Articles | Volume 20, issue 7
https://doi.org/10.5194/tc-20-3977-2026
https://doi.org/10.5194/tc-20-3977-2026
Research article
 | 
20 Jul 2026
Research article |  | 20 Jul 2026

Late Holocene stabilization of Conway Ice Ridge

Andrew O. Hoffman, Paul T. Summers, Jenny Suckale, Knut Christianson, Ginny Catania, and Howard Conway

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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) (15 Oct 2025) by Reinhard Drews
AR by Andrew Hoffman on behalf of the Authors (16 Jan 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (23 Jan 2026) by Reinhard Drews
RR by Antoine Hermant (03 Feb 2026)
ED: Publish subject to technical corrections (04 Feb 2026) by Reinhard Drews
AR by Andrew Hoffman on behalf of the Authors (21 Feb 2026)  Author's response   Manuscript 
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Short summary
In Antarctica, fast-flowing ice streams drive most ice loss. Radar data from Conway Ice Ridge reveal that the van der Veen and Mercer Ice Streams were wider ~3000 years ago and narrowed progressively. Numerical modeling demonstrates that small thickness changes can rapidly alter shear-margin locations. These findings offer crucial insights into Late Holocene Ice Sheet readvance.
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