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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 (and often humid) summers, and cold (sometimes severely cold in the northern areas) and snowy winters.
- Continental climate - Wikipedia
Dwa = Monsoon-influenced hot-summer humid continental...
- Humid continental climate - Simple English Wikipedia, the free encyclopedia
A humid continental climate is a climatic region defined by...
- Continental climate - Wikipedia
The Köppen climate classification divides climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are A (tropical), B (arid), C (temperate), D (continental), and E (polar). Each group and subgroup is represented by a letter.
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
The cool summer subtype of the humid continental climate in North America is found in New England, throughout much of the Great Lakes region and upper Midwest extending into south and south central Canada. Much of Scandinavia, eastern Europe and Russia fall into the cool summer subtype as well.
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 (and often humid) summers, and cold (sometimes severely cold in the northern areas) and snowy winters.
