Articles | Volume 17, issue 1
https://doi.org/10.5194/cp-17-21-2021
https://doi.org/10.5194/cp-17-21-2021
Research article
 | 
06 Jan 2021
Research article |  | 06 Jan 2021

PMIP4/CMIP6 last interglacial simulations using three different versions of MIROC: importance of vegetation

Ryouta O'ishi, Wing-Le Chan, Ayako Abe-Ouchi, Sam Sherriff-Tadano, Rumi Ohgaito, and Masakazu Yoshimori

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Latest update: 25 Apr 2024
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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.