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Quaestiones Geographicae

The Journal of Adam Mickiewicz University

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Spatial Distribution And Synoptic Conditions Of Snow Accumulation And Snow Ablation In The West Siberian Plain

Ewa Bednorz
  • Corresponding author
  • Department of Climatology, Adam Mickiewicz University in Poznań, Poland
  • Email:
/ Joanna Wibig
  • Department of Meteorology and Climatology, University of Łódź, Poland
Published Online: 2015-12-30 | DOI: https://doi.org/10.1515/quageo-2015-0029

Abstract

The mean duration of snow coverage in the West Siberian Plain is approximately eight months in the north to about five months in the south. While the period of intense snow melting is short (one or two months between March and May), snow accumulation persists for most of the cold season. Snow accumulation is associated with negative anomalies of sea level pressure, which means increased cyclonal activity and weaker than normal Siberian High. Much lower anomalies of sea level pressure occur during snow ablation. This suggests smaller influence of air circulation on snow cover reduction in spring.

Keywords: snow accumulation; snow ablation; West Siberian Plain; air circulation

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About the article

Received: 2014-12-29

Revised: 2015-08-15

Published Online: 2015-12-30

Published in Print: 2015-09-01



Citation Information: Quaestiones Geographicae, ISSN (Online) 2081-6383, DOI: https://doi.org/10.1515/quageo-2015-0029. Export Citation

© 2015 Faculty of Geographical and Geological Sciences, Adam Mickiewicz University. This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License. (CC BY-NC-ND 3.0)

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