Articles | Volume 13, issue 4
The Cryosphere, 13, 1125–1146, 2019
https://doi.org/10.5194/tc-13-1125-2019
The Cryosphere, 13, 1125–1146, 2019
https://doi.org/10.5194/tc-13-1125-2019

Research article 09 Apr 2019

Research article | 09 Apr 2019

Modelling the future evolution of glaciers in the European Alps under the EURO-CORDEX RCM ensemble

Harry Zekollari et al.

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Lorena Grabowski on behalf of the Authors (01 Mar 2019)  Author's response
ED: Referee Nomination & Report Request started (02 Mar 2019) by Andreas Vieli
RR by Ben Marzeion (24 Mar 2019)
ED: Publish subject to technical corrections (27 Mar 2019) by Andreas Vieli
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Short summary
Glaciers in the European Alps play an important role in the hydrological cycle, act as a source for hydroelectricity and have a large touristic importance. We model the future evolution of all glaciers in the Alps with a novel model that combines both ice flow and melt processes. We find that under a limited warming scenario about one-third of the present-day ice volume will still be present by the end of the century, while under strong warming more than 90 % of the volume will be lost by 2100.