Articles | Volume 9, issue 2
The Cryosphere, 9, 767–779, 2015
The Cryosphere, 9, 767–779, 2015

Research article 27 Apr 2015

Research article | 27 Apr 2015

A model study of Abrahamsenbreen, a surging glacier in northern Spitsbergen

J. Oerlemans and W. J. J. van Pelt


Interactive discussion

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Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Anna Mirena Feist-Polner on behalf of the Authors (10 Mar 2015)  Author's response    Manuscript
ED: Publish as is (02 Apr 2015) by Andreas Vieli
Short summary
Many glaciers on Svalbard are surging glaciers. A surge is a rapid advance of the glacier snout during a few years, followed by a long period of quiescence. During the surge ice flows to lower terrain and experiences higher melt rates in summer. Here we investigate the impact of surging on the long-term effects of climate warming. We have modelled Abrahamsenbreen in northern Spitsbergen as a typical case. We show that surges tend to accelerate glacier retreat when temperature increases.