The Cryosphere
The Cryosphere
TC
Articles | Volume 18, issue 10
Articles | Volume 18, issue 10
https://doi.org/10.5194/tc-18-4743-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-18-4743-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 18, issue 10
Research article
 | 
18 Oct 2024
Research article |  | 18 Oct 2024

The cryostratigraphy of thermo-erosion gullies in the Canadian High Arctic demonstrates the resilience of permafrost

Samuel Gagnon, Daniel Fortier, Étienne Godin, and Audrey Veillette

Viewed

Total article views: 510 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
395 77 38 510 52 21 39
  • HTML: 395
  • PDF: 77
  • XML: 38
  • Total: 510
  • Supplement: 52
  • BibTeX: 21
  • EndNote: 39
Views and downloads (calculated since 14 Mar 2024)
Cumulative views and downloads (calculated since 14 Mar 2024)

Viewed (geographical distribution)

Total article views: 510 (including HTML, PDF, and XML) Thereof 517 with geography defined and -7 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 27 Oct 2024
Download
Short summary
Thermo-erosion gullies (TEGs) are one of the most common forms of abrupt permafrost degradation. While their inception has been examined in several studies, the processes of their stabilization remain poorly documented. For this study, we investigated two TEGs in the Canadian High Arctic. We found that, while the formation of a TEG leaves permanent geomorphological scars in landscapes, in the long term, permafrost can recover to conditions similar to those pre-dating the initial disturbance.
Read more