Nothern parts of Russia recive precipitation in the form of snow give reason
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Answer:
Several basic factors determine Russia’s variable climates. The country’s vast size and compact shape—the great bulk of the land is more than 250 miles (400 km) from the sea, while certain parts lie as much as 1,500 miles (2,400 km) away—produce a dominance of continental regimes. The country’s northerly latitude ensures that these are cold continental regimes—only southwestern Russia (the North Caucasus region and the lower Don and Volga basins), small sections of southern Siberia, and the maritime region of southeastern Siberia are below latitude 50° N, and more than half the federation is north of latitude 60° N. The great mountain barriers to the south and east prevent the ingress of ameliorating influences from the Indian and Pacific oceans, but the absence of relief barriers on the western and northern sides leaves the country open to Atlantic and Arctic influences. In effect there are only two seasons, winter and summer; spring and autumn are brief periods of rapid change from one extreme to the other.
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As we all know Precipitation is mainly in the form of Rain.
But in the northern parts of Russia temperatures reach really low so the rain freezes and comes in the form of snow.
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