- Wladimir Koeppen provided his scheme of classification in 1900 which was modified later multiple times.
BASIS OF CLASSIFICATION
- He used french plant physiologist Candolle classification of major global vegetation types to classify major climatic types as he believed vegetation is holistic expression of climate of a place
- Koppen used annual temperature and precipitation data and seasonal variations to delineate different climatic zones.
- He used alphabets as symbols of these climates.Capital letters for major types and small letter for subtypes of climate.
Vegetation zones by Candolle
|
Major climate types(symbols)
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Temperature and precipitation criteria
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Megatherms
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Tropical,A
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Average temperature of all months is greater than 18 °C
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Xerophytes
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Dry,B
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Evaporation exceeds precipitation
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Mesotherms
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Warm Temperates,C
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Temperature of coldest month less than 18 °C but greater than -3;Temperature of warmest month greater than 10 °C
|
Microtherms
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Humid cold,D
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Temperature of coldest month below -3 °C but warmest month above 10
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Hekistotherms
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polar,E
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Temperature of warmest month less than 10 °C
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- He further classified these major climatic zones into subtypes primarily based on precipitation pattern and has used small case letter for this second level of classification.
f
|
Precipitation throughout the year
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m
|
Monsoon climate i.e short dry season
|
s
|
Summer dry
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w
|
Winter dry
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- On the basis of these, he categorised these 5 major types into further 11 subtypes.
SOME CLIMATE TYPES
- Western european type (Cf)
- China Type(Cw)
- Mediterranean type(Cs)
EVALUATION
Merits
- Relation between vegetation types and climate
- Descriptive,generalized and simple.
Demrits
- Overemphasis on average temperature and precipitation and neglecting other whether elements like no of rainy days,temperature extremes,wind,etc
- No importance to air mass influence.
- Lots of symbols makes it difficult to memorize.
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