Articles | Volume 16, issue 6
https://doi.org/10.5194/cp-16-2573-2020
© 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-16-2573-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
23 Dec 2020
Research article |
| 23 Dec 2020
| 23 Dec 2020
The middle to late Eocene greenhouse climate modelled using the CESM 1.0.5
Department of Physics, Institute for Marine and Atmospheric Research, Utrecht University, Princetonplein 5, 3584CC Utrecht, the Netherlands
Anna S. von der Heydt
Department of Physics, Institute for Marine and Atmospheric Research, Utrecht University, Princetonplein 5, 3584CC Utrecht, the Netherlands
Matthew Huber
Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, 610 Purdue Mall, West Lafayette, IN 47906, USA
Michael A. Kliphuis
Department of Physics, Institute for Marine and Atmospheric Research, Utrecht University, Princetonplein 5, 3584CC Utrecht, the Netherlands
Peter K. Bijl
Department of Earth Sciences, Marine Palynology and Paleoceanography, Laboratory of Palaeobotany and Palynology, Utrecht University, Princetonlaan 8a, 3584CB Utrecht, the Netherlands
Appy Sluijs
Department of Earth Sciences, Marine Palynology and Paleoceanography, Laboratory of Palaeobotany and Palynology, Utrecht University, Princetonlaan 8a, 3584CB Utrecht, the Netherlands
Henk A. Dijkstra
Department of Physics, Institute for Marine and Atmospheric Research, Utrecht University, Princetonplein 5, 3584CC Utrecht, the Netherlands
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Latest update: 13 Jul 2025
Short summary
Warm climates of the deep past have proven to be challenging to reconstruct with the same numerical models used for future predictions. We present results of CESM simulations for the middle to late Eocene (∼ 38 Ma), in which we managed to match the available indications of temperature well. With these results we can now look into regional features and the response to external changes to ultimately better understand the climate when it is in such a warm state.
Warm climates of the deep past have proven to be challenging to reconstruct with the same...
