In the winter, what kind of weather would you expect in a continental warm summer climate

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. Precipitation is usually well distributed through the year. The definition of this climate regarding temperature is as follows: the mean temperature of the coldest month must be below −3 °C (26.6 °F) and there must be at least four months whose mean temperatures are at or above 10 °C (50 °F). In addition, the location in question must not be semi-arid or arid.

Humid continental climates tend to be found between latitudes 37° N and 60° N,[2] within the central and northeastern portions of North America, Europe, and Asia. They are much less commonly found in the Southern Hemisphere due to the larger ocean area at that latitude and the consequent greater maritime moderation. In the Northern Hemisphere some of the humid continental climates, typically in Scandinavia, Nova Scotia, and Newfoundland are heavily maritime-influenced, with relatively cool summers and winters being just below the freezing mark.[3] More extreme humid continental climates found in southern Siberia and the American Midwest combine hotter summer maxima and colder winters than the marine-based variety. In some areas there are both strong subtropical and subarctic air mass influences depending on season, like the humid and hot summers and the frigid winters of Milwaukee, Wisconsin[4] in the Upper Midwest of the United States!

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