Articles | Volume 19, issue 11
https://doi.org/10.5194/tc-19-5903-2025
https://doi.org/10.5194/tc-19-5903-2025
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: 5,159 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,509 1,109 541 5,159 109 151 232
  • HTML: 3,509
  • PDF: 1,109
  • XML: 541
  • Total: 5,159
  • Supplement: 109
  • BibTeX: 151
  • EndNote: 232
Views and downloads (calculated since 24 Oct 2024)
Cumulative views and downloads (calculated since 24 Oct 2024)

Viewed (geographical distribution)

Total article views: 5,159 (including HTML, PDF, and XML) Thereof 5,061 with geography defined and 98 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Saved (final revised paper)

Latest update: 17 Aug 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.
Share