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The cool summer subtype is marked by mild summers, long cold winters and less precipitation than the hot summer subtype; however, short periods of extreme heat are not uncommon. Northern Japan has a similar climate.
Dfa = 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).
Dsb = Mediterranean-influenced warm-summer humid continental climate; coldest month averaging below 0 °C (32 °F) (or −3 °C (27 °F)), average temperature of the warmest month below 22 °C (71.6 °F) and at least four months averaging above 10 °C (50 °F).
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.
A humid continental climate (Köppen prefix D and a third letter of a or b) is a climatic region defined by Russian German climatologist Wladimir Köppen in 1900, [1] which is typified by large seasonal temperature differences, with warm to hot (and often humid) summers and cold (sometimes severely cold) winters.
A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900. A place with a humid continental climate has big seasonal temperature differences. It has warm to hot (and often humid) summers and cold (sometimes very cold in the northern areas) winters. Precipitation usually happens ...
Typical of the humid continental climate most of its precipitation falls during the summer when air masses are warmer and wetter. Cool Summer Subtype 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 ...
