Abstract
Climate-warming-induced changes in the natural resources and the storage reserves of phreatic waters in zones of massive-insular, discontinuous, and continuous permafrost in the region are discussed. The relationship between a long-term trend toward rise in the phreatic water table and an increase in the period of their infiltration recharge is substantiated. The increments of phreatic-water natural resources typical of hydrogeological subdivisions of the region over a many-year period are evaluated. It is shown that the natural resources and storage reserves of phreatic waters in taliks increase almost over the entire territory of the Pechora-Ural Region.
Published Version
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