Articles | Volume 15, issue 10
https://doi.org/10.5194/tc-15-4675-2021
https://doi.org/10.5194/tc-15-4675-2021
Research article
 | 
06 Oct 2021
Research article |  | 06 Oct 2021

Quantifying the potential future contribution to global mean sea level from the Filchner–Ronne basin, Antarctica

Emily A. Hill, Sebastian H. R. Rosier, G. Hilmar Gudmundsson, and Matthew Collins

Viewed

Total article views: 3,400 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,271 1,060 69 3,400 266 67 61
  • HTML: 2,271
  • PDF: 1,060
  • XML: 69
  • Total: 3,400
  • Supplement: 266
  • BibTeX: 67
  • EndNote: 61
Views and downloads (calculated since 23 Apr 2021)
Cumulative views and downloads (calculated since 23 Apr 2021)

Viewed (geographical distribution)

Total article views: 3,400 (including HTML, PDF, and XML) Thereof 3,257 with geography defined and 143 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Dec 2024
Download
Short summary
Using an ice flow model and uncertainty quantification methods, we provide probabilistic projections of future sea level rise from the Filchner–Ronne region of Antarctica. We find that it is most likely that this region will contribute negatively to sea level rise over the next 300 years, largely as a result of increased surface mass balance. We identify parameters controlling ice shelf melt and snowfall contribute most to uncertainties in projections.