Modelling glaciers’ melting in Central Caucasus (the Djankuat and Bashkara Glacier case study)

Belozerov, E.; Rets, E.; Petrakov, D.; Popovnin, V.

Информация о цитировании статьи получена из Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 25 ноября 2020 г.

Авторы: Belozerov Egor, Rets Ekaterina, Petrakov Dmitry, Popovnin Viktor
Журнал: E3S Web of Conferences
Том: 163
Год издания: 2020
Издательство: EDP Sciences
Местоположение издательства: France
Первая страница: 1
Последняя страница: 6
DOI: 10.1051/e3sconf/202016301002
Аннотация: The A-melt model was applied to assess the contribution snowand ice melting to river flow during the summer period of 2017 for theBashkara and Djankuat glaciers located in the Caucasus. During the studyperiod, the Djankuat river runoff amounted to 120 thousand m3, while thepeak value of snow and ice melting was 300-400 thousand m3 per day, andon average 189 thousand m3. The significant influence of groundwater onthe river flow is traced. The melt water contribution to the glacial lakeBashkara outburst manifested in the gradual accumulation of water largevolumes over the summer period. The melting of snow and ice the daybefore the lake outburst reached 31 thousand m3, with an average value of192 thousand m3 for the Bashkara basin. The total melting volume of theDjankuat basin was 0.016 km3, and of the Bashkara basin – 0.017 km3. Asa result, the A-Melt model demonstrates the evaluation ability of glaciers’impact on mountain rivers runoff.
Добавил в систему: Петраков Дмитрий Александрович

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Modelling glaciers’ melting in Central Caucasus (the Djankuat and Bashkara Glacier case study)статья

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