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 Iran, northern Iraq, 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.
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 Iran, northern Iraq, 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.