The Cryosphere
The Cryosphere
TC
Articles | Volume 16, issue 10
Articles | Volume 16, issue 10
https://doi.org/10.5194/tc-16-4305-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-16-4305-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 16, issue 10
Research article
 | 
13 Oct 2022
Research article |  | 13 Oct 2022

Observed mechanism for sustained glacier retreat and acceleration in response to ocean warming around Greenland

Evan Carnahan, Ginny Catania, and Timothy C. Bartholomaus

Viewed

Total article views: 1,644 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,114 488 42 1,644 62 24 28
  • HTML: 1,114
  • PDF: 488
  • XML: 42
  • Total: 1,644
  • Supplement: 62
  • BibTeX: 24
  • EndNote: 28
Views and downloads (calculated since 07 Jun 2022)
Cumulative views and downloads (calculated since 07 Jun 2022)

Viewed (geographical distribution)

Total article views: 1,644 (including HTML, PDF, and XML) Thereof 1,593 with geography defined and 51 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 25 Apr 2024
Download
Short summary
The Greenland Ice Sheet primarily loses mass through increased ice discharge. We find changes in discharge from outlet glaciers are initiated by ocean warming, which causes a change in the balance of forces resisting gravity and leads to acceleration. Vulnerable conditions for sustained retreat and acceleration are predetermined by the glacier-fjord geometry and exist around Greenland, suggesting increases in ice discharge may be sustained into the future despite a pause in ocean warming.
Read more