that due to CO2 alone. Although this feedback process involves an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[25] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.
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| − | | |
| − | Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models. Nevertheless, cloud feedback is second only to water vapor feedback and is positive in all the models that were used in the IPCC Fourth Assessment Report.[25]
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| − | | |
| − | Another important feedback process is ice-albedo feedback.[26] When global temperatures increase, ice near the poles melts at an increasing rate. As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.
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| − | | |
| − | Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism contributing to warming.[27] A massive release of CH4 from methane clathrates could cause rapid warming, according to the clathrate gun hypothesis.
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| − | | |
| − | The ocean's ability to sequester carbon is expected to decline as it warms, because the resulting low nutrient levels of the mesopelagic zone limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[28]
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| − | | |
| − | Solar variation
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| − | Solar variation over the last 30 years.
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| − | Solar variation over the last 30 years.
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| − | | |
| − | Main article: Solar variation
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| − | A few papers suggest that the Sun's contribution may have been underestimated. Two researchers at Duke University, Bruce West and Nicola Scafetta, have estimated that the Sun may have contributed about 45–50% of the increase in the average global surface temperature over the period 1900–2000, and about 25–35% between 1980 and 2000.[29] A paper by Peter Stott and other researchers suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.[30] They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases.
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| − | A different hypothesis is that variations in solar output, possibly amplified by cloud seeding via galactic cosmic rays, may have contributed to recent warming.[31] It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.[32]
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| − | One predicted effect of an increase in solar activity would be a warming of the stratosphere; however, the observed effect since at least 1960 has been a cooling of the lower stratosphere, which is one of the predicted results of greenhouse gas warming.[33] Reduction of stratospheric ozone also has a cooling influence, although substantial ozone depletion did not occur until the late 1970s. Solar variation combined with changes in volcanic activity probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.[1] In 2006, Peter Foukal and other researchers from the United States, Germany, and Switzerland found no net increase of solar brightness over the last thousand years. Solar cycles led to a small increase of 0.07% in brightness over the last 30 years. This effect is far too small to contribute significantly to global warming.[34][35] A paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in cosmic rays.[36] Henrik Svensmark and Eigil Friis-Christensen, the main proponents of cloud seeding by galactic cosmic rays, disputed the findings of Lockwood and Fröhlich.[37] Another recent study speculates that other bodies within the Solar System may influence the climate in a complex manner.[38]
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| − | Temperature changes
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | | |
| − | Main article: Temperature record
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| − | | |
| − | Recent
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| − | Global temperatures on both land and sea have increased by 0.75 °C (1.35 °F) relative to the period 1860–1900, according to the instrumental temperature record. This measured temperature increase is not significantly affected by the urban heat island effect.[39] Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[40] Temperatures in the lower troposphere have increased between 0.12 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with possibly regional fluctuations such as the Medieval Warm Period or the Little Ice Age.
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| − | Sea temperatures increase more slowly than those on land both because of the larger effective heat capacity of the oceans and because the ocean can lose heat by evaporation more readily than the land.[41] Since the Northern Hemisphere has more land mass than the Southern Hemisphere it warms faster; also there are extensive areas of seasonal snow cover subject to the snow-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the asymmetry of warming as the major gases are essentially well-mixed between hemispheres.
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| − | Based on estimates by NASA's Goddard Institute for Space Studies, 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[42] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit concluded that 2005 was the second warmest year, behind 1998.[43][44]
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| − | Anthropogenic emissions of other pollutants—notably sulfate aerosols—can exert a cooling effect by increasing the reflection of incoming sunlight. This partially accounts for the cooling seen in the temperature record in the middle of the twentieth century,[45] though the cooling may also be due in part to natural variability. James Hansen and colleagues have proposed that the effects of the products of fossil fuel combustion—CO2 and aerosols—have largely offset one another, so that warming in recent decades has been driven mainly by non-CO2 greenhouse gases.[46]
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| − | Paleoclimatologist William Ruddiman has argued that human influence on the global climate began around 8,000 years ago with the start of forest clearing to provide land for agriculture and 5,000 years ago with the start of Asian rice irrigation.[47] Ruddiman's interpretation of the historical record, with respect to the methane data, has been disputed.[48]
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| − | | |
| − | Pre-human climate variations
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | | |
| − | Further information: Paleoclimatology
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| − | See also: Snowball Earth
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| − | | |
| − | Earth has experienced warming and cooling many times in the past. The recent Antarctic EPICA ice core spans 800,000 years, including eight glacial cycles timed by orbital variations with interglacial warm periods comparable to present temperatures.[49]
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| − | | |
| − | A rapid buildup of greenhouse gases caused warming in the early Jurassic period (about 180 million years ago), with average temperatures rising by 5 °C (9 °F). Research by the Open University indicates that the warming caused the rate of rock weathering to increase by 400%. As such weathering locks away carbon in calcite and dolomite, CO2 levels dropped back to normal over roughly the next 150,000 years.[50][51]
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| − | Sudden releases of methane from clathrate compounds (the clathrate gun hypothesis) have been hypothesized as a cause for other warming events in the distant past, including the Permian-Triassic extinction event (about 251 million years ago) and the Paleocene-Eocene Thermal Maximum (about 55 million years ago).
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| − | Climate models
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | | |
| − | Main article: Global climate model
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| − | | |
| − | Scientists have studied global warming with computer models of the climate. These models are based on physical principles of fluid dynamics, radiative transfer, and other processes, with simplifications being necessary because of limitations in computer power and the complexity of the underlying system (climate). These models predict that the effect of adding greenhouse gases is to produce a warmer climate.[52] However, even when the same assumptions of future greenhouse gas levels are used, there still remains a considerable range of climate sensitivity.
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| − | Including uncertainties in future greenhouse gas concentrations and climate modeling, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999.[1] Models have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes.
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| − | Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.[53] These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.
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| − | Most global climate models, when run to project future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.[54][55][56]
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| − | The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem.[57] There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability.
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| − | | |
| − | Attributed and expected effects
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| − | | |
| − | Main article: Effects of global warming
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| − | | |
| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Although it is difficult to connect specific weather events to global warming, an increase in global temperatures may in turn cause broader changes, including glacial retreat, Arctic shrinkage, and worldwide sea level rise. Changes in the amount and pattern of precipitation may result in flooding and drought. There may also be changes in the frequency and intensity of extreme weather events. Other effects may include changes in agricultural yields, addition of new trade routes,[58] reduced summer streamflows, species extinctions, and increases in the range of disease vectors.
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| − | | |
| − | Some effects on both the natural environment and human life are, at least in part, already being attributed to global warming. A 2001 report by the IPCC suggests that glacier retreat, ice shelf disruption such as that of the Larsen Ice Shelf, sea level rise, changes in rainfall patterns, and increased intensity and frequency of extreme weather events, are being attributed in part to global warming.[59] While changes are expected for overall patterns, intensity, and frequencies, it is difficult to attribute specific events to global warming. Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.[60]
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| − | Increasing deaths, displacements, and economic losses projected due to extreme weather attributed to global warming may be exacerbated by growing population densities in affected areas, although temperate regions are projected to experience some minor benefits, such as fewer deaths due to cold exposure.[61] A summary of probable effects and recent understanding can be found in the report made for the IPCC Third Assessment Report by Working Group II.[59] The newer IPCC Fourth Assessment Report summary reports that there is observational evidence for an increase in intense tropical cyclone activity in the North Atlantic Ocean since about 1970, in correlation with the increase in sea surface temperature, but that the detection of long-term trends is complicated by the quality of records prior to routine satellite observations. The summary also states that there is no clear trend in the annual worldwide number of tropical cyclones.[1]
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| − | | |
| − | Additional anticipated effects include sea level rise of 110 to 770 millimeters (0.36 to 2.5 ft) between 1990 and 2100,[62] repercussions to agriculture, possible slowing of the thermohaline circulation, reductions in the ozone layer, increased intensity of hurricanes and extreme weather events, lowering of ocean pH, and the spread of diseases such as malaria and dengue fever. One study predicts 18% to 35% of a sample of 1,103 animal and plant species would be extinct by 2050, based on future climate projections.[63] However, few mechanistic studies have documented extinctions due to recent climate change[64] and one study suggests that projected rates of extinction are uncertain.[65]
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| − | | |
| − | Economic
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | | |
| − | Main articles: Economics of global warming and Low-carbon economy
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| − | | |
| − | Some economists have tried to estimate the aggregate net economic costs of damages from climate change across the globe. Such estimates have so far failed to reach conclusive findings; in a survey of 100 estimates, the values ran from US$-10 per tonne of carbon (tC) (US$-3 per tonne of carbon dioxide) up to US$350/tC (US$95 per tonne of carbon dioxide), with a mean of US$43 per tonne of carbon (US$12 per tonne of carbon dioxide).[61] One widely publicized report on potential economic impact is the Stern Review; it suggests that extreme weather might reduce global gross domestic product by up to 1%, and that in a worst-case scenario global per capita consumption could fall 20%.[66] The report's methodology, advocacy and conclusions have been criticized by many economists, primarily around the Review's assumptions of discounting and its choices of scenarios,[67] while others have supported the general attempt to quantify economic risk, even if not the specific numbers.[68][69]
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| − | | |
| − | In a summary of economic cost associated with climate change, the United Nations Environment Programme emphasizes the risks to insurers, reinsurers, and banks of increasingly traumatic and costly weather events. Other economic sectors likely to face difficulties related to climate change include agriculture and transport. Developing countries, rather than the developed world, are at greatest economic risk.[70]
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| − | Security
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| − | In November 2007, the Center for Strategic and International Studies and the Center for a New American Security published a report highlighting the national security effects of climate change.[71] These security effects include increased competition for resources between countries, mass migration from the worst affected areas, challenges to the cohesion of major states threatened by the rise in sea levels, and, as a consequence of these factors, an increased risk of armed conflict, including even nuclear conflicts.
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| − | Adaptation and mitigation
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| − | | |
| − | Main articles: Adaptation to global warming, Mitigation of global warming, and Kyoto Protocol
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| − | | |
| − | The broad agreement among climate scientists that global temperatures will continue to increase has led some nations, states, corporations and individuals to implement actions to try to curtail global warming or adjust to it. Many environmental groups encourage action against global warming, often by the consumer, but also by community and regional organizations. Others have suggested a quota on worldwide fossil fuel production, citing a direct link between fossil fuel production and CO2 emissions.[72][73]
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| − | | |
| − | There has also been business action on climate change, including efforts at increased energy efficiency and limited moves towards use of alternative fuels. One important innovation has been the development of greenhouse gas emissions trading through which companies, in conjunction with government, agree to cap their emissions or to purchase credits from those below their allowances.
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| − | | |
| − | The world's primary international agreement on combating global warming is the Kyoto Protocol, an amendment to the United Nations Framework Convention on Climate Change (UNFCCC) negotiated in 1997. The Protocol now covers more than 160 countries globally and over 55% of global greenhouse gas emissions.[74] Only the United States and Kazakhstan have not ratified the treaty, with the United States historically being the world's largest emitter of greenhouse gas. This treaty expires in 2012, and international talks began in May 2007 on a future treaty to succeed the current one.[75]
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| − | Claiming "serious harm" to the United States economy and the exemption of "80 percent of the world, including major population centers" like China and India, from the treaty, George W. Bush contends that the Kyoto Protocol is an unfair and ineffective means of addressing global climate change concerns.[76] Still, various state, local, and regional governments within the United States have begun their own initiatives to indicate support and compliance with the Kyoto Protocol on a local basis. For example, the Regional Greenhouse Gas Initiative is a state-level emissions capping and trading program involving eight Northeastern U.S. states, which was founded on December 20, 2005.[77]
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| − | China and India, though exempt from its provisions as developing countries, have ratified the Kyoto Protocol. China may have passed the U.S. in total annual greenhouse gas emissions according to some recent studies. Chinese Premier Wen Jiabao has called on the nation to redouble its efforts to tackle pollution and global warming.[78]
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| − | | |
| − | The IPCC's Working Group III is responsible for crafting reports that deal with the mitigation of global warming and analyzing the costs and benefits of different approaches. In the 2007 IPCC Fourth Assessment Report, they conclude that no one technology or sector can be completely responsible for mitigating future warming. They find there are key practices and technologies in various sectors, such as energy supply, transportation, industry, and agriculture, that should be implemented to reduced global emissions. They estimate that stabilization of carbon dioxide equivalent between 445 and 710 ppm by 2030 will result in between a 0.6% increase and 3% decrease in global gross domestic product.[79]
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| − | | |
| − | Social and political debate
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| − | | |
| − | Main articles: Global warming controversy, Politics of global warming, and Economics of global warming
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| − | See also: Climate change denial
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | | |
| − | Over the past several years, public perceptions and attitudes concerning the causes and importance of global warming have changed.[80] Increased awareness of the scientific findings surrounding global warming has resulted in political and economic debate. Poor regions, particularly Africa, appear at greatest risk from the suggested effects of global warming, while their actual emissions have been small compared to the developed world.[81] At the same time, developing country exemptions from provisions of the Kyoto Protocol have been criticized by the United States and Australia, and have been used as part of the rationale for continued non-ratification by the U.S.[82] In the Western world, the idea of human influence on climate has gained wider acceptance in Europe than in the United States.[83][84]
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| − | The issue of climate change has sparked debate weighing the benefits of limiting industrial emissions of greenhouse gases against the costs that such changes would entail. There has been discussion in several countries about the cost and benefits of adopting alternative energy sources in order to reduce carbon emissions.[85] Organizations and companies such as the Competitive Enterprise Institute and ExxonMobil have emphasized more conservative climate change scenarios while highlighting the potential economic cost of stricter controls.[86][87][88][89] Likewise, various environmental lobbies and a number of public figures have launched campaigns to emphasize the potential risks of climate change and promote the implementation of stricter controls. Some fossil fuel companies have scaled back their efforts in recent years,[90] or called for policies to reduce global warming.[91]
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| − | Another point of debate is the degree to which newly developed economies such as India and China should be expected to constrain their emissions. China's gross national CO2 emissions are expected to exceed those of the U.S. within the next few years, and may have already done so according to a 2006 report.[92] China has contended that it has less of an obligation to reduce emissions since its per capita emissions are roughly one-fifth that of the United States.[93] India, also exempt from Kyoto restrictions and another of the biggest sources of industrial emissions, has made similar assertions.[94] However, the U.S. contends that if they must bear the cost of reducing emissions, then China should do the same.[95]
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| − | Related climatic issues
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| − | | |
| − | Main articles: Ocean acidification, global dimming, and ozone depletion
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| − | | |
| − | A variety of issues are often raised in relation to global warming. One is ocean acidification. Increased atmospheric CO2 increases the amount of CO2 dissolved in the oceans.[96] CO2 dissolved in the ocean reacts with water to form carbonic acid, resulting in acidification. Ocean surface pH is estimated to have decreased from 8.25 near the beginning of the industrial era to 8.14 by 2004,[97] and is projected to decrease by a further 0.14 to 0.5 units by 2100 as the ocean absorbs more CO2.[1][98] Since organisms and ecosystems are adapted to a narrow range of pH, this raises extinction concerns, directly driven by increased atmospheric CO2, that could disrupt food webs and impact human societies that depend on marine ecosystem services.[99]
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| − | | |
| − | Global dimming, the gradual reduction in the amount of global direct irradiance at the Earth's surface, may have partially mitigated global warming in the late twentieth century. From 1960 to 1990 human-caused aerosols likely precipitated this effect. Scientists have stated with 66–90% confidence that the effects of human-caused aerosols, along with volcanic activity, have offset some of the global warming, and that greenhouse gases would have resulted in more warming than observed if not for these dimming agents.[1]
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| − | Ozone depletion, the steady decline in the total amount of ozone in Earth's stratosphere, is frequently cited in relation to global warming. Although there are areas of linkage, the relationship between the two is not strong.
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| − | See also
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| − | | |
| − | * Glossary of climate change
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| − | | |
| − | References
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| − | | |
| − | 1. ^ a b c d e f g h i Summary for Policymakers (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change (2007-02-05). Retrieved on 2007-02-02. “The updated 100-year linear trend (1906 to 2005) of 0.74°C [0.56°C to 0.92°C] is therefore larger than the corresponding trend for 1901 to 2000 given in the TAR of 0.6°C [0.4°C to 0.8°C].”
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| − | 2. ^ Hegerl, Gabriele C.; et al. (2007-05-07). Understanding and Attributing Climate Change (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 690. Intergovernmental Panel on Climate Change. Retrieved on 2007-05-20. “Recent estimates (Figure 9.9) indicate a relatively small combined effect of natural forcings on the global mean temperature evolution of the seconds half of the 20th century, with a small net cooling from the combined effects of solar and volcanic forcings”
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| − | 3. ^ Ammann, Caspar; et al. (2007-04-06). "Solar influence on climate during the past millennium: Results from ransient simulations with the NCAR Climate Simulation Model" (PDF). Proceedings of the National Academy of Sciences of the United States of America 104 (10): 3713–3718. “However, because of a lack of interactive ozone, the model cannot fully simulate features discussed in (44)." "While the NH temperatures of the high-scaled experiment are often colder than the lower bound from proxy data, the modeled decadal-scale NH surface temperature for the medium-scaled case falls within the uncertainty range of the available temperature reconstructions. The medium-scaled simulation also broadly reproduces the main features seen in the proxy records." "Without anthropogenic forcing, the 20th century warming is small. The simulations with only natural forcing components included yield an early 20th century peak warming of ≈0.2 °C (≈1950 AD), which is reduced to about half by the end of the century because of increased volcanism.”
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| − | 4. ^ A guide to facts and fictions about climate change. Royal Society (March 2005). Retrieved on 2007-11-18. “"However, the overwhelming majority of scientists who work on climate change agree on the main points"”
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| − | 5. ^ Climate Change: Basic Information. United States Environmental Protection Agency (2006-12-14). Retrieved on 2007-02-09. “In common usage, 'global warming' often refers to the warming that can occur as a result of increased emissions of greenhouse gases from human activities.”
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| − | 6. ^ United Nations Framework Convention on Climate Change, Article I. United Nations Framework Convention on Climate Change. Retrieved on 2007-01-15.
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| − | 7. ^ Berger, A.; et al. (2005-12-10). "On the origin of the 100-kyr cycles in the astronomical forcing". Paleoceanography 20 (4). PA4019. Retrieved on 2007-11-05.
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| − | 8. ^ Genthon, C.; et al. (1987-10-01). "Vostok Ice Core - Climatic response to CO2 and orbital forcing changes over the last climatic cycle". Nature 329 (6138): 414–418. Retrieved on 2007-11-05.
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| − | 9. ^ Alley, Richard B.; et al. (January 2002). "A northern lead in the orbital band: north-south phasing of Ice-Age events". Quaternary Science Reviews 21 (1-3): 431–441. Retrieved on 2007-11-05.
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| − | 10. ^ Joint science academies' statement: The science of climate change (ASP). Royal Society (2001-05-17). Retrieved on 2007-04-01. “The work of the Intergovernmental Panel on Climate Change (IPCC) represents the consensus of the international scientific community on climate change science”
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| − | 11. ^ (2007-10-18) "Rising to the climate challenge". Nature 449 (7164). Retrieved on 2007-11-06.
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| − | 12. ^ Svensmark, Henrik (February 2007). "Cosmoclimatology: a new theory emerges". Astronomy & Geophysics 48 (1): 18-24. doi:10.1111/j.1468-4004.2007.48118.x.
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| − | 13. ^ Forster, Piers; et al. (2007-02-05). Changes in Atmospheric Constituents and in Radiative Forcing (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 188-193. Intergovernmental Panel on Climate Change. Retrieved on 2007-09-17.
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| − | 14. ^ Bard, Edouard; Frank, Martin (2006-06-09). "Climate change and solar variability: What's new under the sun?". Earth and Planetary Science Letters 248 (1-2): 1-14. Retrieved on 2007-09-17.
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| − | 15. ^ Meehl, Gerald A.; et al. (2005-03-18). "How Much More Global Warming and Sea Level Rise" (PDF). Science 307 (5716): 1769–1772. doi:10.1126/science.1106663. Retrieved on 2007-02-11.
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| − | 16. ^ IPCC WG1 AR4 Report — Chapter 1: Historical Overview of Climate Change Science (PDF). IPCC WG1 AR4 Report p97 (pdf page 5 of 36). IPCC (2007). Retrieved on 2007-10-07. “To emit 240 W m–2, a surface would have to have a temperature of around –19 °C. This is much colder than the conditions that actually exist at the Earth’s surface (the global mean surface temperature is about 14 °C). Instead, the necessary –19 °C is found at an altitude about 5 km above the surface.”
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| − | 17. ^ Note that the Greenhouse Effect produces a temperature increase of about 33 °C (59 °F) with respect to black body predictions and not a surface temperature of 33 °C (91 °F) which is 32 °F higher. The average surface temperature is about 14 °C (57 °F). Also note that both the Celsius and Fahrenheit temperatures are expressed to 2 significant figures even though the conversion formula produces 3.
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| − | 18. ^ Kiehl, J. T.; Kevin E. Trenberth (February 1997). "Earth’s Annual Global Mean Energy Budget" (PDF). Bulletin of the American Meteorological Society 78 (2): 197-208. Retrieved on 2006-05-01.
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| − | 19. ^ Water vapour: feedback or forcing?. RealClimate (6 Apr 2005). Retrieved on 2006-05-01.
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| − | 20. ^ Pearson, Paul N.; Palmer, Martin R. (2000-08-17). "Atmospheric carbon dioxide concentrations over the past 60 million years". Nature 406 (6797): 695–699. doi:10.1038/35021000.
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| − | 22. ^ Tans, Pieter. Trends in Atmospheric Carbon Dioxide – Mauna Loa. National Oceanic and Atmospheric Administration. Retrieved on 2007-04-28.
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| − | 23. ^ Prentice, I. Colin; et al. (2001-01-20). 3.7.3.3 SRES scenarios and their implications for future CO2 concentration. Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change. Retrieved on 2007-04-28.
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| − | 24. ^ 4.4.6. Resource Availability. IPCC Special Report on Emissions Scenarios. Intergovernmental Panel on Climate Change. Retrieved on 2007-04-28.
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| − | 25. ^ a b Soden, Brian J.; Held, Isacc M. (2005-11-01). "An Assessment of Climate Feedbacks in Coupled Ocean–Atmosphere Models" (PDF). Journal of Climate 19 (14). Retrieved on 2007-04-21. “Interestingly, the true feedback is consistently weaker than the constant relative humidity value, implying a small but robust reduction in relative humidity in all models on average" "clouds appear to provide a positive feedback in all models”
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| − | 26. ^ Stocker, Thomas F.; et al. (2001-01-20). 7.5.2 Sea Ice. Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change. Retrieved on 2007-02-11.
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| − | 27. ^ Sample, Ian. "Warming Hits 'Tipping Point'", The Guardian, 2005-08-11. Retrieved on 2007-01-18.
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| − | 28. ^ Buesseler, Ken O.; et al. (2007-04-27). "Revisiting Carbon Flux Through the Ocean's Twilight Zone". Science 316 (5824): 567–570. Retrieved on 2007-11-16.
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| − | 29. ^ Scafetta, Nicola; West, Bruce J. (2006-03-09). "Phenomenological solar contribution to the 1900–2000 global surface warming" (PDF). Geophysical Research Letters 33 (5). doi:10.1029/2005GL025539. L05708. Retrieved on 2007-05-08.
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| − | 30. ^ Stott, Peter A.; et al. (2003-12-03). "Do Models Underestimate the Solar Contribution to Recent Climate Change?". Journal of Climate 16 (24): 4079–4093. doi:10.1175/1520-0442(2003)016%3C4079:DMUTSC%3E2.0.CO;2. Retrieved on 2007-04-16.
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| − | 64. ^ McLaughlin, John F.; et al. (2002-04-30). "Climate change hastens population extinctions" (PDF). PNAS 99 (9): 6070–6074. doi:10.1073/pnas.052131199. Retrieved on 2007-03-29.
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| − | 93. ^ China: US should take lead on climate, by Michael Casey, Associated Press, 12/7/07.
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| − | | |
| − | Global warming is the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.
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| − | | |
| − | The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 year period ending in 2005, which is higher than the earlier estimate of 0.6 ± 0.2 °C for the period ending in 2000.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations"[1] via the greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3] These basic conclusions have been endorsed by at least 30 scientific societies and academies of science, including all of the national academies of science of the major industrialized countries. While individual scientists have voiced disagreement with the conclusions of the IPCC, the overwhelming majority of scientists working on climate change are in agreement with the conclusions.[4]
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| − | | |
| − | Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[1] The range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a millennium even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]
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| − | | |
| − | Increasing global temperature will cause sea level to rise, and is expected to increase the intensity of extreme weather events and to change the amount and pattern of precipitation. Other effects of global warming include changes in agricultural yields, trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.
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| − | | |
| − | Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. There is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences. Most national governments have signed and ratified the Kyoto Protocol, aimed at reducing greenhouse gas emissions.
| |
| − | Contents
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| − | [hide]
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| − | | |
| − | * 1 Terminology
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| − | * 2 Causes
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| − | o 2.1 Greenhouse gases in the atmosphere
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| − | o 2.2 Feedbacks
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| − | o 2.3 Solar variation
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| − | * 3 Temperature changes
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| − | o 3.1 Recent
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| − | o 3.2 Pre-human climate variations
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| − | * 4 Climate models
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| − | * 5 Attributed and expected effects
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| − | o 5.1 Economic
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| − | o 5.2 Security
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| − | * 6 Adaptation and mitigation
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| − | * 7 Social and political debate
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| − | * 8 Related climatic issues
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| − | * 9 See also
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| − | * 10 References
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| − | * 11 Further reading
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| − | * 12 External links
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| − | | |
| − | Terminology
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| − | | |
| − | The term "global warming" is a specific example of the broader term climate change, which can also refer to global cooling. In common usage, the term refers to recent warming and implies a human influence.[5] The United Nations Framework Convention on Climate Change (UNFCCC) uses the term "climate change" for human-caused change, and "climate variability" for other changes.[6] The term "anthropogenic global warming" is sometimes used when focusing on human-induced changes.
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| − | | |
| − | Causes
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | | |
| − | Main articles: Attribution of recent climate change and scientific opinion on climate change
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| − | | |
| − | The Earth's climate changes in response to external forcing, including variations in its orbit around the sun (orbital forcing),[7][8][9] volcanic eruptions, and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[10][11] identifies elevated levels of greenhouse gases due to human activity as the main influence. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain the observed increase in mean global temperature. One such hypothesis proposes that warming may be the result of variations in solar activity.[12][13][14]
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| − | | |
| − | None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[15]
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| − | | |
| − | Greenhouse gases in the atmosphere
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| − | | |
| − | Main article: Greenhouse effect
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| − | | |
| − | The greenhouse effect was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. It is the process by which absorption and emission of infrared radiation by atmospheric gases warm a planet's atmosphere and surface.
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| − | | |
| − | Existence of the greenhouse effect as such is not disputed. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F), without which Earth would be uninhabitable.[16][17] Rather, the issue is how the strength of the greenhouse effect is changed when human activity increases the atmospheric concentrations of some greenhouse gases.
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| − | | |
| − | On Earth, the major greenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect (not including clouds); carbon dioxide (CO2), which causes 9–26%; methane (CH4), which causes 4–9%; and ozone, which causes 3–7%.[18][19] Some other naturally occurring gases contribute very small fractions of the greenhouse effect; one of these, nitrous oxide (N2O), is increasing in concentration owing to human activity such as agriculture. The atmospheric concentrations of CO2 and CH4 have increased by 31% and 149% respectively above pre-industrial levels since 1750. Molecule for molecule, methane is a more effective greenhouse gas than carbon dioxide, but its concentration is much smaller so that its total radiative forcing is only about a fourth of that from carbon dioxide. These levels are considerably higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores. From less direct geological evidence it is believed that CO2 values this high were last attained 20 million years ago.[20] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, in particular deforestation.[21]
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| − | | |
| − | The present atmospheric concentration of CO2 is about 383 parts per million (ppm) by volume.[22] Future CO2 levels are expected to rise due to ongoing burning of fossil fuels and land-use change. The rate of rise will depend on uncertain economic, sociological, technological, and natural developments, but may be ultimately limited by the availability of fossil fuels. The IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[23] Fossil fuel reserves are sufficient to reach this level and continue emissions past 2100, if coal, tar sands or methane clathrates are extensively used.[24]
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| − | | |
| − | Feedbacks
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| − | | |
| − | Main article: Effects of global warming#Further global warming (positive feedback)
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| − | | |
| − | The effects of forcing agents on the climate are complicated by various feedback processes.
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| − | | |
| − | One of the most pronounced feedback effects relates to the evaporation of water. In the case of warming by the addition of long-lived greenhouse gases such as CO2, the initial warming will cause more water to be evaporated into the atmosphere. Since water vapor itself acts as a greenhouse gas, this causes still more warming; the warming causes more water vapor to be evaporated, and so forth until a new dynamic equilibrium concentration of water vapor is reached with a much larger greenhouse effect than that due to CO2 alone. Although this feedback process involves an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[25] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.
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| − | | |
| − | Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models. Nevertheless, cloud feedback is second only to water vapor feedback and is positive in all the models that were used in the IPCC Fourth Assessment Report.[25]
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| − | | |
| − | Another important feedback process is ice-albedo feedback.[26] When global temperatures increase, ice near the poles melts at an increasing rate. As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.
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| − | | |
| − | Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism contributing to warming.[27] A massive release of CH4 from methane clathrates could cause rapid warming, according to the clathrate gun hypothesis.
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| − | | |
| − | The ocean's ability to sequester carbon is expected to decline as it warms, because the resulting low nutrient levels of the mesopelagic zone limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[28]
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| − | | |
| − | Solar variation
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| − | Solar variation over the last 30 years.
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| − | Solar variation over the last 30 years.
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| − | | |
| − | Main article: Solar variation
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| − | | |
| − | A few papers suggest that the Sun's contribution may have been underestimated. Two researchers at Duke University, Bruce West and Nicola Scafetta, have estimated that the Sun may have contributed about 45–50% of the increase in the average global surface temperature over the period 1900–2000, and about 25–35% between 1980 and 2000.[29] A paper by Peter Stott and other researchers suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.[30] They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases.
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| − | | |
| − | A different hypothesis is that variations in solar output, possibly amplified by cloud seeding via galactic cosmic rays, may have contributed to recent warming.[31] It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.[32]
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| − | | |
| − | One predicted effect of an increase in solar activity would be a warming of the stratosphere; however, the observed effect since at least 1960 has been a cooling of the lower stratosphere, which is one of the predicted results of greenhouse gas warming.[33] Reduction of stratospheric ozone also has a cooling influence, although substantial ozone depletion did not occur until the late 1970s. Solar variation combined with changes in volcanic activity probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.[1] In 2006, Peter Foukal and other researchers from the United States, Germany, and Switzerland found no net increase of solar brightness over the last thousand years. Solar cycles led to a small increase of 0.07% in brightness over the last 30 years. This effect is far too small to contribute significantly to global warming.[34][35] A paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in cosmic rays.[36] Henrik Svensmark and Eigil Friis-Christensen, the main proponents of cloud seeding by galactic cosmic rays, disputed the findings of Lockwood and Fröhlich.[37] Another recent study speculates that other bodies within the Solar System may influence the climate in a complex manner.[38]
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| − | | |
| − | Temperature changes
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | | |
| − | Main article: Temperature record
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| − | | |
| − | Recent
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| − | | |
| − | Global temperatures on both land and sea have increased by 0.75 °C (1.35 °F) relative to the period 1860–1900, according to the instrumental temperature record. This measured temperature increase is not significantly affected by the urban heat island effect.[39] Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[40] Temperatures in the lower troposphere have increased between 0.12 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with possibly regional fluctuations such as the Medieval Warm Period or the Little Ice Age.
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| − | | |
| − | Sea temperatures increase more slowly than those on land both because of the larger effective heat capacity of the oceans and because the ocean can lose heat by evaporation more readily than the land.[41] Since the Northern Hemisphere has more land mass than the Southern Hemisphere it warms faster; also there are extensive areas of seasonal snow cover subject to the snow-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the asymmetry of warming as the major gases are essentially well-mixed between hemispheres.
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| − | | |
| − | Based on estimates by NASA's Goddard Institute for Space Studies, 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[42] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit concluded that 2005 was the second warmest year, behind 1998.[43][44]
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| − | Anthropogenic emissions of other pollutants—notably sulfate aerosols—can exert a cooling effect by increasing the reflection of incoming sunlight. This partially accounts for the cooling seen in the temperature record in the middle of the twentieth century,[45] though the cooling may also be due in part to natural variability. James Hansen and colleagues have proposed that the effects of the products of fossil fuel combustion—CO2 and aerosols—have largely offset one another, so that warming in recent decades has been driven mainly by non-CO2 greenhouse gases.[46]
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| − | Paleoclimatologist William Ruddiman has argued that human influence on the global climate began around 8,000 years ago with the start of forest clearing to provide land for agriculture and 5,000 years ago with the start of Asian rice irrigation.[47] Ruddiman's interpretation of the historical record, with respect to the methane data, has been disputed.[48]
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| − | Pre-human climate variations
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Further information: Paleoclimatology
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| − | See also: Snowball Earth
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| − | Earth has experienced warming and cooling many times in the past. The recent Antarctic EPICA ice core spans 800,000 years, including eight glacial cycles timed by orbital variations with interglacial warm periods comparable to present temperatures.[49]
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| − | A rapid buildup of greenhouse gases caused warming in the early Jurassic period (about 180 million years ago), with average temperatures rising by 5 °C (9 °F). Research by the Open University indicates that the warming caused the rate of rock weathering to increase by 400%. As such weathering locks away carbon in calcite and dolomite, CO2 levels dropped back to normal over roughly the next 150,000 years.[50][51]
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| − | Sudden releases of methane from clathrate compounds (the clathrate gun hypothesis) have been hypothesized as a cause for other warming events in the distant past, including the Permian-Triassic extinction event (about 251 million years ago) and the Paleocene-Eocene Thermal Maximum (about 55 million years ago).
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| − | Climate models
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | Main article: Global climate model
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| − | | |
| − | Scientists have studied global warming with computer models of the climate. These models are based on physical principles of fluid dynamics, radiative transfer, and other processes, with simplifications being necessary because of limitations in computer power and the complexity of the underlying system (climate). These models predict that the effect of adding greenhouse gases is to produce a warmer climate.[52] However, even when the same assumptions of future greenhouse gas levels are used, there still remains a considerable range of climate sensitivity.
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| − | Including uncertainties in future greenhouse gas concentrations and climate modeling, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999.[1] Models have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes.
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| − | Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.[53] These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.
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| − | Most global climate models, when run to project future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.[54][55][56]
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| − | The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem.[57] There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability.
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| − | | |
| − | Attributed and expected effects
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| − | | |
| − | Main article: Effects of global warming
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| − | | |
| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | | |
| − | Although it is difficult to connect specific weather events to global warming, an increase in global temperatures may in turn cause broader changes, including glacial retreat, Arctic shrinkage, and worldwide sea level rise. Changes in the amount and pattern of precipitation may result in flooding and drought. There may also be changes in the frequency and intensity of extreme weather events. Other effects may include changes in agricultural yields, addition of new trade routes,[58] reduced summer streamflows, species extinctions, and increases in the range of disease vectors.
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| − | | |
| − | Some effects on both the natural environment and human life are, at least in part, already being attributed to global warming. A 2001 report by the IPCC suggests that glacier retreat, ice shelf disruption such as that of the Larsen Ice Shelf, sea level rise, changes in rainfall patterns, and increased intensity and frequency of extreme weather events, are being attributed in part to global warming.[59] While changes are expected for overall patterns, intensity, and frequencies, it is difficult to attribute specific events to global warming. Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.[60]
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| − | Increasing deaths, displacements, and economic losses projected due to extreme weather attributed to global warming may be exacerbated by growing population densities in affected areas, although temperate regions are projected to experience some minor benefits, such as fewer deaths due to cold exposure.[61] A summary of probable effects and recent understanding can be found in the report made for the IPCC Third Assessment Report by Working Group II.[59] The newer IPCC Fourth Assessment Report summary reports that there is observational evidence for an increase in intense tropical cyclone activity in the North Atlantic Ocean since about 1970, in correlation with the increase in sea surface temperature, but that the detection of long-term trends is complicated by the quality of records prior to routine satellite observations. The summary also states that there is no clear trend in the annual worldwide number of tropical cyclones.[1]
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| − | | |
| − | Additional anticipated effects include sea level rise of 110 to 770 millimeters (0.36 to 2.5 ft) between 1990 and 2100,[62] repercussions to agriculture, possible slowing of the thermohaline circulation, reductions in the ozone layer, increased intensity of hurricanes and extreme weather events, lowering of ocean pH, and the spread of diseases such as malaria and dengue fever. One study predicts 18% to 35% of a sample of 1,103 animal and plant species would be extinct by 2050, based on future climate projections.[63] However, few mechanistic studies have documented extinctions due to recent climate change[64] and one study suggests that projected rates of extinction are uncertain.[65]
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| − | | |
| − | Economic
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | | |
| − | Main articles: Economics of global warming and Low-carbon economy
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| − | | |
| − | Some economists have tried to estimate the aggregate net economic costs of damages from climate change across the globe. Such estimates have so far failed to reach conclusive findings; in a survey of 100 estimates, the values ran from US$-10 per tonne of carbon (tC) (US$-3 per tonne of carbon dioxide) up to US$350/tC (US$95 per tonne of carbon dioxide), with a mean of US$43 per tonne of carbon (US$12 per tonne of carbon dioxide).[61] One widely publicized report on potential economic impact is the Stern Review; it suggests that extreme weather might reduce global gross domestic product by up to 1%, and that in a worst-case scenario global per capita consumption could fall 20%.[66] The report's methodology, advocacy and conclusions have been criticized by many economists, primarily around the Review's assumptions of discounting and its choices of scenarios,[67] while others have supported the general attempt to quantify economic risk, even if not the specific numbers.[68][69]
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| − | | |
| − | In a summary of economic cost associated with climate change, the United Nations Environment Programme emphasizes the risks to insurers, reinsurers, and banks of increasingly traumatic and costly weather events. Other economic sectors likely to face difficulties related to climate change include agriculture and transport. Developing countries, rather than the developed world, are at greatest economic risk.[70]
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| − | Security
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| − | In November 2007, the Center for Strategic and International Studies and the Center for a New American Security published a report highlighting the national security effects of climate change.[71] These security effects include increased competition for resources between countries, mass migration from the worst affected areas, challenges to the cohesion of major states threatened by the rise in sea levels, and, as a consequence of these factors, an increased risk of armed conflict, including even nuclear conflicts.
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| − | Adaptation and mitigation
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| − | | |
| − | Main articles: Adaptation to global warming, Mitigation of global warming, and Kyoto Protocol
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| − | | |
| − | The broad agreement among climate scientists that global temperatures will continue to increase has led some nations, states, corporations and individuals to implement actions to try to curtail global warming or adjust to it. Many environmental groups encourage action against global warming, often by the consumer, but also by community and regional organizations. Others have suggested a quota on worldwide fossil fuel production, citing a direct link between fossil fuel production and CO2 emissions.[72][73]
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| − | | |
| − | There has also been business action on climate change, including efforts at increased energy efficiency and limited moves towards use of alternative fuels. One important innovation has been the development of greenhouse gas emissions trading through which companies, in conjunction with government, agree to cap their emissions or to purchase credits from those below their allowances.
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| − | The world's primary international agreement on combating global warming is the Kyoto Protocol, an amendment to the United Nations Framework Convention on Climate Change (UNFCCC) negotiated in 1997. The Protocol now covers more than 160 countries globally and over 55% of global greenhouse gas emissions.[74] Only the United States and Kazakhstan have not ratified the treaty, with the United States historically being the world's largest emitter of greenhouse gas. This treaty expires in 2012, and international talks began in May 2007 on a future treaty to succeed the current one.[75]
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| − | Claiming "serious harm" to the United States economy and the exemption of "80 percent of the world, including major population centers" like China and India, from the treaty, George W. Bush contends that the Kyoto Protocol is an unfair and ineffective means of addressing global climate change concerns.[76] Still, various state, local, and regional governments within the United States have begun their own initiatives to indicate support and compliance with the Kyoto Protocol on a local basis. For example, the Regional Greenhouse Gas Initiative is a state-level emissions capping and trading program involving eight Northeastern U.S. states, which was founded on December 20, 2005.[77]
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| − | China and India, though exempt from its provisions as developing countries, have ratified the Kyoto Protocol. China may have passed the U.S. in total annual greenhouse gas emissions according to some recent studies. Chinese Premier Wen Jiabao has called on the nation to redouble its efforts to tackle pollution and global warming.[78]
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| − | | |
| − | The IPCC's Working Group III is responsible for crafting reports that deal with the mitigation of global warming and analyzing the costs and benefits of different approaches. In the 2007 IPCC Fourth Assessment Report, they conclude that no one technology or sector can be completely responsible for mitigating future warming. They find there are key practices and technologies in various sectors, such as energy supply, transportation, industry, and agriculture, that should be implemented to reduced global emissions. They estimate that stabilization of carbon dioxide equivalent between 445 and 710 ppm by 2030 will result in between a 0.6% increase and 3% decrease in global gross domestic product.[79]
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| − | Social and political debate
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| − | | |
| − | Main articles: Global warming controversy, Politics of global warming, and Economics of global warming
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| − | See also: Climate change denial
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | | |
| − | Over the past several years, public perceptions and attitudes concerning the causes and importance of global warming have changed.[80] Increased awareness of the scientific findings surrounding global warming has resulted in political and economic debate. Poor regions, particularly Africa, appear at greatest risk from the suggested effects of global warming, while their actual emissions have been small compared to the developed world.[81] At the same time, developing country exemptions from provisions of the Kyoto Protocol have been criticized by the United States and Australia, and have been used as part of the rationale for continued non-ratification by the U.S.[82] In the Western world, the idea of human influence on climate has gained wider acceptance in Europe than in the United States.[83][84]
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| − | The issue of climate change has sparked debate weighing the benefits of limiting industrial emissions of greenhouse gases against the costs that such changes would entail. There has been discussion in several countries about the cost and benefits of adopting alternative energy sources in order to reduce carbon emissions.[85] Organizations and companies such as the Competitive Enterprise Institute and ExxonMobil have emphasized more conservative climate change scenarios while highlighting the potential economic cost of stricter controls.[86][87][88][89] Likewise, various environmental lobbies and a number of public figures have launched campaigns to emphasize the potential risks of climate change and promote the implementation of stricter controls. Some fossil fuel companies have scaled back their efforts in recent years,[90] or called for policies to reduce global warming.[91]
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| − | Another point of debate is the degree to which newly developed economies such as India and China should be expected to constrain their emissions. China's gross national CO2 emissions are expected to exceed those of the U.S. within the next few years, and may have already done so according to a 2006 report.[92] China has contended that it has less of an obligation to reduce emissions since its per capita emissions are roughly one-fifth that of the United States.[93] India, also exempt from Kyoto restrictions and another of the biggest sources of industrial emissions, has made similar assertions.[94] However, the U.S. contends that if they must bear the cost of reducing emissions, then China should do the same.[95]
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| − | Related climatic issues
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| − | Main articles: Ocean acidification, global dimming, and ozone depletion
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| − | | |
| − | A variety of issues are often raised in relation to global warming. One is ocean acidification. Increased atmospheric CO2 increases the amount of CO2 dissolved in the oceans.[96] CO2 dissolved in the ocean reacts with water to form carbonic acid, resulting in acidification. Ocean surface pH is estimated to have decreased from 8.25 near the beginning of the industrial era to 8.14 by 2004,[97] and is projected to decrease by a further 0.14 to 0.5 units by 2100 as the ocean absorbs more CO2.[1][98] Since organisms and ecosystems are adapted to a narrow range of pH, this raises extinction concerns, directly driven by increased atmospheric CO2, that could disrupt food webs and impact human societies that depend on marine ecosystem services.[99]
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| − | Global dimming, the gradual reduction in the amount of global direct irradiance at the Earth's surface, may have partially mitigated global warming in the late twentieth century. From 1960 to 1990 human-caused aerosols likely precipitated this effect. Scientists have stated with 66–90% confidence that the effects of human-caused aerosols, along with volcanic activity, have offset some of the global warming, and that greenhouse gases would have resulted in more warming than observed if not for these dimming agents.[1]
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| − | Ozone depletion, the steady decline in the total amount of ozone in Earth's stratosphere, is frequently cited in relation to global warming. Although there are areas of linkage, the relationship between the two is not strong.
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| − | See also
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| − | | |
| − | * Glossary of climate change
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| − | | |
| − | References
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| − | | |
| − | 1. ^ a b c d e f g h i Summary for Policymakers (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change (2007-02-05). Retrieved on 2007-02-02. “The updated 100-year linear trend (1906 to 2005) of 0.74°C [0.56°C to 0.92°C] is therefore larger than the corresponding trend for 1901 to 2000 given in the TAR of 0.6°C [0.4°C to 0.8°C].”
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| − | 2. ^ Hegerl, Gabriele C.; et al. (2007-05-07). Understanding and Attributing Climate Change (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 690. Intergovernmental Panel on Climate Change. Retrieved on 2007-05-20. “Recent estimates (Figure 9.9) indicate a relatively small combined effect of natural forcings on the global mean temperature evolution of the seconds half of the 20th century, with a small net cooling from the combined effects of solar and volcanic forcings”
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| − | 3. ^ Ammann, Caspar; et al. (2007-04-06). "Solar influence on climate during the past millennium: Results from ransient simulations with the NCAR Climate Simulation Model" (PDF). Proceedings of the National Academy of Sciences of the United States of America 104 (10): 3713–3718. “However, because of a lack of interactive ozone, the model cannot fully simulate features discussed in (44)." "While the NH temperatures of the high-scaled experiment are often colder than the lower bound from proxy data, the modeled decadal-scale NH surface temperature for the medium-scaled case falls within the uncertainty range of the available temperature reconstructions. The medium-scaled simulation also broadly reproduces the main features seen in the proxy records." "Without anthropogenic forcing, the 20th century warming is small. The simulations with only natural forcing components included yield an early 20th century peak warming of ≈0.2 °C (≈1950 AD), which is reduced to about half by the end of the century because of increased volcanism.”
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| − | 4. ^ A guide to facts and fictions about climate change. Royal Society (March 2005). Retrieved on 2007-11-18. “"However, the overwhelming majority of scientists who work on climate change agree on the main points"”
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| − | 5. ^ Climate Change: Basic Information. United States Environmental Protection Agency (2006-12-14). Retrieved on 2007-02-09. “In common usage, 'global warming' often refers to the warming that can occur as a result of increased emissions of greenhouse gases from human activities.”
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| − | 6. ^ United Nations Framework Convention on Climate Change, Article I. United Nations Framework Convention on Climate Change. Retrieved on 2007-01-15.
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| − | 17. ^ Note that the Greenhouse Effect produces a temperature increase of about 33 °C (59 °F) with respect to black body predictions and not a surface temperature of 33 °C (91 °F) which is 32 °F higher. The average surface temperature is about 14 °C (57 °F). Also note that both the Celsius and Fahrenheit temperatures are expressed to 2 significant figures even though the conversion formula produces 3.
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| − | 49. ^ Hansen, James; et al. (2006-09-26). "Global temperature change" (PDF). PNAS 103: 14288–14293. Retrieved on 2007-04-20.
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| − | 55. ^ Harte, John; et al. (2006-10-30). "Shifts in plant dominance control carbon-cycle responses to experimental warming and widespread drought". Environmental Research Letters 1 (1). 014001. Retrieved on 2007-05-02.
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| − | 56. ^ Scheffer, Marten; et al. (2006-05-26). "Positive feedback between global warming and atmospheric CO2 concentration inferred from past climate change.". Geophysical Research Letters 33. doi:10.1029/2005gl025044. Retrieved on 2007-05-04.
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| − | 57. ^ Stocker, Thomas F.; et al. (2001-01-20). 7.2.2 Cloud Processes and Feedbacks. Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change. Retrieved on 2007-03-04.
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| − | 58. ^ Macey, Jennifer. "Global warming opens up Northwest Passage", ABC News, September 19, 2007. Retrieved on 2007-12-11.
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| − | 60. ^ McMichael AJ, Woodruff RE, Hales S (2006). "Climate change and human health: present and future risks". Lancet 367 (9513): 859-69. doi:10.1016/S0140-6736(06)68079-3. PMID 16530580.
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| − | 61. ^ a b Summary for Policymakers (PDF). Climate Change 2007: Impacts, Adaptation and Vulnerability. Working Group II Contribution to the Intergovernmental Panel on Climate Change Fourth Assessment Report. Intergovernmental Panel on Climate Change (2007-04-13). Retrieved on 2007-04-28.
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| − | 62. ^ Church, John A.; et al. (2001-01-20). Executive Summary of Chapter 11. Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change. Retrieved on 2005-12-19.
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| − | 63. ^ Thomas, Chris D.; et al. (2004-01-08). "Extinction risk from climate change" (PDF). Nature 427 (6970): 145-138. doi:10.1038/nature02121. Retrieved on 2007-03-18.
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| − | 64. ^ McLaughlin, John F.; et al. (2002-04-30). "Climate change hastens population extinctions" (PDF). PNAS 99 (9): 6070–6074. doi:10.1073/pnas.052131199. Retrieved on 2007-03-29.
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| − | 65. ^ Botkin, Daniel B.; et al. (March 2007). "Forecasting the Effects of Global Warming on Biodiversity". BioScience 57 (3): 227–236. doi:10.1641/B570306. Retrieved on 2007-11-30.
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| − | 66. ^ At-a-glance: The Stern Review. BBC (2006-10-30). Retrieved on 2007-04-29.
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| − | 67. ^ Tol and Yohe (2006) "A Review of the Stern Review" World Economics 7(4): 233-50. See also other critiques in World Economics 7(4).
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| − | 68. ^ Brad DeLong. Do unto others....
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| − | 69. ^ John Quiggin. Stern and the critics on discounting.
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| − | 70. ^ Dlugolecki, Andrew; et al. (2002). Climate Risk to Global Economy (PDF). CEO Briefing: UNEP FI Climate Change Working Group. United Nations Environment Programme. Retrieved on 2007-04-29.
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| − | 71. ^ Kurt M. Campbell, Jay Gulledge, J.R. McNeill, John Podesta, Peter Ogden, Leon Fuerth, R. James Woolsey, Alexander T.J. Lennon, Julianne Smith, Richard Weitz, Derek Mix (Oktober 2007). The Age of Consequences: The Foreign Policy and National Security Implications of Global Climate Change (PDF). Retrieved on 2007-11-06.
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| − | 72. ^ Climate Control: a proposal for controlling global greenhouse gas emissions (PDF). Sustento Institute. Retrieved on 2007-12-10.
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| − | 73. ^ Monbiot, George. Rigged - The climate talks are a stitch-up, as no one is talking about supply. (HTML). Retrieved on 2007-12-22.
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| − | 74. ^ Kyoto Protocol Status of Ratification (PDF). United Nations Framework Convention on Climate Change (2006-07-10). Retrieved on 2007-04-27.
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| − | 75. ^ Climate talks face international hurdles, by Arthur Max, Associated press, 5/14/07.
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| − | 81. ^ Revkin, Andrew. "Poor Nations to Bear Brunt as World Warms", The New York Times, 2007-04-01. Retrieved on 2007-05-02.
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| − | 82. ^ Brahic, Catherine (2006-04-25). China's emissions may surpass the US in 2007. New Scientist. Retrieved on 2007-05-02.
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| − | 83. ^ Crampton, Thomas. "More in Europe worry about climate than in U.S., poll shows", International Herald Tribune, 2007-01-04. Retrieved on 2007-04-14.
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| − | 84. ^ Summary of Findings. Little Consensus on Global Warming. Partisanship Drives Opinion. Pew Research Center (2006-07-12). Retrieved on 2007-04-14.
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| − | 85. ^ "EU agrees on carbon dioxide cuts", BCC, 2007-03-09. Retrieved on 2007-05-04.
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| − | 86. ^ Begley, Sharon. "The Truth About Denial", Newsweek, 2007-08-13. Retrieved on 2007-08-13.
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| − | 87. ^ Adams, David (2006-09-20). Royal Society tells Exxon: stop funding climate change denial. The Guardian. Retrieved on 2007-08-09.
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| − | 88. ^ "Exxon cuts ties to global warming skeptics", MSNBC, 2007-01-12. Retrieved on 2007-05-02.
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| − | 89. ^ Sandell, Clayton. "Report: Big Money Confusing Public on Global Warming", ABC, 2007-01-03. Retrieved on 2007-04-27.
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| − | 90. ^ "Greenpeace: Exxon still funding climate skeptics", USA TODAY, 2007-05-18. Retrieved on 2007-07-09.
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| − | 91. ^ Ceres (April 28, 2004). "Global Warming Resolutions at U.S. Oil Companies Bring Policy Commitments from Leaders, and Record High Votes at Laggards". Press release. Retrieved on 2007-07-27.
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| − | 93. ^ China: US should take lead on climate, by Michael Casey, Associated Press, 12/7/07.
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| − | 94. ^ India's glaciers give grim message on warming, by Somni Sengupta, 7/17/07, New York Times via oregonlive.com.
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| − | 95. ^ Chinese object to climate draft, BBC, 5/1/07; In Battle for U.S. Carbon Caps, Eyes and Efforts Focus on China,by Steven Mufson, Washington Post, 6/6/07.
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| − | 96. ^ The Ocean and the Carbon Cycle. NASA (2005-06-21). Retrieved on 2007-03-04.
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| − | 97. ^ Jacobson, Mark Z. (2005-04-02). "Studying ocean acidification with conservative, stable numerical schemes for nonequilibrium air-ocean exchange and ocean equilibrium chemistry" (PDF). Journal of Geophysical Research 110 (D7). doi:10.1029/2004JD005220. D07302. Retrieved on 2007-04-28.
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| − | 98. ^ Caldeira, Ken; Wickett, Michael E. (2005-09-21). "Ocean model predictions of chemistry changes from carbon dioxide emissions to the atmosphere and ocean". Journal of Geophysical Research 110 (C09S04): 1–12. Retrieved on 2006-02-14.
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| − | 99. ^ Raven, John A.; et al. (2005-06-30). "Ocean acidification due to increasing atmospheric carbon dioxide" (ASP). Royal Society. Retrieved on 2007-05-04.
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| − | | |
| − | Global warming is the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.
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| − | | |
| − | The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 year period ending in 2005, which is higher than the earlier estimate of 0.6 ± 0.2 °C for the period ending in 2000.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations"[1] via the greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3] These basic conclusions have been endorsed by at least 30 scientific societies and academies of science, including all of the national academies of science of the major industrialized countries. While individual scientists have voiced disagreement with the conclusions of the IPCC, the overwhelming majority of scientists working on climate change are in agreement with the conclusions.[4]
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| − | | |
| − | Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[1] The range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a millennium even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]
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| − | | |
| − | Increasing global temperature will cause sea level to rise, and is expected to increase the intensity of extreme weather events and to change the amount and pattern of precipitation. Other effects of global warming include changes in agricultural yields, trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.
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| − | | |
| − | Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. There is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences. Most national governments have signed and ratified the Kyoto Protocol, aimed at reducing greenhouse gas emissions.
| |
| − | Contents
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| − | [hide]
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| − | | |
| − | * 1 Terminology
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| − | * 2 Causes
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| − | o 2.1 Greenhouse gases in the atmosphere
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| − | o 2.2 Feedbacks
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| − | o 2.3 Solar variation
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| − | * 3 Temperature changes
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| − | o 3.1 Recent
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| − | o 3.2 Pre-human climate variations
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| − | * 4 Climate models
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| − | * 5 Attributed and expected effects
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| − | o 5.1 Economic
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| − | o 5.2 Security
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| − | * 6 Adaptation and mitigation
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| − | * 7 Social and political debate
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| − | * 8 Related climatic issues
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| − | * 9 See also
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| − | * 10 References
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| − | * 11 Further reading
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| − | * 12 External links
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| − | | |
| − | Terminology
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| − | | |
| − | The term "global warming" is a specific example of the broader term climate change, which can also refer to global cooling. In common usage, the term refers to recent warming and implies a human influence.[5] The United Nations Framework Convention on Climate Change (UNFCCC) uses the term "climate change" for human-caused change, and "climate variability" for other changes.[6] The term "anthropogenic global warming" is sometimes used when focusing on human-induced changes.
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| − | | |
| − | Causes
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | | |
| − | Main articles: Attribution of recent climate change and scientific opinion on climate change
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| − | | |
| − | The Earth's climate changes in response to external forcing, including variations in its orbit around the sun (orbital forcing),[7][8][9] volcanic eruptions, and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[10][11] identifies elevated levels of greenhouse gases due to human activity as the main influence. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain the observed increase in mean global temperature. One such hypothesis proposes that warming may be the result of variations in solar activity.[12][13][14]
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| − | | |
| − | None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[15]
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| − | | |
| − | Greenhouse gases in the atmosphere
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| − | | |
| − | Main article: Greenhouse effect
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| − | | |
| − | The greenhouse effect was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. It is the process by which absorption and emission of infrared radiation by atmospheric gases warm a planet's atmosphere and surface.
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| − | | |
| − | Existence of the greenhouse effect as such is not disputed. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F), without which Earth would be uninhabitable.[16][17] Rather, the issue is how the strength of the greenhouse effect is changed when human activity increases the atmospheric concentrations of some greenhouse gases.
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| − | | |
| − | On Earth, the major greenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect (not including clouds); carbon dioxide (CO2), which causes 9–26%; methane (CH4), which causes 4–9%; and ozone, which causes 3–7%.[18][19] Some other naturally occurring gases contribute very small fractions of the greenhouse effect; one of these, nitrous oxide (N2O), is increasing in concentration owing to human activity such as agriculture. The atmospheric concentrations of CO2 and CH4 have increased by 31% and 149% respectively above pre-industrial levels since 1750. Molecule for molecule, methane is a more effective greenhouse gas than carbon dioxide, but its concentration is much smaller so that its total radiative forcing is only about a fourth of that from carbon dioxide. These levels are considerably higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores. From less direct geological evidence it is believed that CO2 values this high were last attained 20 million years ago.[20] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, in particular deforestation.[21]
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| − | | |
| − | The present atmospheric concentration of CO2 is about 383 parts per million (ppm) by volume.[22] Future CO2 levels are expected to rise due to ongoing burning of fossil fuels and land-use change. The rate of rise will depend on uncertain economic, sociological, technological, and natural developments, but may be ultimately limited by the availability of fossil fuels. The IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[23] Fossil fuel reserves are sufficient to reach this level and continue emissions past 2100, if coal, tar sands or methane clathrates are extensively used.[24]
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| − | | |
| − | Feedbacks
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| − | | |
| − | Main article: Effects of global warming#Further global warming (positive feedback)
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| − | | |
| − | The effects of forcing agents on the climate are complicated by various feedback processes.
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| − | | |
| − | One of the most pronounced feedback effects relates to the evaporation of water. In the case of warming by the addition of long-lived greenhouse gases such as CO2, the initial warming will cause more water to be evaporated into the atmosphere. Since water vapor itself acts as a greenhouse gas, this causes still more warming; the warming causes more water vapor to be evaporated, and so forth until a new dynamic equilibrium concentration of water vapor is reached with a much larger greenhouse effect than that due to CO2 alone. Although this feedback process involves an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[25] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.
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| − | | |
| − | Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models. Nevertheless, cloud feedback is second only to water vapor feedback and is positive in all the models that were used in the IPCC Fourth Assessment Report.[25]
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| − | | |
| − | Another important feedback process is ice-albedo feedback.[26] When global temperatures increase, ice near the poles melts at an increasing rate. As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.
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| − | | |
| − | Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism contributing to warming.[27] A massive release of CH4 from methane clathrates could cause rapid warming, according to the clathrate gun hypothesis.
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| − | | |
| − | The ocean's ability to sequester carbon is expected to decline as it warms, because the resulting low nutrient levels of the mesopelagic zone limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[28]
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| − | | |
| − | Solar variation
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| − | Solar variation over the last 30 years.
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| − | Solar variation over the last 30 years.
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| − | | |
| − | Main article: Solar variation
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| − | | |
| − | A few papers suggest that the Sun's contribution may have been underestimated. Two researchers at Duke University, Bruce West and Nicola Scafetta, have estimated that the Sun may have contributed about 45–50% of the increase in the average global surface temperature over the period 1900–2000, and about 25–35% between 1980 and 2000.[29] A paper by Peter Stott and other researchers suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.[30] They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases.
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| − | | |
| − | A different hypothesis is that variations in solar output, possibly amplified by cloud seeding via galactic cosmic rays, may have contributed to recent warming.[31] It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.[32]
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| − | | |
| − | One predicted effect of an increase in solar activity would be a warming of the stratosphere; however, the observed effect since at least 1960 has been a cooling of the lower stratosphere, which is one of the predicted results of greenhouse gas warming.[33] Reduction of stratospheric ozone also has a cooling influence, although substantial ozone depletion did not occur until the late 1970s. Solar variation combined with changes in volcanic activity probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.[1] In 2006, Peter Foukal and other researchers from the United States, Germany, and Switzerland found no net increase of solar brightness over the last thousand years. Solar cycles led to a small increase of 0.07% in brightness over the last 30 years. This effect is far too small to contribute significantly to global warming.[34][35] A paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in cosmic rays.[36] Henrik Svensmark and Eigil Friis-Christensen, the main proponents of cloud seeding by galactic cosmic rays, disputed the findings of Lockwood and Fröhlich.[37] Another recent study speculates that other bodies within the Solar System may influence the climate in a complex manner.[38]
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| − | | |
| − | Temperature changes
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | | |
| − | Main article: Temperature record
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| − | | |
| − | Recent
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| − | | |
| − | Global temperatures on both land and sea have increased by 0.75 °C (1.35 °F) relative to the period 1860–1900, according to the instrumental temperature record. This measured temperature increase is not significantly affected by the urban heat island effect.[39] Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[40] Temperatures in the lower troposphere have increased between 0.12 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with possibly regional fluctuations such as the Medieval Warm Period or the Little Ice Age.
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| − | | |
| − | Sea temperatures increase more slowly than those on land both because of the larger effective heat capacity of the oceans and because the ocean can lose heat by evaporation more readily than the land.[41] Since the Northern Hemisphere has more land mass than the Southern Hemisphere it warms faster; also there are extensive areas of seasonal snow cover subject to the snow-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the asymmetry of warming as the major gases are essentially well-mixed between hemispheres.
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| − | | |
| − | Based on estimates by NASA's Goddard Institute for Space Studies, 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[42] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit concluded that 2005 was the second warmest year, behind 1998.[43][44]
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| − | | |
| − | Anthropogenic emissions of other pollutants—notably sulfate aerosols—can exert a cooling effect by increasing the reflection of incoming sunlight. This partially accounts for the cooling seen in the temperature record in the middle of the twentieth century,[45] though the cooling may also be due in part to natural variability. James Hansen and colleagues have proposed that the effects of the products of fossil fuel combustion—CO2 and aerosols—have largely offset one another, so that warming in recent decades has been driven mainly by non-CO2 greenhouse gases.[46]
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| − | | |
| − | Paleoclimatologist William Ruddiman has argued that human influence on the global climate began around 8,000 years ago with the start of forest clearing to provide land for agriculture and 5,000 years ago with the start of Asian rice irrigation.[47] Ruddiman's interpretation of the historical record, with respect to the methane data, has been disputed.[48]
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| − | | |
| − | Pre-human climate variations
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | | |
| − | Further information: Paleoclimatology
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| − | See also: Snowball Earth
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| − | | |
| − | Earth has experienced warming and cooling many times in the past. The recent Antarctic EPICA ice core spans 800,000 years, including eight glacial cycles timed by orbital variations with interglacial warm periods comparable to present temperatures.[49]
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| − | | |
| − | A rapid buildup of greenhouse gases caused warming in the early Jurassic period (about 180 million years ago), with average temperatures rising by 5 °C (9 °F). Research by the Open University indicates that the warming caused the rate of rock weathering to increase by 400%. As such weathering locks away carbon in calcite and dolomite, CO2 levels dropped back to normal over roughly the next 150,000 years.[50][51]
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| − | | |
| − | Sudden releases of methane from clathrate compounds (the clathrate gun hypothesis) have been hypothesized as a cause for other warming events in the distant past, including the Permian-Triassic extinction event (about 251 million years ago) and the Paleocene-Eocene Thermal Maximum (about 55 million years ago).
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| − | | |
| − | Climate models
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | | |
| − | Main article: Global climate model
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| − | | |
| − | Scientists have studied global warming with computer models of the climate. These models are based on physical principles of fluid dynamics, radiative transfer, and other processes, with simplifications being necessary because of limitations in computer power and the complexity of the underlying system (climate). These models predict that the effect of adding greenhouse gases is to produce a warmer climate.[52] However, even when the same assumptions of future greenhouse gas levels are used, there still remains a considerable range of climate sensitivity.
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| − | | |
| − | Including uncertainties in future greenhouse gas concentrations and climate modeling, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999.[1] Models have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes.
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| − | | |
| − | Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.[53] These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.
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| − | Most global climate models, when run to project future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.[54][55][56]
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| − | The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem.[57] There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability.
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| − | | |
| − | Attributed and expected effects
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| − | | |
| − | Main article: Effects of global warming
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| − | | |
| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | | |
| − | Although it is difficult to connect specific weather events to global warming, an increase in global temperatures may in turn cause broader changes, including glacial retreat, Arctic shrinkage, and worldwide sea level rise. Changes in the amount and pattern of precipitation may result in flooding and drought. There may also be changes in the frequency and intensity of extreme weather events. Other effects may include changes in agricultural yields, addition of new trade routes,[58] reduced summer streamflows, species extinctions, and increases in the range of disease vectors.
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| − | | |
| − | Some effects on both the natural environment and human life are, at least in part, already being attributed to global warming. A 2001 report by the IPCC suggests that glacier retreat, ice shelf disruption such as that of the Larsen Ice Shelf, sea level rise, changes in rainfall patterns, and increased intensity and frequency of extreme weather events, are being attributed in part to global warming.[59] While changes are expected for overall patterns, intensity, and frequencies, it is difficult to attribute specific events to global warming. Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.[60]
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| − | | |
| − | Increasing deaths, displacements, and economic losses projected due to extreme weather attributed to global warming may be exacerbated by growing population densities in affected areas, although temperate regions are projected to experience some minor benefits, such as fewer deaths due to cold exposure.[61] A summary of probable effects and recent understanding can be found in the report made for the IPCC Third Assessment Report by Working Group II.[59] The newer IPCC Fourth Assessment Report summary reports that there is observational evidence for an increase in intense tropical cyclone activity in the North Atlantic Ocean since about 1970, in correlation with the increase in sea surface temperature, but that the detection of long-term trends is complicated by the quality of records prior to routine satellite observations. The summary also states that there is no clear trend in the annual worldwide number of tropical cyclones.[1]
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| − | | |
| − | Additional anticipated effects include sea level rise of 110 to 770 millimeters (0.36 to 2.5 ft) between 1990 and 2100,[62] repercussions to agriculture, possible slowing of the thermohaline circulation, reductions in the ozone layer, increased intensity of hurricanes and extreme weather events, lowering of ocean pH, and the spread of diseases such as malaria and dengue fever. One study predicts 18% to 35% of a sample of 1,103 animal and plant species would be extinct by 2050, based on future climate projections.[63] However, few mechanistic studies have documented extinctions due to recent climate change[64] and one study suggests that projected rates of extinction are uncertain.[65]
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| − | | |
| − | Economic
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | | |
| − | Main articles: Economics of global warming and Low-carbon economy
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| − | | |
| − | Some economists have tried to estimate the aggregate net economic costs of damages from climate change across the globe. Such estimates have so far failed to reach conclusive findings; in a survey of 100 estimates, the values ran from US$-10 per tonne of carbon (tC) (US$-3 per tonne of carbon dioxide) up to US$350/tC (US$95 per tonne of carbon dioxide), with a mean of US$43 per tonne of carbon (US$12 per tonne of carbon dioxide).[61] One widely publicized report on potential economic impact is the Stern Review; it suggests that extreme weather might reduce global gross domestic product by up to 1%, and that in a worst-case scenario global per capita consumption could fall 20%.[66] The report's methodology, advocacy and conclusions have been criticized by many economists, primarily around the Review's assumptions of discounting and its choices of scenarios,[67] while others have supported the general attempt to quantify economic risk, even if not the specific numbers.[68][69]
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| − | | |
| − | In a summary of economic cost associated with climate change, the United Nations Environment Programme emphasizes the risks to insurers, reinsurers, and banks of increasingly traumatic and costly weather events. Other economic sectors likely to face difficulties related to climate change include agriculture and transport. Developing countries, rather than the developed world, are at greatest economic risk.[70]
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| − | Security
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| − | | |
| − | In November 2007, the Center for Strategic and International Studies and the Center for a New American Security published a report highlighting the national security effects of climate change.[71] These security effects include increased competition for resources between countries, mass migration from the worst affected areas, challenges to the cohesion of major states threatened by the rise in sea levels, and, as a consequence of these factors, an increased risk of armed conflict, including even nuclear conflicts.
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| − | Adaptation and mitigation
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| − | | |
| − | Main articles: Adaptation to global warming, Mitigation of global warming, and Kyoto Protocol
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| − | | |
| − | The broad agreement among climate scientists that global temperatures will continue to increase has led some nations, states, corporations and individuals to implement actions to try to curtail global warming or adjust to it. Many environmental groups encourage action against global warming, often by the consumer, but also by community and regional organizations. Others have suggested a quota on worldwide fossil fuel production, citing a direct link between fossil fuel production and CO2 emissions.[72][73]
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| − | | |
| − | There has also been business action on climate change, including efforts at increased energy efficiency and limited moves towards use of alternative fuels. One important innovation has been the development of greenhouse gas emissions trading through which companies, in conjunction with government, agree to cap their emissions or to purchase credits from those below their allowances.
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| − | | |
| − | The world's primary international agreement on combating global warming is the Kyoto Protocol, an amendment to the United Nations Framework Convention on Climate Change (UNFCCC) negotiated in 1997. The Protocol now covers more than 160 countries globally and over 55% of global greenhouse gas emissions.[74] Only the United States and Kazakhstan have not ratified the treaty, with the United States historically being the world's largest emitter of greenhouse gas. This treaty expires in 2012, and international talks began in May 2007 on a future treaty to succeed the current one.[75]
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| − | | |
| − | Claiming "serious harm" to the United States economy and the exemption of "80 percent of the world, including major population centers" like China and India, from the treaty, George W. Bush contends that the Kyoto Protocol is an unfair and ineffective means of addressing global climate change concerns.[76] Still, various state, local, and regional governments within the United States have begun their own initiatives to indicate support and compliance with the Kyoto Protocol on a local basis. For example, the Regional Greenhouse Gas Initiative is a state-level emissions capping and trading program involving eight Northeastern U.S. states, which was founded on December 20, 2005.[77]
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| − | China and India, though exempt from its provisions as developing countries, have ratified the Kyoto Protocol. China may have passed the U.S. in total annual greenhouse gas emissions according to some recent studies. Chinese Premier Wen Jiabao has called on the nation to redouble its efforts to tackle pollution and global warming.[78]
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| − | | |
| − | The IPCC's Working Group III is responsible for crafting reports that deal with the mitigation of global warming and analyzing the costs and benefits of different approaches. In the 2007 IPCC Fourth Assessment Report, they conclude that no one technology or sector can be completely responsible for mitigating future warming. They find there are key practices and technologies in various sectors, such as energy supply, transportation, industry, and agriculture, that should be implemented to reduced global emissions. They estimate that stabilization of carbon dioxide equivalent between 445 and 710 ppm by 2030 will result in between a 0.6% increase and 3% decrease in global gross domestic product.[79]
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| − | Social and political debate
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| − | | |
| − | Main articles: Global warming controversy, Politics of global warming, and Economics of global warming
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| − | See also: Climate change denial
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | | |
| − | Over the past several years, public perceptions and attitudes concerning the causes and importance of global warming have changed.[80] Increased awareness of the scientific findings surrounding global warming has resulted in political and economic debate. Poor regions, particularly Africa, appear at greatest risk from the suggested effects of global warming, while their actual emissions have been small compared to the developed world.[81] At the same time, developing country exemptions from provisions of the Kyoto Protocol have been criticized by the United States and Australia, and have been used as part of the rationale for continued non-ratification by the U.S.[82] In the Western world, the idea of human influence on climate has gained wider acceptance in Europe than in the United States.[83][84]
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| − | The issue of climate change has sparked debate weighing the benefits of limiting industrial emissions of greenhouse gases against the costs that such changes would entail. There has been discussion in several countries about the cost and benefits of adopting alternative energy sources in order to reduce carbon emissions.[85] Organizations and companies such as the Competitive Enterprise Institute and ExxonMobil have emphasized more conservative climate change scenarios while highlighting the potential economic cost of stricter controls.[86][87][88][89] Likewise, various environmental lobbies and a number of public figures have launched campaigns to emphasize the potential risks of climate change and promote the implementation of stricter controls. Some fossil fuel companies have scaled back their efforts in recent years,[90] or called for policies to reduce global warming.[91]
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| − | Another point of debate is the degree to which newly developed economies such as India and China should be expected to constrain their emissions. China's gross national CO2 emissions are expected to exceed those of the U.S. within the next few years, and may have already done so according to a 2006 report.[92] China has contended that it has less of an obligation to reduce emissions since its per capita emissions are roughly one-fifth that of the United States.[93] India, also exempt from Kyoto restrictions and another of the biggest sources of industrial emissions, has made similar assertions.[94] However, the U.S. contends that if they must bear the cost of reducing emissions, then China should do the same.[95]
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| − | Related climatic issues
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| − | | |
| − | Main articles: Ocean acidification, global dimming, and ozone depletion
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| − | | |
| − | A variety of issues are often raised in relation to global warming. One is ocean acidification. Increased atmospheric CO2 increases the amount of CO2 dissolved in the oceans.[96] CO2 dissolved in the ocean reacts with water to form carbonic acid, resulting in acidification. Ocean surface pH is estimated to have decreased from 8.25 near the beginning of the industrial era to 8.14 by 2004,[97] and is projected to decrease by a further 0.14 to 0.5 units by 2100 as the ocean absorbs more CO2.[1][98] Since organisms and ecosystems are adapted to a narrow range of pH, this raises extinction concerns, directly driven by increased atmospheric CO2, that could disrupt food webs and impact human societies that depend on marine ecosystem services.[99]
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| − | Global dimming, the gradual reduction in the amount of global direct irradiance at the Earth's surface, may have partially mitigated global warming in the late twentieth century. From 1960 to 1990 human-caused aerosols likely precipitated this effect. Scientists have stated with 66–90% confidence that the effects of human-caused aerosols, along with volcanic activity, have offset some of the global warming, and that greenhouse gases would have resulted in more warming than observed if not for these dimming agents.[1]
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| − | Ozone depletion, the steady decline in the total amount of ozone in Earth's stratosphere, is frequently cited in relation to global warming. Although there are areas of linkage, the relationship between the two is not strong.
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| − | See also
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| − | | |
| − | * Glossary of climate change
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| − | | |
| − | References
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| − | | |
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| − | 65. ^ Botkin, Daniel B.; et al. (March 2007). "Forecasting the Effects of Global Warming on Biodiversity". BioScience 57 (3): 227–236. doi:10.1641/B570306. Retrieved on 2007-11-30.
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| − | 66. ^ At-a-glance: The Stern Review. BBC (2006-10-30). Retrieved on 2007-04-29.
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| − | 67. ^ Tol and Yohe (2006) "A Review of the Stern Review" World Economics 7(4): 233-50. See also other critiques in World Economics 7(4).
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| − | 68. ^ Brad DeLong. Do unto others....
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| − | 69. ^ John Quiggin. Stern and the critics on discounting.
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| − | 70. ^ Dlugolecki, Andrew; et al. (2002). Climate Risk to Global Economy (PDF). CEO Briefing: UNEP FI Climate Change Working Group. United Nations Environment Programme. Retrieved on 2007-04-29.
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| − | 71. ^ Kurt M. Campbell, Jay Gulledge, J.R. McNeill, John Podesta, Peter Ogden, Leon Fuerth, R. James Woolsey, Alexander T.J. Lennon, Julianne Smith, Richard Weitz, Derek Mix (Oktober 2007). The Age of Consequences: The Foreign Policy and National Security Implications of Global Climate Change (PDF). Retrieved on 2007-11-06.
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| − | 72. ^ Climate Control: a proposal for controlling global greenhouse gas emissions (PDF). Sustento Institute. Retrieved on 2007-12-10.
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| − | 73. ^ Monbiot, George. Rigged - The climate talks are a stitch-up, as no one is talking about supply. (HTML). Retrieved on 2007-12-22.
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| − | 74. ^ Kyoto Protocol Status of Ratification (PDF). United Nations Framework Convention on Climate Change (2006-07-10). Retrieved on 2007-04-27.
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| − | 75. ^ Climate talks face international hurdles, by Arthur Max, Associated press, 5/14/07.
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| − | 76. ^ George W. Bush (March 13, 2001). Text of a Letter from the President to Senators Hagel, Helms, Craig, and Roberts. Office of the Press Secretary. Retrieved on 2007-11-21.
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| − | 77. ^ Regional Greenhouse Gas Initiative. Retrieved on 2006-11-07.
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| − | 78. ^ www.planetark.com/dailynewsstory.cfm/newsid/43027/story.htm. Retrieved on 2007-07-27.
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| − | 79. ^ Summary for Policymakers (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group III to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change (2007-05-04). Retrieved on 2007-12-09.
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| − | 80. ^ Weart, Spencer (2006), "The Public and Climate Change", in Weart, Spencer, The Discovery of Global Warming, American Institute of Physics, <http://www.aip.org/history/climate/Public.htm>. Retrieved on 2007-04-14
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| − | 81. ^ Revkin, Andrew. "Poor Nations to Bear Brunt as World Warms", The New York Times, 2007-04-01. Retrieved on 2007-05-02.
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| − | 82. ^ Brahic, Catherine (2006-04-25). China's emissions may surpass the US in 2007. New Scientist. Retrieved on 2007-05-02.
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| − | 83. ^ Crampton, Thomas. "More in Europe worry about climate than in U.S., poll shows", International Herald Tribune, 2007-01-04. Retrieved on 2007-04-14.
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| − | 84. ^ Summary of Findings. Little Consensus on Global Warming. Partisanship Drives Opinion. Pew Research Center (2006-07-12). Retrieved on 2007-04-14.
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| − | 85. ^ "EU agrees on carbon dioxide cuts", BCC, 2007-03-09. Retrieved on 2007-05-04.
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| − | 86. ^ Begley, Sharon. "The Truth About Denial", Newsweek, 2007-08-13. Retrieved on 2007-08-13.
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| − | 87. ^ Adams, David (2006-09-20). Royal Society tells Exxon: stop funding climate change denial. The Guardian. Retrieved on 2007-08-09.
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| − | 88. ^ "Exxon cuts ties to global warming skeptics", MSNBC, 2007-01-12. Retrieved on 2007-05-02.
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| − | 89. ^ Sandell, Clayton. "Report: Big Money Confusing Public on Global Warming", ABC, 2007-01-03. Retrieved on 2007-04-27.
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| − | 90. ^ "Greenpeace: Exxon still funding climate skeptics", USA TODAY, 2007-05-18. Retrieved on 2007-07-09.
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| − | 91. ^ Ceres (April 28, 2004). "Global Warming Resolutions at U.S. Oil Companies Bring Policy Commitments from Leaders, and Record High Votes at Laggards". Press release. Retrieved on 2007-07-27.
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| − | 92. ^ "Group: China tops world in CO2 emissions", Associated Press, 2007-06-20. Retrieved on 2007-10-16. ; "Group: China surpassed US in carbon emissions in 2006: Dutch report", Reuters, 2007-06-20. Retrieved on 2007-10-16.
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| − | 93. ^ China: US should take lead on climate, by Michael Casey, Associated Press, 12/7/07.
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| − | 94. ^ India's glaciers give grim message on warming, by Somni Sengupta, 7/17/07, New York Times via oregonlive.com.
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| − | 95. ^ Chinese object to climate draft, BBC, 5/1/07; In Battle for U.S. Carbon Caps, Eyes and Efforts Focus on China,by Steven Mufson, Washington Post, 6/6/07.
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| − | 96. ^ The Ocean and the Carbon Cycle. NASA (2005-06-21). Retrieved on 2007-03-04.
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| − | 97. ^ Jacobson, Mark Z. (2005-04-02). "Studying ocean acidification with conservative, stable numerical schemes for nonequilibrium air-ocean exchange and ocean equilibrium chemistry" (PDF). Journal of Geophysical Research 110 (D7). doi:10.1029/2004JD005220. D07302. Retrieved on 2007-04-28.
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| − | 98. ^ Caldeira, Ken; Wickett, Michael E. (2005-09-21). "Ocean model predictions of chemistry changes from carbon dioxide emissions to the atmosphere and ocean". Journal of Geophysical Research 110 (C09S04): 1–12. Retrieved on 2006-02-14.
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| − | 99. ^ Raven, John A.; et al. (2005-06-30). "Ocean acidification due to increasing atmospheric carbon dioxide" (ASP). Royal Society. Retrieved on 2007-05-04.
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| − | | |
| − | Global warming is the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.
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| − | | |
| − | The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 year period ending in 2005, which is higher than the earlier estimate of 0.6 ± 0.2 °C for the period ending in 2000.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations"[1] via the greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3] These basic conclusions have been endorsed by at least 30 scientific societies and academies of science, including all of the national academies of science of the major industrialized countries. While individual scientists have voiced disagreement with the conclusions of the IPCC, the overwhelming majority of scientists working on climate change are in agreement with the conclusions.[4]
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| − | | |
| − | Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[1] The range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a millennium even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]
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| − | | |
| − | Increasing global temperature will cause sea level to rise, and is expected to increase the intensity of extreme weather events and to change the amount and pattern of precipitation. Other effects of global warming include changes in agricultural yields, trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.
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| − | | |
| − | Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. There is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences. Most national governments have signed and ratified the Kyoto Protocol, aimed at reducing greenhouse gas emissions.
| |
| − | Contents
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| − | [hide]
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| − | | |
| − | * 1 Terminology
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| − | * 2 Causes
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| − | o 2.1 Greenhouse gases in the atmosphere
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| − | o 2.2 Feedbacks
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| − | o 2.3 Solar variation
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| − | * 3 Temperature changes
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| − | o 3.1 Recent
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| − | o 3.2 Pre-human climate variations
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| − | * 4 Climate models
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| − | * 5 Attributed and expected effects
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| − | o 5.1 Economic
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| − | o 5.2 Security
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| − | * 6 Adaptation and mitigation
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| − | * 7 Social and political debate
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| − | * 8 Related climatic issues
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| − | * 9 See also
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| − | * 10 References
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| − | * 11 Further reading
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| − | * 12 External links
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| − | | |
| − | Terminology
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| − | | |
| − | The term "global warming" is a specific example of the broader term climate change, which can also refer to global cooling. In common usage, the term refers to recent warming and implies a human influence.[5] The United Nations Framework Convention on Climate Change (UNFCCC) uses the term "climate change" for human-caused change, and "climate variability" for other changes.[6] The term "anthropogenic global warming" is sometimes used when focusing on human-induced changes.
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| − | | |
| − | Causes
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | | |
| − | Main articles: Attribution of recent climate change and scientific opinion on climate change
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| − | | |
| − | The Earth's climate changes in response to external forcing, including variations in its orbit around the sun (orbital forcing),[7][8][9] volcanic eruptions, and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[10][11] identifies elevated levels of greenhouse gases due to human activity as the main influence. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain the observed increase in mean global temperature. One such hypothesis proposes that warming may be the result of variations in solar activity.[12][13][14]
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| − | | |
| − | None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[15]
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| − | | |
| − | Greenhouse gases in the atmosphere
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| − | | |
| − | Main article: Greenhouse effect
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| − | | |
| − | The greenhouse effect was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. It is the process by which absorption and emission of infrared radiation by atmospheric gases warm a planet's atmosphere and surface.
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| − | | |
| − | Existence of the greenhouse effect as such is not disputed. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F), without which Earth would be uninhabitable.[16][17] Rather, the issue is how the strength of the greenhouse effect is changed when human activity increases the atmospheric concentrations of some greenhouse gases.
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| − | | |
| − | On Earth, the major greenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect (not including clouds); carbon dioxide (CO2), which causes 9–26%; methane (CH4), which causes 4–9%; and ozone, which causes 3–7%.[18][19] Some other naturally occurring gases contribute very small fractions of the greenhouse effect; one of these, nitrous oxide (N2O), is increasing in concentration owing to human activity such as agriculture. The atmospheric concentrations of CO2 and CH4 have increased by 31% and 149% respectively above pre-industrial levels since 1750. Molecule for molecule, methane is a more effective greenhouse gas than carbon dioxide, but its concentration is much smaller so that its total radiative forcing is only about a fourth of that from carbon dioxide. These levels are considerably higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores. From less direct geological evidence it is believed that CO2 values this high were last attained 20 million years ago.[20] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, in particular deforestation.[21]
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| − | | |
| − | The present atmospheric concentration of CO2 is about 383 parts per million (ppm) by volume.[22] Future CO2 levels are expected to rise due to ongoing burning of fossil fuels and land-use change. The rate of rise will depend on uncertain economic, sociological, technological, and natural developments, but may be ultimately limited by the availability of fossil fuels. The IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[23] Fossil fuel reserves are sufficient to reach this level and continue emissions past 2100, if coal, tar sands or methane clathrates are extensively used.[24]
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| − | | |
| − | Feedbacks
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| − | | |
| − | Main article: Effects of global warming#Further global warming (positive feedback)
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| − | | |
| − | The effects of forcing agents on the climate are complicated by various feedback processes.
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| − | | |
| − | One of the most pronounced feedback effects relates to the evaporation of water. In the case of warming by the addition of long-lived greenhouse gases such as CO2, the initial warming will cause more water to be evaporated into the atmosphere. Since water vapor itself acts as a greenhouse gas, this causes still more warming; the warming causes more water vapor to be evaporated, and so forth until a new dynamic equilibrium concentration of water vapor is reached with a much larger greenhouse effect than that due to CO2 alone. Although this feedback process involves an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[25] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.
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| − | | |
| − | Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models. Nevertheless, cloud feedback is second only to water vapor feedback and is positive in all the models that were used in the IPCC Fourth Assessment Report.[25]
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| − | | |
| − | Another important feedback process is ice-albedo feedback.[26] When global temperatures increase, ice near the poles melts at an increasing rate. As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.
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| − | | |
| − | Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism contributing to warming.[27] A massive release of CH4 from methane clathrates could cause rapid warming, according to the clathrate gun hypothesis.
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| − | | |
| − | The ocean's ability to sequester carbon is expected to decline as it warms, because the resulting low nutrient levels of the mesopelagic zone limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[28]
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| − | | |
| − | Solar variation
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| − | Solar variation over the last 30 years.
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| − | Solar variation over the last 30 years.
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| − | | |
| − | Main article: Solar variation
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| − | | |
| − | A few papers suggest that the Sun's contribution may have been underestimated. Two researchers at Duke University, Bruce West and Nicola Scafetta, have estimated that the Sun may have contributed about 45–50% of the increase in the average global surface temperature over the period 1900–2000, and about 25–35% between 1980 and 2000.[29] A paper by Peter Stott and other researchers suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.[30] They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases.
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| − | | |
| − | A different hypothesis is that variations in solar output, possibly amplified by cloud seeding via galactic cosmic rays, may have contributed to recent warming.[31] It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.[32]
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| − | | |
| − | One predicted effect of an increase in solar activity would be a warming of the stratosphere; however, the observed effect since at least 1960 has been a cooling of the lower stratosphere, which is one of the predicted results of greenhouse gas warming.[33] Reduction of stratospheric ozone also has a cooling influence, although substantial ozone depletion did not occur until the late 1970s. Solar variation combined with changes in volcanic activity probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.[1] In 2006, Peter Foukal and other researchers from the United States, Germany, and Switzerland found no net increase of solar brightness over the last thousand years. Solar cycles led to a small increase of 0.07% in brightness over the last 30 years. This effect is far too small to contribute significantly to global warming.[34][35] A paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in cosmic rays.[36] Henrik Svensmark and Eigil Friis-Christensen, the main proponents of cloud seeding by galactic cosmic rays, disputed the findings of Lockwood and Fröhlich.[37] Another recent study speculates that other bodies within the Solar System may influence the climate in a complex manner.[38]
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| − | | |
| − | Temperature changes
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | | |
| − | Main article: Temperature record
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| − | | |
| − | Recent
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| − | | |
| − | Global temperatures on both land and sea have increased by 0.75 °C (1.35 °F) relative to the period 1860–1900, according to the instrumental temperature record. This measured temperature increase is not significantly affected by the urban heat island effect.[39] Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[40] Temperatures in the lower troposphere have increased between 0.12 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with possibly regional fluctuations such as the Medieval Warm Period or the Little Ice Age.
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| − | | |
| − | Sea temperatures increase more slowly than those on land both because of the larger effective heat capacity of the oceans and because the ocean can lose heat by evaporation more readily than the land.[41] Since the Northern Hemisphere has more land mass than the Southern Hemisphere it warms faster; also there are extensive areas of seasonal snow cover subject to the snow-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the asymmetry of warming as the major gases are essentially well-mixed between hemispheres.
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| − | | |
| − | Based on estimates by NASA's Goddard Institute for Space Studies, 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[42] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit concluded that 2005 was the second warmest year, behind 1998.[43][44]
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| − | | |
| − | Anthropogenic emissions of other pollutants—notably sulfate aerosols—can exert a cooling effect by increasing the reflection of incoming sunlight. This partially accounts for the cooling seen in the temperature record in the middle of the twentieth century,[45] though the cooling may also be due in part to natural variability. James Hansen and colleagues have proposed that the effects of the products of fossil fuel combustion—CO2 and aerosols—have largely offset one another, so that warming in recent decades has been driven mainly by non-CO2 greenhouse gases.[46]
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| − | | |
| − | Paleoclimatologist William Ruddiman has argued that human influence on the global climate began around 8,000 years ago with the start of forest clearing to provide land for agriculture and 5,000 years ago with the start of Asian rice irrigation.[47] Ruddiman's interpretation of the historical record, with respect to the methane data, has been disputed.[48]
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| − | | |
| − | Pre-human climate variations
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | | |
| − | Further information: Paleoclimatology
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| − | See also: Snowball Earth
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| − | | |
| − | Earth has experienced warming and cooling many times in the past. The recent Antarctic EPICA ice core spans 800,000 years, including eight glacial cycles timed by orbital variations with interglacial warm periods comparable to present temperatures.[49]
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| − | | |
| − | A rapid buildup of greenhouse gases caused warming in the early Jurassic period (about 180 million years ago), with average temperatures rising by 5 °C (9 °F). Research by the Open University indicates that the warming caused the rate of rock weathering to increase by 400%. As such weathering locks away carbon in calcite and dolomite, CO2 levels dropped back to normal over roughly the next 150,000 years.[50][51]
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| − | | |
| − | Sudden releases of methane from clathrate compounds (the clathrate gun hypothesis) have been hypothesized as a cause for other warming events in the distant past, including the Permian-Triassic extinction event (about 251 million years ago) and the Paleocene-Eocene Thermal Maximum (about 55 million years ago).
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| − | | |
| − | Climate models
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | | |
| − | Main article: Global climate model
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| − | | |
| − | Scientists have studied global warming with computer models of the climate. These models are based on physical principles of fluid dynamics, radiative transfer, and other processes, with simplifications being necessary because of limitations in computer power and the complexity of the underlying system (climate). These models predict that the effect of adding greenhouse gases is to produce a warmer climate.[52] However, even when the same assumptions of future greenhouse gas levels are used, there still remains a considerable range of climate sensitivity.
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| − | | |
| − | Including uncertainties in future greenhouse gas concentrations and climate modeling, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999.[1] Models have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes.
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| − | | |
| − | Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.[53] These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.
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| − | | |
| − | Most global climate models, when run to project future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.[54][55][56]
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| − | | |
| − | The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem.[57] There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability.
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| − | | |
| − | Attributed and expected effects
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| − | | |
| − | Main article: Effects of global warming
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| − | | |
| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | | |
| − | Although it is difficult to connect specific weather events to global warming, an increase in global temperatures may in turn cause broader changes, including glacial retreat, Arctic shrinkage, and worldwide sea level rise. Changes in the amount and pattern of precipitation may result in flooding and drought. There may also be changes in the frequency and intensity of extreme weather events. Other effects may include changes in agricultural yields, addition of new trade routes,[58] reduced summer streamflows, species extinctions, and increases in the range of disease vectors.
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| − | | |
| − | Some effects on both the natural environment and human life are, at least in part, already being attributed to global warming. A 2001 report by the IPCC suggests that glacier retreat, ice shelf disruption such as that of the Larsen Ice Shelf, sea level rise, changes in rainfall patterns, and increased intensity and frequency of extreme weather events, are being attributed in part to global warming.[59] While changes are expected for overall patterns, intensity, and frequencies, it is difficult to attribute specific events to global warming. Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.[60]
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| − | | |
| − | Increasing deaths, displacements, and economic losses projected due to extreme weather attributed to global warming may be exacerbated by growing population densities in affected areas, although temperate regions are projected to experience some minor benefits, such as fewer deaths due to cold exposure.[61] A summary of probable effects and recent understanding can be found in the report made for the IPCC Third Assessment Report by Working Group II.[59] The newer IPCC Fourth Assessment Report summary reports that there is observational evidence for an increase in intense tropical cyclone activity in the North Atlantic Ocean since about 1970, in correlation with the increase in sea surface temperature, but that the detection of long-term trends is complicated by the quality of records prior to routine satellite observations. The summary also states that there is no clear trend in the annual worldwide number of tropical cyclones.[1]
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| − | | |
| − | Additional anticipated effects include sea level rise of 110 to 770 millimeters (0.36 to 2.5 ft) between 1990 and 2100,[62] repercussions to agriculture, possible slowing of the thermohaline circulation, reductions in the ozone layer, increased intensity of hurricanes and extreme weather events, lowering of ocean pH, and the spread of diseases such as malaria and dengue fever. One study predicts 18% to 35% of a sample of 1,103 animal and plant species would be extinct by 2050, based on future climate projections.[63] However, few mechanistic studies have documented extinctions due to recent climate change[64] and one study suggests that projected rates of extinction are uncertain.[65]
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| − | | |
| − | Economic
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | | |
| − | Main articles: Economics of global warming and Low-carbon economy
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| − | | |
| − | Some economists have tried to estimate the aggregate net economic costs of damages from climate change across the globe. Such estimates have so far failed to reach conclusive findings; in a survey of 100 estimates, the values ran from US$-10 per tonne of carbon (tC) (US$-3 per tonne of carbon dioxide) up to US$350/tC (US$95 per tonne of carbon dioxide), with a mean of US$43 per tonne of carbon (US$12 per tonne of carbon dioxide).[61] One widely publicized report on potential economic impact is the Stern Review; it suggests that extreme weather might reduce global gross domestic product by up to 1%, and that in a worst-case scenario global per capita consumption could fall 20%.[66] The report's methodology, advocacy and conclusions have been criticized by many economists, primarily around the Review's assumptions of discounting and its choices of scenarios,[67] while others have supported the general attempt to quantify economic risk, even if not the specific numbers.[68][69]
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| − | | |
| − | In a summary of economic cost associated with climate change, the United Nations Environment Programme emphasizes the risks to insurers, reinsurers, and banks of increasingly traumatic and costly weather events. Other economic sectors likely to face difficulties related to climate change include agriculture and transport. Developing countries, rather than the developed world, are at greatest economic risk.[70]
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| − | | |
| − | Security
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| − | | |
| − | In November 2007, the Center for Strategic and International Studies and the Center for a New American Security published a report highlighting the national security effects of climate change.[71] These security effects include increased competition for resources between countries, mass migration from the worst affected areas, challenges to the cohesion of major states threatened by the rise in sea levels, and, as a consequence of these factors, an increased risk of armed conflict, including even nuclear conflicts.
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| − | | |
| − | Adaptation and mitigation
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| − | | |
| − | Main articles: Adaptation to global warming, Mitigation of global warming, and Kyoto Protocol
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| − | | |
| − | The broad agreement among climate scientists that global temperatures will continue to increase has led some nations, states, corporations and individuals to implement actions to try to curtail global warming or adjust to it. Many environmental groups encourage action against global warming, often by the consumer, but also by community and regional organizations. Others have suggested a quota on worldwide fossil fuel production, citing a direct link between fossil fuel production and CO2 emissions.[72][73]
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| − | | |
| − | There has also been business action on climate change, including efforts at increased energy efficiency and limited moves towards use of alternative fuels. One important innovation has been the development of greenhouse gas emissions trading through which companies, in conjunction with government, agree to cap their emissions or to purchase credits from those below their allowances.
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| − | | |
| − | The world's primary international agreement on combating global warming is the Kyoto Protocol, an amendment to the United Nations Framework Convention on Climate Change (UNFCCC) negotiated in 1997. The Protocol now covers more than 160 countries globally and over 55% of global greenhouse gas emissions.[74] Only the United States and Kazakhstan have not ratified the treaty, with the United States historically being the world's largest emitter of greenhouse gas. This treaty expires in 2012, and international talks began in May 2007 on a future treaty to succeed the current one.[75]
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| − | | |
| − | Claiming "serious harm" to the United States economy and the exemption of "80 percent of the world, including major population centers" like China and India, from the treaty, George W. Bush contends that the Kyoto Protocol is an unfair and ineffective means of addressing global climate change concerns.[76] Still, various state, local, and regional governments within the United States have begun their own initiatives to indicate support and compliance with the Kyoto Protocol on a local basis. For example, the Regional Greenhouse Gas Initiative is a state-level emissions capping and trading program involving eight Northeastern U.S. states, which was founded on December 20, 2005.[77]
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| − | | |
| − | China and India, though exempt from its provisions as developing countries, have ratified the Kyoto Protocol. China may have passed the U.S. in total annual greenhouse gas emissions according to some recent studies. Chinese Premier Wen Jiabao has called on the nation to redouble its efforts to tackle pollution and global warming.[78]
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| − | | |
| − | The IPCC's Working Group III is responsible for crafting reports that deal with the mitigation of global warming and analyzing the costs and benefits of different approaches. In the 2007 IPCC Fourth Assessment Report, they conclude that no one technology or sector can be completely responsible for mitigating future warming. They find there are key practices and technologies in various sectors, such as energy supply, transportation, industry, and agriculture, that should be implemented to reduced global emissions. They estimate that stabilization of carbon dioxide equivalent between 445 and 710 ppm by 2030 will result in between a 0.6% increase and 3% decrease in global gross domestic product.[79]
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| − | | |
| − | Social and political debate
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| − | | |
| − | Main articles: Global warming controversy, Politics of global warming, and Economics of global warming
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| − | See also: Climate change denial
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| − | | |
| − | Per capita greenhouse gas emissions in 2000
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | | |
| − | Over the past several years, public perceptions and attitudes concerning the causes and importance of global warming have changed.[80] Increased awareness of the scientific findings surrounding global warming has resulted in political and economic debate. Poor regions, particularly Africa, appear at greatest risk from the suggested effects of global warming, while their actual emissions have been small compared to the developed world.[81] At the same time, developing country exemptions from provisions of the Kyoto Protocol have been criticized by the United States and Australia, and have been used as part of the rationale for continued non-ratification by the U.S.[82] In the Western world, the idea of human influence on climate has gained wider acceptance in Europe than in the United States.[83][84]
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| − | | |
| − | The issue of climate change has sparked debate weighing the benefits of limiting industrial emissions of greenhouse gases against the costs that such changes would entail. There has been discussion in several countries about the cost and benefits of adopting alternative energy sources in order to reduce carbon emissions.[85] Organizations and companies such as the Competitive Enterprise Institute and ExxonMobil have emphasized more conservative climate change scenarios while highlighting the potential economic cost of stricter controls.[86][87][88][89] Likewise, various environmental lobbies and a number of public figures have launched campaigns to emphasize the potential risks of climate change and promote the implementation of stricter controls. Some fossil fuel companies have scaled back their efforts in recent years,[90] or called for policies to reduce global warming.[91]
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| − | | |
| − | Another point of debate is the degree to which newly developed economies such as India and China should be expected to constrain their emissions. China's gross national CO2 emissions are expected to exceed those of the U.S. within the next few years, and may have already done so according to a 2006 report.[92] China has contended that it has less of an obligation to reduce emissions since its per capita emissions are roughly one-fifth that of the United States.[93] India, also exempt from Kyoto restrictions and another of the biggest sources of industrial emissions, has made similar assertions.[94] However, the U.S. contends that if they must bear the cost of reducing emissions, then China should do the same.[95]
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| − | | |
| − | Related climatic issues
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| − | | |
| − | Main articles: Ocean acidification, global dimming, and ozone depletion
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| − | | |
| − | A variety of issues are often raised in relation to global warming. One is ocean acidification. Increased atmospheric CO2 increases the amount of CO2 dissolved in the oceans.[96] CO2 dissolved in the ocean reacts with water to form carbonic acid, resulting in acidification. Ocean surface pH is estimated to have decreased from 8.25 near the beginning of the industrial era to 8.14 by 2004,[97] and is projected to decrease by a further 0.14 to 0.5 units by 2100 as the ocean absorbs more CO2.[1][98] Since organisms and ecosystems are adapted to a narrow range of pH, this raises extinction concerns, directly driven by increased atmospheric CO2, that could disrupt food webs and impact human societies that depend on marine ecosystem services.[99]
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| − | Global dimming, the gradual reduction in the amount of global direct irradiance at the Earth's surface, may have partially mitigated global warming in the late twentieth century. From 1960 to 1990 human-caused aerosols likely precipitated this effect. Scientists have stated with 66–90% confidence that the effects of human-caused aerosols, along with volcanic activity, have offset some of the global warming, and that greenhouse gases would have resulted in more warming than observed if not for these dimming agents.[1]
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| − | | |
| − | Ozone depletion, the steady decline in the total amount of ozone in Earth's stratosphere, is frequently cited in relation to global warming. Although there are areas of linkage, the relationship between the two is not strong.
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| − | | |
| − | See also
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| − | | |
| − | * Glossary of climate change
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| − | | |
| − | References
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| − | | |
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| − | 86. ^ Begley, Sharon. "The Truth About Denial", Newsweek, 2007-08-13. Retrieved on 2007-08-13.
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| − | 87. ^ Adams, David (2006-09-20). Royal Society tells Exxon: stop funding climate change denial. The Guardian. Retrieved on 2007-08-09.
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| − | 88. ^ "Exxon cuts ties to global warming skeptics", MSNBC, 2007-01-12. Retrieved on 2007-05-02.
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| − | 89. ^ Sandell, Clayton. "Report: Big Money Confusing Public on Global Warming", ABC, 2007-01-03. Retrieved on 2007-04-27.
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| − | 90. ^ "Greenpeace: Exxon still funding climate skeptics", USA TODAY, 2007-05-18. Retrieved on 2007-07-09.
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| − | 91. ^ Ceres (April 28, 2004). "Global Warming Resolutions at U.S. Oil Companies Bring Policy Commitments from Leaders, and Record High Votes at Laggards". Press release. Retrieved on 2007-07-27.
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| − | 92. ^ "Group: China tops world in CO2 emissions", Associated Press, 2007-06-20. Retrieved on 2007-10-16. ; "Group: China surpassed US in carbon emissions in 2006: Dutch report", Reuters, 2007-06-20. Retrieved on 2007-10-16.
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| − | 93. ^ China: US should take lead on climate, by Michael Casey, Associated Press, 12/7/07.
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| − | 94. ^ India's glaciers give grim message on warming, by Somni Sengupta, 7/17/07, New York Times via oregonlive.com.
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| − | 95. ^ Chinese object to climate draft, BBC, 5/1/07; In Battle for U.S. Carbon Caps, Eyes and Efforts Focus on China,by Steven Mufson, Washington Post, 6/6/07.
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| − | 96. ^ The Ocean and the Carbon Cycle. NASA (2005-06-21). Retrieved on 2007-03-04.
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| − | 97. ^ Jacobson, Mark Z. (2005-04-02). "Studying ocean acidification with conservative, stable numerical schemes for nonequilibrium air-ocean exchange and ocean equilibrium chemistry" (PDF). Journal of Geophysical Research 110 (D7). doi:10.1029/2004JD005220. D07302. Retrieved on 2007-04-28.
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| − | 98. ^ Caldeira, Ken; Wickett, Michael E. (2005-09-21). "Ocean model predictions of chemistry changes from carbon dioxide emissions to the atmosphere and ocean". Journal of Geophysical Research 110 (C09S04): 1–12. Retrieved on 2006-02-14.
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| − | 99. ^ Raven, John A.; et al. (2005-06-30). "Ocean acidification due to increasing atmospheric carbon dioxide" (ASP). Royal Society. Retrieved on 2007-05-04.
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| − | | |
| − | Global warming is the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.
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| − | | |
| − | The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 year period ending in 2005, which is higher than the earlier estimate of 0.6 ± 0.2 °C for the period ending in 2000.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations"[1] via the greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3] These basic conclusions have been endorsed by at least 30 scientific societies and academies of science, including all of the national academies of science of the major industrialized countries. While individual scientists have voiced disagreement with the conclusions of the IPCC, the overwhelming majority of scientists working on climate change are in agreement with the conclusions.[4]
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| − | | |
| − | Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[1] The range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a millennium even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]
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| − | | |
| − | Increasing global temperature will cause sea level to rise, and is expected to increase the intensity of extreme weather events and to change the amount and pattern of precipitation. Other effects of global warming include changes in agricultural yields, trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.
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| − | | |
| − | Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. There is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences. Most national governments have signed and ratified the Kyoto Protocol, aimed at reducing greenhouse gas emissions.
| |
| − | Contents
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| − | [hide]
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| − | | |
| − | * 1 Terminology
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| − | * 2 Causes
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| − | o 2.1 Greenhouse gases in the atmosphere
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| − | o 2.2 Feedbacks
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| − | o 2.3 Solar variation
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| − | * 3 Temperature changes
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| − | o 3.1 Recent
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| − | o 3.2 Pre-human climate variations
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| − | * 4 Climate models
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| − | * 5 Attributed and expected effects
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| − | o 5.1 Economic
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| − | o 5.2 Security
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| − | * 6 Adaptation and mitigation
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| − | * 7 Social and political debate
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| − | * 8 Related climatic issues
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| − | * 9 See also
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| − | * 10 References
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| − | * 11 Further reading
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| − | * 12 External links
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| − | | |
| − | Terminology
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| − | | |
| − | The term "global warming" is a specific example of the broader term climate change, which can also refer to global cooling. In common usage, the term refers to recent warming and implies a human influence.[5] The United Nations Framework Convention on Climate Change (UNFCCC) uses the term "climate change" for human-caused change, and "climate variability" for other changes.[6] The term "anthropogenic global warming" is sometimes used when focusing on human-induced changes.
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| − | | |
| − | Causes
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | | |
| − | Main articles: Attribution of recent climate change and scientific opinion on climate change
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| − | | |
| − | The Earth's climate changes in response to external forcing, including variations in its orbit around the sun (orbital forcing),[7][8][9] volcanic eruptions, and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[10][11] identifies elevated levels of greenhouse gases due to human activity as the main influence. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain the observed increase in mean global temperature. One such hypothesis proposes that warming may be the result of variations in solar activity.[12][13][14]
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| − | | |
| − | None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[15]
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| − | | |
| − | Greenhouse gases in the atmosphere
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| − | | |
| − | Main article: Greenhouse effect
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| − | | |
| − | The greenhouse effect was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. It is the process by which absorption and emission of infrared radiation by atmospheric gases warm a planet's atmosphere and surface.
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| − | | |
| − | Existence of the greenhouse effect as such is not disputed. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F), without which Earth would be uninhabitable.[16][17] Rather, the issue is how the strength of the greenhouse effect is changed when human activity increases the atmospheric concentrations of some greenhouse gases.
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| − | | |
| − | On Earth, the major greenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect (not including clouds); carbon dioxide (CO2), which causes 9–26%; methane (CH4), which causes 4–9%; and ozone, which causes 3–7%.[18][19] Some other naturally occurring gases contribute very small fractions of the greenhouse effect; one of these, nitrous oxide (N2O), is increasing in concentration owing to human activity such as agriculture. The atmospheric concentrations of CO2 and CH4 have increased by 31% and 149% respectively above pre-industrial levels since 1750. Molecule for molecule, methane is a more effective greenhouse gas than carbon dioxide, but its concentration is much smaller so that its total radiative forcing is only about a fourth of that from carbon dioxide. These levels are considerably higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores. From less direct geological evidence it is believed that CO2 values this high were last attained 20 million years ago.[20] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, in particular deforestation.[21]
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| − | | |
| − | The present atmospheric concentration of CO2 is about 383 parts per million (ppm) by volume.[22] Future CO2 levels are expected to rise due to ongoing burning of fossil fuels and land-use change. The rate of rise will depend on uncertain economic, sociological, technological, and natural developments, but may be ultimately limited by the availability of fossil fuels. The IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[23] Fossil fuel reserves are sufficient to reach this level and continue emissions past 2100, if coal, tar sands or methane clathrates are extensively used.[24]
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| − | | |
| − | Feedbacks
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| − | | |
| − | Main article: Effects of global warming#Further global warming (positive feedback)
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| − | | |
| − | The effects of forcing agents on the climate are complicated by various feedback processes.
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| − | | |
| − | One of the most pronounced feedback effects relates to the evaporation of water. In the case of warming by the addition of long-lived greenhouse gases such as CO2, the initial warming will cause more water to be evaporated into the atmosphere. Since water vapor itself acts as a greenhouse gas, this causes still more warming; the warming causes more water vapor to be evaporated, and so forth until a new dynamic equilibrium concentration of water vapor is reached with a much larger greenhouse effect than that due to CO2 alone. Although this feedback process involves an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[25] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.
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| − | | |
| − | Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models. Nevertheless, cloud feedback is second only to water vapor feedback and is positive in all the models that were used in the IPCC Fourth Assessment Report.[25]
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| − | | |
| − | Another important feedback process is ice-albedo feedback.[26] When global temperatures increase, ice near the poles melts at an increasing rate. As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.
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| − | | |
| − | Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism contributing to warming.[27] A massive release of CH4 from methane clathrates could cause rapid warming, according to the clathrate gun hypothesis.
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| − | | |
| − | The ocean's ability to sequester carbon is expected to decline as it warms, because the resulting low nutrient levels of the mesopelagic zone limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[28]
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| − | | |
| − | Solar variation
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| − | Solar variation over the last 30 years.
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| − | Solar variation over the last 30 years.
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| − | | |
| − | Main article: Solar variation
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| − | | |
| − | A few papers suggest that the Sun's contribution may have been underestimated. Two researchers at Duke University, Bruce West and Nicola Scafetta, have estimated that the Sun may have contributed about 45–50% of the increase in the average global surface temperature over the period 1900–2000, and about 25–35% between 1980 and 2000.[29] A paper by Peter Stott and other researchers suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.[30] They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases.
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| − | | |
| − | A different hypothesis is that variations in solar output, possibly amplified by cloud seeding via galactic cosmic rays, may have contributed to recent warming.[31] It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.[32]
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| − | | |
| − | One predicted effect of an increase in solar activity would be a warming of the stratosphere; however, the observed effect since at least 1960 has been a cooling of the lower stratosphere, which is one of the predicted results of greenhouse gas warming.[33] Reduction of stratospheric ozone also has a cooling influence, although substantial ozone depletion did not occur until the late 1970s. Solar variation combined with changes in volcanic activity probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.[1] In 2006, Peter Foukal and other researchers from the United States, Germany, and Switzerland found no net increase of solar brightness over the last thousand years. Solar cycles led to a small increase of 0.07% in brightness over the last 30 years. This effect is far too small to contribute significantly to global warming.[34][35] A paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in cosmic rays.[36] Henrik Svensmark and Eigil Friis-Christensen, the main proponents of cloud seeding by galactic cosmic rays, disputed the findings of Lockwood and Fröhlich.[37] Another recent study speculates that other bodies within the Solar System may influence the climate in a complex manner.[38]
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| − | | |
| − | Temperature changes
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | | |
| − | Main article: Temperature record
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| − | | |
| − | Recent
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| − | | |
| − | Global temperatures on both land and sea have increased by 0.75 °C (1.35 °F) relative to the period 1860–1900, according to the instrumental temperature record. This measured temperature increase is not significantly affected by the urban heat island effect.[39] Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[40] Temperatures in the lower troposphere have increased between 0.12 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with possibly regional fluctuations such as the Medieval Warm Period or the Little Ice Age.
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| − | | |
| − | Sea temperatures increase more slowly than those on land both because of the larger effective heat capacity of the oceans and because the ocean can lose heat by evaporation more readily than the land.[41] Since the Northern Hemisphere has more land mass than the Southern Hemisphere it warms faster; also there are extensive areas of seasonal snow cover subject to the snow-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the asymmetry of warming as the major gases are essentially well-mixed between hemispheres.
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| − | | |
| − | Based on estimates by NASA's Goddard Institute for Space Studies, 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[42] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit concluded that 2005 was the second warmest year, behind 1998.[43][44]
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| − | | |
| − | Anthropogenic emissions of other pollutants—notably sulfate aerosols—can exert a cooling effect by increasing the reflection of incoming sunlight. This partially accounts for the cooling seen in the temperature record in the middle of the twentieth century,[45] though the cooling may also be due in part to natural variability. James Hansen and colleagues have proposed that the effects of the products of fossil fuel combustion—CO2 and aerosols—have largely offset one another, so that warming in recent decades has been driven mainly by non-CO2 greenhouse gases.[46]
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| − | | |
| − | Paleoclimatologist William Ruddiman has argued that human influence on the global climate began around 8,000 years ago with the start of forest clearing to provide land for agriculture and 5,000 years ago with the start of Asian rice irrigation.[47] Ruddiman's interpretation of the historical record, with respect to the methane data, has been disputed.[48]
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| − | | |
| − | Pre-human climate variations
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | | |
| − | Further information: Paleoclimatology
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| − | See also: Snowball Earth
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| − | | |
| − | Earth has experienced warming and cooling many times in the past. The recent Antarctic EPICA ice core spans 800,000 years, including eight glacial cycles timed by orbital variations with interglacial warm periods comparable to present temperatures.[49]
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| − | | |
| − | A rapid buildup of greenhouse gases caused warming in the early Jurassic period (about 180 million years ago), with average temperatures rising by 5 °C (9 °F). Research by the Open University indicates that the warming caused the rate of rock weathering to increase by 400%. As such weathering locks away carbon in calcite and dolomite, CO2 levels dropped back to normal over roughly the next 150,000 years.[50][51]
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| − | | |
| − | Sudden releases of methane from clathrate compounds (the clathrate gun hypothesis) have been hypothesized as a cause for other warming events in the distant past, including the Permian-Triassic extinction event (about 251 million years ago) and the Paleocene-Eocene Thermal Maximum (about 55 million years ago).
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| − | Climate models
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | | |
| − | Main article: Global climate model
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| − | | |
| − | Scientists have studied global warming with computer models of the climate. These models are based on physical principles of fluid dynamics, radiative transfer, and other processes, with simplifications being necessary because of limitations in computer power and the complexity of the underlying system (climate). These models predict that the effect of adding greenhouse gases is to produce a warmer climate.[52] However, even when the same assumptions of future greenhouse gas levels are used, there still remains a considerable range of climate sensitivity.
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| − | Including uncertainties in future greenhouse gas concentrations and climate modeling, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999.[1] Models have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes.
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| − | | |
| − | Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.[53] These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.
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| − | | |
| − | Most global climate models, when run to project future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.[54][55][56]
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| − | | |
| − | The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem.[57] There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability.
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| − | | |
| − | Attributed and expected effects
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| − | | |
| − | Main article: Effects of global warming
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| − | | |
| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | | |
| − | Although it is difficult to connect specific weather events to global warming, an increase in global temperatures may in turn cause broader changes, including glacial retreat, Arctic shrinkage, and worldwide sea level rise. Changes in the amount and pattern of precipitation may result in flooding and drought. There may also be changes in the frequency and intensity of extreme weather events. Other effects may include changes in agricultural yields, addition of new trade routes,[58] reduced summer streamflows, species extinctions, and increases in the range of disease vectors.
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| − | | |
| − | Some effects on both the natural environment and human life are, at least in part, already being attributed to global warming. A 2001 report by the IPCC suggests that glacier retreat, ice shelf disruption such as that of the Larsen Ice Shelf, sea level rise, changes in rainfall patterns, and increased intensity and frequency of extreme weather events, are being attributed in part to global warming.[59] While changes are expected for overall patterns, intensity, and frequencies, it is difficult to attribute specific events to global warming. Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.[60]
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| − | Increasing deaths, displacements, and economic losses projected due to extreme weather attributed to global warming may be exacerbated by growing population densities in affected areas, although temperate regions are projected to experience some minor benefits, such as fewer deaths due to cold exposure.[61] A summary of probable effects and recent understanding can be found in the report made for the IPCC Third Assessment Report by Working Group II.[59] The newer IPCC Fourth Assessment Report summary reports that there is observational evidence for an increase in intense tropical cyclone activity in the North Atlantic Ocean since about 1970, in correlation with the increase in sea surface temperature, but that the detection of long-term trends is complicated by the quality of records prior to routine satellite observations. The summary also states that there is no clear trend in the annual worldwide number of tropical cyclones.[1]
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| − | | |
| − | Additional anticipated effects include sea level rise of 110 to 770 millimeters (0.36 to 2.5 ft) between 1990 and 2100,[62] repercussions to agriculture, possible slowing of the thermohaline circulation, reductions in the ozone layer, increased intensity of hurricanes and extreme weather events, lowering of ocean pH, and the spread of diseases such as malaria and dengue fever. One study predicts 18% to 35% of a sample of 1,103 animal and plant species would be extinct by 2050, based on future climate projections.[63] However, few mechanistic studies have documented extinctions due to recent climate change[64] and one study suggests that projected rates of extinction are uncertain.[65]
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| − | | |
| − | Economic
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | | |
| − | Main articles: Economics of global warming and Low-carbon economy
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| − | | |
| − | Some economists have tried to estimate the aggregate net economic costs of damages from climate change across the globe. Such estimates have so far failed to reach conclusive findings; in a survey of 100 estimates, the values ran from US$-10 per tonne of carbon (tC) (US$-3 per tonne of carbon dioxide) up to US$350/tC (US$95 per tonne of carbon dioxide), with a mean of US$43 per tonne of carbon (US$12 per tonne of carbon dioxide).[61] One widely publicized report on potential economic impact is the Stern Review; it suggests that extreme weather might reduce global gross domestic product by up to 1%, and that in a worst-case scenario global per capita consumption could fall 20%.[66] The report's methodology, advocacy and conclusions have been criticized by many economists, primarily around the Review's assumptions of discounting and its choices of scenarios,[67] while others have supported the general attempt to quantify economic risk, even if not the specific numbers.[68][69]
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| − | In a summary of economic cost associated with climate change, the United Nations Environment Programme emphasizes the risks to insurers, reinsurers, and banks of increasingly traumatic and costly weather events. Other economic sectors likely to face difficulties related to climate change include agriculture and transport. Developing countries, rather than the developed world, are at greatest economic risk.[70]
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| − | Security
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| − | | |
| − | In November 2007, the Center for Strategic and International Studies and the Center for a New American Security published a report highlighting the national security effects of climate change.[71] These security effects include increased competition for resources between countries, mass migration from the worst affected areas, challenges to the cohesion of major states threatened by the rise in sea levels, and, as a consequence of these factors, an increased risk of armed conflict, including even nuclear conflicts.
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| − | Adaptation and mitigation
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| − | | |
| − | Main articles: Adaptation to global warming, Mitigation of global warming, and Kyoto Protocol
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| − | | |
| − | The broad agreement among climate scientists that global temperatures will continue to increase has led some nations, states, corporations and individuals to implement actions to try to curtail global warming or adjust to it. Many environmental groups encourage action against global warming, often by the consumer, but also by community and regional organizations. Others have suggested a quota on worldwide fossil fuel production, citing a direct link between fossil fuel production and CO2 emissions.[72][73]
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| − | There has also been business action on climate change, including efforts at increased energy efficiency and limited moves towards use of alternative fuels. One important innovation has been the development of greenhouse gas emissions trading through which companies, in conjunction with government, agree to cap their emissions or to purchase credits from those below their allowances.
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| − | The world's primary international agreement on combating global warming is the Kyoto Protocol, an amendment to the United Nations Framework Convention on Climate Change (UNFCCC) negotiated in 1997. The Protocol now covers more than 160 countries globally and over 55% of global greenhouse gas emissions.[74] Only the United States and Kazakhstan have not ratified the treaty, with the United States historically being the world's largest emitter of greenhouse gas. This treaty expires in 2012, and international talks began in May 2007 on a future treaty to succeed the current one.[75]
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| − | Claiming "serious harm" to the United States economy and the exemption of "80 percent of the world, including major population centers" like China and India, from the treaty, George W. Bush contends that the Kyoto Protocol is an unfair and ineffective means of addressing global climate change concerns.[76] Still, various state, local, and regional governments within the United States have begun their own initiatives to indicate support and compliance with the Kyoto Protocol on a local basis. For example, the Regional Greenhouse Gas Initiative is a state-level emissions capping and trading program involving eight Northeastern U.S. states, which was founded on December 20, 2005.[77]
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| − | China and India, though exempt from its provisions as developing countries, have ratified the Kyoto Protocol. China may have passed the U.S. in total annual greenhouse gas emissions according to some recent studies. Chinese Premier Wen Jiabao has called on the nation to redouble its efforts to tackle pollution and global warming.[78]
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| − | The IPCC's Working Group III is responsible for crafting reports that deal with the mitigation of global warming and analyzing the costs and benefits of different approaches. In the 2007 IPCC Fourth Assessment Report, they conclude that no one technology or sector can be completely responsible for mitigating future warming. They find there are key practices and technologies in various sectors, such as energy supply, transportation, industry, and agriculture, that should be implemented to reduced global emissions. They estimate that stabilization of carbon dioxide equivalent between 445 and 710 ppm by 2030 will result in between a 0.6% increase and 3% decrease in global gross domestic product.[79]
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| − | Social and political debate
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| − | | |
| − | Main articles: Global warming controversy, Politics of global warming, and Economics of global warming
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| − | See also: Climate change denial
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| − | | |
| − | Per capita greenhouse gas emissions in 2000
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | | |
| − | Over the past several years, public perceptions and attitudes concerning the causes and importance of global warming have changed.[80] Increased awareness of the scientific findings surrounding global warming has resulted in political and economic debate. Poor regions, particularly Africa, appear at greatest risk from the suggested effects of global warming, while their actual emissions have been small compared to the developed world.[81] At the same time, developing country exemptions from provisions of the Kyoto Protocol have been criticized by the United States and Australia, and have been used as part of the rationale for continued non-ratification by the U.S.[82] In the Western world, the idea of human influence on climate has gained wider acceptance in Europe than in the United States.[83][84]
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| − | | |
| − | The issue of climate change has sparked debate weighing the benefits of limiting industrial emissions of greenhouse gases against the costs that such changes would entail. There has been discussion in several countries about the cost and benefits of adopting alternative energy sources in order to reduce carbon emissions.[85] Organizations and companies such as the Competitive Enterprise Institute and ExxonMobil have emphasized more conservative climate change scenarios while highlighting the potential economic cost of stricter controls.[86][87][88][89] Likewise, various environmental lobbies and a number of public figures have launched campaigns to emphasize the potential risks of climate change and promote the implementation of stricter controls. Some fossil fuel companies have scaled back their efforts in recent years,[90] or called for policies to reduce global warming.[91]
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| − | | |
| − | Another point of debate is the degree to which newly developed economies such as India and China should be expected to constrain their emissions. China's gross national CO2 emissions are expected to exceed those of the U.S. within the next few years, and may have already done so according to a 2006 report.[92] China has contended that it has less of an obligation to reduce emissions since its per capita emissions are roughly one-fifth that of the United States.[93] India, also exempt from Kyoto restrictions and another of the biggest sources of industrial emissions, has made similar assertions.[94] However, the U.S. contends that if they must bear the cost of reducing emissions, then China should do the same.[95]
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| − | | |
| − | Related climatic issues
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| − | | |
| − | Main articles: Ocean acidification, global dimming, and ozone depletion
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| − | | |
| − | A variety of issues are often raised in relation to global warming. One is ocean acidification. Increased atmospheric CO2 increases the amount of CO2 dissolved in the oceans.[96] CO2 dissolved in the ocean reacts with water to form carbonic acid, resulting in acidification. Ocean surface pH is estimated to have decreased from 8.25 near the beginning of the industrial era to 8.14 by 2004,[97] and is projected to decrease by a further 0.14 to 0.5 units by 2100 as the ocean absorbs more CO2.[1][98] Since organisms and ecosystems are adapted to a narrow range of pH, this raises extinction concerns, directly driven by increased atmospheric CO2, that could disrupt food webs and impact human societies that depend on marine ecosystem services.[99]
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| − | Global dimming, the gradual reduction in the amount of global direct irradiance at the Earth's surface, may have partially mitigated global warming in the late twentieth century. From 1960 to 1990 human-caused aerosols likely precipitated this effect. Scientists have stated with 66–90% confidence that the effects of human-caused aerosols, along with volcanic activity, have offset some of the global warming, and that greenhouse gases would have resulted in more warming than observed if not for these dimming agents.[1]
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| − | | |
| − | Ozone depletion, the steady decline in the total amount of ozone in Earth's stratosphere, is frequently cited in relation to global warming. Although there are areas of linkage, the relationship between the two is not strong.
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| − | | |
| − | See also
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| − | | |
| − | * Glossary of climate change
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| − | | |
| − | References
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| − | | |
| − | 1. ^ a b c d e f g h i Summary for Policymakers (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change (2007-02-05). Retrieved on 2007-02-02. “The updated 100-year linear trend (1906 to 2005) of 0.74°C [0.56°C to 0.92°C] is therefore larger than the corresponding trend for 1901 to 2000 given in the TAR of 0.6°C [0.4°C to 0.8°C].”
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| − | 2. ^ Hegerl, Gabriele C.; et al. (2007-05-07). Understanding and Attributing Climate Change (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 690. Intergovernmental Panel on Climate Change. Retrieved on 2007-05-20. “Recent estimates (Figure 9.9) indicate a relatively small combined effect of natural forcings on the global mean temperature evolution of the seconds half of the 20th century, with a small net cooling from the combined effects of solar and volcanic forcings”
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| − | 3. ^ Ammann, Caspar; et al. (2007-04-06). "Solar influence on climate during the past millennium: Results from ransient simulations with the NCAR Climate Simulation Model" (PDF). Proceedings of the National Academy of Sciences of the United States of America 104 (10): 3713–3718. “However, because of a lack of interactive ozone, the model cannot fully simulate features discussed in (44)." "While the NH temperatures of the high-scaled experiment are often colder than the lower bound from proxy data, the modeled decadal-scale NH surface temperature for the medium-scaled case falls within the uncertainty range of the available temperature reconstructions. The medium-scaled simulation also broadly reproduces the main features seen in the proxy records." "Without anthropogenic forcing, the 20th century warming is small. The simulations with only natural forcing components included yield an early 20th century peak warming of ≈0.2 °C (≈1950 AD), which is reduced to about half by the end of the century because of increased volcanism.”
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| − | 4. ^ A guide to facts and fictions about climate change. Royal Society (March 2005). Retrieved on 2007-11-18. “"However, the overwhelming majority of scientists who work on climate change agree on the main points"”
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| − | 5. ^ Climate Change: Basic Information. United States Environmental Protection Agency (2006-12-14). Retrieved on 2007-02-09. “In common usage, 'global warming' often refers to the warming that can occur as a result of increased emissions of greenhouse gases from human activities.”
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| − | 6. ^ United Nations Framework Convention on Climate Change, Article I. United Nations Framework Convention on Climate Change. Retrieved on 2007-01-15.
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| − | 10. ^ Joint science academies' statement: The science of climate change (ASP). Royal Society (2001-05-17). Retrieved on 2007-04-01. “The work of the Intergovernmental Panel on Climate Change (IPCC) represents the consensus of the international scientific community on climate change science”
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| − | 13. ^ Forster, Piers; et al. (2007-02-05). Changes in Atmospheric Constituents and in Radiative Forcing (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 188-193. Intergovernmental Panel on Climate Change. Retrieved on 2007-09-17.
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| − | 17. ^ Note that the Greenhouse Effect produces a temperature increase of about 33 °C (59 °F) with respect to black body predictions and not a surface temperature of 33 °C (91 °F) which is 32 °F higher. The average surface temperature is about 14 °C (57 °F). Also note that both the Celsius and Fahrenheit temperatures are expressed to 2 significant figures even though the conversion formula produces 3.
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| − | 66. ^ At-a-glance: The Stern Review. BBC (2006-10-30). Retrieved on 2007-04-29.
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| − | 67. ^ Tol and Yohe (2006) "A Review of the Stern Review" World Economics 7(4): 233-50. See also other critiques in World Economics 7(4).
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| − | 68. ^ Brad DeLong. Do unto others....
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| − | 93. ^ China: US should take lead on climate, by Michael Casey, Associated Press, 12/7/07.
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| − | 94. ^ India's glaciers give grim message on warming, by Somni Sengupta, 7/17/07, New York Times via oregonlive.com.
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| − | 95. ^ Chinese object to climate draft, BBC, 5/1/07; In Battle for U.S. Carbon Caps, Eyes and Efforts Focus on China,by Steven Mufson, Washington Post, 6/6/07.
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| − | 97. ^ Jacobson, Mark Z. (2005-04-02). "Studying ocean acidification with conservative, stable numerical schemes for nonequilibrium air-ocean exchange and ocean equilibrium chemistry" (PDF). Journal of Geophysical Research 110 (D7). doi:10.1029/2004JD005220. D07302. Retrieved on 2007-04-28.
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| − | 99. ^ Raven, John A.; et al. (2005-06-30). "Ocean acidification due to increasing atmospheric carbon dioxide" (ASP). Royal Society. Retrieved on 2007-05-04.
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| − | | |
| − | Global warming is the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.
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| − | | |
| − | The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 year period ending in 2005, which is higher than the earlier estimate of 0.6 ± 0.2 °C for the period ending in 2000.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations"[1] via the greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3] These basic conclusions have been endorsed by at least 30 scientific societies and academies of science, including all of the national academies of science of the major industrialized countries. While individual scientists have voiced disagreement with the conclusions of the IPCC, the overwhelming majority of scientists working on climate change are in agreement with the conclusions.[4]
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| − | | |
| − | Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[1] The range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a millennium even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]
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| − | Increasing global temperature will cause sea level to rise, and is expected to increase the intensity of extreme weather events and to change the amount and pattern of precipitation. Other effects of global warming include changes in agricultural yields, trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.
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| − | Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. There is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences. Most national governments have signed and ratified the Kyoto Protocol, aimed at reducing greenhouse gas emissions.
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| − | Contents
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| − | [hide]
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| − | | |
| − | * 1 Terminology
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| − | * 2 Causes
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| − | o 2.1 Greenhouse gases in the atmosphere
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| − | o 2.2 Feedbacks
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| − | o 2.3 Solar variation
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| − | * 3 Temperature changes
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| − | o 3.1 Recent
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| − | o 3.2 Pre-human climate variations
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| − | * 4 Climate models
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| − | * 5 Attributed and expected effects
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| − | o 5.1 Economic
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| − | o 5.2 Security
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| − | * 6 Adaptation and mitigation
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| − | * 7 Social and political debate
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| − | * 8 Related climatic issues
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| − | * 9 See also
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| − | * 10 References
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| − | * 11 Further reading
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| − | * 12 External links
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| − | | |
| − | Terminology
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| − | The term "global warming" is a specific example of the broader term climate change, which can also refer to global cooling. In common usage, the term refers to recent warming and implies a human influence.[5] The United Nations Framework Convention on Climate Change (UNFCCC) uses the term "climate change" for human-caused change, and "climate variability" for other changes.[6] The term "anthropogenic global warming" is sometimes used when focusing on human-induced changes.
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| − | | |
| − | Causes
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | | |
| − | Main articles: Attribution of recent climate change and scientific opinion on climate change
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| − | | |
| − | The Earth's climate changes in response to external forcing, including variations in its orbit around the sun (orbital forcing),[7][8][9] volcanic eruptions, and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[10][11] identifies elevated levels of greenhouse gases due to human activity as the main influence. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain the observed increase in mean global temperature. One such hypothesis proposes that warming may be the result of variations in solar activity.[12][13][14]
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| − | | |
| − | None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[15]
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| − | | |
| − | Greenhouse gases in the atmosphere
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| − | | |
| − | Main article: Greenhouse effect
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| − | | |
| − | The greenhouse effect was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. It is the process by which absorption and emission of infrared radiation by atmospheric gases warm a planet's atmosphere and surface.
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| − | | |
| − | Existence of the greenhouse effect as such is not disputed. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F), without which Earth would be uninhabitable.[16][17] Rather, the issue is how the strength of the greenhouse effect is changed when human activity increases the atmospheric concentrations of some greenhouse gases.
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| − | On Earth, the major greenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect (not including clouds); carbon dioxide (CO2), which causes 9–26%; methane (CH4), which causes 4–9%; and ozone, which causes 3–7%.[18][19] Some other naturally occurring gases contribute very small fractions of the greenhouse effect; one of these, nitrous oxide (N2O), is increasing in concentration owing to human activity such as agriculture. The atmospheric concentrations of CO2 and CH4 have increased by 31% and 149% respectively above pre-industrial levels since 1750. Molecule for molecule, methane is a more effective greenhouse gas than carbon dioxide, but its concentration is much smaller so that its total radiative forcing is only about a fourth of that from carbon dioxide. These levels are considerably higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores. From less direct geological evidence it is believed that CO2 values this high were last attained 20 million years ago.[20] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, in particular deforestation.[21]
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| − | The present atmospheric concentration of CO2 is about 383 parts per million (ppm) by volume.[22] Future CO2 levels are expected to rise due to ongoing burning of fossil fuels and land-use change. The rate of rise will depend on uncertain economic, sociological, technological, and natural developments, but may be ultimately limited by the availability of fossil fuels. The IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[23] Fossil fuel reserves are sufficient to reach this level and continue emissions past 2100, if coal, tar sands or methane clathrates are extensively used.[24]
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| − | Feedbacks
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| − | | |
| − | Main article: Effects of global warming#Further global warming (positive feedback)
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| − | | |
| − | The effects of forcing agents on the climate are complicated by various feedback processes.
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| − | One of the most pronounced feedback effects relates to the evaporation of water. In the case of warming by the addition of long-lived greenhouse gases such as CO2, the initial warming will cause more water to be evaporated into the atmosphere. Since water vapor itself acts as a greenhouse gas, this causes still more warming; the warming causes more water vapor to be evaporated, and so forth until a new dynamic equilibrium concentration of water vapor is reached with a much larger greenhouse effect than that due to CO2 alone. Although this feedback process involves an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[25] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.
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| − | | |
| − | Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models. Nevertheless, cloud feedback is second only to water vapor feedback and is positive in all the models that were used in the IPCC Fourth Assessment Report.[25]
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| − | | |
| − | Another important feedback process is ice-albedo feedback.[26] When global temperatures increase, ice near the poles melts at an increasing rate. As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.
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| − | | |
| − | Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism contributing to warming.[27] A massive release of CH4 from methane clathrates could cause rapid warming, according to the clathrate gun hypothesis.
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| − | The ocean's ability to sequester carbon is expected to decline as it warms, because the resulting low nutrient levels of the mesopelagic zone limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[28]
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| − | Solar variation
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| − | Solar variation over the last 30 years.
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| − | Solar variation over the last 30 years.
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| − | Main article: Solar variation
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| − | | |
| − | A few papers suggest that the Sun's contribution may have been underestimated. Two researchers at Duke University, Bruce West and Nicola Scafetta, have estimated that the Sun may have contributed about 45–50% of the increase in the average global surface temperature over the period 1900–2000, and about 25–35% between 1980 and 2000.[29] A paper by Peter Stott and other researchers suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.[30] They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases.
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| − | A different hypothesis is that variations in solar output, possibly amplified by cloud seeding via galactic cosmic rays, may have contributed to recent warming.[31] It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.[32]
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| − | One predicted effect of an increase in solar activity would be a warming of the stratosphere; however, the observed effect since at least 1960 has been a cooling of the lower stratosphere, which is one of the predicted results of greenhouse gas warming.[33] Reduction of stratospheric ozone also has a cooling influence, although substantial ozone depletion did not occur until the late 1970s. Solar variation combined with changes in volcanic activity probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.[1] In 2006, Peter Foukal and other researchers from the United States, Germany, and Switzerland found no net increase of solar brightness over the last thousand years. Solar cycles led to a small increase of 0.07% in brightness over the last 30 years. This effect is far too small to contribute significantly to global warming.[34][35] A paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in cosmic rays.[36] Henrik Svensmark and Eigil Friis-Christensen, the main proponents of cloud seeding by galactic cosmic rays, disputed the findings of Lockwood and Fröhlich.[37] Another recent study speculates that other bodies within the Solar System may influence the climate in a complex manner.[38]
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| − | Temperature changes
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | | |
| − | Main article: Temperature record
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| − | | |
| − | Recent
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| − | | |
| − | Global temperatures on both land and sea have increased by 0.75 °C (1.35 °F) relative to the period 1860–1900, according to the instrumental temperature record. This measured temperature increase is not significantly affected by the urban heat island effect.[39] Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[40] Temperatures in the lower troposphere have increased between 0.12 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with possibly regional fluctuations such as the Medieval Warm Period or the Little Ice Age.
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| − | Sea temperatures increase more slowly than those on land both because of the larger effective heat capacity of the oceans and because the ocean can lose heat by evaporation more readily than the land.[41] Since the Northern Hemisphere has more land mass than the Southern Hemisphere it warms faster; also there are extensive areas of seasonal snow cover subject to the snow-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the asymmetry of warming as the major gases are essentially well-mixed between hemispheres.
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| − | Based on estimates by NASA's Goddard Institute for Space Studies, 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[42] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit concluded that 2005 was the second warmest year, behind 1998.[43][44]
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| − | Anthropogenic emissions of other pollutants—notably sulfate aerosols—can exert a cooling effect by increasing the reflection of incoming sunlight. This partially accounts for the cooling seen in the temperature record in the middle of the twentieth century,[45] though the cooling may also be due in part to natural variability. James Hansen and colleagues have proposed that the effects of the products of fossil fuel combustion—CO2 and aerosols—have largely offset one another, so that warming in recent decades has been driven mainly by non-CO2 greenhouse gases.[46]
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| − | Paleoclimatologist William Ruddiman has argued that human influence on the global climate began around 8,000 years ago with the start of forest clearing to provide land for agriculture and 5,000 years ago with the start of Asian rice irrigation.[47] Ruddiman's interpretation of the historical record, with respect to the methane data, has been disputed.[48]
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| − | Pre-human climate variations
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Further information: Paleoclimatology
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| − | See also: Snowball Earth
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| − | | |
| − | Earth has experienced warming and cooling many times in the past. The recent Antarctic EPICA ice core spans 800,000 years, including eight glacial cycles timed by orbital variations with interglacial warm periods comparable to present temperatures.[49]
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| − | A rapid buildup of greenhouse gases caused warming in the early Jurassic period (about 180 million years ago), with average temperatures rising by 5 °C (9 °F). Research by the Open University indicates that the warming caused the rate of rock weathering to increase by 400%. As such weathering locks away carbon in calcite and dolomite, CO2 levels dropped back to normal over roughly the next 150,000 years.[50][51]
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| − | | |
| − | Sudden releases of methane from clathrate compounds (the clathrate gun hypothesis) have been hypothesized as a cause for other warming events in the distant past, including the Permian-Triassic extinction event (about 251 million years ago) and the Paleocene-Eocene Thermal Maximum (about 55 million years ago).
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| − | Climate models
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | | |
| − | Main article: Global climate model
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| − | | |
| − | Scientists have studied global warming with computer models of the climate. These models are based on physical principles of fluid dynamics, radiative transfer, and other processes, with simplifications being necessary because of limitations in computer power and the complexity of the underlying system (climate). These models predict that the effect of adding greenhouse gases is to produce a warmer climate.[52] However, even when the same assumptions of future greenhouse gas levels are used, there still remains a considerable range of climate sensitivity.
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| − | Including uncertainties in future greenhouse gas concentrations and climate modeling, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999.[1] Models have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes.
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| − | Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.[53] These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.
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| − | | |
| − | Most global climate models, when run to project future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.[54][55][56]
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| − | The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem.[57] There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability.
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| − | Attributed and expected effects
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| − | | |
| − | Main article: Effects of global warming
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| − | | |
| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Although it is difficult to connect specific weather events to global warming, an increase in global temperatures may in turn cause broader changes, including glacial retreat, Arctic shrinkage, and worldwide sea level rise. Changes in the amount and pattern of precipitation may result in flooding and drought. There may also be changes in the frequency and intensity of extreme weather events. Other effects may include changes in agricultural yields, addition of new trade routes,[58] reduced summer streamflows, species extinctions, and increases in the range of disease vectors.
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| − | | |
| − | Some effects on both the natural environment and human life are, at least in part, already being attributed to global warming. A 2001 report by the IPCC suggests that glacier retreat, ice shelf disruption such as that of the Larsen Ice Shelf, sea level rise, changes in rainfall patterns, and increased intensity and frequency of extreme weather events, are being attributed in part to global warming.[59] While changes are expected for overall patterns, intensity, and frequencies, it is difficult to attribute specific events to global warming. Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.[60]
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| − | Increasing deaths, displacements, and economic losses projected due to extreme weather attributed to global warming may be exacerbated by growing population densities in affected areas, although temperate regions are projected to experience some minor benefits, such as fewer deaths due to cold exposure.[61] A summary of probable effects and recent understanding can be found in the report made for the IPCC Third Assessment Report by Working Group II.[59] The newer IPCC Fourth Assessment Report summary reports that there is observational evidence for an increase in intense tropical cyclone activity in the North Atlantic Ocean since about 1970, in correlation with the increase in sea surface temperature, but that the detection of long-term trends is complicated by the quality of records prior to routine satellite observations. The summary also states that there is no clear trend in the annual worldwide number of tropical cyclones.[1]
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| − | Additional anticipated effects include sea level rise of 110 to 770 millimeters (0.36 to 2.5 ft) between 1990 and 2100,[62] repercussions to agriculture, possible slowing of the thermohaline circulation, reductions in the ozone layer, increased intensity of hurricanes and extreme weather events, lowering of ocean pH, and the spread of diseases such as malaria and dengue fever. One study predicts 18% to 35% of a sample of 1,103 animal and plant species would be extinct by 2050, based on future climate projections.[63] However, few mechanistic studies have documented extinctions due to recent climate change[64] and one study suggests that projected rates of extinction are uncertain.[65]
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| − | Economic
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | Main articles: Economics of global warming and Low-carbon economy
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| − | | |
| − | Some economists have tried to estimate the aggregate net economic costs of damages from climate change across the globe. Such estimates have so far failed to reach conclusive findings; in a survey of 100 estimates, the values ran from US$-10 per tonne of carbon (tC) (US$-3 per tonne of carbon dioxide) up to US$350/tC (US$95 per tonne of carbon dioxide), with a mean of US$43 per tonne of carbon (US$12 per tonne of carbon dioxide).[61] One widely publicized report on potential economic impact is the Stern Review; it suggests that extreme weather might reduce global gross domestic product by up to 1%, and that in a worst-case scenario global per capita consumption could fall 20%.[66] The report's methodology, advocacy and conclusions have been criticized by many economists, primarily around the Review's assumptions of discounting and its choices of scenarios,[67] while others have supported the general attempt to quantify economic risk, even if not the specific numbers.[68][69]
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| − | In a summary of economic cost associated with climate change, the United Nations Environment Programme emphasizes the risks to insurers, reinsurers, and banks of increasingly traumatic and costly weather events. Other economic sectors likely to face difficulties related to climate change include agriculture and transport. Developing countries, rather than the developed world, are at greatest economic risk.[70]
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| − | Security
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| − | In November 2007, the Center for Strategic and International Studies and the Center for a New American Security published a report highlighting the national security effects of climate change.[71] These security effects include increased competition for resources between countries, mass migration from the worst affected areas, challenges to the cohesion of major states threatened by the rise in sea levels, and, as a consequence of these factors, an increased risk of armed conflict, including even nuclear conflicts.
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| − | Adaptation and mitigation
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| − | | |
| − | Main articles: Adaptation to global warming, Mitigation of global warming, and Kyoto Protocol
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| − | | |
| − | The broad agreement among climate scientists that global temperatures will continue to increase has led some nations, states, corporations and individuals to implement actions to try to curtail global warming or adjust to it. Many environmental groups encourage action against global warming, often by the consumer, but also by community and regional organizations. Others have suggested a quota on worldwide fossil fuel production, citing a direct link between fossil fuel production and CO2 emissions.[72][73]
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| − | There has also been business action on climate change, including efforts at increased energy efficiency and limited moves towards use of alternative fuels. One important innovation has been the development of greenhouse gas emissions trading through which companies, in conjunction with government, agree to cap their emissions or to purchase credits from those below their allowances.
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| − | | |
| − | The world's primary international agreement on combating global warming is the Kyoto Protocol, an amendment to the United Nations Framework Convention on Climate Change (UNFCCC) negotiated in 1997. The Protocol now covers more than 160 countries globally and over 55% of global greenhouse gas emissions.[74] Only the United States and Kazakhstan have not ratified the treaty, with the United States historically being the world's largest emitter of greenhouse gas. This treaty expires in 2012, and international talks began in May 2007 on a future treaty to succeed the current one.[75]
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| − | Claiming "serious harm" to the United States economy and the exemption of "80 percent of the world, including major population centers" like China and India, from the treaty, George W. Bush contends that the Kyoto Protocol is an unfair and ineffective means of addressing global climate change concerns.[76] Still, various state, local, and regional governments within the United States have begun their own initiatives to indicate support and compliance with the Kyoto Protocol on a local basis. For example, the Regional Greenhouse Gas Initiative is a state-level emissions capping and trading program involving eight Northeastern U.S. states, which was founded on December 20, 2005.[77]
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| − | China and India, though exempt from its provisions as developing countries, have ratified the Kyoto Protocol. China may have passed the U.S. in total annual greenhouse gas emissions according to some recent studies. Chinese Premier Wen Jiabao has called on the nation to redouble its efforts to tackle pollution and global warming.[78]
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| − | The IPCC's Working Group III is responsible for crafting reports that deal with the mitigation of global warming and analyzing the costs and benefits of different approaches. In the 2007 IPCC Fourth Assessment Report, they conclude that no one technology or sector can be completely responsible for mitigating future warming. They find there are key practices and technologies in various sectors, such as energy supply, transportation, industry, and agriculture, that should be implemented to reduced global emissions. They estimate that stabilization of carbon dioxide equivalent between 445 and 710 ppm by 2030 will result in between a 0.6% increase and 3% decrease in global gross domestic product.[79]
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| − | | |
| − | Social and political debate
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| − | | |
| − | Main articles: Global warming controversy, Politics of global warming, and Economics of global warming
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| − | See also: Climate change denial
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| − | | |
| − | Per capita greenhouse gas emissions in 2000
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | | |
| − | Over the past several years, public perceptions and attitudes concerning the causes and importance of global warming have changed.[80] Increased awareness of the scientific findings surrounding global warming has resulted in political and economic debate. Poor regions, particularly Africa, appear at greatest risk from the suggested effects of global warming, while their actual emissions have been small compared to the developed world.[81] At the same time, developing country exemptions from provisions of the Kyoto Protocol have been criticized by the United States and Australia, and have been used as part of the rationale for continued non-ratification by the U.S.[82] In the Western world, the idea of human influence on climate has gained wider acceptance in Europe than in the United States.[83][84]
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| − | The issue of climate change has sparked debate weighing the benefits of limiting industrial emissions of greenhouse gases against the costs that such changes would entail. There has been discussion in several countries about the cost and benefits of adopting alternative energy sources in order to reduce carbon emissions.[85] Organizations and companies such as the Competitive Enterprise Institute and ExxonMobil have emphasized more conservative climate change scenarios while highlighting the potential economic cost of stricter controls.[86][87][88][89] Likewise, various environmental lobbies and a number of public figures have launched campaigns to emphasize the potential risks of climate change and promote the implementation of stricter controls. Some fossil fuel companies have scaled back their efforts in recent years,[90] or called for policies to reduce global warming.[91]
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| − | Another point of debate is the degree to which newly developed economies such as India and China should be expected to constrain their emissions. China's gross national CO2 emissions are expected to exceed those of the U.S. within the next few years, and may have already done so according to a 2006 report.[92] China has contended that it has less of an obligation to reduce emissions since its per capita emissions are roughly one-fifth that of the United States.[93] India, also exempt from Kyoto restrictions and another of the biggest sources of industrial emissions, has made similar assertions.[94] However, the U.S. contends that if they must bear the cost of reducing emissions, then China should do the same.[95]
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| − | | |
| − | Related climatic issues
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| − | | |
| − | Main articles: Ocean acidification, global dimming, and ozone depletion
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| − | | |
| − | A variety of issues are often raised in relation to global warming. One is ocean acidification. Increased atmospheric CO2 increases the amount of CO2 dissolved in the oceans.[96] CO2 dissolved in the ocean reacts with water to form carbonic acid, resulting in acidification. Ocean surface pH is estimated to have decreased from 8.25 near the beginning of the industrial era to 8.14 by 2004,[97] and is projected to decrease by a further 0.14 to 0.5 units by 2100 as the ocean absorbs more CO2.[1][98] Since organisms and ecosystems are adapted to a narrow range of pH, this raises extinction concerns, directly driven by increased atmospheric CO2, that could disrupt food webs and impact human societies that depend on marine ecosystem services.[99]
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| − | Global dimming, the gradual reduction in the amount of global direct irradiance at the Earth's surface, may have partially mitigated global warming in the late twentieth century. From 1960 to 1990 human-caused aerosols likely precipitated this effect. Scientists have stated with 66–90% confidence that the effects of human-caused aerosols, along with volcanic activity, have offset some of the global warming, and that greenhouse gases would have resulted in more warming than observed if not for these dimming agents.[1]
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| − | | |
| − | Ozone depletion, the steady decline in the total amount of ozone in Earth's stratosphere, is frequently cited in relation to global warming. Although there are areas of linkage, the relationship between the two is not strong.
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| − | | |
| − | See also
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| − | | |
| − | * Glossary of climate change
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| − | | |
| − | References
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| − | | |
| − | 1. ^ a b c d e f g h i Summary for Policymakers (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change (2007-02-05). Retrieved on 2007-02-02. “The updated 100-year linear trend (1906 to 2005) of 0.74°C [0.56°C to 0.92°C] is therefore larger than the corresponding trend for 1901 to 2000 given in the TAR of 0.6°C [0.4°C to 0.8°C].”
| |
| − | 2. ^ Hegerl, Gabriele C.; et al. (2007-05-07). Understanding and Attributing Climate Change (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 690. Intergovernmental Panel on Climate Change. Retrieved on 2007-05-20. “Recent estimates (Figure 9.9) indicate a relatively small combined effect of natural forcings on the global mean temperature evolution of the seconds half of the 20th century, with a small net cooling from the combined effects of solar and volcanic forcings”
| |
| − | 3. ^ Ammann, Caspar; et al. (2007-04-06). "Solar influence on climate during the past millennium: Results from ransient simulations with the NCAR Climate Simulation Model" (PDF). Proceedings of the National Academy of Sciences of the United States of America 104 (10): 3713–3718. “However, because of a lack of interactive ozone, the model cannot fully simulate features discussed in (44)." "While the NH temperatures of the high-scaled experiment are often colder than the lower bound from proxy data, the modeled decadal-scale NH surface temperature for the medium-scaled case falls within the uncertainty range of the available temperature reconstructions. The medium-scaled simulation also broadly reproduces the main features seen in the proxy records." "Without anthropogenic forcing, the 20th century warming is small. The simulations with only natural forcing components included yield an early 20th century peak warming of ≈0.2 °C (≈1950 AD), which is reduced to about half by the end of the century because of increased volcanism.”
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| − | 4. ^ A guide to facts and fictions about climate change. Royal Society (March 2005). Retrieved on 2007-11-18. “"However, the overwhelming majority of scientists who work on climate change agree on the main points"”
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| − | 5. ^ Climate Change: Basic Information. United States Environmental Protection Agency (2006-12-14). Retrieved on 2007-02-09. “In common usage, 'global warming' often refers to the warming that can occur as a result of increased emissions of greenhouse gases from human activities.”
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| − | 6. ^ United Nations Framework Convention on Climate Change, Article I. United Nations Framework Convention on Climate Change. Retrieved on 2007-01-15.
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| − | 7. ^ Berger, A.; et al. (2005-12-10). "On the origin of the 100-kyr cycles in the astronomical forcing". Paleoceanography 20 (4). PA4019. Retrieved on 2007-11-05.
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| − | 8. ^ Genthon, C.; et al. (1987-10-01). "Vostok Ice Core - Climatic response to CO2 and orbital forcing changes over the last climatic cycle". Nature 329 (6138): 414–418. Retrieved on 2007-11-05.
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| − | 9. ^ Alley, Richard B.; et al. (January 2002). "A northern lead in the orbital band: north-south phasing of Ice-Age events". Quaternary Science Reviews 21 (1-3): 431–441. Retrieved on 2007-11-05.
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| − | 10. ^ Joint science academies' statement: The science of climate change (ASP). Royal Society (2001-05-17). Retrieved on 2007-04-01. “The work of the Intergovernmental Panel on Climate Change (IPCC) represents the consensus of the international scientific community on climate change science”
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| − | 11. ^ (2007-10-18) "Rising to the climate challenge". Nature 449 (7164). Retrieved on 2007-11-06.
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| − | 12. ^ Svensmark, Henrik (February 2007). "Cosmoclimatology: a new theory emerges". Astronomy & Geophysics 48 (1): 18-24. doi:10.1111/j.1468-4004.2007.48118.x.
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| − | 13. ^ Forster, Piers; et al. (2007-02-05). Changes in Atmospheric Constituents and in Radiative Forcing (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 188-193. Intergovernmental Panel on Climate Change. Retrieved on 2007-09-17.
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| − | 14. ^ Bard, Edouard; Frank, Martin (2006-06-09). "Climate change and solar variability: What's new under the sun?". Earth and Planetary Science Letters 248 (1-2): 1-14. Retrieved on 2007-09-17.
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| − | 15. ^ Meehl, Gerald A.; et al. (2005-03-18). "How Much More Global Warming and Sea Level Rise" (PDF). Science 307 (5716): 1769–1772. doi:10.1126/science.1106663. Retrieved on 2007-02-11.
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| − | 16. ^ IPCC WG1 AR4 Report — Chapter 1: Historical Overview of Climate Change Science (PDF). IPCC WG1 AR4 Report p97 (pdf page 5 of 36). IPCC (2007). Retrieved on 2007-10-07. “To emit 240 W m–2, a surface would have to have a temperature of around –19 °C. This is much colder than the conditions that actually exist at the Earth’s surface (the global mean surface temperature is about 14 °C). Instead, the necessary –19 °C is found at an altitude about 5 km above the surface.”
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| − | 17. ^ Note that the Greenhouse Effect produces a temperature increase of about 33 °C (59 °F) with respect to black body predictions and not a surface temperature of 33 °C (91 °F) which is 32 °F higher. The average surface temperature is about 14 °C (57 °F). Also note that both the Celsius and Fahrenheit temperatures are expressed to 2 significant figures even though the conversion formula produces 3.
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| − | 24. ^ 4.4.6. Resource Availability. IPCC Special Report on Emissions Scenarios. Intergovernmental Panel on Climate Change. Retrieved on 2007-04-28.
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| − | 26. ^ Stocker, Thomas F.; et al. (2001-01-20). 7.5.2 Sea Ice. Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change. Retrieved on 2007-02-11.
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| − | 64. ^ McLaughlin, John F.; et al. (2002-04-30). "Climate change hastens population extinctions" (PDF). PNAS 99 (9): 6070–6074. doi:10.1073/pnas.052131199. Retrieved on 2007-03-29.
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| − | 65. ^ Botkin, Daniel B.; et al. (March 2007). "Forecasting the Effects of Global Warming on Biodiversity". BioScience 57 (3): 227–236. doi:10.1641/B570306. Retrieved on 2007-11-30.
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| − | 66. ^ At-a-glance: The Stern Review. BBC (2006-10-30). Retrieved on 2007-04-29.
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| − | 67. ^ Tol and Yohe (2006) "A Review of the Stern Review" World Economics 7(4): 233-50. See also other critiques in World Economics 7(4).
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| − | 68. ^ Brad DeLong. Do unto others....
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| − | 69. ^ John Quiggin. Stern and the critics on discounting.
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| − | 73. ^ Monbiot, George. Rigged - The climate talks are a stitch-up, as no one is talking about supply. (HTML). Retrieved on 2007-12-22.
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| − | 85. ^ "EU agrees on carbon dioxide cuts", BCC, 2007-03-09. Retrieved on 2007-05-04.
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| − | 93. ^ China: US should take lead on climate, by Michael Casey, Associated Press, 12/7/07.
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| − | 94. ^ India's glaciers give grim message on warming, by Somni Sengupta, 7/17/07, New York Times via oregonlive.com.
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| − | 95. ^ Chinese object to climate draft, BBC, 5/1/07; In Battle for U.S. Carbon Caps, Eyes and Efforts Focus on China,by Steven Mufson, Washington Post, 6/6/07.
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| − | | |
| − | Global warming is the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.
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| − | | |
| − | The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 year period ending in 2005, which is higher than the earlier estimate of 0.6 ± 0.2 °C for the period ending in 2000.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations"[1] via the greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3] These basic conclusions have been endorsed by at least 30 scientific societies and academies of science, including all of the national academies of science of the major industrialized countries. While individual scientists have voiced disagreement with the conclusions of the IPCC, the overwhelming majority of scientists working on climate change are in agreement with the conclusions.[4]
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| − | | |
| − | Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the 21st century.[1] The range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a millennium even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]
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| − | | |
| − | Increasing global temperature will cause sea level to rise, and is expected to increase the intensity of extreme weather events and to change the amount and pattern of precipitation. Other effects of global warming include changes in agricultural yields, trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.
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| − | | |
| − | Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. There is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences. Most national governments have signed and ratified the Kyoto Protocol, aimed at reducing greenhouse gas emissions.
| |
| − | Contents
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| − | [hide]
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| − | | |
| − | * 1 Terminology
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| − | * 2 Causes
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| − | o 2.1 Greenhouse gases in the atmosphere
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| − | o 2.2 Feedbacks
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| − | o 2.3 Solar variation
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| − | * 3 Temperature changes
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| − | o 3.1 Recent
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| − | o 3.2 Pre-human climate variations
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| − | * 4 Climate models
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| − | * 5 Attributed and expected effects
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| − | o 5.1 Economic
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| − | o 5.2 Security
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| − | * 6 Adaptation and mitigation
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| − | * 7 Social and political debate
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| − | * 8 Related climatic issues
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| − | * 9 See also
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| − | * 10 References
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| − | * 11 Further reading
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| − | * 12 External links
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| − | | |
| − | Terminology
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| − | | |
| − | The term "global warming" is a specific example of the broader term climate change, which can also refer to global cooling. In common usage, the term refers to recent warming and implies a human influence.[5] The United Nations Framework Convention on Climate Change (UNFCCC) uses the term "climate change" for human-caused change, and "climate variability" for other changes.[6] The term "anthropogenic global warming" is sometimes used when focusing on human-induced changes.
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| − | | |
| − | Causes
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Carbon dioxide during the last 400,000 years and (inset above) the rapid rise since the Industrial Revolution; changes in the Earth's orbit around the Sun, known as Milankovitch cycles, are believed to be the pacemaker of the 100,000 year ice age cycle.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | Recent increases in atmospheric carbon dioxide (CO2). The monthly CO2 measurements display small seasonal oscillations in an overall yearly uptrend; each year's maximum is reached during the Northern Hemisphere's late spring, and declines during the Northern Hemisphere growing season as plants remove some CO2 from the atmosphere.
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| − | | |
| − | Main articles: Attribution of recent climate change and scientific opinion on climate change
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| − | | |
| − | The Earth's climate changes in response to external forcing, including variations in its orbit around the sun (orbital forcing),[7][8][9] volcanic eruptions, and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[10][11] identifies elevated levels of greenhouse gases due to human activity as the main influence. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain the observed increase in mean global temperature. One such hypothesis proposes that warming may be the result of variations in solar activity.[12][13][14]
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| − | | |
| − | None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[15]
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| − | | |
| − | Greenhouse gases in the atmosphere
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| − | | |
| − | Main article: Greenhouse effect
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| − | | |
| − | The greenhouse effect was discovered by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. It is the process by which absorption and emission of infrared radiation by atmospheric gases warm a planet's atmosphere and surface.
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| − | Existence of the greenhouse effect as such is not disputed. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F), without which Earth would be uninhabitable.[16][17] Rather, the issue is how the strength of the greenhouse effect is changed when human activity increases the atmospheric concentrations of some greenhouse gases.
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| − | On Earth, the major greenhouse gases are water vapor, which causes about 36–70% of the greenhouse effect (not including clouds); carbon dioxide (CO2), which causes 9–26%; methane (CH4), which causes 4–9%; and ozone, which causes 3–7%.[18][19] Some other naturally occurring gases contribute very small fractions of the greenhouse effect; one of these, nitrous oxide (N2O), is increasing in concentration owing to human activity such as agriculture. The atmospheric concentrations of CO2 and CH4 have increased by 31% and 149% respectively above pre-industrial levels since 1750. Molecule for molecule, methane is a more effective greenhouse gas than carbon dioxide, but its concentration is much smaller so that its total radiative forcing is only about a fourth of that from carbon dioxide. These levels are considerably higher than at any time during the last 650,000 years, the period for which reliable data has been extracted from ice cores. From less direct geological evidence it is believed that CO2 values this high were last attained 20 million years ago.[20] Fossil fuel burning has produced about three-quarters of the increase in CO2 from human activity over the past 20 years. Most of the rest is due to land-use change, in particular deforestation.[21]
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| − | The present atmospheric concentration of CO2 is about 383 parts per million (ppm) by volume.[22] Future CO2 levels are expected to rise due to ongoing burning of fossil fuels and land-use change. The rate of rise will depend on uncertain economic, sociological, technological, and natural developments, but may be ultimately limited by the availability of fossil fuels. The IPCC Special Report on Emissions Scenarios gives a wide range of future CO2 scenarios, ranging from 541 to 970 ppm by the year 2100.[23] Fossil fuel reserves are sufficient to reach this level and continue emissions past 2100, if coal, tar sands or methane clathrates are extensively used.[24]
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| − | Feedbacks
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| − | | |
| − | Main article: Effects of global warming#Further global warming (positive feedback)
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| − | | |
| − | The effects of forcing agents on the climate are complicated by various feedback processes.
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| − | One of the most pronounced feedback effects relates to the evaporation of water. In the case of warming by the addition of long-lived greenhouse gases such as CO2, the initial warming will cause more water to be evaporated into the atmosphere. Since water vapor itself acts as a greenhouse gas, this causes still more warming; the warming causes more water vapor to be evaporated, and so forth until a new dynamic equilibrium concentration of water vapor is reached with a much larger greenhouse effect than that due to CO2 alone. Although this feedback process involves an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[25] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.
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| − | Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models. Nevertheless, cloud feedback is second only to water vapor feedback and is positive in all the models that were used in the IPCC Fourth Assessment Report.[25]
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| − | | |
| − | Another important feedback process is ice-albedo feedback.[26] When global temperatures increase, ice near the poles melts at an increasing rate. As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.
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| − | | |
| − | Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism contributing to warming.[27] A massive release of CH4 from methane clathrates could cause rapid warming, according to the clathrate gun hypothesis.
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| − | The ocean's ability to sequester carbon is expected to decline as it warms, because the resulting low nutrient levels of the mesopelagic zone limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[28]
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| − | Solar variation
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| − | Solar variation over the last 30 years.
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| − | Solar variation over the last 30 years.
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| − | Main article: Solar variation
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| − | | |
| − | A few papers suggest that the Sun's contribution may have been underestimated. Two researchers at Duke University, Bruce West and Nicola Scafetta, have estimated that the Sun may have contributed about 45–50% of the increase in the average global surface temperature over the period 1900–2000, and about 25–35% between 1980 and 2000.[29] A paper by Peter Stott and other researchers suggests that climate models overestimate the relative effect of greenhouse gases compared to solar forcing; they also suggest that the cooling effects of volcanic dust and sulfate aerosols have been underestimated.[30] They nevertheless conclude that even with an enhanced climate sensitivity to solar forcing, most of the warming since the mid-20th century is likely attributable to the increases in greenhouse gases.
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| − | A different hypothesis is that variations in solar output, possibly amplified by cloud seeding via galactic cosmic rays, may have contributed to recent warming.[31] It suggests magnetic activity of the sun is a crucial factor which deflects cosmic rays that may influence the generation of cloud condensation nuclei and thereby affect the climate.[32]
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| − | One predicted effect of an increase in solar activity would be a warming of the stratosphere; however, the observed effect since at least 1960 has been a cooling of the lower stratosphere, which is one of the predicted results of greenhouse gas warming.[33] Reduction of stratospheric ozone also has a cooling influence, although substantial ozone depletion did not occur until the late 1970s. Solar variation combined with changes in volcanic activity probably did have a warming effect from pre-industrial times to 1950, but a cooling effect since.[1] In 2006, Peter Foukal and other researchers from the United States, Germany, and Switzerland found no net increase of solar brightness over the last thousand years. Solar cycles led to a small increase of 0.07% in brightness over the last 30 years. This effect is far too small to contribute significantly to global warming.[34][35] A paper by Mike Lockwood and Claus Fröhlich found no relation between global warming and solar radiation since 1985, whether through variations in solar output or variations in cosmic rays.[36] Henrik Svensmark and Eigil Friis-Christensen, the main proponents of cloud seeding by galactic cosmic rays, disputed the findings of Lockwood and Fröhlich.[37] Another recent study speculates that other bodies within the Solar System may influence the climate in a complex manner.[38]
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| − | Temperature changes
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | Two millennia of mean surface temperatures according to different reconstructions, each smoothed on a decadal scale. The unsmoothed, annual value for 2004 is also plotted for reference.
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| − | | |
| − | Main article: Temperature record
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| − | | |
| − | Recent
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| − | Global temperatures on both land and sea have increased by 0.75 °C (1.35 °F) relative to the period 1860–1900, according to the instrumental temperature record. This measured temperature increase is not significantly affected by the urban heat island effect.[39] Since 1979, land temperatures have increased about twice as fast as ocean temperatures (0.25 °C per decade against 0.13 °C per decade).[40] Temperatures in the lower troposphere have increased between 0.12 and 0.22 °C (0.22 and 0.4 °F) per decade since 1979, according to satellite temperature measurements. Temperature is believed to have been relatively stable over the one or two thousand years before 1850, with possibly regional fluctuations such as the Medieval Warm Period or the Little Ice Age.
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| − | Sea temperatures increase more slowly than those on land both because of the larger effective heat capacity of the oceans and because the ocean can lose heat by evaporation more readily than the land.[41] Since the Northern Hemisphere has more land mass than the Southern Hemisphere it warms faster; also there are extensive areas of seasonal snow cover subject to the snow-albedo feedback. Although more greenhouse gases are emitted in the Northern than Southern Hemisphere this does not contribute to the asymmetry of warming as the major gases are essentially well-mixed between hemispheres.
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| − | Based on estimates by NASA's Goddard Institute for Space Studies, 2005 was the warmest year since reliable, widespread instrumental measurements became available in the late 1800s, exceeding the previous record set in 1998 by a few hundredths of a degree.[42] Estimates prepared by the World Meteorological Organization and the Climatic Research Unit concluded that 2005 was the second warmest year, behind 1998.[43][44]
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| − | Anthropogenic emissions of other pollutants—notably sulfate aerosols—can exert a cooling effect by increasing the reflection of incoming sunlight. This partially accounts for the cooling seen in the temperature record in the middle of the twentieth century,[45] though the cooling may also be due in part to natural variability. James Hansen and colleagues have proposed that the effects of the products of fossil fuel combustion—CO2 and aerosols—have largely offset one another, so that warming in recent decades has been driven mainly by non-CO2 greenhouse gases.[46]
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| − | | |
| − | Paleoclimatologist William Ruddiman has argued that human influence on the global climate began around 8,000 years ago with the start of forest clearing to provide land for agriculture and 5,000 years ago with the start of Asian rice irrigation.[47] Ruddiman's interpretation of the historical record, with respect to the methane data, has been disputed.[48]
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| − | | |
| − | Pre-human climate variations
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | Curves of reconstructed temperature at two locations in Antarctica and a global record of variations in glacial ice volume. Today's date is on the left side of the graph.
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| − | | |
| − | Further information: Paleoclimatology
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| − | See also: Snowball Earth
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| − | | |
| − | Earth has experienced warming and cooling many times in the past. The recent Antarctic EPICA ice core spans 800,000 years, including eight glacial cycles timed by orbital variations with interglacial warm periods comparable to present temperatures.[49]
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| − | | |
| − | A rapid buildup of greenhouse gases caused warming in the early Jurassic period (about 180 million years ago), with average temperatures rising by 5 °C (9 °F). Research by the Open University indicates that the warming caused the rate of rock weathering to increase by 400%. As such weathering locks away carbon in calcite and dolomite, CO2 levels dropped back to normal over roughly the next 150,000 years.[50][51]
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| − | | |
| − | Sudden releases of methane from clathrate compounds (the clathrate gun hypothesis) have been hypothesized as a cause for other warming events in the distant past, including the Permian-Triassic extinction event (about 251 million years ago) and the Paleocene-Eocene Thermal Maximum (about 55 million years ago).
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| − | Climate models
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | Calculations of global warming prepared in or before 2001 from a range of climate models under the SRES A2 emissions scenario, which assumes no action is taken to reduce emissions.
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | The geographic distribution of surface warming during the 21st century calculated by the HadCM3 climate model if a business as usual scenario is assumed for economic growth and greenhouse gas emissions. In this figure, the globally averaged warming corresponds to 3.0 °C (5.4 °F).
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| − | | |
| − | Main article: Global climate model
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| − | | |
| − | Scientists have studied global warming with computer models of the climate. These models are based on physical principles of fluid dynamics, radiative transfer, and other processes, with simplifications being necessary because of limitations in computer power and the complexity of the underlying system (climate). These models predict that the effect of adding greenhouse gases is to produce a warmer climate.[52] However, even when the same assumptions of future greenhouse gas levels are used, there still remains a considerable range of climate sensitivity.
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| − | Including uncertainties in future greenhouse gas concentrations and climate modeling, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999.[1] Models have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes.
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| − | Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.[53] These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.
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| − | | |
| − | Most global climate models, when run to project future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.[54][55][56]
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| − | The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem.[57] There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability.
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| − | | |
| − | Attributed and expected effects
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| − | | |
| − | Main article: Effects of global warming
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| − | | |
| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | Sparse records indicate that glaciers have been retreating since the early 1800s. In the 1950s measurements began that allow the monitoring of glacial mass balance, reported to the WGMS and the NSIDC.
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| − | | |
| − | Although it is difficult to connect specific weather events to global warming, an increase in global temperatures may in turn cause broader changes, including glacial retreat, Arctic shrinkage, and worldwide sea level rise. Changes in the amount and pattern of precipitation may result in flooding and drought. There may also be changes in the frequency and intensity of extreme weather events. Other effects may include changes in agricultural yields, addition of new trade routes,[58] reduced summer streamflows, species extinctions, and increases in the range of disease vectors.
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| − | | |
| − | Some effects on both the natural environment and human life are, at least in part, already being attributed to global warming. A 2001 report by the IPCC suggests that glacier retreat, ice shelf disruption such as that of the Larsen Ice Shelf, sea level rise, changes in rainfall patterns, and increased intensity and frequency of extreme weather events, are being attributed in part to global warming.[59] While changes are expected for overall patterns, intensity, and frequencies, it is difficult to attribute specific events to global warming. Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.[60]
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| − | Increasing deaths, displacements, and economic losses projected due to extreme weather attributed to global warming may be exacerbated by growing population densities in affected areas, although temperate regions are projected to experience some minor benefits, such as fewer deaths due to cold exposure.[61] A summary of probable effects and recent understanding can be found in the report made for the IPCC Third Assessment Report by Working Group II.[59] The newer IPCC Fourth Assessment Report summary reports that there is observational evidence for an increase in intense tropical cyclone activity in the North Atlantic Ocean since about 1970, in correlation with the increase in sea surface temperature, but that the detection of long-term trends is complicated by the quality of records prior to routine satellite observations. The summary also states that there is no clear trend in the annual worldwide number of tropical cyclones.[1]
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| − | Additional anticipated effects include sea level rise of 110 to 770 millimeters (0.36 to 2.5 ft) between 1990 and 2100,[62] repercussions to agriculture, possible slowing of the thermohaline circulation, reductions in the ozone layer, increased intensity of hurricanes and extreme weather events, lowering of ocean pH, and the spread of diseases such as malaria and dengue fever. One study predicts 18% to 35% of a sample of 1,103 animal and plant species would be extinct by 2050, based on future climate projections.[63] However, few mechanistic studies have documented extinctions due to recent climate change[64] and one study suggests that projected rates of extinction are uncertain.[65]
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| − | | |
| − | Economic
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | The projected temperature increase for a range of stabilization scenarios (the colored bands). The black line in middle of the shaded area indicates 'best estimates'; the red and the blue lines the likely limits. From the work of IPCC AR4.
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| − | | |
| − | Main articles: Economics of global warming and Low-carbon economy
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| − | | |
| − | Some economists have tried to estimate the aggregate net economic costs of damages from climate change across the globe. Such estimates have so far failed to reach conclusive findings; in a survey of 100 estimates, the values ran from US$-10 per tonne of carbon (tC) (US$-3 per tonne of carbon dioxide) up to US$350/tC (US$95 per tonne of carbon dioxide), with a mean of US$43 per tonne of carbon (US$12 per tonne of carbon dioxide).[61] One widely publicized report on potential economic impact is the Stern Review; it suggests that extreme weather might reduce global gross domestic product by up to 1%, and that in a worst-case scenario global per capita consumption could fall 20%.[66] The report's methodology, advocacy and conclusions have been criticized by many economists, primarily around the Review's assumptions of discounting and its choices of scenarios,[67] while others have supported the general attempt to quantify economic risk, even if not the specific numbers.[68][69]
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| − | In a summary of economic cost associated with climate change, the United Nations Environment Programme emphasizes the risks to insurers, reinsurers, and banks of increasingly traumatic and costly weather events. Other economic sectors likely to face difficulties related to climate change include agriculture and transport. Developing countries, rather than the developed world, are at greatest economic risk.[70]
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| − | Security
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| − | In November 2007, the Center for Strategic and International Studies and the Center for a New American Security published a report highlighting the national security effects of climate change.[71] These security effects include increased competition for resources between countries, mass migration from the worst affected areas, challenges to the cohesion of major states threatened by the rise in sea levels, and, as a consequence of these factors, an increased risk of armed conflict, including even nuclear conflicts.
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| − | Adaptation and mitigation
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| − | | |
| − | Main articles: Adaptation to global warming, Mitigation of global warming, and Kyoto Protocol
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| − | | |
| − | The broad agreement among climate scientists that global temperatures will continue to increase has led some nations, states, corporations and individuals to implement actions to try to curtail global warming or adjust to it. Many environmental groups encourage action against global warming, often by the consumer, but also by community and regional organizations. Others have suggested a quota on worldwide fossil fuel production, citing a direct link between fossil fuel production and CO2 emissions.[72][73]
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| − | There has also been business action on climate change, including efforts at increased energy efficiency and limited moves towards use of alternative fuels. One important innovation has been the development of greenhouse gas emissions trading through which companies, in conjunction with government, agree to cap their emissions or to purchase credits from those below their allowances.
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| − | The world's primary international agreement on combating global warming is the Kyoto Protocol, an amendment to the United Nations Framework Convention on Climate Change (UNFCCC) negotiated in 1997. The Protocol now covers more than 160 countries globally and over 55% of global greenhouse gas emissions.[74] Only the United States and Kazakhstan have not ratified the treaty, with the United States historically being the world's largest emitter of greenhouse gas. This treaty expires in 2012, and international talks began in May 2007 on a future treaty to succeed the current one.[75]
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| − | Claiming "serious harm" to the United States economy and the exemption of "80 percent of the world, including major population centers" like China and India, from the treaty, George W. Bush contends that the Kyoto Protocol is an unfair and ineffective means of addressing global climate change concerns.[76] Still, various state, local, and regional governments within the United States have begun their own initiatives to indicate support and compliance with the Kyoto Protocol on a local basis. For example, the Regional Greenhouse Gas Initiative is a state-level emissions capping and trading program involving eight Northeastern U.S. states, which was founded on December 20, 2005.[77]
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| − | China and India, though exempt from its provisions as developing countries, have ratified the Kyoto Protocol. China may have passed the U.S. in total annual greenhouse gas emissions according to some recent studies. Chinese Premier Wen Jiabao has called on the nation to redouble its efforts to tackle pollution and global warming.[78]
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| − | | |
| − | The IPCC's Working Group III is responsible for crafting reports that deal with the mitigation of global warming and analyzing the costs and benefits of different approaches. In the 2007 IPCC Fourth Assessment Report, they conclude that no one technology or sector can be completely responsible for mitigating future warming. They find there are key practices and technologies in various sectors, such as energy supply, transportation, industry, and agriculture, that should be implemented to reduced global emissions. They estimate that stabilization of carbon dioxide equivalent between 445 and 710 ppm by 2030 will result in between a 0.6% increase and 3% decrease in global gross domestic product.[79]
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| − | | |
| − | Social and political debate
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| − | | |
| − | Main articles: Global warming controversy, Politics of global warming, and Economics of global warming
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| − | See also: Climate change denial
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per capita greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | Per country greenhouse gas emissions in 2000
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| − | | |
| − | Over the past several years, public perceptions and attitudes concerning the causes and importance of global warming have changed.[80] Increased awareness of the scientific findings surrounding global warming has resulted in political and economic debate. Poor regions, particularly Africa, appear at greatest risk from the suggested effects of global warming, while their actual emissions have been small compared to the developed world.[81] At the same time, developing country exemptions from provisions of the Kyoto Protocol have been criticized by the United States and Australia, and have been used as part of the rationale for continued non-ratification by the U.S.[82] In the Western world, the idea of human influence on climate has gained wider acceptance in Europe than in the United States.[83][84]
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| − | The issue of climate change has sparked debate weighing the benefits of limiting industrial emissions of greenhouse gases against the costs that such changes would entail. There has been discussion in several countries about the cost and benefits of adopting alternative energy sources in order to reduce carbon emissions.[85] Organizations and companies such as the Competitive Enterprise Institute and ExxonMobil have emphasized more conservative climate change scenarios while highlighting the potential economic cost of stricter controls.[86][87][88][89] Likewise, various environmental lobbies and a number of public figures have launched campaigns to emphasize the potential risks of climate change and promote the implementation of stricter controls. Some fossil fuel companies have scaled back their efforts in recent years,[90] or called for policies to reduce global warming.[91]
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| − | Another point of debate is the degree to which newly developed economies such as India and China should be expected to constrain their emissions. China's gross national CO2 emissions are expected to exceed those of the U.S. within the next few years, and may have already done so according to a 2006 report.[92] China has contended that it has less of an obligation to reduce emissions since its per capita emissions are roughly one-fifth that of the United States.[93] India, also exempt from Kyoto restrictions and another of the biggest sources of industrial emissions, has made similar assertions.[94] However, the U.S. contends that if they must bear the cost of reducing emissions, then China should do the same.[95]
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| − | Related climatic issues
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| − | | |
| − | Main articles: Ocean acidification, global dimming, and ozone depletion
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| − | | |
| − | A variety of issues are often raised in relation to global warming. One is ocean acidification. Increased atmospheric CO2 increases the amount of CO2 dissolved in the oceans.[96] CO2 dissolved in the ocean reacts with water to form carbonic acid, resulting in acidification. Ocean surface pH is estimated to have decreased from 8.25 near the beginning of the industrial era to 8.14 by 2004,[97] and is projected to decrease by a further 0.14 to 0.5 units by 2100 as the ocean absorbs more CO2.[1][98] Since organisms and ecosystems are adapted to a narrow range of pH, this raises extinction concerns, directly driven by increased atmospheric CO2, that could disrupt food webs and impact human societies that depend on marine ecosystem services.[99]
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| − | Global dimming, the gradual reduction in the amount of global direct irradiance at the Earth's surface, may have partially mitigated global warming in the late twentieth century. From 1960 to 1990 human-caused aerosols likely precipitated this effect. Scientists have stated with 66–90% confidence that the effects of human-caused aerosols, along with volcanic activity, have offset some of the global warming, and that greenhouse gases would have resulted in more warming than observed if not for these dimming agents.[1]
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| − | | |
| − | Ozone depletion, the steady decline in the total amount of ozone in Earth's stratosphere, is frequently cited in relation to global warming. Although there are areas of linkage, the relationship between the two is not strong.
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| − | See also
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| − | | |
| − | * Glossary of climate change
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| − | | |
| − | References
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| − | | |
| − | 1. ^ a b c d e f g h i Summary for Policymakers (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change (2007-02-05). Retrieved on 2007-02-02. “The updated 100-year linear trend (1906 to 2005) of 0.74°C [0.56°C to 0.92°C] is therefore larger than the corresponding trend for 1901 to 2000 given in the TAR of 0.6°C [0.4°C to 0.8°C].”
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| − | 2. ^ Hegerl, Gabriele C.; et al. (2007-05-07). Understanding and Attributing Climate Change (PDF). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change 690. Intergovernmental Panel on Climate Change. Retrieved on 2007-05-20. “Recent estimates (Figure 9.9) indicate a relatively small combined effect of natural forcings on the global mean temperature evolution of the seconds half of the 20th century, with a small net cooling from the combined effects of solar and volcanic forcings”
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| − | 3. ^ Ammann, Caspar; et al. (2007-04-06). "Solar influence on climate during the past millennium: Results from ransient simulations with the NCAR Climate Simulation Model" (PDF). Proceedings of the National Academy of Sciences of the United States of America 104 (10): 3713–3718. “However, because of a lack of interactive ozone, the model cannot fully simulate features discussed in (44)." "While the NH temperatures of the high-scaled experiment are often colder than the lower bound from proxy data, the modeled decadal-scale NH surface temperature for the medium-scaled case falls within the uncertainty range of the available temperature reconstructions. The medium-scaled simulation also broadly reproduces the main features seen in the proxy records." "Without anthropogenic forcing, the 20th century warming is small. The simulations with only natural forcing components included yield an early 20th century peak warming of ≈0.2 °C (≈1950 AD), which is reduced to about half by the end of the century because of increased volcanism.”
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| − | 4. ^ A guide to facts and fictions about climate change. Royal Society (March 2005). Retrieved on 2007-11-18. “"However, the overwhelming majority of scientists who work on climate change agree on the main points"”
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| − | 5. ^ Climate Change: Basic Information. United States Environmental Protection Agency (2006-12-14). Retrieved on 2007-02-09. “In common usage, 'global warming' often refers to the warming that can occur as a result of increased emissions of greenhouse gases from human activities.”
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| − | 6. ^ United Nations Framework Convention on Climate Change, Article I. United Nations Framework Convention on Climate Change. Retrieved on 2007-01-15.
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| − | 7. ^ Berger, A.; et al. (2005-12-10). "On the origin of the 100-kyr cycles in the astronomical forcing". Paleoceanography 20 (4). PA4019. Retrieved on 2007-11-05.
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| − | 8. ^ Genthon, C.; et al. (1987-10-01). "Vostok Ice Core - Climatic response to CO2 and orbital forcing changes over the last climatic cycle". Nature 329 (6138): 414–418. Retrieved on 2007-11-05.
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| − | 9. ^ Alley, Richard B.; et al. (January 2002). "A northern lead in the orbital band: north-south phasing of Ice-Age events". Quaternary Science Reviews 21 (1-3): 431–441. Retrieved on 2007-11-05.
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| − | 10. ^ Joint science academies' statement: The science of climate change (ASP). Royal Society (2001-05-17). Retrieved on 2007-04-01. “The work of the Intergovernmental Panel on Climate Change (IPCC) represents the consensus of the international scientific community on climate change science”
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| − | | |
| − | ge Temperature Series] by Stephen McIntyre and Ross McKitrick, ''Energy & Enviornment'' volume 14, 2003.
| |
| − | *[http://blogs.nature.com/climatefeedback/2007/05/the_decay_of_the_hockey_stick.html The Decay of the Hockey Stick by Von Storch] published on the journal ''Nature'''s blog, May 3, 2007.
| |
| − | *[http://www.technologyreview.com/Energy/13830/ A Global Warming Bombshell] by Richard A. Muller, ''Technology Review'' , Oct. 2004; calls into question famous graph by Michael Mann.
| |
| − | *[http://www.sciencemag.org/cgi/content/abstract/306/5696/679 Reconstructing Past Climate from Noisy Data] by Hans von Storch, Eduardo Zorita, Julie M. Jones, Yegor Dimitriev, Fidel González-Rouco, Simon F. B. Tett, ''Science'' magazine, 22 October 2004.
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| − | </small>
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| − | Now this article has facts in it. S out.
| |
| − | ==References==
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| − | {{reflist|1}} | |
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