Articles | Volume 16, issue 6
https://doi.org/10.5194/tc-16-2545-2022
https://doi.org/10.5194/tc-16-2545-2022
Research article
 | 
27 Jun 2022
Research article |  | 27 Jun 2022

Rapid fragmentation of Thwaites Eastern Ice Shelf

Douglas I. Benn, Adrian Luckman, Jan A. Åström, Anna J. Crawford, Stephen L. Cornford, Suzanne L. Bevan, Thomas Zwinger, Rupert Gladstone, Karen Alley, Erin Pettit, and Jeremy Bassis

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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) (01 Feb 2022) by Josefin Ahlkrona
AR by Adrian Luckman on behalf of the Authors (06 Mar 2022)  Author's response   Author's tracked changes 
EF by Polina Shvedko (09 Mar 2022)  Manuscript 
ED: Referee Nomination & Report Request started (14 Mar 2022) by Josefin Ahlkrona
RR by Stef Lhermitte (29 Mar 2022)
RR by Anonymous Referee #1 (25 Apr 2022)
ED: Publish as is (25 Apr 2022) by Josefin Ahlkrona
AR by Adrian Luckman on behalf of the Authors (13 May 2022)
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Short summary
Thwaites Glacier (TG), in West Antarctica, is potentially unstable and may contribute significantly to sea-level rise as global warming continues. Using satellite data, we show that Thwaites Eastern Ice Shelf, the largest remaining floating extension of TG, has started to accelerate as it fragments along a shear zone. Computer modelling does not indicate that fragmentation will lead to imminent glacier collapse, but it is clear that major, rapid, and unpredictable changes are underway.