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Assessment of climatic and anthropogenic impact on spring runoff in the Don River basin

Abstract

The article examines the flow features of the spring flood in the Don River basin during 1930-2017. Its large-scale changes over the past half century took place in 1980 and 2006-2010. During these periods the most significant climatic changes were observed, aggravated in the 20th century by significantly increased anthropogenic runoff regulation by numerous reservoirs. The application of the method of integral curves in combination with statistical analysis of the spring runoff by the data of 50 stream gauges made it possible to separate the contribution of climatic changes and anthropogenic impacts to the formation of modern decrease of flood runoff on the rivers of the Don River basin. According to our results over the past 40 years the flood runoff has decreased by an average of 30-40%, i.e. from 10% in the upper reaches of the Voronezh, Khoper and Medveditsa rivers to more than 50-60% in the basins of the Seversky Donets and Oskol rivers. In terms of the changes in spring runoff, the rivers of the Don River basin are divided into three groups: with the runoff decrease after 1980, after 2006-2010 and with no changes in spring runoff. According to calculations, the amount of visible evaporation from the surface of reservoirs in the Don River basin upstream the Tsimlyansk reservoir is relatively small and equals to 0.09 km3 or 0.5% of the Don River's average annual flow for the Kalach-on-Don section. However, in dry years this factor can significantly increase the deficit of water resources for most watersheds with intensive economic activity. It is estimated that the total usable volume of reservoirs in the basins of the largest Don River tributaries averages 43% of the decrease in their runoff during the flood period, thus indicating highly possible seasonal redistribution of water runoff by reservoirs with a volume of more than 0.1 km3. The potential of technogenic regulation (PTR) of reservoirs with a volume of more than 0.1 km3 was evaluated. A decrease of the spring river flow with increasing PTR of reservoirs in their basins was noted. 

About the Authors

N. A. Varentsova
Lomonosov Moscow State University; Central Department of Hydrometeorology and Environmental Monitoring
Russian Federation

Engineer, Faculty of Geography, Department of Land Hydrology, Lomonosov Moscow State University; Head of the Department of Hydrological Forecasts, Central Department of Hydrometeorology and Environmental Monitoring.



M. G. Grechushnikova
Lomonosov Moscow State University
Russian Federation

Leading Scientific Researcher, Ph.D. in Geography, Faculty of Geography, Department of Land Hydrology.



E. S. Povalishnikova
Lomonosov Moscow State University
Russian Federation

Senior Scientific Researcher, Ph.D. in Geography, Faculty of Geography, Department of Land Hydrology.



M. B. Kireeva
Lomonosov Moscow State University
Russian Federation

Associate Professor, Ph.D. in Geography, Faculty of Geography, Department of Land Hydrology.



M. A. Kharlamov
Lomonosov Moscow State University; Water Problems Institute of RAS, Laboratory for Surface Water Modeling
Russian Federation

Engineer, Ph.D. in Geography, Faculty of Geography, Department of Land Hydrology; Junior Researcher, Water Problems Institute of RAS, Laboratory for Surface Water Modeling.



N. L. Frolova
Lomonosov Moscow State University
Russian Federation

Professor, D.Sc. in Geography, Faculty of Geography, Department of Land Hydrology.



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Review

For citations:


Varentsova N.A., Grechushnikova M.G., Povalishnikova E.S., Kireeva M.B., Kharlamov M.A., Frolova N.L. Assessment of climatic and anthropogenic impact on spring runoff in the Don River basin. Lomonosov Geography Journal. 2021;(5):91-108. (In Russ.)

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ISSN 0579-9414 (Print)