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Preliminary estimation of Lake El'gygytgyn water balance and sediment income
Ist Teil von
Climate of the past, 2013-07, Vol.9 (4), p.1455-1465
Ort / Verlag
Katlenburg-Lindau: Copernicus GmbH
Erscheinungsjahr
2013
Link zum Volltext
Quelle
EZB Electronic Journals Library
Beschreibungen/Notizen
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.