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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. Regions where the continental climates (Dfa, Dfb, Dfc, Dfd) are found. Dfa = Hot-summer humid continental climate; coldest month averaging below 0 °C

  3. A cidade tem um clima continental úmido (Köppen Dfa). Usando a classificação climática de Köppen, um clima é classificado como continental úmido quando a temperatura do mês mais frio é inferior a −3 °C ou 0 °C, e deve haver pelo menos quatro meses cujas temperaturas médias são iguais ou superiores a 10 °C.

  4. 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).

  5. 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
  6. As áreas com esse subtipo do clima continental têm uma temperatura média no mês mais quente abaixo de 22 °C. As altas temperaturas do verão nesta zona geralmente ficam em média entre 21 e 28 °C durante o dia e as temperaturas médias no mês mais frio geralmente ficam muito abaixo dos −3 °C ou 0 °C.

  7. The humid continental climate 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.