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Arctic moisture source for Eurasian snow cover variations in autumn

Bibliographic Data

ID15548435
AuthorsMartin Wegmann (0000-0002-5294-2978, Oeschger Centre for Climate Change Research, corresponding author), Yvan Orsolini (0000-0001-7454-026X, Norwegian Institute for Air Research), Marta Vázquez (0000-0001-5261-4926), Luís Gimeno (0000-0002-0778-3605, Universidade de Vigo), Raquel Nieto (0000-0002-8984-0959, Universidade de Vigo), Olga Bulygina (All Russian Research Institute of Hydrometeorological information World Data Center), Ralf Jaiser (0000-0002-5685-9637, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung), Dörthe Handorf (0000-0002-3305-6882, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung), Annette Rinke (0000-0002-6685-9219, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung), Klaus Dethloff (0000-0003-4162-148X, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung), Alexander Sterin (All Russian Research Institute of Hydrometeorological information World Data Center), Brönnimann (0000-0001-9502-7991, University of Bern)
Year2015
Volume10
Issue5
Pages054015-054015
Publication date2015-05-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/10/5/054015
OpenAlexW2122854452
LanguageEN
Citations received6
References cited43

Eurasian fall snow cover changes have been suggested as a driver for changes in the Arctic Oscillation and might provide a link between sea-ice decline in the Arctic during summer and atmospheric circulation in the following winter. However, the mechanism connecting snow cover in Eurasia to sea-ice decline in autumn is still under debate. Our analysis is based on snow observations from 820 Russian land stations, moisture transport using a Lagrangian approach derived from meteorological re-analyses. We show that declining sea-ice in the Barents and Kara Seas (BKS) acts as moisture source for the enhanced Western Siberian snow depth as a result of changed tropospheric moisture transport. Transient disturbances enter the continent from the BKS region related to anomalies in the planetary wave pattern and move southward along the Ural mountains where they merge into the extension of the Mediterranean storm track

Arctic · Arctic ice pack · Arctic oscillation · Climatology · Geography · Merge (version control · Meteorology · Moisture · Northern Hemisphere · Sea ice · Snow · Arctic and Antarctic ice dynamics · Climate change and permafrost · Climate variability and models · Environmental Science · Geology · Oceanography

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Unique citing works6
Citations per year0,6
Citation span2016 - 2022 (7)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 6
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