Articles | Volume 16, issue 4
https://doi.org/10.5194/cp-16-1523-2020
© 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-16-1523-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
17 Aug 2020
Research article |
| 17 Aug 2020
| 17 Aug 2020
Pliocene Model Intercomparison Project (PlioMIP2) simulations using the Model for Interdisciplinary Research on Climate (MIROC4m)
Atmosphere and Ocean Research Institute, The University of Tokyo,
Kashiwa, 277-8564, Japan
Ayako Abe-Ouchi
Atmosphere and Ocean Research Institute, The University of Tokyo,
Kashiwa, 277-8564, Japan
National Institute for Polar Research, Tachikawa, 190-8518, Japan
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24 citations as recorded by crossref.
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- On the climatic influence of CO2forcing in the Pliocene L. Burton et al. 10.5194/cp-19-747-2023
- The Yorktown Formation: Improved Stratigraphy, Chronology, and Paleoclimate Interpretations from the U.S. Mid-Atlantic Coastal Plain H. Dowsett et al. 10.3390/geosciences11120486
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- Using paleoecological data to inform decision making: A deep-time perspective H. Dowsett et al. 10.3389/fevo.2022.972179
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- The Pliocene Model Intercomparison Project Phase 2: large-scale climate features and climate sensitivity A. Haywood et al. 10.5194/cp-16-2095-2020
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- The warm winter paradox in the Pliocene northern high latitudes J. Tindall et al. 10.5194/cp-18-1385-2022
- Differences Between Present‐Day and Cretaceous Hydrological Cycle Responses to Rising CO2 Concentration T. Higuchi et al. 10.1029/2021GL094341
- Meridional Heat Transport in the DeepMIP Eocene Ensemble: Non‐CO2 and CO2 Effects F. Kelemen et al. 10.1029/2022PA004607
- Mid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2 Z. Zhang et al. 10.5194/cp-17-529-2021
- Does a difference in ice sheets between Marine Isotope Stages 3 and 5a affect the duration of stadials? Implications from hosing experiments S. Sherriff-Tadano et al. 10.5194/cp-17-1919-2021
- 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
- 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
24 citations as recorded by crossref.
- Mid-Pliocene El Niño/Southern Oscillation suppressed by Pacific intertropical convergence zone shift G. Pontes et al. 10.1038/s41561-022-00999-y
- Evaluation of Arctic warming in mid-Pliocene climate simulations W. de Nooijer et al. 10.5194/cp-16-2325-2020
- A proxy-model comparison for mid-Pliocene warm period hydroclimate in the Southwestern US S. Menemenlis et al. 10.1016/j.epsl.2022.117803
- Amplified seasonality in western Europe in a warmer world N. de Winter et al. 10.1126/sciadv.adl6717
- On the climatic influence of CO2forcing in the Pliocene L. Burton et al. 10.5194/cp-19-747-2023
- The Yorktown Formation: Improved Stratigraphy, Chronology, and Paleoclimate Interpretations from the U.S. Mid-Atlantic Coastal Plain H. Dowsett et al. 10.3390/geosciences11120486
- Past terrestrial hydroclimate sensitivity controlled by Earth system feedbacks R. Feng et al. 10.1038/s41467-022-28814-7
- Using paleoecological data to inform decision making: A deep-time perspective H. Dowsett et al. 10.3389/fevo.2022.972179
- Mid-Pliocene West African Monsoon rainfall as simulated in the PlioMIP2 ensemble E. Berntell et al. 10.5194/cp-17-1777-2021
- 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
- Reduced El Niño variability in the mid-Pliocene according to the PlioMIP2 ensemble A. Oldeman et al. 10.5194/cp-17-2427-2021
- Influence of stationary waves on mid-Pliocene atmospheric rivers and hydroclimate S. Menemenlis et al. 10.1016/j.gloplacha.2021.103557
- Highly stratified mid-Pliocene Southern Ocean in PlioMIP2 J. Weiffenbach et al. 10.5194/cp-20-1067-2024
- Semi-equilibrated global sea-level change projections for the next 10 000 years J. Van Breedam et al. 10.5194/esd-11-953-2020
- 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
- The Pliocene Model Intercomparison Project Phase 2: large-scale climate features and climate sensitivity A. Haywood et al. 10.5194/cp-16-2095-2020
- A middle Miocene to Quaternary sedimentary and palaeoenvironmental record from the western continental shelf of South Africa P. Louw & E. Bergh 10.1016/j.margeo.2024.107304
- The warm winter paradox in the Pliocene northern high latitudes J. Tindall et al. 10.5194/cp-18-1385-2022
- Differences Between Present‐Day and Cretaceous Hydrological Cycle Responses to Rising CO2 Concentration T. Higuchi et al. 10.1029/2021GL094341
- Meridional Heat Transport in the DeepMIP Eocene Ensemble: Non‐CO2 and CO2 Effects F. Kelemen et al. 10.1029/2022PA004607
- Mid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2 Z. Zhang et al. 10.5194/cp-17-529-2021
- Does a difference in ice sheets between Marine Isotope Stages 3 and 5a affect the duration of stadials? Implications from hosing experiments S. Sherriff-Tadano et al. 10.5194/cp-17-1919-2021
- 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
- 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
Latest update: 29 Jun 2024
Short summary
We carry out several modelling experiments to investigate the climate of the mid-Piacenzian warm period (~ 3.205 Ma) when CO2 levels were similar to those of present day. The global surface air temperature is 3.1 °C higher compared to pre-industrial ones. Like previous experiments, the scale of warming suggested by proxy sea surface temperature (SST) data in the northern North Atlantic is not replicated. However, tropical Pacific SST shows good agreement with more recently published proxy data.
We carry out several modelling experiments to investigate the climate of the mid-Piacenzian warm...
