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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 6
The Cryosphere, 9, 2009–2025, 2015
https://doi.org/10.5194/tc-9-2009-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 9, 2009–2025, 2015
https://doi.org/10.5194/tc-9-2009-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 02 Nov 2015

Research article | 02 Nov 2015

Elevation change of the Greenland Ice Sheet due to surface mass balance and firn processes, 1960–2014

P. Kuipers Munneke 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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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Peter Kuipers Munneke on behalf of the Authors (09 Oct 2015)  Author's response
ED: Publish subject to minor revisions (Editor review) (13 Oct 2015) by Jonathan Bamber
AR by Peter Kuipers Munneke on behalf of the Authors (15 Oct 2015)  Author's response    Manuscript
ED: Publish as is (16 Oct 2015) by Jonathan Bamber
Publications Copernicus
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Short summary
The snow layer on top of the Greenland Ice Sheet is changing: it is thickening in the high and cold interior due to increased snowfall, while it is thinning around the margins. The marginal thinning is caused by compaction, and by more melt. This knowledge is important: there are satellites that measure volume change of the ice sheet. It can be caused by increased ice discharge, or by compaction of the snow layer. Here, we quantify the latter, so that we can translate volume to mass change.
The snow layer on top of the Greenland Ice Sheet is changing: it is thickening in the high and...
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