Continental climate is a climate characterized by important annual variation in temperature due to the lack of significant bodies of water nearby. Often winter temperature is cold enough to support a fixed period of snow each year, and relatively moderate precipitation occurring mostly in summer, although there are exceptions such as the east coast areas of North America which show an even distribution of precipitation: this pattern is called Humid continental climate, but dry continental climates also exist. Regions with 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 the mountains of the Pacific Northwest and in Iran, northern Iraq, adjacent Turkey, Afghanistan, Pakistan, and Central Asia show a winter maximum in precipitation.
Read more about Continental Climate: Ecosystems, Temperatures, Spring and Fall, Köppen Climate Classification, Climatology, Neighboring Climates, Examples
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“Culture is the name for what people are interested in, their thoughts, their models, the books they read and the speeches they hear, their table-talk, gossip, controversies, historical sense and scientific training, the values they appreciate, the quality of life they admire. All communities have a culture. It is the climate of their civilization.”
—Walter Lippmann (1889–1974)