Abstract
On the basis of the years-long observations summing-up a mechanism of the climate change impact on the Volga basin rivers winter and spring runoff has been revealed. It has been stated that the major factors affecting the winter rivers’ runoff increase over the past decades are the following: average daily air temperature increase; frost penetration into soil and winter moisture migration to the frosty penetration front decrease; increase of fall runoff; as well as increase of the winter thaws number.
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