Articles | Volume 20, issue 3
https://doi.org/10.5194/cp-20-597-2024
https://doi.org/10.5194/cp-20-597-2024
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: 1,642 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,218 352 72 1,642 62 52
  • HTML: 1,218
  • PDF: 352
  • XML: 72
  • Total: 1,642
  • BibTeX: 62
  • EndNote: 52
Views and downloads (calculated since 04 Jul 2023)
Cumulative views and downloads (calculated since 04 Jul 2023)

Viewed (geographical distribution)

Total article views: 1,642 (including HTML, PDF, and XML) Thereof 1,705 with geography defined and -63 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 Nov 2024
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.