Articles | Volume 19, issue 11
https://doi.org/10.5194/tc-19-5509-2025
https://doi.org/10.5194/tc-19-5509-2025
Research article
 | 
10 Nov 2025
Research article |  | 10 Nov 2025

Ocean-induced weakening of George VI Ice Shelf, West Antarctica

Ann-Sofie P. Zinck, Bert Wouters, Franka Jesse, and Stef Lhermitte

Viewed

Total article views: 1,476 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,289 140 47 1,476 36 59
  • HTML: 1,289
  • PDF: 140
  • XML: 47
  • Total: 1,476
  • BibTeX: 36
  • EndNote: 59
Views and downloads (calculated since 19 Mar 2025)
Cumulative views and downloads (calculated since 19 Mar 2025)

Viewed (geographical distribution)

Total article views: 1,476 (including HTML, PDF, and XML) Thereof 1,476 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 30 Nov 2025
Download
Short summary
Ocean-driven basal melting of ice shelves can carve channels into the ice shelf base. These channels represent potential weak areas of the ice shelf. On George VI Ice shelf we discover a new channel which onset coincides with the 2015 El-Nino Southern Oscillation event. Since the channel has developed rapidly and is located within a highly channelized area close to the ice shelf front it poses a potential thread of ice shelf retreat.
Share