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Koeppen Classification
The most widely used classification of climate is the climate classification scheme developed by German climatologist and plant geographer V. Koeppen. in 1918. The annual as well as monthly averages of temperature and precipitation formed the basis of Koeppen classification of climate. He also based his classification on the distribution of weather conditions. This classification is both empirical and genetic type. Koeppen in his classification laid great emphasis that all the characteristics of climate can well be expressed through the distribution of
natural vegetation that’s why he tried to associate his climate types with vegetation zones of the world. He made use of annual averages of temperature and precipitation in fixing the climate regions of the world. He presented five main climate types. Each of these climate types was represented by capital English alphabets of A, B, C, D and E. He used the letter 'H' for highland type of climates. While keeping temperature and precipitation variations in view these five climate types were further subdivided as shown in the following table:
S.N. | Chief Climatic Groups | Climatic Types | ||||
A | Tropical Climate (Average temperature of the coldest month is 18° C or higher) | 1. Tropical rain forest type climate 2. Savannah type climate 3. Monsoon type climate | ||||
B | Dry Climate precipitation) | (Potential | evaporation | exceeds | 4. Desert climate 5. Steppe (Semi-desert) climate | |
C | Temperate Climate (The average temperature of the coldest month is higher than minus 3°C but below 18°C) | 6. Mediterranean climate 7. China type climate 8. West European type climate | ||||
D | Continental Climate (The average temperature of the coldest month is minus 3° C or below) | 9. Taiga climate 10. Eastern coastal climate 11. Continental climate | cold | |||
E | Polar Climate (Average temperature for all months is below 10° C) | 12. Tundra climate 13. Snow-capped region type climate | ||||
H | Highland Climate (Cold due to elevation) |