Articles | Volume 17, issue 1
https://doi.org/10.5194/cp-17-21-2021
© 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-17-21-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
06 Jan 2021
Research article |
| 06 Jan 2021
| 06 Jan 2021
PMIP4/CMIP6 last interglacial simulations using three different versions of MIROC: importance of vegetation
Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa, 2778568 Japan
Wing-Le Chan
Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa, 2778568 Japan
Ayako Abe-Ouchi
Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa, 2778568 Japan
National Institute of Polar Research, Tachikawa, 1908518 Japan
Japan Agency for Marine–Earth Science and Technology, Yokohama, 2360001 Japan
Sam Sherriff-Tadano
Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa, 2778568 Japan
Rumi Ohgaito
Japan Agency for Marine–Earth Science and Technology, Yokohama, 2360001 Japan
Masakazu Yoshimori
Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa, 2778568 Japan
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Cited
13 citations as recorded by crossref.
- New insights to be gained from a Virtual Ecosystem R. Ewers et al. 10.1016/j.ecolmodel.2024.110866
- Northwestward shift of the northern boundary of the East Asian summer monsoon during the mid-Holocene caused by orbital forcing and vegetation feedbacks J. Chen et al. 10.1016/j.quascirev.2021.107136
- Astronomical forcing shaped the timing of early Pleistocene glacial cycles Y. Watanabe et al. 10.1038/s43247-023-00765-x
- Similarities and Differences in Arctic Sea‐Ice Loss During the Solar‐Forced Last Interglacial Warming (127 Kyr BP) and CO2‐Forced Future Warming M. Sicard et al. 10.1029/2023GL104782
- 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
- Response of convective systems to the orbital forcing of the last interglacial in a global nonhydrostatic atmospheric model with and without a convective parameterization M. Chikira et al. 10.1007/s00382-021-06056-5
- A model-based comparison of paleo-physical processes in the Bay of Bengal M. Khan et al. 10.1007/s40808-024-02165-2
- Differences Between Present‐Day and Cretaceous Hydrological Cycle Responses to Rising CO2 Concentration T. Higuchi et al. 10.1029/2021GL094341
- Effect of Climatic Precession on Dansgaard‐Oeschger‐Like Oscillations Y. Kuniyoshi et al. 10.1029/2021GL095695
- PMIP4 experiments using MIROC-ES2L Earth system model R. Ohgaito et al. 10.5194/gmd-14-1195-2021
- 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
- A multi-model CMIP6-PMIP4 study of Arctic sea ice at 127 ka: sea ice data compilation and model differences M. Kageyama et al. 10.5194/cp-17-37-2021
- 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
11 citations as recorded by crossref.
- New insights to be gained from a Virtual Ecosystem R. Ewers et al. 10.1016/j.ecolmodel.2024.110866
- Northwestward shift of the northern boundary of the East Asian summer monsoon during the mid-Holocene caused by orbital forcing and vegetation feedbacks J. Chen et al. 10.1016/j.quascirev.2021.107136
- Astronomical forcing shaped the timing of early Pleistocene glacial cycles Y. Watanabe et al. 10.1038/s43247-023-00765-x
- Similarities and Differences in Arctic Sea‐Ice Loss During the Solar‐Forced Last Interglacial Warming (127 Kyr BP) and CO2‐Forced Future Warming M. Sicard et al. 10.1029/2023GL104782
- 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
- Response of convective systems to the orbital forcing of the last interglacial in a global nonhydrostatic atmospheric model with and without a convective parameterization M. Chikira et al. 10.1007/s00382-021-06056-5
- A model-based comparison of paleo-physical processes in the Bay of Bengal M. Khan et al. 10.1007/s40808-024-02165-2
- Differences Between Present‐Day and Cretaceous Hydrological Cycle Responses to Rising CO2 Concentration T. Higuchi et al. 10.1029/2021GL094341
- Effect of Climatic Precession on Dansgaard‐Oeschger‐Like Oscillations Y. Kuniyoshi et al. 10.1029/2021GL095695
- PMIP4 experiments using MIROC-ES2L Earth system model R. Ohgaito et al. 10.5194/gmd-14-1195-2021
- 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
2 citations as recorded by crossref.
- A multi-model CMIP6-PMIP4 study of Arctic sea ice at 127 ka: sea ice data compilation and model differences M. Kageyama et al. 10.5194/cp-17-37-2021
- 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
Latest update: 20 Nov 2024
Short summary
The last interglacial is known as the warmest period in the recent glacial–interglacial cycle. We carry out a last interglacial experiment using three versions of general circulation models to reproduce the warm climate indicated by geological evidence. Our result clearly shows that vegetation change in the last interglacial is a necessary factor to predict a strong warming in northern high latitudes, which is indicated by geological evidence.
The last interglacial is known as the warmest period in the recent glacial–interglacial cycle....
