E3S Web Conf.
Volume 163, 2020IV Vinogradov Conference “Hydrology: from Learning to Worldview” in Memory of Outstanding Russian Hydrologist Yury Vinogradov
|Number of page(s)||5|
|Section||Regional Water Problems: Anthropogenic Impact and / or Climate Change?|
|Published online||17 April 2020|
Landscape-permafrost conditions and factors of summer runoff formation of small coastal lowland rivers
North-Eastern Interdisciplinary Scientific Research Institute N.A. Shilo FEB RAS, Portovaya 16, 685000, Magadan, Russia
2 Water Problems Institute RAS, Gubkina 3, 119333, Moscow, Russia
3 Melnikov Permafrost Institute SB RAS, Merzlotnaya 36, 677010, Yakutsk, Russia
4 Lomonosov Moscow State University, Faculty of Geography, Leninskiye Gory 1, 119991, Moscow, Russia
5 Pacific Geographical Institute FEB RAS, Radio 7, 690041, Vladivostok, Russia
* Corresponding author: firstname.lastname@example.org
River feed and flow regime in the Anadyr lowland remain stable with significant interannual fluctuations in the amount of summer precipitation (70-180 mm). The lack of summer precipitation is compensated by the suprapermafrost groundwater of the active layer, which is formed by meltwater from seasonal underground ice. In July 2019, complex permafrost-hydrological studies were conducted in the Ugolnaya-Dionisia river basin (Chukotka, Russia) to determine the patterns of formation and dynamics of underground and surface runoff. Seasonal active layer groundwater storage that formed as a result of the melting of seasonal ice was estimated. The territory was classified according to the unite discharge, potential and established water sources. Patterns and factors of seasonal and daily dynamics of the river regime are revealed.
© The Authors, published by EDP Sciences, 2020
This is an Open Access article distributed under the terms of the Creative Commons Attribution License 4.0, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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