Articles | Volume 15, issue 12
The Cryosphere, 15, 5739–5764, 2021
https://doi.org/10.5194/tc-15-5739-2021
The Cryosphere, 15, 5739–5764, 2021
https://doi.org/10.5194/tc-15-5739-2021
Research article
 | Highlight paper
20 Dec 2021
Research article  | Highlight paper | 20 Dec 2021

Impact of the melt–albedo feedback on the future evolution of the Greenland Ice Sheet with PISM-dEBM-simple

Maria Zeitz et al.

Viewed

Total article views: 2,556 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,924 594 38 2,556 50 26 18
  • HTML: 1,924
  • PDF: 594
  • XML: 38
  • Total: 2,556
  • Supplement: 50
  • BibTeX: 26
  • EndNote: 18
Views and downloads (calculated since 24 Mar 2021)
Cumulative views and downloads (calculated since 24 Mar 2021)

Viewed (geographical distribution)

Total article views: 2,466 (including HTML, PDF, and XML) Thereof 2,466 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 04 Jul 2022
Download
Short summary
With the increasing melt of the Greenland Ice Sheet, which contributes to sea level rise, the surface of the ice darkens. The dark surfaces absorb more radiation and thus experience increased melt, resulting in the melt–albedo feedback. Using a simple surface melt model, we estimate that this positive feedback contributes to an additional 60 % ice loss in a high-warming scenario and additional 90 % ice loss for moderate warming. Albedo changes are important for Greenland’s future ice loss.