The Cryosphere
The Cryosphere
TC
Articles | Volume 14, issue 12
Articles | Volume 14, issue 12
https://doi.org/10.5194/tc-14-4299-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-14-4299-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 14, issue 12
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: 10,432 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
8,300 1,964 168 10,432 192 249
  • HTML: 8,300
  • PDF: 1,964
  • XML: 168
  • Total: 10,432
  • BibTeX: 192
  • EndNote: 249
Views and downloads (calculated since 16 Apr 2020)
Cumulative views and downloads (calculated since 16 Apr 2020)

Viewed (geographical distribution)

Total article views: 10,432 (including HTML, PDF, and XML) Thereof 9,485 with geography defined and 947 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 30 Nov 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.
Read more
Share