Articles | Volume 18, issue 11
https://doi.org/10.5194/tc-18-5117-2024
https://doi.org/10.5194/tc-18-5117-2024
Research article
 | 
13 Nov 2024
Research article |  | 13 Nov 2024

Sensitivity of the future evolution of the Wilkes Subglacial Basin ice sheet to grounding-line melt parameterizations

Yu Wang, Chen Zhao, Rupert Gladstone, Thomas Zwinger, Benjamin K. Galton-Fenzi, and Poul Christoffersen

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-1005', Tijn Berends, 12 May 2024
    • AC1: 'Reply on RC1', Yu Wang, 08 Aug 2024
  • RC2: 'Comment on egusphere-2024-1005', Anonymous Referee #2, 22 May 2024
    • AC2: 'Reply on RC2', Yu Wang, 08 Aug 2024

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) (15 Aug 2024) by Jan De Rydt
AR by Yu Wang on behalf of the Authors (26 Aug 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (16 Sep 2024) by Jan De Rydt
AR by Yu Wang on behalf of the Authors (26 Sep 2024)  Manuscript 
Download
Short summary
Our research delves into the future evolution of Antarctica's Wilkes Subglacial Basin (WSB) and its potential contribution to sea level rise, focusing on how basal melt is implemented at the grounding line in ice flow models. Our findings suggest that these implementation methods can significantly impact the magnitude of future ice loss projections. Under a high-emission scenario, the WSB ice sheet could undergo massive and rapid retreat between 2200 and 2300.