Articles | Volume 10, issue 2
https://doi.org/10.5194/tc-10-895-2016
https://doi.org/10.5194/tc-10-895-2016
Research article
 | 
26 Apr 2016
Research article |  | 26 Apr 2016

Improved GRACE regional mass balance estimates of the Greenland ice sheet cross-validated with the input–output method

Zheng Xu, Ernst J. O. Schrama, Wouter van der Wal, Michiel van den Broeke, and Ellyn M. Enderlin

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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 Zheng Xu on behalf of the Authors (27 Dec 2015)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (06 Jan 2016) by Etienne Berthier
RR by Anonymous Referee #3 (13 Jan 2016)
RR by Anonymous Referee #1 (24 Jan 2016)
ED: Reconsider after major revisions (02 Feb 2016) by Etienne Berthier
AR by Zheng Xu on behalf of the Authors (09 Mar 2016)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (12 Mar 2016) by Etienne Berthier
RR by Anonymous Referee #1 (29 Mar 2016)
ED: Publish subject to minor revisions (Editor review) (29 Mar 2016) by Etienne Berthier
AR by Zheng Xu on behalf of the Authors (07 Apr 2016)  Author's response    Manuscript
ED: Publish subject to technical corrections (11 Apr 2016) by Etienne Berthier
AR by Zheng Xu on behalf of the Authors (18 Apr 2016)  Author's response    Manuscript
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Short summary
In this paper, we compare the regional mass changes of the Greenland ice sheet between the solutions based on GRACE data and input/output method. Differences are found in some regions and indicate errors in those solutions. Therefore we improve our GRACE and IOM solutions by applying a simulation. We show the improved regional mass changes approximations are more consistent in regions. The remaining difference in the northwester Greenland is due to the underestimated uncertainty in IOM solution.