Articles | Volume 13, issue 2
https://doi.org/10.5194/tc-13-723-2019
https://doi.org/10.5194/tc-13-723-2019
Research article
 | 
01 Mar 2019
Research article |  | 01 Mar 2019

Modeling the response of northwest Greenland to enhanced ocean thermal forcing and subglacial discharge

Mathieu Morlighem, Michael Wood, Hélène Seroussi, Youngmin Choi, and Eric Rignot

Viewed

Total article views: 3,425 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,325 1,021 79 3,425 411 81 73
  • HTML: 2,325
  • PDF: 1,021
  • XML: 79
  • Total: 3,425
  • Supplement: 411
  • BibTeX: 81
  • EndNote: 73
Views and downloads (calculated since 26 Oct 2018)
Cumulative views and downloads (calculated since 26 Oct 2018)

Viewed (geographical distribution)

Total article views: 3,425 (including HTML, PDF, and XML) Thereof 2,989 with geography defined and 436 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 25 Apr 2024
Download
Short summary
Many glaciers along the coast of Greenland have been retreating. It has been suggested that this retreat is triggered by the presence of warm water in the fjords, and surface melt at the top of the ice sheet is exacerbating this problem. Here, we quantify the vulnerability of northwestern Greenland to further warming using a numerical model. We find that in current conditions, this sector alone will contribute more than 1 cm to sea rise level by 2100, and up to 3 cm in the most extreme scenario.