Articles | Volume 20, issue 7
https://doi.org/10.5194/tc-20-4061-2026
https://doi.org/10.5194/tc-20-4061-2026
Research article
 | 
24 Jul 2026
Research article |  | 24 Jul 2026

Evolution of the Antarctic Ice Sheet from 2000–2300 and beyond: model sensitivity and uncertainty analysis using MPAS-Albany Land Ice

Trevor R. Hillebrand, Matthew J. Hoffman, Holly K. Han, Mauro Perego, Alexander O. Hager, Andrew Nolan, Xylar Asay-Davis, Stephen F. Price, Jerry Watkins, and Max Carlson

Viewed

Total article views: 16,291 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
14,604 1,485 202 16,291 405 403
  • HTML: 14,604
  • PDF: 1,485
  • XML: 202
  • Total: 16,291
  • BibTeX: 405
  • EndNote: 403
Views and downloads (calculated since 28 Aug 2025)
Cumulative views and downloads (calculated since 28 Aug 2025)

Viewed (geographical distribution)

Total article views: 16,291 (including HTML, PDF, and XML) Thereof 16,266 with geography defined and 25 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 24 Jul 2026
Download
Short summary
We present new simulations that complement our contribution to the ISMIP6-Antarctica-2300 ensemble. We find significant mass loss after 2300 under both low-emissions and present-day forcing. Thermal evolution is extremely important, with fixed temperature yielding up to almost twice as much mass loss as simulations with evolving temperature. External forcing uncertainty, rather than parameter uncertainty, dominates the ensemble spread after 2050.
Share