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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Continental climate is a climate that is characterized by winter temperatures cold enough to support a fixed period of snow each year, and relatively moderate precipitation occurring mostly in summer, although east coast areas (chiefly in North America) may show an even distribution of precipitation. Regions containing a continental climate exist in portions of the Northern Hemisphere continents (especially North America and Asia), and also at higher elevations in other parts of the world. Only a few areas in Iran, adjacent Turkey, Afghanistan, Pakistan, and Central Asia show a winter maximum in precipitation, and this typically melts in early spring to give short-lived floods.