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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. Precipitation is usually ...
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). At least ten times as much rain in the wettest month of summer as in the driest ...
Das Dfa-Klima – Sommerheißes feuchtes Kontinentalklima, nach Übersetzung der englischen Bezeichnung Hot-summer humid continental climate, von Köppen auch „Sioux-Klima“ genannt, – grenzt verschiedene kontinentale Klimaregionen mit Wäldern oder Grassteppen im Übergangsbereich zwischen kühlgemäßigter und subtropischer ...
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). At least ten times as much rain in the wettest month of summer as in the driest ...
Das Dwb-Klima – Sommerwarmes monsunbeeinflusstes feuchtes Kontinentalklima, nach Übersetzung der englischen Bezeichnung Monsoon-influenced warm-summer humid continental climate, von Köppen auch Amur-Klima genannt, – umfasst kühlere Regionen mit warmen Sommern im Anschluss an das Dwa-Klima.
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.
Humid continental climate (Köppen Dfa/b), a climatic type typified by four distinct seasons and large seasonal temperature differences. Humid subtropical climate (Köppen Cfa), a zone of climate characterized by hot and humid summers, and cool to mild winters.
