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A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, [1] typified by four distinct seasons and large seasonal temperature differences, with warm to hot (and often humid) summers, and cold (sometimes severely cold in the northern areas) and snowy winters.
- Continental climate
In western and eastern Asia, and the central United States...
- Clima continental húmido
O clima continental úmido ( português brasileiro) ou clima...
- Continental climate
Humid continental climate, major climate type of the Köppen classification that exhibits large seasonal temperature contrasts with hot summers and cold winters. It is found between 30° and 60° N in central and eastern North America and Asia in the major zone of conflict between polar and tropical
- The Editors of Encyclopaedia Britannica
A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900. A place with a humid continental climate has big seasonal temperature differences. It has warm to hot (and often humid ) summers and cold (sometimes very cold in the northern areas) winters.
O clima continental é um grupo climático que abrange os climas subárticos e continentais úmidos. Na classificação climática de Köppen eles estão no grupo D.[ 1] Os climas continentais geralmente apresentam uma variação anual significativa de temperatura, com verões quentes e invernos frios.
A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by four distinct seasons and large seasonal temperature differences, with warm to hot summers, and cold and snowy winters. Precipitation is usually distributed throughout the year, but often these regions do have dry seasons.
