The Cryosphere
The Cryosphere
TC
Articles | Volume 19, issue 2
Articles | Volume 19, issue 2
https://doi.org/10.5194/tc-19-541-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/tc-19-541-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 19, issue 2
Research article
 | 
04 Feb 2025
Research article |  | 04 Feb 2025

ISMIP6-based Antarctic projections to 2100: simulations with the BISICLES ice sheet model

James F. O'Neill, Tamsin L. Edwards, Daniel F. Martin, Courtney Shafer, Stephen L. Cornford, Hélène L. Seroussi, Sophie Nowicki, Mira Adhikari, and Lauren J. Gregoire

Viewed

Total article views: 1,712 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,147 294 271 1,712 25 41 59
  • HTML: 1,147
  • PDF: 294
  • XML: 271
  • Total: 1,712
  • Supplement: 25
  • BibTeX: 41
  • EndNote: 59
Views and downloads (calculated since 27 Feb 2024)
Cumulative views and downloads (calculated since 27 Feb 2024)

Viewed (geographical distribution)

Total article views: 1,712 (including HTML, PDF, and XML) Thereof 1,695 with geography defined and 17 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 17 Apr 2025
Download
Short summary
We use an ice sheet model to simulate the Antarctic contribution to sea level over the 21st century under a range of future climates and varying how sensitive the ice sheet is to different processes. We find that ocean temperatures increase and more snow falls on the ice sheet under stronger warming scenarios. When the ice sheet is sensitive to ocean warming, ocean melt-driven loss exceeds snowfall-driven gains, meaning that the sea level contribution is greater with more climate warming.
Read more
Share
Special issue
The Ice Sheet Model Intercomparison Project for CMIP6...