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
21 citations as recorded by crossref.
- Impact of the temperature-cloud phase relationship on the simulated Arctic warming during the Last Interglacial N. Arima et al.
- New insights to be gained from a Virtual Ecosystem R. Ewers et al.
- 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.
- Changing Movements in a Changing World: Modelling Early Pleistocene and Early Middle Pleistocene Climatic and Ecological Environments and Influences on Hominin Dispersal in Eurasia K. Lomborg et al.
- Astronomical forcing shaped the timing of early Pleistocene glacial cycles Y. Watanabe et al.
- 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.
- Possible influences of tropical vegetation shift on the glacial-interglacial temperature changes L. Tian et al.
- Intensified Atmospheric Branch of the Hydrological Cycle Over the Tibetan Plateau During the Last Interglacial From a Dynamical Downscaling Perspective N. Jiang et al.
- Differences Between Present‐Day and Cretaceous Hydrological Cycle Responses to Rising CO2 Concentration T. Higuchi et al.
- Arctic Amplification in the Past, Present, and Future: A Review for the Challenge to the Integrative Understanding of its Mechanism M. YOSHIMORI et al.
- Effect of Climatic Precession on Dansgaard‐Oeschger‐Like Oscillations Y. Kuniyoshi et al.
- PMIP4 experiments using MIROC-ES2L Earth system model R. Ohgaito et al.
- Long- and short-term variability of Arctic sea-ice cover during the Last Interglacial and Marine Isotope Stage 11c B. Crow & M. Prange
- How temperature seasonality drives interglacial permafrost dynamics: implications for paleo reconstructions and future thaw trajectories J. Nitzbon et al.
- Climate and stratospheric ozone during the mid-Holocene and Last Interglacial simulated by MRI-ESM2.0 Y. Watanabe et al.
- Climate and ocean circulation changes toward a modern snowball Earth T. Obase et al.
- 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.
- A model-based comparison of paleo-physical processes in the Bay of Bengal M. Khan et al.
- The Late Pliocene jet stream: Changes and drivers of the mean state and variability A. Buchan et al.
- Assessment of the southern polar and subpolar warming in the PMIP4 last interglacial simulations using paleoclimate data syntheses Q. Gao et al.
- 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.
21 citations as recorded by crossref.
- Impact of the temperature-cloud phase relationship on the simulated Arctic warming during the Last Interglacial N. Arima et al.
- New insights to be gained from a Virtual Ecosystem R. Ewers et al.
- 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.
- Changing Movements in a Changing World: Modelling Early Pleistocene and Early Middle Pleistocene Climatic and Ecological Environments and Influences on Hominin Dispersal in Eurasia K. Lomborg et al.
- Astronomical forcing shaped the timing of early Pleistocene glacial cycles Y. Watanabe et al.
- 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.
- Possible influences of tropical vegetation shift on the glacial-interglacial temperature changes L. Tian et al.
- Intensified Atmospheric Branch of the Hydrological Cycle Over the Tibetan Plateau During the Last Interglacial From a Dynamical Downscaling Perspective N. Jiang et al.
- Differences Between Present‐Day and Cretaceous Hydrological Cycle Responses to Rising CO2 Concentration T. Higuchi et al.
- Arctic Amplification in the Past, Present, and Future: A Review for the Challenge to the Integrative Understanding of its Mechanism M. YOSHIMORI et al.
- Effect of Climatic Precession on Dansgaard‐Oeschger‐Like Oscillations Y. Kuniyoshi et al.
- PMIP4 experiments using MIROC-ES2L Earth system model R. Ohgaito et al.
- Long- and short-term variability of Arctic sea-ice cover during the Last Interglacial and Marine Isotope Stage 11c B. Crow & M. Prange
- How temperature seasonality drives interglacial permafrost dynamics: implications for paleo reconstructions and future thaw trajectories J. Nitzbon et al.
- Climate and stratospheric ozone during the mid-Holocene and Last Interglacial simulated by MRI-ESM2.0 Y. Watanabe et al.
- Climate and ocean circulation changes toward a modern snowball Earth T. Obase et al.
- 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.
- A model-based comparison of paleo-physical processes in the Bay of Bengal M. Khan et al.
- The Late Pliocene jet stream: Changes and drivers of the mean state and variability A. Buchan et al.
- Assessment of the southern polar and subpolar warming in the PMIP4 last interglacial simulations using paleoclimate data syntheses Q. Gao et al.
- 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.
Saved (final revised paper)
Latest update: 30 Apr 2026
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....
