Menu

Javascript is not activated in your browser. This website needs javascript activated to work properly.
You are here

The Changing Face of Arctic Snow Cover: A Synthesis of Observed and Projected Changes

Author:
  • Terry V. Callaghan
  • Margareta Johansson
  • Ross D. Brown
  • Pavel Ya Groisman
  • Niklas Labba
  • Vladimir Radionov
  • Roger G. Barry
  • Olga N. Bulygina
  • Richard L. H. Essery
  • D. M. Frolov
  • Vladimir N. Golubev
  • Thomas C. Grenfell
  • Marina N. Petrushina
  • Vyacheslav N. Razuvaev
  • David A. Robinson
  • Peter Romanov
  • Drew Shindell
  • Andrey B. Shmakin
  • Sergey A. Sokratov
  • Stephen Warren
  • Daquing Yang
Publishing year: 2011
Language: English
Pages: 17-31
Publication/Series: Ambio: a Journal of Human Environment
Volume: 40
Document type: Journal article
Publisher: Springer

Abstract english

Analysis of in situ and satellite data shows evidence of different regional snow cover responses to the widespread warming and increasing winter precipitation that has characterized the Arctic climate for the past 40-50 years. The largest and most rapid decreases in snow water equivalent (SWE) and snow cover duration (SCD) are observed over maritime regions of the Arctic with the highest precipitation amounts. There is also evidence of marked differences in the response of snow cover between the North American and Eurasian sectors of the Arctic, with the North American sector exhibiting decreases in snow cover and snow depth over the entire period of available in situ observations from around 1950, while widespread decreases in snow cover are not apparent over Eurasia until after around 1980. However, snow depths are increasing in many regions of Eurasia. Warming and more frequent winter thaws are contributing to changes in snow pack structure with important implications for land use and provision of ecosystem services. Projected changes in snow cover from Global Climate Models for the 2050 period indicate increases in maximum SWE of up to 15% over much of the Arctic, with the largest increases (15-30%) over the Siberian sector. In contrast, SCD is projected to decrease by about 10-20% over much of the Arctic, with the smallest decreases over Siberia (<10%) and the largest decreases over Alaska and northern Scandinavia (30-40%) by 2050. These projected changes will have far-reaching consequences for the climate system, human activities, hydrology, and ecology.

Keywords

  • Physical Geography
  • extent
  • Snow cover
  • Snow cover duration
  • Snow water equivalent
  • Snow depth

Other

Published
  • ISSN: 0044-7447
E-mail: margareta [dot] johansson [at] nateko [dot] lu [dot] se

Researcher

Dept of Physical Geography and Ecosystem Science

+46 46 222 44 80

450

16

Department of Physical Geography and Ecosystem Science
Lund University
Sölvegatan 12
S-223 62 Lund
Sweden

Processing of personal data