The Cryosphere
The Cryosphere
TC
Articles | Volume 16, issue 4
Articles | Volume 16, issue 4
https://doi.org/10.5194/tc-16-1315-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-16-1315-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 16, issue 4
Research article
 | 
11 Apr 2022
Research article |  | 11 Apr 2022

Net effect of ice-sheet–atmosphere interactions reduces simulated transient Miocene Antarctic ice-sheet variability

Lennert B. Stap, Constantijn J. Berends, Meike D. W. Scherrenberg, Roderik S. W. van de Wal, and Edward G. W. Gasson

Viewed

Total article views: 3,579 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,645 836 98 3,579 311 118 196
  • HTML: 2,645
  • PDF: 836
  • XML: 98
  • Total: 3,579
  • Supplement: 311
  • BibTeX: 118
  • EndNote: 196
Views and downloads (calculated since 01 Nov 2021)
Cumulative views and downloads (calculated since 01 Nov 2021)

Viewed (geographical distribution)

Total article views: 3,579 (including HTML, PDF, and XML) Thereof 3,467 with geography defined and 112 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 25 Apr 2026
Download
Short summary
To gain understanding of how the Antarctic ice sheet responded to CO2 changes during past warm climate conditions, we simulate its variability during the Miocene. We include feedbacks between the ice sheet and atmosphere in our model and force the model using time-varying climate conditions. We find that these feedbacks reduce the amplitude of ice volume variations. Erosion-induced changes in the bedrock below the ice sheet that manifested during the Miocene also have a damping effect.
Read more
Share