Climate Simulations Using MRI-AGCM3.2 with 20-km Grid

By R. Mizuta, Hiromasa Yoshimura, H. Murakami, M. Matsueda, H. Endo, T. Ose, K. Kamiguchi, M. Hosaka, M. Sugi, S. Yukimoto and 2 more. 2012

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Coupled Model Intercomparison Project 5 (CMIP5) simulations of climate following volcanic eruptions (2012, methodology): “As with S06 the eruptions listed in 2 are a subset of the volcanic 135 events analyzed by Robock and Mao [1992]. In the same approach as S06, high-latitude 136 eruptions from those studied by Robock and Mao are not included because they appear to 137 produce a qualitatively different effect on circu”
Dynamic genesis potential index for diagnosing present-day and future global tropical cyclone genesis (2020, background): “2 S; Mizuta et al 2012, Murakami et al 2012).”
The GFDL Global Atmosphere and Land Model AM4.0/LM4.0: 1. Simulation Characteristics With Prescribed SSTs (2018, result): “The comparison with the CMIP5 models is also favorable overall, with the high resolution (20–60 km) MRI AGCMs (Mizuta et al., 2012) evidently being the best examples of CMIP5 AMIP simulations of comparable overall quality to AM4.”