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The Cryosphere An interactive open-access journal of the European Geosciences Union
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TC | Volume 13, issue 9
The Cryosphere, 13, 2281–2301, 2019
https://doi.org/10.5194/tc-13-2281-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 13, 2281–2301, 2019
https://doi.org/10.5194/tc-13-2281-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 05 Sep 2019

Research article | 05 Sep 2019

Modeling the response of Greenland outlet glaciers to global warming using a coupled flow line–plume model

Johanna Beckmann et al.
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Interactive discussion
Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
AR by Johanna Beckmann on behalf of the Authors (19 Oct 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (10 Nov 2018) by G. Hilmar Gudmundsson
RR by Anonymous Referee #2 (22 Nov 2018)
RR by Anonymous Referee #3 (24 Dec 2018)
ED: Reconsider after major revisions (14 Jan 2019) by G. Hilmar Gudmundsson
AR by Johanna Beckmann on behalf of the Authors (14 May 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (30 May 2019) by G. Hilmar Gudmundsson
RR by Anonymous Referee #3 (11 Jun 2019)
ED: Publish subject to minor revisions (review by editor) (15 Jun 2019) by G. Hilmar Gudmundsson
AR by Johanna Beckmann on behalf of the Authors (23 Jun 2019)  Author's response    Manuscript
ED: Publish as is (17 Jul 2019) by G. Hilmar Gudmundsson
Post-review adjustments
AA: Author's adjustment | EA: Editor approval
AA by Johanna Beckmann on behalf of the Authors (15 Aug 2019)   Author's adjustment   Manuscript
EA: Adjustments approved (29 Aug 2019) by G. Hilmar Gudmundsson
Publications Copernicus
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Short summary
Submarine melting (SM) has been discussed as potentially triggering the recently observed retreat at outlet glaciers in Greenland. How much it may contribute in terms of future sea level rise (SLR) has not been quantified yet. When accounting for SM in our experiments, SLR contribution of 12 outlet glaciers increases by over 3-fold until the year 2100 under RCP8.5. Scaling up from 12 to all of Greenland's outlet glaciers increases future SLR contribution of Greenland by 50 %.
Submarine melting (SM) has been discussed as potentially triggering the recently observed...
Citation