Articles | Volume 20, issue 3
https://doi.org/10.5194/tc-20-1655-2026
https://doi.org/10.5194/tc-20-1655-2026
Research article
 | 
20 Mar 2026
Research article |  | 20 Mar 2026

How to model crevasse initiation? Lessons from the artificial drainage of a water-filled cavity on the Tête Rousse Glacier (Mont Blanc range, France)

Julien Brondex, Olivier Gagliardini, Adrien Gilbert, and Emmanuel Thibert

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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: Reconsider after major revisions (further review by editor and referees) (18 Nov 2025) by Evgeny A. Podolskiy
AR by Julien Brondex on behalf of the Authors (25 Nov 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Reconsider after major revisions (further review by editor and referees) (26 Nov 2025) by Evgeny A. Podolskiy
AR by Julien Brondex on behalf of the Authors (26 Nov 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (27 Nov 2025) by Evgeny A. Podolskiy
RR by Sarah Wells-Moran (13 Dec 2025)
RR by Lizz Ultee (25 Feb 2026)
ED: Publish subject to minor revisions (review by editor) (27 Feb 2026) by Evgeny A. Podolskiy
AR by Julien Brondex on behalf of the Authors (05 Mar 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (06 Mar 2026) by Evgeny A. Podolskiy
AR by Julien Brondex on behalf of the Authors (06 Mar 2026)
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Short summary
We investigate crevasse initiation by analyzing the artificial drainage of a water-filled cavity at Tête Rousse Glacier (Mont Blanc, France). Using a numerical model, we compute stress fields in response to water level variations in the cavity and compare them to observed crevasse patterns. Results show that a non-linear viscous rheology and a maximum principal stress criterion (with a stress threshold of 100–130 kPa) best predict crevasse occurrence.
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