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Continental climates are considered as temperate climate varieties due to their location in the temperate zones, [2] [3] but are classified separately from other temperate climates in the Köppen climate classification system where they are identified by their first letter, a capital D.
Continental climate distribution. These climates have an average temperature above 10 °C (50 °F) in their warmest months, and the coldest month average below 0 °C (32 °F) (or −3 °C (26.6 °F), as noted previously). These usually occur in the interiors of continents and on their upper east coasts, normally north of 40°N.
Humid continental climates are considered as a variety of temperate climates due to lying in the temperate zones, [12] although they are classified separately from other temperate climates in the Köppen climate classification. In contrast to oceanic climates, they are created by large land masses and seasonal changes in wind direction.
Under Köppen, Chicago is classified as a humid continental climate (Dfa). Deep within continents, cities like Chicago are defined by huge temperature swings from cold, snowy winters to warm summers.
A humid continental climate is marked by variable weather patterns and a large seasonal temperature variance, cold and often very snowy winters, and warm summers. Places with more than three months of average daily temperatures above 10 °C (50 °F) and a coldest month temperature below −3 °C (27 °F) and which do not meet the criteria for ...
According to the Köppen climate classification system, the most popular climate classification system in the world, only South Florida is considered tropical. ... (temperate), D (continental ...
The region from the southern Plains, to the lower Midwest, eastward to parts of the Upper South, and the central East Coast (the New York City/coastal Connecticut region southward to Virginia) has a humid temperate climate, transitional between the humid continental and humid subtropical climate zones, becoming semi-arid in the western plains.
German climatologists Carl Troll and Karlheinz Paffen defined warm temperate zones as plain and hilly lands having an average temperature of the coldest month between 2 °C (35.6 °F) and 13 °C (55.4 °F) in the Northern Hemisphere and between 6 °C (42.8 °F) and 13 °C (55.4 °F) in the Southern Hemisphere, excluding oceanic and continental ...