Articles | Volume 14, issue 12
https://doi.org/10.5194/tc-14-4299-2020
https://doi.org/10.5194/tc-14-4299-2020
Research article
 | 
01 Dec 2020
Research article |  | 01 Dec 2020

Large and irreversible future decline of the Greenland ice sheet

Jonathan M. Gregory, Steven E. George, and Robin S. Smith

Viewed

Total article views: 8,953 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
7,049 1,766 138 8,953 141 144
  • HTML: 7,049
  • PDF: 1,766
  • XML: 138
  • Total: 8,953
  • BibTeX: 141
  • EndNote: 144
Views and downloads (calculated since 16 Apr 2020)
Cumulative views and downloads (calculated since 16 Apr 2020)

Viewed (geographical distribution)

Total article views: 8,953 (including HTML, PDF, and XML) Thereof 8,037 with geography defined and 916 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 02 Apr 2025
Download
Short summary
Melting of the Greenland ice sheet as a consequence of global warming could raise global-mean sea level by up to 7 m. We have studied this using a newly developed computer model. With recent climate maintained, sea level would rise by 0.5–2.5 m over many millennia due to Greenland ice loss: the warmer the climate, the greater the sea level rise. Beyond about 3.5 m it would become partially irreversible. In order to avoid this outcome, anthropogenic climate change must be reversed soon enough.
Share