The Cryosphere
The Cryosphere
TC
Articles | Volume 18, issue 5
Articles | Volume 18, issue 5
https://doi.org/10.5194/tc-18-2583-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-18-2583-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 18, issue 5
Research article
 | 
28 May 2024
Research article |  | 28 May 2024

Responses of the Pine Island and Thwaites glaciers to melt and sliding parameterizations

Ian Joughin, Daniel Shapero, and Pierre Dutrieux

Viewed

Total article views: 1,343 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,026 280 37 1,343 60 31 30
  • HTML: 1,026
  • PDF: 280
  • XML: 37
  • Total: 1,343
  • Supplement: 60
  • BibTeX: 31
  • EndNote: 30
Views and downloads (calculated since 08 Jan 2024)
Cumulative views and downloads (calculated since 08 Jan 2024)

Viewed (geographical distribution)

Total article views: 1,343 (including HTML, PDF, and XML) Thereof 1,334 with geography defined and 9 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 01 Nov 2024
Download

The requested paper has a corresponding corrigendum published. Please read the corrigendum first before downloading the article.

Short summary
The Pine Island and Thwaites glaciers are losing ice to the ocean rapidly as warmer water melts their floating ice shelves. Models help determine how much such glaciers will contribute to sea level. We find that ice loss varies in response to how much melting the ice shelves are subjected to. Our estimated losses are also sensitive to how much the friction beneath the glaciers is reduced as it goes afloat. Melt-forced sea level rise from these glaciers is likely to be less than 10 cm by 2300.
Read more