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Climate Classification
Ch. 14 Sec. 2 Climate Classification
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Koeppen Classification System
Developed by Russian-born Germ climatologist Wladimir Koeppen Based on monthly values of . . . 1) Temperature 2) Precipitation Also distinguished natural vegetation Designed a map to classify
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Koeppen Classification System
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Classification System
Tropical climate: High temperatures 600 cm of rain Along w/ mT air, formations of rain forests
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Classification System
Dry climate: 30% of earth’s area, largest cT air mass, desert areas Low precipitation and vegetation High evaporation
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Classification System
Mild climates: Generally on the coasts Warm, muggy, high precipitation areas Can receive west air from ocean Warm winter and cool summers
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Classification System
Continental climates: Warm summer Cool summer Subarctic Climate battleground: rapid, violent changes in weather
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Classification System
Polar climates Coldest regions on earth (warmest month <10oC) Precipitation low: clouds hold less moisture High elevations
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Microclimates Localized area that differs from surrounding region
Heat Island Concrete buildings create a warmer climate than rural areas Large areas of asphalt and buildings
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