Articles | Volume 17, issue 7
https://doi.org/10.5194/tc-17-2755-2023
https://doi.org/10.5194/tc-17-2755-2023
Research article
 | 
13 Jul 2023
Research article |  | 13 Jul 2023

Basal melt rates and ocean circulation under the Ryder Glacier ice tongue and their response to climate warming: a high-resolution modelling study

Jonathan Wiskandt, Inga Monika Koszalka, and Johan Nilsson

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-1296', William Scott, 15 Jan 2023
    • AC1: 'Reply on RC1', Jonathan Wiskandt, 28 Apr 2023
  • RC2: 'Comment on egusphere-2022-1296', Margaret Lindeman, 12 Feb 2023
    • AC2: 'Reply on RC2', Jonathan Wiskandt, 28 Apr 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (04 May 2023) by Jan De Rydt
AR by Jonathan Wiskandt on behalf of the Authors (12 May 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (21 May 2023) by Jan De Rydt
AR by Jonathan Wiskandt on behalf of the Authors (26 May 2023)
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Short summary
Understanding ice–ocean interactions under floating ice tongues in Greenland and Antarctica is a major challenge in climate modelling and a source of uncertainty in future sea level projections. We use a high-resolution ocean model to investigate basal melting and melt-driven circulation under the floating tongue of Ryder Glacier, northwestern Greenland. We study the response to oceanic and atmospheric warming. Our results are universal and relevant for the development of climate models.