Preliminary estimation of Lake El'gygytgyn water balance and sediment income

Modern process studies of the hydrologic balance of Lake El'gygytgyn, central Chukotka, and the sediment income from the catchment were carried out during a field campaign in spring and summer 2003. Despite high uncertainties due to the limited data, the results provide important first estimate...

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Bibliographic Details
Published in:Climate of the Past
Main Authors: G. Fedorov, M. Nolan, J. Brigham-Grette, D. Bolshiyanov, G. Schwamborn, O. Juschus
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2013
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Online Access:https://doi.org/10.5194/cp-9-1455-2013
https://doaj.org/article/17bf607a7f314a14b508aecf1628999d
Description
Summary:Modern process studies of the hydrologic balance of Lake El'gygytgyn, central Chukotka, and the sediment income from the catchment were carried out during a field campaign in spring and summer 2003. Despite high uncertainties due to the limited data, the results provide important first estimates for better understanding the modern and past sedimentation processes in this basin. Formed ca. 3.6 million years ago as a result of a meteorite impact, the basin contains one of the longest paleoclimate records in the terrestrial Arctic. Fluvial activity is concentrated over the short snowmelt period (about 20 days in second part of June). Underground outflow plays a very important role in the water balance and predominates over surface outflow. The residence time of the lake water is estimated to be about 100 yr.