Articles | Volume 16, issue 6
https://doi.org/10.5194/cp-16-2275-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-16-2275-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
20 Nov 2020
Research article |
| 20 Nov 2020
| 20 Nov 2020
Contribution of the coupled atmosphere–ocean–sea ice–vegetation model COSMOS to the PlioMIP2
Christian Stepanek
CORRESPONDING AUTHOR
Alfred Wegener Institute – Helmholtz-Centre for Polar and Marine Research, Bremerhaven, Germany
Eric Samakinwa
Alfred Wegener Institute – Helmholtz-Centre for Polar and Marine Research, Bremerhaven, Germany
Institute of Geography, University of Bern, Bern, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
Gregor Knorr
Alfred Wegener Institute – Helmholtz-Centre for Polar and Marine Research, Bremerhaven, Germany
Gerrit Lohmann
Alfred Wegener Institute – Helmholtz-Centre for Polar and Marine Research, Bremerhaven, Germany
Institute for Environmental Physics, University of Bremen, Bremen, Germany
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Latest update: 31 Mar 2025
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.
Future climate is expected to be warmer than today. We study climate based on simulations of the...
