Articles | Volume 16, issue 6
https://doi.org/10.5194/cp-16-2275-2020
https://doi.org/10.5194/cp-16-2275-2020
Research article
 | 
20 Nov 2020
Research article |  | 20 Nov 2020

Contribution of the coupled atmosphere–ocean–sea ice–vegetation model COSMOS to the PlioMIP2

Christian Stepanek, Eric Samakinwa, Gregor Knorr, and Gerrit Lohmann

Viewed

Total article views: 5,851 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
4,218 1,463 170 5,851 234 146 166
  • HTML: 4,218
  • PDF: 1,463
  • XML: 170
  • Total: 5,851
  • Supplement: 234
  • BibTeX: 146
  • EndNote: 166
Views and downloads (calculated since 04 Feb 2020)
Cumulative views and downloads (calculated since 04 Feb 2020)

Viewed (geographical distribution)

Total article views: 5,851 (including HTML, PDF, and XML) Thereof 5,418 with geography defined and 433 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 17 Mar 2026
Short summary
Future climate is expected to be warmer than today. We study climate based on simulations of the mid-Pliocene (about 3 million years ago), which was a time of elevated temperatures, and discuss implications for the future. Our results are provided towards a comparison to both proxy evidence and output of other climate models. We simulate a mid-Pliocene climate that is both warmer and wetter than today. Some climate characteristics can be more directly transferred to the near future than others.
Share