Articles | Volume 14, issue 2
https://doi.org/10.5194/gmd-14-1195-2021
© 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/gmd-14-1195-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
PMIP4 experiments using MIROC-ES2L Earth system model
Research Center for Environmental Modeling and Application, Japan
Agency for Marine-Earth Science and Technology, 3173-25 Showamachi,
Kanazawaku, Yokohama 236-0001, Japan
Akitomo Yamamoto
Research Center for Environmental Modeling and Application, Japan
Agency for Marine-Earth Science and Technology, 3173-25 Showamachi,
Kanazawaku, Yokohama 236-0001, Japan
Tomohiro Hajima
Research Center for Environmental Modeling and Application, Japan
Agency for Marine-Earth Science and Technology, 3173-25 Showamachi,
Kanazawaku, Yokohama 236-0001, Japan
Ryouta O'ishi
Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa
2778568, Japan
Manabu Abe
Research Center for Environmental Modeling and Application, Japan
Agency for Marine-Earth Science and Technology, 3173-25 Showamachi,
Kanazawaku, Yokohama 236-0001, Japan
Hiroaki Tatebe
Research Center for Environmental Modeling and Application, Japan
Agency for Marine-Earth Science and Technology, 3173-25 Showamachi,
Kanazawaku, Yokohama 236-0001, Japan
Ayako Abe-Ouchi
Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa
2778568, Japan
National Institute of Polar Research, Tachikawa 1908518, Japan
Research Center for Environmental Modeling and Application, Japan
Agency for Marine-Earth Science and Technology, 3173-25 Showamachi,
Kanazawaku, Yokohama 236-0001, Japan
Michio Kawamiya
Research Center for Environmental Modeling and Application, Japan
Agency for Marine-Earth Science and Technology, 3173-25 Showamachi,
Kanazawaku, Yokohama 236-0001, Japan
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- The Role of Wet Processes in Extratropical Thermal Stratification During the Glacial Period Z. Xie et al. 10.1029/2023GL106400
- Increased effective radiative forcing enhanced the modulating effect of Pacific Decadal Oscillation on late Little Ice Age precipitation in the Jiang-Huai region, China S. Jiang et al. 10.1007/s00382-023-06805-8
- Last Glacial Maximum ITCZ Changes From PMIP3/4 Simulations T. Wang et al. 10.1029/2022JD038103
- Assessing transient changes in the ocean carbon cycle during the last deglaciation through carbon isotope modeling H. Kobayashi et al. 10.5194/cp-20-769-2024
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- Intensified Atmospheric Branch of the Hydrological Cycle Over the Tibetan Plateau During the Last Interglacial From a Dynamical Downscaling Perspective N. Jiang et al. 10.1029/2022JD036470
- Last Glacial Maximum climate and atmospheric circulation over the Australian region from climate models Y. Du et al. 10.5194/cp-20-393-2024
- Enhanced Interannual Variability in Temperature during the Last Glacial Maximum J. Shi et al. 10.1175/JCLI-D-21-0739.1
- The PMIP4 Last Glacial Maximum experiments: preliminary results and comparison with the PMIP3 simulations M. Kageyama et al. 10.5194/cp-17-1065-2021
- Shrub cover declined as Indigenous populations expanded across southeast Australia M. Mariani et al. 10.1126/science.adn8668
- Deciphering the variations and mechanisms of the westerly jets across the Northern Hemisphere during the Last Interglacial based on PMIP4 models N. Jiang et al. 10.1007/s00382-021-06100-4
- Global simulation of dissolved <sup>231</sup>Pa and <sup>230</sup>Th in the ocean and the sedimentary <sup>231</sup>Pa∕<sup>230</sup>Th ratios with the ocean general circulation model COCO ver4.0 Y. Sasaki et al. 10.5194/gmd-15-2013-2022
- Enhanced CO2 Degassing From the Tropical Indian Ocean During Cold Climatic Events of the Last Glacial Cycle M. Tarique et al. 10.1029/2022PA004570
- Contribution of lakes in sustaining the Sahara greening during the mid-Holocene Y. Li et al. 10.5194/cp-19-1891-2023
- Sahel Droughts Induced by Large Volcanic Eruptions Over the Last Millennium in PMIP4/Past1000 Simulations J. Villamayor et al. 10.1029/2022GL101478
- A First Intercomparison of the Simulated LGM Carbon Results Within PMIP‐Carbon: Role of the Ocean Boundary Conditions F. Lhardy et al. 10.1029/2021PA004302
- Large Ensemble Particle Filter for Spatial Climate Reconstructions Using a Linear Inverse Model B. Jebri & M. Khodri 10.1029/2022MS003094
- A model-based comparison of paleo-physical processes in the Bay of Bengal M. Khan et al. 10.1007/s40808-024-02165-2
- Revisiting East Asian monsoon change during the Last Glacial Maximum using PMIP4 simulations Z. Tian 10.1016/j.aosl.2024.100467
- Antiphase change in Walker Circulation between the Pacific Ocean and the Indian Ocean during the Last Interglacial induced by interbasin sea surface temperature anomaly contrast J. Ma et al. 10.1007/s00382-023-07039-4
- Disentangling Internal and External Contributions to Atlantic Multidecadal Variability Over the Past Millennium S. Fang et al. 10.1029/2021GL095990
- Causes of the weak emergent constraint on climate sensitivity at the Last Glacial Maximum M. Renoult et al. 10.5194/cp-19-323-2023
- A paleoecological investigation of recent cyanobacterial blooms and their drivers in two contrasting lakes C. Wheeler et al. 10.1016/j.hal.2023.102563
5 citations as recorded by crossref.
- Large-scale features and evaluation of the PMIP4-CMIP6 <i>midHolocene</i> simulations C. Brierley et al. 10.5194/cp-16-1847-2020
- A model-based comparison of paleo-physical processes in the Bay of Bengal M. Khan et al. 10.1007/s40808-024-02165-2
- A Bayesian framework for emergent constraints: case studies of climate sensitivity with PMIP M. Renoult et al. 10.5194/cp-16-1715-2020
- Large-scale features of Last Interglacial climate: results from evaluating the <i>lig127k</i> simulations for the Coupled Model Intercomparison Project (CMIP6)–Paleoclimate Modeling Intercomparison Project (PMIP4) B. Otto-Bliesner et al. 10.5194/cp-17-63-2021
- PMIP4/CMIP6 last interglacial simulations using three different versions of MIROC: importance of vegetation R. O'ishi et al. 10.5194/cp-17-21-2021
Latest update: 22 Nov 2024
Short summary
Using the MIROC-ES2L Earth system model, selected time periods of the past were simulated. The ability to simulate the past is also an evaluation of the performance of the model in projecting global warming. Simulations for 21 000, 6000, and 127 000 years ago, and a simulation for 1000 years starting in 850 CE were simulated. The results showed that the model can generally describe past climate change.
Using the MIROC-ES2L Earth system model, selected time periods of the past were simulated. The...