Articles | Volume 18, issue 4
https://doi.org/10.5194/cp-18-657-2022
© Author(s) 2022. 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-18-657-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Warm mid-Pliocene conditions without high climate sensitivity: the CCSM4-Utrecht (CESM 1.0.5) contribution to the PlioMIP2
Michiel L. J. Baatsen
CORRESPONDING AUTHOR
Institute for Marine and Atmospheric Research Utrecht (IMAU), Department of Physics, Utrecht University, Utrecht, the Netherlands
Anna S. von der Heydt
Institute for Marine and Atmospheric Research Utrecht (IMAU), Department of Physics, Utrecht University, Utrecht, the Netherlands
Centre for Complex Systems Science, Utrecht University, Utrecht, the Netherlands
Michael A. Kliphuis
Institute for Marine and Atmospheric Research Utrecht (IMAU), Department of Physics, Utrecht University, Utrecht, the Netherlands
Arthur M. Oldeman
Institute for Marine and Atmospheric Research Utrecht (IMAU), Department of Physics, Utrecht University, Utrecht, the Netherlands
Julia E. Weiffenbach
Institute for Marine and Atmospheric Research Utrecht (IMAU), Department of Physics, Utrecht University, Utrecht, the Netherlands
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Cited
16 citations as recorded by crossref.
- The hydrological cycle and ocean circulation of the Maritime Continent in the Pliocene: results from PlioMIP2 X. Ren et al. 10.5194/cp-19-2053-2023
- Revisiting the physical processes controlling the tropical atmospheric circulation changes during the Mid-Piacenzian Warm Period K. Zhang et al. 10.1016/j.quaint.2024.01.001
- Impacts of an active Pacific Meridional Overturning Circulation on the Pliocene climate and hydrological cycle M. Fu & A. Fedorov 10.1016/j.epsl.2024.118878
- Mid-Pliocene not analogous to high-CO2 climate when considering Northern Hemisphere winter variability A. Oldeman et al. 10.5194/wcd-5-395-2024
- Amplified seasonality in western Europe in a warmer world N. de Winter et al. 10.1126/sciadv.adl6717
- The warm winter paradox in the Pliocene northern high latitudes J. Tindall et al. 10.5194/cp-18-1385-2022
- Simulating surface warming in Earth's three polar regions during the Middle Miocene Climatic Optimum using isotopic and non-isotopic versions of the Community Earth System Model Y. Sun et al. 10.1016/j.palaeo.2024.112156
- The changes in south Asian summer monsoon circulation during the mid-Piacenzian warm period Z. Han & G. Li 10.1007/s00382-024-07179-1
- Modeling the mid-piacenzian warm climate using the water isotope-enabled Community Earth System Model (iCESM1.2-ITPCAS) Y. Sun et al. 10.1007/s00382-024-07304-0
- Geologically constrained 2-million-year-long simulations of Antarctic Ice Sheet retreat and expansion through the Pliocene A. Halberstadt et al. 10.1038/s41467-024-51205-z
- Unraveling the mechanisms and implications of a stronger mid-Pliocene Atlantic Meridional Overturning Circulation (AMOC) in PlioMIP2 J. Weiffenbach et al. 10.5194/cp-19-61-2023
- How changing the height of the Antarctic ice sheet affects global climate: a mid-Pliocene case study X. Huang et al. 10.5194/cp-19-731-2023
- Highly stratified mid-Pliocene Southern Ocean in PlioMIP2 J. Weiffenbach et al. 10.5194/cp-20-1067-2024
- Similar North Pacific variability despite suppressed El Niño variability in the warm mid-Pliocene climate A. Oldeman et al. 10.5194/esd-15-1037-2024
- Using paleoecological data to inform decision making: A deep-time perspective H. Dowsett et al. 10.3389/fevo.2022.972179
- Reduced El Niño variability in the mid-Pliocene according to the PlioMIP2 ensemble A. Oldeman et al. 10.5194/cp-17-2427-2021
14 citations as recorded by crossref.
- The hydrological cycle and ocean circulation of the Maritime Continent in the Pliocene: results from PlioMIP2 X. Ren et al. 10.5194/cp-19-2053-2023
- Revisiting the physical processes controlling the tropical atmospheric circulation changes during the Mid-Piacenzian Warm Period K. Zhang et al. 10.1016/j.quaint.2024.01.001
- Impacts of an active Pacific Meridional Overturning Circulation on the Pliocene climate and hydrological cycle M. Fu & A. Fedorov 10.1016/j.epsl.2024.118878
- Mid-Pliocene not analogous to high-CO2 climate when considering Northern Hemisphere winter variability A. Oldeman et al. 10.5194/wcd-5-395-2024
- Amplified seasonality in western Europe in a warmer world N. de Winter et al. 10.1126/sciadv.adl6717
- The warm winter paradox in the Pliocene northern high latitudes J. Tindall et al. 10.5194/cp-18-1385-2022
- Simulating surface warming in Earth's three polar regions during the Middle Miocene Climatic Optimum using isotopic and non-isotopic versions of the Community Earth System Model Y. Sun et al. 10.1016/j.palaeo.2024.112156
- The changes in south Asian summer monsoon circulation during the mid-Piacenzian warm period Z. Han & G. Li 10.1007/s00382-024-07179-1
- Modeling the mid-piacenzian warm climate using the water isotope-enabled Community Earth System Model (iCESM1.2-ITPCAS) Y. Sun et al. 10.1007/s00382-024-07304-0
- Geologically constrained 2-million-year-long simulations of Antarctic Ice Sheet retreat and expansion through the Pliocene A. Halberstadt et al. 10.1038/s41467-024-51205-z
- Unraveling the mechanisms and implications of a stronger mid-Pliocene Atlantic Meridional Overturning Circulation (AMOC) in PlioMIP2 J. Weiffenbach et al. 10.5194/cp-19-61-2023
- How changing the height of the Antarctic ice sheet affects global climate: a mid-Pliocene case study X. Huang et al. 10.5194/cp-19-731-2023
- Highly stratified mid-Pliocene Southern Ocean in PlioMIP2 J. Weiffenbach et al. 10.5194/cp-20-1067-2024
- Similar North Pacific variability despite suppressed El Niño variability in the warm mid-Pliocene climate A. Oldeman et al. 10.5194/esd-15-1037-2024
Latest update: 14 Oct 2024
Short summary
The Pliocene was a period during which atmospheric CO2 was similar to today (i.e. ~ 400 ppm). We present the results of model simulations carried out within the Pliocene Model Intercomparison Project Phase 2 (PlioMIP2) using the CESM 1.0.5. We find a climate that is much warmer than today, with augmented polar warming, increased precipitation, and strongly reduced sea ice cover. In addition, several leading modes of variability in temperature show an altered behaviour.
The Pliocene was a period during which atmospheric CO2 was similar to today (i.e. ~ 400 ppm). We...