The Cryosphere
The Cryosphere
TC
Articles | Volume 16, issue 2
Articles | Volume 16, issue 2
https://doi.org/10.5194/tc-16-451-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-16-451-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 16, issue 2
Research article
 | Highlight paper
 | 
08 Feb 2022
Research article | Highlight paper |  | 08 Feb 2022

Layered seawater intrusion and melt under grounded ice

Alexander A. Robel, Earle Wilson, and Helene Seroussi

Viewed

Total article views: 7,316 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
6,286 929 101 7,316 89 103
  • HTML: 6,286
  • PDF: 929
  • XML: 101
  • Total: 7,316
  • BibTeX: 89
  • EndNote: 103
Views and downloads (calculated since 29 Sep 2021)
Cumulative views and downloads (calculated since 29 Sep 2021)

Viewed (geographical distribution)

Total article views: 7,316 (including HTML, PDF, and XML) Thereof 6,959 with geography defined and 357 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Dec 2024
Download
Short summary
Warm seawater may intrude as a thin layer below glaciers in contact with the ocean. Mathematical theory predicts that this intrusion may extend over distances of kilometers under realistic conditions. Computer models demonstrate that if this warm seawater causes melting of a glacier bottom, it can cause rates of glacier ice loss and sea level rise to be up to 2 times faster in response to potential future ocean warming.
Read more