The Cryosphere
The Cryosphere
TC
Articles | Volume 20, issue 3
Articles | Volume 20, issue 3
https://doi.org/10.5194/tc-20-1655-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-20-1655-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 20, issue 3
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

Viewed

Total article views: 3,734 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,107 512 115 3,734 258 118 165
  • HTML: 3,107
  • PDF: 512
  • XML: 115
  • Total: 3,734
  • Supplement: 258
  • BibTeX: 118
  • EndNote: 165
Views and downloads (calculated since 20 May 2025)
Cumulative views and downloads (calculated since 20 May 2025)

Viewed (geographical distribution)

Total article views: 3,734 (including HTML, PDF, and XML) Thereof 3,718 with geography defined and 16 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 25 Jun 2026
Download
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.
Read more
Share