Articles | Volume 14, issue 3
https://doi.org/10.5194/tc-14-905-2020
https://doi.org/10.5194/tc-14-905-2020
Research article
 | 
11 Mar 2020
Research article |  | 11 Mar 2020

Coupled modelling of subglacial hydrology and calving-front melting at Store Glacier, West Greenland

Samuel J. Cook, Poul Christoffersen, Joe Todd, Donald Slater, and Nolwenn Chauché

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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
ED: Publish subject to revisions (further review by editor and referees) (08 Aug 2019) by Kenichi Matsuoka
AR by Samuel Cook on behalf of the Authors (27 Aug 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (09 Sep 2019) by Kenichi Matsuoka
RR by Anonymous Referee #3 (16 Nov 2019)
ED: Publish subject to minor revisions (review by editor) (12 Dec 2019) by Kenichi Matsuoka
AR by Samuel Cook on behalf of the Authors (20 Dec 2019)  Author's response    Manuscript
ED: Publish subject to technical corrections (13 Feb 2020) by Kenichi Matsuoka
AR by Samuel Cook on behalf of the Authors (13 Feb 2020)  Author's response    Manuscript
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Short summary
This paper models how water flows beneath a large Greenlandic glacier and how the structure of the drainage system it flows in changes over time. We also look at how this affects melting driven by freshwater plumes at the glacier front, as well as the implications for glacier flow and sea-level rise. We find an active drainage system and plumes exist year round, contradicting previous assumptions and suggesting more melting may not slow the glacier down, unlike at other sites in Greenland.