Sediment Yield of Kamchatka Krai Rivers into the Pacific Ocean and the Seas of Bering and Okhotsk
- Authors: Kuksina L.V.1, Alekseevskii N.I.1
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Affiliations:
- Faculty of Geography
- Issue: Vol 45, No 4 (2018)
- Pages: 479-489
- Section: Water Resources and the Regime of Water Bodies
- URL: https://journals.rcsi.science/0097-8078/article/view/174531
- DOI: https://doi.org/10.1134/S0097807818040140
- ID: 174531
Cite item
Abstract
Sediment yield of Kamchatka Krai rivers into the Pacific Ocean and the seas of Bering and Okhotsk, is evaluated, including that from the drainage basins that are not covered by regular observations. Regression dependences of specific suspended sediment yield (SSSY) on factors determining it were constructed for erosion regions identified in Kamchatka Krai. The total average many-year yield of suspended sediments of Kamchatka Krai rivers into the Pacific is 11.4 × 106 t/year, 73.9% of which is transported by rivers of the eastern coast and 26.1%, by those of the western coast. Among other factors, such distribution is attributed to the location of the majority of volcanoes on Kamchatka eastern coast. About one third of all sediments transported from Kamchatka Krai territory is discharged by the two largest rivers in the region, i.e., the Penzhina and Kamchatka.
About the authors
L. V. Kuksina
Faculty of Geography
Author for correspondence.
Email: ludmilakuksina@gmail.com
Russian Federation, Moscow, 119991
N. I. Alekseevskii
Faculty of Geography
Email: ludmilakuksina@gmail.com
Russian Federation, Moscow, 119991
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