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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. Learn about the characteristics, distribution, and subtypes of humid continental climate, a major climate type with large seasonal temperature contrasts. Find out how it differs from other Köppen climate types and how it relates to vegetation zones.

    • The Editors of Encyclopaedia Britannica
  3. Dsa = Mediterranean-influenced hot-summer humid continental climate; coldest month averaging below 0 °C (32 °F) (or −3 °C (27 °F)), average temperature of the warmest month above 22 °C (71.6 °F) and at least four months averaging above 10 °C (50 °F).