The Cryosphere
The Cryosphere
TC
Articles | Volume 19, issue 11
Articles | Volume 19, issue 11
https://doi.org/10.5194/tc-19-5903-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-19-5903-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 19, issue 11
Brief communication
 | 
18 Nov 2025
Brief communication |  | 18 Nov 2025

Brief communication: Tides and damage as drivers of lake drainages on Shackleton Ice Shelf

Julius Sommer, Maaike Izeboud, Sophie de Roda Husman, Bert Wouters, and Stef Lhermitte

Viewed

Total article views: 5,002 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,416 1,059 527 5,002 101 141 217
  • HTML: 3,416
  • PDF: 1,059
  • XML: 527
  • Total: 5,002
  • Supplement: 101
  • BibTeX: 141
  • EndNote: 217
Views and downloads (calculated since 24 Oct 2024)
Cumulative views and downloads (calculated since 24 Oct 2024)

Viewed (geographical distribution)

Total article views: 5,002 (including HTML, PDF, and XML) Thereof 4,954 with geography defined and 48 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Saved (final revised paper)

Latest update: 13 Jun 2026
Download
Short summary
Ice shelves, the floating extensions of Antarctica’s ice sheet, play a crucial role in preventing mass ice loss, and understanding their stability is crucial. If surface meltwater lakes drain rapidly through fractures, the ice shelf can destabilize. We analyzed satellite images of four years from the Shackleton Ice Shelf and found that lake drainages occurred in areas where damage is present and developing, and coincided with rising tides, offering insights into the drivers of this process.
Read more
Share