Articles | Volume 20, issue 2
https://doi.org/10.5194/tc-20-1071-2026
https://doi.org/10.5194/tc-20-1071-2026
Research article
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13 Feb 2026
Research article | Highlight paper |  | 13 Feb 2026

Exploring the conditions conducive to convection within the Greenland Ice Sheet

Robert Law, Andreas Born, Philipp Voigt, Joseph A. MacGregor, and Claire Marie Guimond

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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) (04 Nov 2025) by Carlos Martin
AR by Robert Law on behalf of the Authors (05 Nov 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (06 Nov 2025) by Carlos Martin
RR by Yu Zhang (24 Nov 2025)
RR by Michael Wolovick (27 Nov 2025)
ED: Publish subject to minor revisions (review by editor) (16 Dec 2025) by Carlos Martin
AR by Robert Law on behalf of the Authors (20 Jan 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (21 Jan 2026) by Carlos Martin
AR by Robert Law on behalf of the Authors (27 Jan 2026)  Manuscript 
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Co-editor-in-chief
This paper investigates a puzzling and still-unresolved phenomenon: the presence of large plume-like features visible in the layers of the Greenland Ice Sheet. Although previous studies have proposed various explanations for these features, none have been confirmed to date. In this study, the authors investigate an unconventional and debated hypothesis: That local thermal convection may be responsible for the observed layer disruptions. This work opens new avenues for research and provides a fresh perspective on an intriguing scientific problem.
Short summary
Convection has been previously, yet contentiously, suggested for ice sheets, but never before comprehensively explored using numerical models. We use mantle dynamics code to test the hypothesis that convection gives rise to enigmatic plume-like features observed in radio-stratigraphy observations of the Greenland Ice Sheet. Our results provide very good agreement with field observations, but could imply that ice in northern Greenland is significantly softer than commonly thought.
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