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The Köppen climate classification is the most widely used climate classification scheme. [2] It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, [3] [4] with several later modifications by Köppen, notably in 1918 and 1936.
Worldwide Köppen climate classifications. Climate classifications are systems that categorize the world's climates. A climate classification may correlate closely with a biome classification, as climate is a major influence on life in a region. The most used is the Köppen climate classification scheme first developed in 1884. [1] [2]
English: Köppen–Geiger climate classification map at 1-km resolution for Temperate 1991–2020. ... Koppen-Geiger Map v2 C 1901–1930.svg;
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English: Köppen–Geiger climate classification map at 1-km resolution for Somalia 1991–2020. ... Koppen-Geiger Map v2 SOM 1931–1960.svg;
The snowy city of Sapporo, Japan, has a humid continental climate (Köppen Dfa).. Using the Köppen climate classification, a climate is classified as humid continental when the temperature of the coldest month is below 0 °C [32.0 °F] or −3 °C [26.6 °F] and there must be at least four months whose mean temperatures are at or above 10 °C (50 °F). [5]
English: Köppen–Geiger climate classification map at 1-km resolution for Tropical, rainforest (Af) 1991–2020. ... Koppen-Geiger Map v2 Af 1931–1960.svg;
The Trewartha climate classification (TCC), or the Köppen–Trewartha climate classification (KTC), is a climate classification system first published by American geographer Glenn Thomas Trewartha in 1966. It is a modified version of the Köppen–Geiger system, created to answer some of its deficiencies. [1]