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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, with several later modifications by Köppen, notably in 1918 and 1936.
May 28, 2024 · Köppen climate classification, widely used, vegetation-based, empirical climate classification system developed by German botanist-climatologist Wladimir Köppen.
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.
On this web site we provide global data, world maps and computer animations of our updated Köppen-Geiger climate classification published by Kottek et al. (2006), Rubel and Kottek (2010) and Rubel et al. (2017).
The Köppen climate classification was developed based on the empirical relationship between climate and vegetation. This type of climate classification scheme provides an efficient way to describe climatic conditions defined by multiple variables and their seasonalities with a single metric.
We present new global maps of the Köppen-Geiger climate classification at a high 1‑km resolution for historical and future climate conditions (1901–2099). The historical maps (encompassing 1901–1930, 1931–1960, 1961–1990, and 1991–2020) are based on high-resolution, observation-based climatologies.
Oct 30, 2018 · The Köppen-Geiger system classifies climate into five main classes and 30 sub-types. The classification is based on threshold values and seasonality of monthly air temperature and precipitation.
The most frequently used climate classification map is that of Wladimir Köppen, presented in its latest version 1961 by Rudolf Geiger. A huge number of climate studies and subsequent publications adopted this or a former release of the Köppen-Geiger map.
May 28, 2024 · Köppen’s classification recognizes three B climates: Tropical and subtropical desert climate (BWh, part of BWk) Mid-latitude steppe and desert climate (BSh) Tropical and subtropical steppe climate (BSk, part of BWk) Type C and D climates.
This updated world map of Köppen-Geiger climate classification was based on temperature and precipitation observations for the period 1951-2000. Here, we present a series of digital world maps for the extended period 1901-2100 to depict global trends in observed climate and projected climate change scenarios.
