20-km-Mesh Global Climate Simulations Using JMA-GSM Model —Mean Climate States—

By R. Mizuta, K. Oouchi, Hiromasa Yoshimura, Akira T. Noda, Keiichi Katayama, S. Yukimoto, M. Hosaka, S. Kusunoki, H. Kawai, Masayuki Nakagawa. 2006

257 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/83f2437018ac3aeb9ec3b3113c78856af24d4004

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Citations in the corpus

Present-day climate and climate sensitivity in the meteorological research institute coupled GCM version 2.3 (MRI-CGCM2.3) (2006, background): “A portion of the simulation results were provided for lower-boundary conditions (the SST and sea-ice distribution), in the time-slice climate change experiments (Oouchi et al. 2006) with a very high-resolution (20-km mesh) atmospheric GCM (Mizuta et al. 2006).”
Nonhydrostatic icosahedral atmospheric model (NICAM) for global cloud resolving simulations (2008, methodology): “The new model is designed to perform ‘‘cloud resolving simulations’’ by directly calculating deep convection and meso-scale circulations, which play key roles not only in the tropical circulations but in the global circulations of the atmosphere.”
Climate Simulations Using MRI-AGCM3.2 with 20-km Grid (2012, methodology): “Many parameterization schemes for various physical processes are newly developed and introduced into the model by both of JMA and MRI.”
The Evolution of Dynamical Cores for Global Atmospheric Models(125th Anniversary Issue of the Meteorological Society of Japan) (2007, background): “However, Mizuta et al. (2006) have developed a quasiconservative semi-Lagrangian model and applied it at very high resolution as well as at resolutions more common in climate models today.”
High-resolution global climate modelling: the UPSCALE project, a large-simulation campaign (2014, unknown): “Following the development of the ﬁrst high-resolution global climate models at the Japanese Earth Simulator (Ohfuchi et al., 2004; Mizuta et al., 2006), investigations into the value of resolution have continued rapidly.”
The Non-hydrostatic Icosahedral Atmospheric Model: description and development (2014, background): “Review of global non-hydrostatic models Thanks to the significant advances in high-performance computers over the last decade, global atmospheric simulations with a horizontal resolution of O (10 km) can be achieved (Ohfuchi et al. 2004; Mizuta et al. 2005; Kinter et al. 2013; Wedi 2014).”