Articles | Volume 11, issue 2
https://doi.org/10.5194/tc-11-1015-2017
https://doi.org/10.5194/tc-11-1015-2017
Research article
 | 
25 Apr 2017
Research article |  | 25 Apr 2017

Reconstructions of the 1900–2015 Greenland ice sheet surface mass balance using the regional climate MAR model

Xavier Fettweis, Jason E. Box, Cécile Agosta, Charles Amory, Christoph Kittel, Charlotte Lang, Dirk van As, Horst Machguth, and Hubert Gallée

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Interactive discussion

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 Xavier Fettweis on behalf of the Authors (28 Feb 2017)  Manuscript 
ED: Referee Nomination & Report Request started (01 Mar 2017) by Edward Hanna
RR by Anonymous Referee #2 (06 Mar 2017)
RR by Anonymous Referee #1 (08 Mar 2017)
ED: Publish subject to minor revisions (Editor review) (08 Mar 2017) by Edward Hanna
AR by Xavier Fettweis on behalf of the Authors (13 Mar 2017)  Author's response   Manuscript 
ED: Publish subject to minor revisions (Editor review) (22 Mar 2017) by Edward Hanna
AR by Xavier Fettweis on behalf of the Authors (22 Mar 2017)  Author's response   Manuscript 
ED: Publish as is (23 Mar 2017) by Edward Hanna
AR by Xavier Fettweis on behalf of the Authors (23 Mar 2017)
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Short summary
This paper shows that the surface melt increase over the Greenland ice sheet since the end of the 1990s has been unprecedented, with respect to the last 120 years, using a regional climate model. These simulations also suggest an increase of the snowfall accumulation through the last century before a surface mass decrease in the 2000s. Such a mass gain could have impacted the ice sheet's dynamic stability and could explain the recent observed increase of the glaciers' velocity.