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  1. The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, [1] [2] with several later modifications by Köppen, notably in 1918 and 1936. [3] [4] Later, German climatologist Rudolf Geiger (1894–1981) introduced ...

  2. Under the Köppen climate classification, Cfa and Cwa climates are either described as humid subtropical climates or warm temperate climates. This climate features mean temperature in the coldest month between 0 °C (32 °F) (or −3 °C (27 °F)) and 18 °C (64 °F) and mean temperature in the warmest month 22 °C (72 °F) or higher.

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  4. Jul 19, 2018 · The modified Koppen classification uses six letters to divide the world into six major climate regions, based on average annual precipitation, average monthly precipitation, and average monthly temperature: Each category is further divided into sub-categories based on temperature and precipitation.

    • Matt Rosenberg
  5. Apr 3, 2024 · humid subtropical climate, major climate type of the Köppen classification characterized by relatively high temperatures and evenly distributed precipitation throughout the year. This climate type is found on the eastern sides of the continents between 20° and 35° N and S latitude. Although the climate is made up of two subtypes (Cfa and Cwa ...

    • The Editors of Encyclopaedia Britannica
  6. Oct 19, 2023 · The Köppen climate classification system categorizes climate zones throughout the world based on local vegetation. Wladimir Köppen, a German botanist and climatologist, first developed this system at the end of the 19th century, basing it on the earlier biome research conducted by scientists. These scientists learned that vegetation and ...

  7. The Köppen Climate Classification divides the Earth's climate into five main climate groups: A (tropical) B (dry) C (temperate) D (continental) E (polar) These are subdivided by seasonal precipitation and heat. It was first published by the Russian-German climatologist Wladimir Köppen in 1884, with several later modifications by Köppen and ...

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