Climate of the Past
Climate of the Past
CP
Articles | Volume 20, issue 3
Articles | Volume 20, issue 3
https://doi.org/10.5194/cp-20-597-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/cp-20-597-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 20, issue 3
Research article
 | 
18 Mar 2024
Research article |  | 18 Mar 2024

Glacial inception through rapid ice area increase driven by albedo and vegetation feedbacks

Matteo Willeit, Reinhard Calov, Stefanie Talento, Ralf Greve, Jorjo Bernales, Volker Klemann, Meike Bagge, and Andrey Ganopolski

Viewed

Total article views: 2,660 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,033 523 104 2,660 104 117
  • HTML: 2,033
  • PDF: 523
  • XML: 104
  • Total: 2,660
  • BibTeX: 104
  • EndNote: 117
Views and downloads (calculated since 04 Jul 2023)
Cumulative views and downloads (calculated since 04 Jul 2023)

Viewed (geographical distribution)

Total article views: 2,660 (including HTML, PDF, and XML) Thereof 2,660 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 24 Oct 2025
Download
Short summary
We present transient simulations of the last glacial inception with the coupled climate–ice sheet model CLIMBER-X showing a rapid increase in Northern Hemisphere ice sheet area and a sea level drop by ~ 35 m, with the vegetation feedback playing a key role. Overall, our simulations confirm and refine previous results showing that climate-vegetation–cryosphere–carbon cycle feedbacks play a fundamental role in the transition from interglacial to glacial states.
Read more
Share
Special issue
Icy landscapes of the past (CP/ESSD/ESurf/TC inter-journal...