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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 10, issue 5
The Cryosphere, 10, 1965–1989, 2016
https://doi.org/10.5194/tc-10-1965-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 10, 1965–1989, 2016
https://doi.org/10.5194/tc-10-1965-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 07 Sep 2016

Research article | 07 Sep 2016

Application of GRACE to the assessment of model-based estimates of monthly Greenland Ice Sheet mass balance (2003–2012)

Nicole-Jeanne Schlegel et al.

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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 Nicole-Jeanne Schlegel on behalf of the Authors (04 Jun 2016)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (09 Jun 2016) by Olivier Gagliardini
RR by Anonymous Referee #3 (14 Jun 2016)
RR by Anonymous Referee #4 (29 Jun 2016)
RR by Anonymous Referee #1 (04 Jul 2016)
ED: Reconsider after major revisions (06 Jul 2016) by Olivier Gagliardini
AR by Nicole-Jeanne Schlegel on behalf of the Authors (10 Aug 2016)  Author's response    Manuscript
ED: Publish subject to technical corrections (19 Aug 2016) by Olivier Gagliardini
AR by Nicole-Jeanne Schlegel on behalf of the Authors (23 Aug 2016)  Author's response    Manuscript
Publications Copernicus
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Short summary
We investigate Greenland Ice Sheet mass change from 2003–2012 by comparing observations from GRACE with state-of-the-art atmospheric and ice sheet model simulations. We find that the largest discrepancies (in the northwest and southeast) are likely controlled by errors in modeled surface climate as well as ice–ocean interaction and hydrological processes (not included in the models). Models should consider such processes at monthly to seasonal resolutions in order to improve future projections.
We investigate Greenland Ice Sheet mass change from 2003–2012 by comparing observations from...
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