Articles | Volume 14, issue 2
https://doi.org/10.5194/gmd-14-889-2021
https://doi.org/10.5194/gmd-14-889-2021
Model description paper
 | 
11 Feb 2021
Model description paper |  | 11 Feb 2021

The Framework For Ice Sheet–Ocean Coupling (FISOC) V1.1

Rupert Gladstone, Benjamin Galton-Fenzi, David Gwyther, Qin Zhou, Tore Hattermann, Chen Zhao, Lenneke Jong, Yuwei Xia, Xiaoran Guo, Konstantinos Petrakopoulos, Thomas Zwinger, Daniel Shapero, and John Moore

Viewed

Total article views: 2,265 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,437 785 43 2,265 277 58 48
  • HTML: 1,437
  • PDF: 785
  • XML: 43
  • Total: 2,265
  • Supplement: 277
  • BibTeX: 58
  • EndNote: 48
Views and downloads (calculated since 04 Aug 2020)
Cumulative views and downloads (calculated since 04 Aug 2020)

Viewed (geographical distribution)

Total article views: 2,265 (including HTML, PDF, and XML) Thereof 2,002 with geography defined and 263 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 18 Apr 2024
Download
Short summary
Retreat of the Antarctic ice sheet, and hence its contribution to sea level rise, is highly sensitive to melting of its floating ice shelves. This melt is caused by warm ocean currents coming into contact with the ice. Computer models used for future ice sheet projections are not able to realistically evolve these melt rates. We describe a new coupling framework to enable ice sheet and ocean computer models to interact, allowing projection of the evolution of melt and its impact on sea level.