The Cryosphere
The Cryosphere
TC
Articles | Volume 20, issue 8
Articles | Volume 20, issue 8
https://doi.org/10.5194/tc-20-4747-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-20-4747-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 20, issue 8
Research article
 | 
26 Aug 2026
Research article |  | 26 Aug 2026

On the non-linear response of Antarctic ice shelf surface melt to warming

Marte Gé Hofsteenge, Willem Jan van de Berg, Christiaan van Dalum, Kristiina Verro, Maurice van Tiggelen, and Michiel van den Broeke

Viewed

Total article views: 9,941 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
6,896 2,721 324 9,941 309 327
  • HTML: 6,896
  • PDF: 2,721
  • XML: 324
  • Total: 9,941
  • BibTeX: 309
  • EndNote: 327
Views and downloads (calculated since 23 Sep 2025)
Cumulative views and downloads (calculated since 23 Sep 2025)

Viewed (geographical distribution)

Total article views: 9,941 (including HTML, PDF, and XML) Thereof 9,877 with geography defined and 64 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 14 Nov 2026
Download
Short summary
We use a regional climate model to study how surface melt on Antarctic ice shelves responds to air temperature. The relationship is strongly non-linear, mainly due to feedbacks in surface albedo, with other energy sources also contributing. Currently colder, drier, and more stable ice shelves will experience more melt at the same temperature than ice shelves in wetter climates, highlighting their vulnerability to fracturing, ice shelf instability, and contributions to global sea-level rise.
Read more
Share
Altmetrics
Final-revised paper
Preprint