Articles | Volume 17, issue 6
https://doi.org/10.5194/cp-17-2537-2021
© Author(s) 2021. 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-17-2537-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
08 Dec 2021
Research article |
| 08 Dec 2021
| 08 Dec 2021
Evaluating the large-scale hydrological cycle response within the Pliocene Model Intercomparison Project Phase 2 (PlioMIP2) ensemble
College of Oceanography, Hohai University, Nanjing, China
Department of Physical Geography and Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Department of Physical Geography and Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Department of Physical Geography and Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Ran Feng
Department of Geosciences, College of Liberal Arts and Sciences, University of Connecticut, CT 06269, USA
Alan M. Haywood
School of Earth and Environment, University of Leeds, Leeds, West Yorkshire, UK
Julia C. Tindall
School of Earth and Environment, University of Leeds, Leeds, West Yorkshire, UK
Stephen J. Hunter
School of Earth and Environment, University of Leeds, Leeds, West Yorkshire, UK
Bette L. Otto-Bliesner
Climate and Global Dynamics Laboratory, National Center for Atmospheric Research, Boulder, CO 80305, USA
Esther C. Brady
Climate and Global Dynamics Laboratory, National Center for Atmospheric Research, Boulder, CO 80305, USA
Nan Rosenbloom
Climate and Global Dynamics Laboratory, National Center for Atmospheric Research, Boulder, CO 80305, USA
Zhongshi Zhang
Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences, Wuhan, China
NORCE Norwegian Research Centre, Bjerknes Centre for Climate Research, Bergen, Norway
Xiangyu Li
Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences, Wuhan, China
Chuncheng Guo
NORCE Norwegian Research Centre, Bjerknes Centre for Climate Research, Bergen, Norway
Kerim H. Nisancioglu
Department of Earth Science, University of Bergen and Bjerknes Centre for Climate Research, Bergen, Norway
Centre for Earth Evolution and Dynamics, University of Oslo, Oslo, Norway
Christian Stepanek
Alfred Wegener Institute, Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
Gerrit Lohmann
Alfred Wegener Institute, Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
Institute for Environmental Physics, University of Bremen, Bremen, Germany
Linda E. Sohl
Center for Climate Systems Research, Columbia University, NY 10025, USA
NASA Goddard Institute for Space Studies, NY, USA
Mark A. Chandler
Center for Climate Systems Research, Columbia University, NY 10025, USA
NASA Goddard Institute for Space Studies, NY, USA
Ning Tan
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Universiteì Paris-Saclay, Gif-sur-Yvette, France
Gilles Ramstein
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Universiteì Paris-Saclay, Gif-sur-Yvette, France
Michiel L. J. Baatsen
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
Deepak Chandan
Department of Physics, University of Toronto, Toronto, Ontario, Canada
W. Richard Peltier
Department of Physics, University of Toronto, Toronto, Ontario, Canada
Charles J. R. Williams
School of Geographical Sciences, University of Bristol, Bristol, UK
NCAS Climate, Department of Meteorology, University of Reading, Reading, UK
Daniel J. Lunt
School of Geographical Sciences, University of Bristol, Bristol, UK
Jianbo Cheng
School of Environmental Science and Engineering, Yancheng Institute of Technology, Yancheng, China
Qin Wen
School of Geography, Nanjing Normal University, Nanjing, 210023, China
Natalie J. Burls
Center for Ocean–Land–Atmosphere Studies, George Mason University, Fairfax, VA 22030, USA
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- Severe Drought Conditions in Northern East Asia During the Early Pliocene Caused by Weakened Pacific Meridional Temperature Gradient Y. Zheng et al. 10.1029/2022GL098813
- Less Dryland Aridity During Pliocene Warmth R. Zhang et al. 10.1029/2023JD039371
- Decomposition of physical processes controlling EASM precipitation changes during the mid-Piacenzian: new insights into data–model integration Y. Sun et al. 10.1038/s41612-024-00668-4
- South Asian Monsoon Variability and Arctic Sea Ice Extent Linkages During the Late Pliocene P. Behera et al. 10.1029/2022PA004436
28 citations as recorded by crossref.
- 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
- Influence of Large‐Scale Atmospheric Dynamics on Precipitation Seasonality of the Tibetan Plateau and Central Asia in Cold and Warm Climates During the Late Cenozoic S. Botsyun et al. 10.1029/2021JD035810
- On the importance of moisture conveyor belts from the tropical eastern Pacific for wetter conditions in the Atacama Desert during the mid-Pliocene M. Reyers et al. 10.5194/cp-19-517-2023
- 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
- Mid-Pliocene El Niño/Southern Oscillation suppressed by Pacific intertropical convergence zone shift G. Pontes et al. 10.1038/s41561-022-00999-y
- 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
- Using paleoecological data to inform decision making: A deep-time perspective H. Dowsett et al. 10.3389/fevo.2022.972179
- Warm mid-Pliocene conditions without high climate sensitivity: the CCSM4-Utrecht (CESM 1.0.5) contribution to the PlioMIP2 M. Baatsen et al. 10.5194/cp-18-657-2022
- 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
- Aerosol uncertainties in tropical precipitation changes for the mid-Pliocene warm period A. Zhao et al. 10.5194/cp-20-1195-2024
- Analysis of the July 2021 extreme precipitation in Henan using the novel moisture budget equation J. Cheng et al. 10.1007/s00704-022-04022-7
- Changes in Sahel summer rainfall in a global warming climate: contrasting the mid-Pliocene and future regional hydrological cycles Z. Han et al. 10.1007/s00382-022-06630-5
- 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
- East Asian climate evolution during the Cenozoic: A review from the modeling perspective R. Zhang et al. 10.1016/j.fmre.2023.09.011
- Unraveling the complexities of the Last Glacial Maximum climate: the role of individual boundary conditions and forcings X. Shi et al. 10.5194/cp-19-2157-2023
- Prolonged South Asian Monsoon variability and weakened denitrification during Mid-Pleistocene Transition S. Tripathi et al. 10.1016/j.palaeo.2023.111637
- Long‐Term Variability in Pliocene North Pacific Ocean Export Production and Its Implications for Ocean Circulation in a Warmer World J. Abell & G. Winckler 10.1029/2022AV000853
- Southern African precipitation changes in a warmer world: insights from the PlioMIP2 mid-Pliocene Warm Period (∼3.3–3.0 Ma) ensemble S. Roffe et al. 10.1080/0035919X.2024.2410945
- A Model‐Data Comparison of the Hydrological Response to Miocene Warmth: Leveraging the MioMIP1 Opportunistic Multi‐Model Ensemble R. Acosta et al. 10.1029/2023PA004726
- 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
- Influence of meridional circulation on extreme high temperature and weakened rainfall over the Yangtze River Valley in August 2022 C. Cang et al. 10.1088/2515-7620/ad33ec
- Meridional circulation dominates the record-breaking “Dragon Boat Water” rainfall over south China in 2022 J. Cheng et al. 10.3389/feart.2022.1032313
- Mid-Pliocene not analogous to high-CO2 climate when considering Northern Hemisphere winter variability A. Oldeman et al. 10.5194/wcd-5-395-2024
- Severe Drought Conditions in Northern East Asia During the Early Pliocene Caused by Weakened Pacific Meridional Temperature Gradient Y. Zheng et al. 10.1029/2022GL098813
- Less Dryland Aridity During Pliocene Warmth R. Zhang et al. 10.1029/2023JD039371
- Decomposition of physical processes controlling EASM precipitation changes during the mid-Piacenzian: new insights into data–model integration Y. Sun et al. 10.1038/s41612-024-00668-4
1 citations as recorded by crossref.
Latest update: 12 Nov 2024
Short summary
Understanding the potential processes responsible for large-scale hydrological cycle changes in a warmer climate is of great importance. Our study implies that an imbalance in interhemispheric atmospheric energy during the mid-Pliocene could have led to changes in the dynamic effect, offsetting the thermodynamic effect and, hence, altering mid-Pliocene hydroclimate cycling. Moreover, a robust westward shift in the Pacific Walker circulation can moisten the northern Indian Ocean.
Understanding the potential processes responsible for large-scale hydrological cycle changes in...
