Articles | Volume 13, issue 7
https://doi.org/10.5194/cp-13-919-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-13-919-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
19 Jul 2017
Research article |
| 19 Jul 2017
Regional and global climate for the mid-Pliocene using the University of Toronto version of CCSM4 and PlioMIP2 boundary conditions
Deepak Chandan
CORRESPONDING AUTHOR
Department of Physics, University of Toronto, 60 St. George Street, Toronto, Ontario, M5S 1A7, Canada
W. Richard Peltier
Department of Physics, University of Toronto, 60 St. George Street, Toronto, Ontario, M5S 1A7, Canada
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- Impacts of Mid‐Pliocene Ice Sheets and Vegetation on Afro‐Asian Summer Monsoon Rainfall Revealed by EC‐Earth Simulations Z. Han et al. 10.1029/2023GL106145
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- Highly stratified mid-Pliocene Southern Ocean in PlioMIP2 J. Weiffenbach et al. 10.5194/cp-20-1067-2024
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- Mid-Pliocene West African Monsoon rainfall as simulated in the PlioMIP2 ensemble E. Berntell et al. 10.5194/cp-17-1777-2021
- Multiproxy Reduced‐Dimension Reconstruction of Pliocene Equatorial Pacific Sea Surface Temperatures J. Wycech et al. 10.1029/2019PA003685
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- Influence of stationary waves on mid-Pliocene atmospheric rivers and hydroclimate S. Menemenlis et al. 10.1016/j.gloplacha.2021.103557
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Latest update: 07 Jan 2025
Short summary
This paper discusses the climate of the mid-Pliocene warm period (~ 3.3–3 Mya) obtained using coupled climate simulations at CMIP5 resolution with the CCSM4 model and the boundary conditions (BCs) prescribed for the PlioMIP2 program. It is found that climate simulations performed with these BCs capture the warming patterns inferred from proxy data much better than what was possible with the BCs for the original PlioMIP program.
This paper discusses the climate of the mid-Pliocene warm period (~ 3.3–3 Mya) obtained using...
