Difference between revisions of "Köppen Climate Classification System"

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(→‎Three basic climate groups: none of E Europe is BS)
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===Temperate climates (C)===
 
===Temperate climates (C)===
 
====Mediterranean Climate (Cs): [[Chaparral]] biome====
 
====Mediterranean Climate (Cs): [[Chaparral]] biome====
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* [[Southern Europe|Southern]] and [[Central Europe]]
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* Much of [[Southern Europe]]  
  
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====Moist Continental Climate (Df): [[Continental climate|Continental temperate forest]] biome====
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====Oceanic climate (Cf)===
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[[British Isles]], [[Benelux]], Western [[France]], most of [[Germany]], [[New Zealand]]
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 +
====Subtropical highland (Cw)====
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High-altitude parts of [[East Africa]] and [[Southern Africa]]
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===Continental climate===
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====Humid Continental Climate (Df): [[Continental climate|Continental temperate forest]] biome====
 
*Eastern parts of the [[United States]] and southern [[Canada]]
 
*Eastern parts of the [[United States]] and southern [[Canada]]
 
*[[China]]
 
*[[China]]
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*[[Northern Europe]]
 
*[[Northern Europe]]
  
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===Group III===
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====Boreal forest Climate (Dfc): [[Taiga]] biome====
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High-latitude climates:
 
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====Boreal forest Climate ( Dfc): [[Taiga]] biome====
 
 
*Central and western [[Alaska]]
 
*Central and western [[Alaska]]
 
*[[Canada]], from the [[Yukon Territory]] to [[Labrador]]
 
*[[Canada]], from the [[Yukon Territory]] to [[Labrador]]
 
*[[Eurasia]], from northern Europe across all of [[Siberia]] to the [[Pacific Ocean]]
 
*[[Eurasia]], from northern Europe across all of [[Siberia]] to the [[Pacific Ocean]]
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====Tundra Climate (E): [[Tundra]] biome====
 
====Tundra Climate (E): [[Tundra]] biome====
 
[[File:Polar bears.jpg|thumb|right|300px]]
 
[[File:Polar bears.jpg|thumb|right|300px]]

Revision as of 12:48, September 6, 2016

The Köppen Climate Classification System is the most widely used for classifying the world's climates. Most classification systems used today are based on the one introduced in 1900 by the Russian-German climatologist Wladimir Köppen. Köppen divided the Earth's surface into climatic regions that generally coincided with world patterns of vegetation and soils.

The Köppen Climate Classification System

The Köppen system recognizes five major climate types based on the annual and monthly averages of temperature and precipitation. Each type is designated by a capital letter.

Further subgroups are designated by a second, lower case letter which distinguish specific seasonal characteristics of temperature and precipitation.

  • f - Moist with adequate precipitation in all months and no dry season. This letter usually accompanies the A, C, and D climates.
  • m - Rainforest climate in spite of short, dry season in monsoon type cycle. This letter only applies to A climates.
  • s - There is a dry season in the summer of the respective hemisphere (high-sun season).
  • w - There is a dry season in the winter of the respective hemisphere (low-sun season).

To further denote variations in climate, a third letter was added to the code.

  • a - Hot summers. These can be found in C and D climates.
  • b - Warm summer. These can also be found in C and D climates.
  • c - Cool, short summers in the C and D climates.
  • d - Very cold winters in the D climate only.
  • h - Dry-hot in B climates only.
  • k - Dry-cold in B climates only.

Tropical climates (A)

Tropical Moist Climates (Af): Rainforest

Rainforest

Wet-Dry Tropical Climates (Aw): Savanna

Arid and semi-arid climates (B)

Dry Tropical Climate (BW): Desert biome

Desert

Semi-arid Climates (BS): Steppe

Steppes

Temperate climates (C)

Mediterranean Climate (Cs): Chaparral biome

=Oceanic climate (Cf)

British Isles, Benelux, Western France, most of Germany, New Zealand

Subtropical highland (Cw)

High-altitude parts of East Africa and Southern Africa

Continental climate

Humid Continental Climate (Df): Continental temperate forest biome

Boreal forest Climate (Dfc): Taiga biome

Tundra Climate (E): Tundra biome

Polar bears.jpg

Highland Climate (H): Alpine Biome

Alpine