Description and basic evaluation of simulated mean state, internal variability, and climate sensitivity in MIROC6

• Published in: Geoscientific Model Development 2019-07, Vol.12 (7), p.2727-2765
• Main Authors: Tatebe, Hiroaki, Ogura, Tomoo, Nitta, Tomoko, Komuro, Yoshiki, Ogochi, Koji, Takemura, Toshihiko, Sudo, Kengo, Sekiguchi, Miho, Abe, Manabu, Saito, Fuyuki, Chikira, Minoru, Watanabe, Shingo, Mori, Masato, Hirota, Nagio, Kawatani, Yoshio, Mochizuki, Takashi, Yoshimura, Kei, Takata, Kumiko, O'ishi, Ryouta, Yamazaki, Dai, Suzuki, Tatsuo, Kurogi, Masao, Kataoka, Takahito, Watanabe, Masahiro, Kimoto, Masahide
• Format: Article
• Language: English
• Subjects: Atmospheric circulation; Atmospheric models; Climate; Climate effects; Climate models; Climate prediction; Climate science; Climate sensitivity; Climate system; Climate variability; Computer simulation; Future climates; Interactions; Intercomparison; Interdisciplinary research; Interdisciplinary studies; Madden-Julian oscillation; Parameterization; Precipitation; Radiative forcing; Sensitivity; Sensitivity analysis; Stratosphere; Temperature; Tropical climate; Tropical climates; Troposphere; Variability; Westerlies
• ISSN: 1991-9603; 1991-962X; 1991-959X; 1991-9603; 1991-962X
• DOI: 10.5194/gmd-12-2727-2019

The sixth version of the Model for Interdisciplinary Research on Climate (MIROC), called MIROC6, was cooperatively developed by a Japanese modeling community. In the present paper, simulated mean climate, internal climate variability, and climate sensitivity in MIROC6 are evaluated and briefly summarized in comparison with the previous version of our climate model (MIROC5) and observations. The results show that the overall reproducibility of mean climate and internal climate variability in MIROC6 is better than that in MIROC5. The tropical climate systems (e.g., summertime precipitation in the western Pacific and the eastward-propagating Madden–Julian oscillation) and the midlatitude atmospheric circulation (e.g., the westerlies, the polar night jet, and troposphere–stratosphere interactions) are significantly improved in MIROC6. These improvements can be attributed to the newly implemented parameterization for shallow convective processes and to the inclusion of the stratosphere. While there are significant differences in climates and variabilities between the two models, the effective climate sensitivity of 2.6 K remains the same because the differences in radiative forcing and climate feedback tend to offset each other. With an aim towards contributing to the sixth phase of the Coupled Model Intercomparison Project, designated simulations tackling a wide range of climate science issues, as well as seasonal to decadal climate predictions and future climate projections, are currently ongoing using MIROC6.