public:publications:theme_auto

NICAM publication list by theme

Please check publication list by year for complete list.

Model framework, description, scheme, dynamics, physics (other schemes in NICAM)

  • Tomita, H. (2009): Analysis of Spurious Surface Temperature at the Atmosphere-Land Interface and a New Method to Solve the Surface Energy Balance Equation. J. Hydorometeor. 10. 833-844.
  • Tomita, H., K. Goto, M. Satoh, 2008: A new approach of atmospheric general circulation model - Global cloud resolving model NICAM and its computational performance -. SIAM, J. Sci. Comput., 30, 2755-2776; DOI. 10.1137/070692273.
  • Tomita, H. (2008a) : A stretched grid on a sphere by new grid transformation. J. Meteor. Soc. Japan, 86A, 107-119.
  • Tomita, H. (2008b) : New microphysical schemes with five and six categories by diagnostic generation of cloud ice. J. Meteor. Soc. Japan, 86A, 121-142.
  • Satoh, M., T. Matsuno, H. Tomita, H. Miura, T. Nasuno, S. Iga, (2008) : Nonhydrostatic Icosahedral Atmospheric Model (NICAM) for global cloud resolving simulations. Journal of Computational Physics, the special issue on Predicting Weather, Climate and Extreme events, 227, 3486-3514, doi:10.1016/j.jcp.2007.02.006.
  • Satoh, M. (2007) : A road to a global nonhydostatic model. Tenki, 54.9 769-772.
  • Iga, S., Tomita, H., Satoh, M., Goto, K. (2007) : Mountain-wave-like spurious waves due to inconsistency of horizontal and vertical resolution associated with cold fronts. Mon. Wea. Rev., 135, 2629-2641.
  • Satoh, M.(2006) : Climate research on a next generation global cloud-resolving model. Parity, 21, 56-57. (in Japanese)
  • Tomita, H., 2006: Development of nonhydrostatic atmospheric general circulation model using an icosahedral grid. (in japanese) Nagare, 25, 181-186.
  • Satoh, M., Tomita, H, Miura, H., Iga, S., and Nasuno, T. (2005) : Development of a global cloud resolving model – a multi-scale structure of tropical convections –. J. Earth Simulator, vol.3, 11-19.
  • Tomita, H. and Satoh, M. (2004) : A new dynamical framework of nonhydrostatic global model using the icosahedral grid. Fluid Dyn. Res., 34, 357-400. DOI:10.1016/j.fluiddyn.2004.03.003
  • Satoh, M. (2003) : Conservative scheme for a compressible nonhydrostatic model with moist processes. Mon. Wea. Rev., 131, 1033-1050
  • Satoh, M. (2002) : Conservative scheme for the compressible nonhydrostatic models with the horizontally explicit and vertically implicit time integration scheme. Mon. Wea. Rev., 130, 1227-1245
  • Satoh,M., Tomita,M., Tsugawa,M. (2002) : Development of a global nonhydrostatic model. Gekkan Kaiyo, 34, 101-106 (in Japanese)
  • Tomita,H., Tsugawa,M., Satoh,M., Goto, K.(2001) : Shallow water model on a modified icosahedral geodesic grid by using spring dynamics. J. Comp. Phys., 174, 579-613
  • Satoh, M., Tomita, H., Tsugawa, M., Xiao, F. (2001) Development of a next generation atmospheric general circulation model at Frontier Research System for Global Change. (in japanese) Nagare, 20, 37-46

Cloud Microphysics (Single-Moment Scheme)

Cloud Microphysics (Double-Moment Scheme)

Aqua planet experiment

MJO

Typhoon / Cyclone

Monsoon

Precipitation

Clouds and their diurnal cycle, physics

  • Suzuki, K., G. L. Stephens, S. C. van den Heever, and T. Y. Nakajima, 2011: Diagnosis of the warm rain process in cloud-resolving models using joint CloudSat and MODIS observations. J. Atmos. Sci., 68, 2655-2670.
  • Inoue, T., Satoh, M., Hagihara, Y., Miura, H., and Schmetz, J., 2010: Comparison of high‐level clouds represented in a global cloud system-resolving model with CALIPSO/CloudSat and geostationary satellite observations, J. Geophys. Res., 115, D00H22, doi:10.1029/2009JD012371.
  • Noda, A. T., K. Oouchi, M Satoh, H. Tomita, S. Iga, and Y. Tsushima, 2010: Importance of the subgrid-scale turbulent moist process: Cloud distribution in global cloud-resolving simulations. Atmos. Res., 96(2-3), 208-217, doi:10.1016/j.atmosres.2009.05.007.
  • Collins, W. D., Satoh, M. 2009: Simulating Global Clouds, Past, Present, and Future. Chap 20 of “Heintzenberg, J., and R. J. Charlson, eds. 2009. Clouds in the Perturbed Climate System: Their Relationship to Energy Balance, Atmospheric Dynamics, and Precipitation.” Struengmann Forum Report, vol. 2. Cambridge, MA: The MIT Press, pp.469-486.
  • Quaas, J. S. Bony, W. D. Collins, L. Donner, A. Illingworth, A. Jones, U. Lohmann, M. Satoh, S. E. Schwartz,W.-K. Tao, and R. Wood, 2009: Current understanding and quantification of clouds in the changing climate system and strategies for reducing critical uncertainties. Chap 24 of “Heintzenberg, J., and R. J. Charlson, eds. 2009. Clouds in the Perturbed Climate System: Their Relationship to Energy Balance, Atmospheric Dynamics, and Precipitation.” Struengmann Forum Report, vol. 2. Cambridge, MA: The MIT Press, pp.557-573.
  • Satoh, M., Matsuda, Y. (2009) : Statistics on high-cloud areas and their sensitivities to cloud microphysics using single-cloud experiments. J. Atmos. Sci., 66, 2659-2677.
  • Suzuki, K., T. Nakajima, M. Satoh, H. Tomita, T. Takemura, T. Y. Nakajima, and G. L. Stephens (2008): Global cloud-system-resolving simulation of aerosol effect on warm clouds. Geophys. Res. Lett., 35, L19817, doi:10.1029/2008GL035449.
  • Tomita, H. (2008b) : New microphysical schemes with five and six categories by diagnostic generation of cloud ice. J. Meteor. Soc. Japan, 86A, 121-142.
  • Sato, T., T. Yoshikane, M. Satoh, H. Miura, and H. Fujinami (2008) : Resolution dependency of the diurnal cycle of convective clouds over the Tibetan Plateau in a mesoscale model. J. Meteor. Soc. Japan, 86A, 17-31.
  • Inoue,T., M. Satoh, H. Miura, B. Mapes (2008) : Characteristics of cloud size of deep convection simulated by a global cloud resolving model over the western tropical Pacific. J. Meteor. Soc. Japan, 86A, 1-15.
  • Satoh, M. (2008) : Numerical simulations of heavy rainfalls by a global cloud-resolving model. J. Disaster Research, 3, 33-38.
  • Sato, T., Miura, H., Satoh, M. (2007) : Spring diurnal cycle of clouds over Tibetan Plateau: global cloud-resolving simulations and satellite observations. Geophys. Res. Lett., 34, L18816, doi:10.1029/2007GL030782

Climate

  • Collins, W. D., Satoh, M. 2009: Simulating Global Clouds, Past, Present, and Future. Chap 20 of “Heintzenberg, J., and R. J. Charlson, eds. 2009. Clouds in the Perturbed Climate System: Their Relationship to Energy Balance, Atmospheric Dynamics, and Precipitation.” Struengmann Forum Report, vol. 2. Cambridge, MA: The MIT Press, pp.469-486.
  • Quaas, J. S. Bony, W. D. Collins, L. Donner, A. Illingworth, A. Jones, U. Lohmann, M. Satoh, S. E. Schwartz,W.-K. Tao, and R. Wood, 2009: Current understanding and quantification of clouds in the changing climate system and strategies for reducing critical uncertainties. Chap 24 of “Heintzenberg, J., and R. J. Charlson, eds. 2009. Clouds in the Perturbed Climate System: Their Relationship to Energy Balance, Atmospheric Dynamics, and Precipitation.” Struengmann Forum Report, vol. 2. Cambridge, MA: The MIT Press, pp.557-573.
  • Suzuki, K., T. Nakajima, M. Satoh, H. Tomita, T. Takemura, T. Y. Nakajima, and G. L. Stephens (2008): Global cloud-system-resolving simulation of aerosol effect on warm clouds. Geophys. Res. Lett., 35, L19817, doi:10.1029/2008GL035449.
  • Iga, S., H. Tomita, Y. Tsushima, M. Satoh (2007) : Climatology of a nonhydrostatic global model with explicit cloud processes. Geophys. Res. Lett., 34, L22814, doi:10.1029/2007GL031048.

Diagnostic evaluation, Predictability

Aerosol

Quasi-realtime forecasting application

  • Oouchi, K., H. Taniguchi, T. Nasuno, M. Satoh, H. Tomita, Y. Yamada, M. Ikeda, R. Shirooka, H. Yamada, K. Yoneyama, 2012: A prototype quasi real-time intra-seasonal forecasting of tropical convection over the warm pool region: a new challenge of global cloud-system-resolving model for a field campaign. Nova Science Publishers, Inc., Eds. K. Oouchi and H. Fudeyasu, pp.233-248.
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