*Nagio Hirota1, Takuro Michibata2, Yoko Yamagami3, Hiroaki Tatebe3, Kentaroh Suzuki4, Masahiro Watanabe4, Takao Kawasaki4, Tomoko Nitta5, Fuyuki SAITO3, Koji Ogochi3, Miho Sekiguchi6, Shingo Watanabe3, Hideo Shiogama1, Tomoo Ogura1, Toshihiko Takemura7, Tomoki Ohno4, Manabu Abe3, Kei Yoshimura5, Hideaki Kawai8, Minoru Chikira1, Hisashi Yashiro1, Daisuke Goto1
(1.National Institute for Environmental Studies, 2.Okayama University, 3.Japan Agency for Marine-Earth Science and Technology, 4.Atmosphere and Ocean Research Institute, University of Tokyo, 5.Institute of Industrial Science, the University of Tokyo, 6.Tokyo University of Marine Science and Technology, 7.Research Institute for Applied Mechanics, Kyushu University, 8.Meteorological Research Institute)
Keywords:climate model, CMIP7, climate projections, energy budget
A new version of the Model for Interdisciplinary Research on Climate, called MIROC7, is under development by a Japanese modeling community. The previous version MIROC6 showed good performances in representing climate mean states and natural variabilities, such as ENSO, MJO, QBO and SSW. However, some notable weaknesses remained in MIROC6. In particular, greenhouse effects of water vapor and sunshade effects of clouds were overly strong compared with observations, resulting in large biases in the energy budget. Moreover, acceleration of global warming by clouds (cloud feedback) was too weak compared with a likely range of cloud feedback values of WCRP assessments. Major updates from MIROC6 to MIROC7 are: more sophisticated cloud physics with prognostic treatment of precipitating particles; radiation processes; ocean mixing processes; and sea-ice treatments. Our preliminary results indicate that the biases in the energy budget is alleviated and cloud feedback is strengthened toward more positive. Given that cloud representation is improved and cloud feedback is more consistent with the WCRP assessments, climate projections by MIROC7 is likely to be more reliable compared with those by previous versions. Further developments is underway toward the seventh phase of Coupled Model Intercomparison Project.
Acknowledgments: This research is supported by the SENTAN Program (JPMXD0722680395) by MEXT, Japan. Simulations were performed on the Earth Simulator (JAMSTEC) and NEC SX-AURORA (NIES) were used.