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continental climate

Also known as: type D climate

Quick Summary

A continental climate is characterized by significant temperature variations between seasons, with hot summers and cold winters. This climate type is found in the interior of large landmasses, far from the moderating influence of oceans.1

In Europe, the continental climate dominates a large portion of the continent, including eastern Belarus, Russia, Finland, and northern Sweden. Winters here are colder and longer than in western Europe, with greater snow cover. Summers are hottest in the southeast. Annual precipitation is generally less than 500 mm (20 inches), with most of it falling in the summer.2

A subtype, the continental subarctic climate, is found further north, from about 50° to 70° N latitude. This climate is dominated by a long, cold winter with low precipitation, mostly as snow. Summers are short and mild, with average temperatures rarely exceeding 16°C (61°F).3

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