Articles | Volume 16, issue 1
https://doi.org/10.5194/cp-16-183-2020
© 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-16-183-2020
© 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 Jan 2020
Research article |
| 23 Jan 2020
| 23 Jan 2020
PlioMIP2 simulations with NorESM-L and NorESM1-F
Xiangyu Li
Climate Change Research Center, Institute of Atmospheric Physics,
Chinese Academy of Sciences, Beijing 100029, China
NORCE Norwegian Research Centre, Bjerknes Centre for Climate Research, Bergen, Norway
Chuncheng Guo
NORCE Norwegian Research Centre, Bjerknes Centre for Climate Research, Bergen, Norway
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
Nansen-Zhu International Research Centre, Institute of Atmospheric
Physics, Chinese Academy of Sciences, Beijing 100029, China
Odd Helge Otterå
NORCE Norwegian Research Centre, Bjerknes Centre for Climate Research, Bergen, Norway
Ran Zhang
Climate Change Research Center, Institute of Atmospheric Physics,
Chinese Academy of Sciences, Beijing 100029, China
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32 citations as recorded by crossref.
- Highly stratified mid-Pliocene Southern Ocean in PlioMIP2 J. Weiffenbach et al. 10.5194/cp-20-1067-2024
- 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
- Understanding the causes and consequences of the northward extension of the tropical monsoon in Asia in the Eocene Z. Zhang et al. 10.1016/j.palaeo.2023.111613
- Closure of tropical seaways favors the climate and vegetation in tropical Africa and South America approaching their present conditions N. Tan et al. 10.1016/j.gloplacha.2023.104351
- Drastic Vegetation Change in the Guajira Peninsula (Colombia) During the Neogene C. Jaramillo et al. 10.1029/2020PA003933
- Mid-Pliocene West African Monsoon rainfall as simulated in the PlioMIP2 ensemble E. Berntell et al. 10.5194/cp-17-1777-2021
- Impact of Mountains in Southern China on the Eocene Climates of East Asia Z. Zhang et al. 10.1029/2022JD036510
- Cenozoic Indo-Pacific warm pool controlled by both atmospheric CO2 and paleogeography R. Zhang et al. 10.1016/j.scib.2024.02.028
- On the climatic influence of CO2forcing in the Pliocene L. Burton et al. 10.5194/cp-19-747-2023
- Pliocene Model Intercomparison Project (PlioMIP2) simulations using the Model for Interdisciplinary Research on Climate (MIROC4m) W. Chan & A. Abe-Ouchi 10.5194/cp-16-1523-2020
- 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 Yorktown Formation: Improved Stratigraphy, Chronology, and Paleoclimate Interpretations from the U.S. Mid-Atlantic Coastal Plain H. Dowsett et al. 10.3390/geosciences11120486
- Climate transition at the Eocene–Oligocene influenced by bathymetric changes to the Atlantic–Arctic oceanic gateways E. Straume et al. 10.1073/pnas.2115346119
- 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
- African Hydroclimate During the Early Eocene From the DeepMIP Simulations C. Williams et al. 10.1029/2022PA004419
- Influence of plate reference frames on deep-time climate simulations Z. Zhang et al. 10.1016/j.gloplacha.2023.104352
- The Pliocene Model Intercomparison Project Phase 2: large-scale climate features and climate sensitivity A. Haywood et al. 10.5194/cp-16-2095-2020
- Recognizing the Role of Tropical Seaways in Modulating the Pacific Circulation N. Tan et al. 10.1029/2022GL099674
- Reduced El Niño variability in the mid-Pliocene according to the PlioMIP2 ensemble A. Oldeman et al. 10.5194/cp-17-2427-2021
- Evaluating the large-scale hydrological cycle response within the Pliocene Model Intercomparison Project Phase 2 (PlioMIP2) ensemble Z. Han et al. 10.5194/cp-17-2537-2021
- 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
- Evaluation of Arctic warming in mid-Pliocene climate simulations W. de Nooijer et al. 10.5194/cp-16-2325-2020
- 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
- Mid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2 Z. Zhang et al. 10.5194/cp-17-529-2021
- Mid-Pliocene El Niño/Southern Oscillation suppressed by Pacific intertropical convergence zone shift G. Pontes et al. 10.1038/s41561-022-00999-y
- Widespread glacier advances across the Tian Shan during Marine Isotope Stage 3 not supported by climate-glaciation simulations Q. Yan et al. 10.1016/j.fmre.2022.01.033
- 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
- The warm winter paradox in the Pliocene northern high latitudes J. Tindall et al. 10.5194/cp-18-1385-2022
- Modeled variations of tropical cyclone genesis potential during Marine Isotope Stage 3 D. Huan et al. 10.1016/j.quascirev.2024.108503
- Amplified seasonality in western Europe in a warmer world N. de Winter et al. 10.1126/sciadv.adl6717
- 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
- The changes in south Asian summer monsoon circulation during the mid-Piacenzian warm period Z. Han & G. Li 10.1007/s00382-024-07179-1
Latest update: 17 Nov 2024
Short summary
Here we report the PlioMIP2 simulations by two versions of the Norwegian Earth System Model (NorESM) with updated boundary conditions derived from Pliocene Research, Interpretation and Synoptic Mapping version 4. The two NorESM versions both produce warmer and wetter Pliocene climate with deeper and stronger Atlantic meridional overturning circulation. Compared to PlioMIP1, PlioMIP2 simulates lower Pliocene warming with NorESM-L, likely due to the closure of seaways at northern high latitudes.
Here we report the PlioMIP2 simulations by two versions of the Norwegian Earth System Model...
