Climate of the Past
Climate of the Past
CP
Articles | Volume 21, issue 1
Articles | Volume 21, issue 1
https://doi.org/10.5194/cp-21-95-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-21-95-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 21, issue 1
Research article
 | 
14 Jan 2025
Research article |  | 14 Jan 2025

Sustainability of regional Antarctic ice sheets under late Eocene seasonal atmospheric conditions

Dennis H. A. Vermeulen, Michiel L. J. Baatsen, and Anna S. von der Heydt

Viewed

Total article views: 2,002 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,545 373 84 2,002 99 141
  • HTML: 1,545
  • PDF: 373
  • XML: 84
  • Total: 2,002
  • BibTeX: 99
  • EndNote: 141
Views and downloads (calculated since 24 May 2024)
Cumulative views and downloads (calculated since 24 May 2024)

Viewed (geographical distribution)

Total article views: 2,002 (including HTML, PDF, and XML) Thereof 2,002 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 27 Jan 2026
Download
Short summary
Late Eocene summers, 34 million years ago, were hot on Antarctica, with temperatures up to 30 °C. We also know that during this period the first Antarctic ice sheet formed. Since climate models do not show the transition from this warm climate to ice sheet formation accurately, we imposed regional ice sheets onto the continent in a realistic climate and show that these ice sheets do not melt away. This suggests that the initiation of ice sheet growth might have happened during warmer periods.
Read more
Share