The Koppean classification system is based on the native vegetation concept. It has can be categorized into the tropical/megathermal climate, the dry climate, the temperate/ mesothermal climate, the continental/microthermal climate and the Polar and Alpine climate.
devised by Waldimir Koppen (1846-1940)
The Köppen classification system is used as a climate classification system. It categorizes climates based on temperature and precipitation patterns, leading to the identification of different climate zones around the world.
Cfb
demerits of koppen's classification of climate
koppen
D
BS
Humid Continental (Dfa)
The Koppen-Geiger classification for Japan is Cfa. It has a humid subtropical climate with hot summers without a dry season, found on the eastern side of continents, with hot and sultry summers.
Wladimir Peter Koppen is the scientist that began the study of climate
The Koppen climate classification of Kashgar is a desert climate or BWk. The climate is also called an arid climate which means failing to meet polar climate criteria and the precipitation is very low.
The koppen system is the six main climate types. High Elevation, Continental, Dry, Polar, Tropical, and Mild. According to the Koppen climate classification system, humid tropical climates do not experience winters.