Koppen Climate Classification

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Koppen Climate Classification The Koppen climate classification system is one of the most widely and technically advanced models used today in foretelling the climate accurately. Precise data/info is used to determine the type of climate for a particular region or location. The climate classification scheme divides the climates into five main groups in which encompasses a specific climate. The tropical climate (group A) includes: rainforests, monsoons, and wet/dry savannas. The tropical climate is characterized by constant high temperatures. All twelve months have an average precipitation of at least 60 mm (2.4 in), whereas in the savanna climate, the annual precipitation is contrastingly 25 mm. In the dry climates (group B) contains: arid and semiarid climates. Desert regions on the West coast are much cooler, due to the nearby presence of cold ocean currents and frequent cloud cover. The mesothermal climate (group C) consists: mediterranean, humid-subtropic, and oceanic climates. These climates have an average temperature above 50 °F in their warmest months. The continental/microthermal climate (group D) involves: continental, subarctic, and boreal climates. These climates have an average temperature above 10 °C 50 °F in their warmest months, and a coldest month average below −3 °C. In the polar climates (group E) includes: tundra and icecap climates. The warmest month in the tundra is 32 °F. Lastly speaking, the alpine climate, in other words excessively cold (group E) is very often −40 °F or below. An example of a dry climate destination is Yuma,

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