Articles | Volume 19, issue 6
https://doi.org/10.5194/tc-19-2133-2025
https://doi.org/10.5194/tc-19-2133-2025
Research article
 | 
23 Jun 2025
Research article |  | 23 Jun 2025

Improved basal drag of the West Antarctic Ice Sheet from L-curve analysis of inverse models utilizing subglacial hydrology simulations

Lea-Sophie Höyns, Thomas Kleiner, Andreas Rademacher, Martin Rückamp, Michael Wolovick, and Angelika Humbert

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-1251', Anonymous Referee #1, 19 Aug 2024
    • AC1: 'Reply on RC1', Lea-Sophie Hoeyns, 11 Oct 2024
  • RC2: 'Comment on egusphere-2024-1251', Anonymous Referee #2, 03 Sep 2024
    • AC2: 'Reply on RC2', Lea-Sophie Hoeyns, 11 Oct 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (further review by editor and referees) (18 Nov 2024) by Felicity McCormack
AR by Lea-Sophie Hoeyns on behalf of the Authors (14 Jan 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to revisions (further review by editor and referees) (24 Jan 2025) by Felicity McCormack
ED: Referee Nomination & Report Request started (27 Jan 2025) by Felicity McCormack
RR by Anonymous Referee #1 (03 Feb 2025)
RR by Anonymous Referee #2 (24 Feb 2025)
ED: Publish subject to minor revisions (review by editor) (04 Mar 2025) by Felicity McCormack
AR by Lea-Sophie Hoeyns on behalf of the Authors (24 Mar 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (25 Mar 2025) by Felicity McCormack
AR by Lea-Sophie Hoeyns on behalf of the Authors (25 Mar 2025)  Manuscript 
Download
Short summary
The sliding of glaciers over bedrock is influenced by water pressure in the underlying hydrological system and the roughness of the land underneath the glacier. We estimate this roughness through a modeling approach that optimizes this unknown parameter. Additionally, we simulate water pressure, enhancing the reliability of the computed drag at the ice sheet base. The resulting data are provided to other modelers and scientists conducting geophysical field observations.
Share