Arctic moisture source for Eurasian snow cover variations in autumn

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...

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Bibliographic Details
Published in:Environmental Research Letters
Main Authors: Martin Wegmann, Yvan Orsolini, Marta Vázquez, Luis Gimeno, Raquel Nieto, Olga Bulygina, Ralf Jaiser, Dörthe Handorf, Annette Rinke, Klaus Dethloff, Alexander Sterin, Stefan Brönnimann
Format: Article in Journal/Newspaper
Language:English
Published: IOP Publishing 2015
Subjects:
snow depth
Arctic warming
global change
global warming
sea ice
Siberia
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Science
Q
Physics
QC1-999
Arctic
Global warming
Sea ice
Online Access:https://doi.org/10.1088/1748-9326/10/5/054015
https://doaj.org/article/c39f5faae62f4edba3100dbec3622e76
Description
Summary: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.

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