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  1. 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.

  2. 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
  3. The humid continental climate is known for its variable weather conditions due to its location in the midlatitudes and the year-round influence of the polar front. This climate lies in the boundary zone between many different air masses, principally polar and tropical ones.

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  4. The humid continental climate, class Df or Dw, is found over great expanses in the temperate regions of the mid-latitudes. The humid continental climate is noted for its variable weather patterns related to cyclonic storms and its large temperature range due to its interior location in mid-latitude continents.

  5. Dwa = Monsoon-influenced hot-summer humid continental climate; coldest month averaging below 0 °C (32 °F) (or −3 °C (27 °F)), at least one month's average temperature above 22 °C (71.6 °F), and at least four months averaging above 10 °C (50 °F).

  6. The humid continental climates are found around the polar front in North America and Europe. In the winter, middle-latitude cyclones bring chilly temperatures and snow. In the summer, westerly winds bring continental weather and warm temperatures.