Abstract

Modern features of the lowland rivers’ runoff within-year distribution in the European part of Russia were analyzed. Its major transformations in the basins of the Volga and, mainly, the Don, were identified. They were accompanied by reduced flood runoff up to 50% or less (the Don basin) and the low flow increase up to 40–60 %. For the North Rivers of the EPR directional trends in annual runoff redistribution were not detected.

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