Articles | Volume 15, issue 1
https://doi.org/10.5194/tc-15-459-2021
https://doi.org/10.5194/tc-15-459-2021
Research article
 | 
28 Jan 2021
Research article |  | 28 Jan 2021

Sensitivity of the Antarctic ice sheets to the warming of marine isotope substage 11c

Martim Mas e Braga, Jorge Bernales, Matthias Prange, Arjen P. Stroeven, and Irina Rogozhina

Viewed

Total article views: 2,955 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,997 839 119 2,955 296 86 100
  • HTML: 1,997
  • PDF: 839
  • XML: 119
  • Total: 2,955
  • Supplement: 296
  • BibTeX: 86
  • EndNote: 100
Views and downloads (calculated since 25 May 2020)
Cumulative views and downloads (calculated since 25 May 2020)

Viewed (geographical distribution)

Total article views: 2,955 (including HTML, PDF, and XML) Thereof 2,802 with geography defined and 153 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 21 Nov 2024
Download
Short summary
We combine a computer model with different climate records to simulate how Antarctica responded to warming during marine isotope substage 11c, which can help understand Antarctica's natural drivers of change. We found that the regional climate warming of Antarctica seen in ice cores was necessary for the model to match the recorded sea level rise. A collapse of its western ice sheet is possible if a modest warming is sustained for ca. 4000 years, contributing 6.7 to 8.2 m to sea level rise.