Articles | Volume 19, issue 6
https://doi.org/10.5194/tc-19-2289-2025
https://doi.org/10.5194/tc-19-2289-2025
Research article
 | 
27 Jun 2025
Research article |  | 27 Jun 2025

Role of elevation feedbacks and ice sheet–climate interactions on future Greenland ice sheet melt

Thirza Feenstra, Miren Vizcaino, Bert Wouters, Michele Petrini, Raymond Sellevold, and Katherine Thayer-Calder

Viewed

Total article views: 3,333 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,540 524 269 3,333 96 144
  • HTML: 2,540
  • PDF: 524
  • XML: 269
  • Total: 3,333
  • BibTeX: 96
  • EndNote: 144
Views and downloads (calculated since 13 May 2024)
Cumulative views and downloads (calculated since 13 May 2024)

Viewed (geographical distribution)

Total article views: 3,333 (including HTML, PDF, and XML) Thereof 3,203 with geography defined and 130 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 10 Mar 2026
Download
Short summary
We present the first evaluation of Greenland ice sheet (GrIS) and climate feedbacks with a CMIP model. Under 4×CO2 forcing, lower elevations reduce GrIS summer blocking and incoming solar radiation and increase precipitation. Simulated increases of near-surface summer temperature are much lower than the 6 K km-1 lapse rate that is commonly used in non-coupled simulations. CO2 reduction to pre-industrial (PI) halts GrIS mass loss regardless of higher global warming and albedo than PI control.
Share