Change in snow flood flow in the southern macro-slope of the Russian Plain in the period 1930-2014

In recent decades, in the southern macro-slope (catchment) of Te Russian Plain, mainly within the basins of the Volga and the Don rivers, the spring flood flow decreased due to both anthropogenic and climatic factors. Of anthropogenic factors, the creation of reservoirs played a signifcant role in cha...

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Bibliographic Details
Main Authors: N. I. Koronkevich, A. G. Georgiadi, S. V. Dolgov, E. A. Barabanova, E. A. Kashutina, I. P. Milyukova
Format: Article
Language:Russian
Published: Nauka 2018-12-01
Series:Лëд и снег
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/512
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