Spatial distribution and synoptic conditions of snow accumulation and snow ablation in the West Siberian Plain
Loading...
Date
2015
Authors
Advisor
Editor
Journal Title
Journal ISSN
Volume Title
Publisher
WydziaĆ Nauk Geograficznych i Geologicznych Uniwersytetu im. Adama Mickiewicza
Title alternative
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.
Description
Sponsor
Keywords
snow accumulation, snow ablation, West Siberian Plain, air circulation
Citation
Quaestiones Geographicae vol. 34 (3), 2015, pp. 5-15
Seria
ISBN
ISSN
0137-477X