Articles | Volume 17, issue 9
https://doi.org/10.5194/tc-17-4021-2023
https://doi.org/10.5194/tc-17-4021-2023
Research article
 | 
18 Sep 2023
Research article |  | 18 Sep 2023

Reconciling ice dynamics and bed topography with a versatile and fast ice thickness inversion

Thomas Frank, Ward J. J. van Pelt, and Jack Kohler

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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 tc-2023-43', Samuel Cook, 06 Apr 2023
    • AC1: 'Reply on RC1', Thomas Frank, 21 Jun 2023
  • RC2: 'Comment on tc-2023-43', Anonymous Referee #2, 17 Apr 2023
    • AC2: 'Reply on RC2', Thomas Frank, 21 Jun 2023

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) (03 Jul 2023) by Daniel Farinotti
AR by Thomas Frank on behalf of the Authors (11 Jul 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (17 Jul 2023) by Daniel Farinotti
RR by Samuel Cook (18 Jul 2023)
RR by Anonymous Referee #2 (24 Jul 2023)
ED: Publish subject to minor revisions (review by editor) (25 Jul 2023) by Daniel Farinotti
AR by Thomas Frank on behalf of the Authors (11 Aug 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (14 Aug 2023) by Daniel Farinotti
AR by Thomas Frank on behalf of the Authors (14 Aug 2023)  Manuscript 
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Short summary
Since the ice thickness of most glaciers worldwide is unknown, and since it is not feasible to visit every glacier and observe their thickness directly, inverse modelling techniques are needed that can calculate ice thickness from abundant surface observations. Here, we present a new method for doing that. Our methodology relies on modelling the rate of surface elevation change for a given glacier, compare this with observations of the same quantity and change the bed until the two are in line.