Articles | Volume 19, issue 7
https://doi.org/10.5194/tc-19-2695-2025
https://doi.org/10.5194/tc-19-2695-2025
Research article
 | 
29 Jul 2025
Research article |  | 29 Jul 2025

Sea level rise contribution from Ryder Glacier in northern Greenland varies by an order of magnitude by 2300 depending on future emissions

Felicity A. Holmes, Jamie Barnett, Henning Åkesson, Mathieu Morlighem, Johan Nilsson, Nina Kirchner, and Martin Jakobsson

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to revisions (further review by editor and referees) (02 Mar 2025) by Felicity McCormack
AR by Felicity Holmes on behalf of the Authors (14 Mar 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (20 Mar 2025) by Felicity McCormack
RR by Anonymous Referee #1 (01 Apr 2025)
RR by Anonymous Referee #2 (03 Apr 2025)
ED: Publish subject to minor revisions (review by editor) (08 Apr 2025) by Felicity McCormack
AR by Felicity Holmes on behalf of the Authors (11 Apr 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (28 Apr 2025) by Felicity McCormack
AR by Felicity Holmes on behalf of the Authors (29 Apr 2025)  Author's response   Manuscript 
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Short summary
Northern Greenland contains some of the ice sheet's last remaining glaciers with floating ice tongues. One of these is Ryder Glacier, which has been relatively stable in recent decades, in contrast to nearby glaciers. Here, we use a computer model to simulate Ryder Glacier until 2300 under both a low- and a high-emissions scenario. Very high levels of surface melt under a high-emissions future lead to a sea level rise contribution that is an order of magnitude higher than under a low-emissions future.
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