Articles | Volume 17, issue 1
https://doi.org/10.5194/tc-17-79-2023
https://doi.org/10.5194/tc-17-79-2023
Research article
 | 
11 Jan 2023
Research article |  | 11 Jan 2023

Antarctic contribution to future sea level from ice shelf basal melt as constrained by ice discharge observations

Eveline C. van der Linden, Dewi Le Bars, Erwin Lambert, and Sybren Drijfhout

Viewed

Total article views: 2,368 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,756 557 55 2,368 40 42
  • HTML: 1,756
  • PDF: 557
  • XML: 55
  • Total: 2,368
  • BibTeX: 40
  • EndNote: 42
Views and downloads (calculated since 24 Nov 2021)
Cumulative views and downloads (calculated since 24 Nov 2021)

Viewed (geographical distribution)

Total article views: 2,368 (including HTML, PDF, and XML) Thereof 2,326 with geography defined and 42 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 26 Apr 2024
Download
Short summary
The Antarctic ice sheet (AIS) is the largest uncertainty in future sea level estimates. The AIS mainly loses mass through ice discharge, the transfer of land ice into the ocean. Ice discharge is triggered by warming ocean water (basal melt). New future estimates of AIS sea level contributions are presented in which basal melt is constrained with ice discharge observations. Despite the different methodology, the resulting projections are in line with previous multimodel assessments.