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

G. Fedorov, M. Nolan, J. Brigham-Grette, D. Bolshiyanov, G. Schwamborn, O. Juschus

Research output: Contribution to journalArticlepeer-review

14 Scopus citations


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.

Original languageEnglish (US)
Pages (from-to)1455-1465
Number of pages11
JournalClimate of the Past
Issue number4
StatePublished - 2013

Bibliographical note

Copyright 2013 Elsevier B.V., All rights reserved.

Fingerprint Dive into the research topics of 'Preliminary estimation of Lake El'gygytgyn water balance and sediment income'. Together they form a unique fingerprint.

Cite this