Spring Slope Runoff on the Russian Plain in Years of Different Water Content
https://doi.org/10.31857/S2587556620010100
Abstract
The important hydrological and hydro-ecological role of slope runoff, especially in spring (SSR), is shown. The data of 28 water balance stations on the SSR value on the territory of the Russian Plain in the years of different water flow are summarized. The hydrological role of autumn ploughing in the forest-steppe and steppe zones is shown. It leads to SSR decrease on the fields of autumn ploughing in comparison with the SSR on the fields not plowed in autumn, and most significantly in high-water and average years. The exception is the driest years, when there is no surface slope runoff on all lands. Two periods are considered – from the 1920s to 1980 and from 1981 to the present time. They are characterized by different climate features and anthropogenic impact. It is revealed that the SSR in the second period has reduced dramatically (by several times), mainly as a result of climate change, which has both positive and negative consequences.
About the Authors
E. A. Kashutina
Institute of Geography RAS
Russian Federation
Moscow
Russian Federation
Moscow
S. V. Yasinskii
Institute of Geography RAS
Russian Federation
Moscow
Russian Federation
Moscow
N. I. Koronkevich
Institute of Geography RAS
Russian Federation
Moscow
Russian Federation
Moscow
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Graphical Abstract
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1. Кривые обеспеченности весеннего поверхностного склонового стока в лесной зоне Русской равнины | |
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2. Curves of spring surface slope runoff probability in the forest zone of the Russian Plain | |
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- The spring slope runoff (SSR) is one of the most important hydrological phenomena on the territory of the Russian Plain.
- The value of SSR was calculated for the years of different dryness in the southern part of the forest, forest-steppe and steppe zones of the Russian Plain.
- In the modern (since 1981) period, there has been a significant decrease in SSR in all natural zones of the Russian Plain.
- The SSR reduction positively affects soil moisture reserves, but at the same time, it leads to the decrease of the river runoff resources.
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For citations:
Kashutina E.A., Yasinskii S.V., Koronkevich N.I. Spring Slope Runoff on the Russian Plain in Years of Different Water Content. Izvestiya Rossiiskoi Akademii Nauk. Seriya Geograficheskaya. 2020;(1):37-46. (In Russ.) https://doi.org/10.31857/S2587556620010100
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