CHANGE OF THE FLOODPLAIN AREAS ALONG SOME RIVERS OF THE VOLGA RIVER BASIN
https://doi.org/10.24057/2071-9388-2013-6-4-13-18
Abstract
The estimation of the area of the territories which are under the threat of flooding is of great importance. The technique, based on a principle of conformity of the area of a floodplain massif, averaged within the part of the river with a particular rank, to this rank has been proposed. The ranks, according to the Scheidegger scheme, were calculated for the mouths of 9907 rivers in the Volga river basin. For 96 rivers of the Volga basin, which has length of more than 200 km, changes of rank within the entire extent were calculated and a map was compiled using the obtained results.
For several rivers in the Volga river basin, change of the average floodplain areas along the rivers was estimated. It allowed establishing dependences between the average floodplain areas and the ranks of the rivers, with higher rank corresponding to bigger floodplain areas.
For several rivers in the Volga river basin, change of the average floodplain areas along the rivers was estimated. It allowed establishing dependences between the average floodplain areas and the ranks of the rivers, with higher rank corresponding to bigger floodplain areas.
About the Authors
Dmitry NesterenkoRussian Federation
Faculty of Geography, Lomonosov Moscow State University, Moscow, Russia
Leninskie gory, 1, 1199911
Nikolay Alexeevsky
Russian Federation
Head of the Department of Hydrology, Faculty of Geography, Lomonosov Moscow State University, Moscow, Russia
Leninskie gory, 1, 1199911
References
1. Dobrovolsky, S.G., M.N. Istomina. (2006). World flooding. Moscow: “GUOS” Publishing
2. House, 255 p.
3. Morphology and dynamics of channels of the rivers of the European part of Russia and
4. the adjacent states. (1999). The Map of scale 1:2000000 from a series “Maps for higher
5. educational institutions.” Russian Federal Service for Geodesy and Cartography.
6. Nesterenko, D.P., A.G. Kositskiy. (2010). Channel network of the river Volga and its indication
7. features. Materials of the VIII Scientific seminar of young scientists at the Interuniversity
8. Council on problems of erosion, channel, and estuary processes at the Lomonosov
9. Moscow State University (April 21–24, 2010).
10. Surface water resources of the USSR. The hydrological study. (1966). Vol. 10. The Upper
11. Volga area. Leningrad: Gidrometeoizdat.
12. Surface water resources of the USSR. The hydrological study. (1966). Vol. 11. Middle Ural
13. Mountains and Priural’e. Part. 1. Kama. Leningrad: Gidrometeoizdat.
14. Surface water resources of the USSR. The hydrological study. (1966). Vol. 12. The Lower Volga region
15. and the Western Kazakhstan. Part. 1. The Lower Volga region. Leningrad: Gidrometeoizdat.
16. Samokhin, M.A. (2006). Genetic features of the level regime formation of the rivers in various
17. regions of Russia. Abstract of the PhD dissertation in geographical sciences. Moscow:
18. M.V. Lomonosov Moscow State University, 31 p.
19. Taratunin, A.A. (2000). Flooding in the territory of the Russian Federation. Yekaterinburg.
20. “Aerokosmoekologiya” Publishing House, 375 p.
21. Vlasov, B.N, R.S. Chalov. (1991). Districts division of the European territory of Russia based
22. on the flow conditions of channel-forming water discharges on the rivers. The Moscow
23. State University Bulletin. Series 5. Geography. N 6.
Review
For citations:
Nesterenko D., Alexeevsky N. CHANGE OF THE FLOODPLAIN AREAS ALONG SOME RIVERS OF THE VOLGA RIVER BASIN. GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY. 2013;6(4):13-18. https://doi.org/10.24057/2071-9388-2013-6-4-13-18
Views:
725
Email this article 