Subarctic climate

Koppen_World_Map_Dfc_Dwc_Dsc_Dfd_Dwd_DsdThe subarctic climate (also called subpolar climate or boreal climate) is a climate characterised by long, usually very cold winters, and short, cool to mild summers. It is found on large landmasses, away from the moderating effects of an ocean, generally at latitudes from 50° to 70°N poleward of the humid continental climates. These climates represent Köppen climate classification Dfc, Dwc, Dsc, Dfd, Dwd and Dsd. In very small areas at high altitudes around the Mediterranean Basin, Iran, Kyrgyzstan, Tajikistan, Turkey, Alaska and other parts of the northwestern United States (Eastern Washington, Eastern Oregon and Idaho) the climate is classified as Dsc with a dry summer climate, such as in Seneca, Oregon. (Source: Wikipedia)

Cold climate with dry cold summer (Dsc)

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Cold climate with dry summer and very cold winter (Dsd)

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Cold climate with dry winter and cold summer (Dwc)

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Cold climate with dry very cold winter (Dwd)

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Cold climate with cold summer and no dry season (Dfc)

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Cold climate with very cold winter and no dry season (Dfd)

Below is a list of countries in which there is an area with this climate:

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