Arakawa A., V. R. Lamb, 1997: Computational design of the basic dynamical processes of the UCLA General Circulation Model. Methods in Computational Physics, Vol. 17, J. Chang, Ed., Academic Press, San Francisco, USA, 173- 265.
Baba Y., K. Takahashi, and T. Sugimura, 2010: Dynamical core of an atmospheric general circulation model on a Yin-Yang grid. Mon. Wea. Rev., 138, 3988- 4005.
Charney J. G., N. A. Philips, 1953: Numerical integration of the quasi-geostrophic equations for barotropic and simple baroclinic Flow. J. Meteor., 10, 71- 99.
Chen D., Coauthors, 2008: New generation of multi-scale NWP system (GRAPES): General scientific design. Chinese Sci. Bull., 53( 18), 3433- 3445.
Jablonowski C., P. Lauritzen, R. Nair, and M. Taylor, 2008: Idealized test cases for the dynamical cores of atmospheric general circulation models: A proposal for the NCAR ASP 2008 summer colloquium. [Available online at http://esse.engin.umich. edu/admg/publications.php.]
Kageyama A., T. Sato, 2004: "Yin-Yang grid": An overset grid in spherical geometry. Geochem. Geophys. Geosyst., 5, Q09005, doi: 10.1029/2004GC000734.
Li X. L., D. H. Chen, X. D. Peng, F. Xiao, and X. S. Chen, 2006: Implementation of the semi-Lagrangian advection scheme on a quasi-uniform overset grid on a sphere. Adv. Atmos. Sci., 23(5), 792-801, doi: 10.1007/s00376-006-0792-9.
Li X. L., D. H. Chen, X. D. Peng, K. Takahashi, and F. Xiao, 2008: A multimoment finite-volume shallow-water model on the Yin-Yang overset spherical grid. Mon. Wea. Rev., 136, 3066- 3086.
Liu Y., J. W. Cao, 2008: ILU preconditioner for NWP system: GRAPES. Computer Engineering and Design, 29( 3), 731- 734. (in Chinese)
McDonald A., J. R. Bates, 1989: Semi-Lagrangian integration of a grid point shallow water model on the sphere. Mon. Wea. Rev., 117, 130- 137.
Peng X., F. Xiao, and K. Takahashi, 2006: Conservative constraint for a quasi-uniform overset grid on the sphere. Quart. J. Roy. Meteor. Soc., 132, 979- 996.
Qian J., F. Semazzi, and J. S. Scroggs, 1998: A global nonhydrastatic semi-Lagrangian atmospheric model with orography. Mon. Wea. Rev., 126, 747- 771.
Qaddouri A., L. Laayouni, J. Côté, and M. Gander, 2008: Optimized Schwarz methods with an overset grid for shallow-water equations: Preliminary results. Appl. Numer. Math., 58( 4), 459- 471.
Ritchie H., C. Beaudoin, 1994: Approximations and sensitivity experiments with a baroclinic semi-Lagrangian spectral model. Mon. Wea. Rev., 122, 2391- 2399.
Sadourny R. A., 1972: Conservative finite-difference approximations of the primitive equations on quasi-uniform spherical grids. Mon. Wea. Rev., 100, 136- 144.
Sadourny R. A., A. Arakawa, and Y. Mintz, 1968: Integration of the nondivergent barotropic vorticity equation with an icosahedral-hexagonal grid for the sphere. Mon. Wea. Rev., 96, 351- 356.
Satoh M., T. Inoue, and H. Miura, 2010: Evaluations of cloud properties of global and local cloud system resolving models using CALIPSO and CloudSat simulators. J. Geophys. Res., 115, D00H14, doi: 10.1029/2009JD012247.
Skamarock W., J. Klemp, M. Duda, L. Fowler, and S. H. Park, 2012: A multi-scale nonhydrostatic atmospheric model using centroidal Voronoi tesselations and C-grid staggering. Mon. Wea. Rev., 140, 3090- 3105.
Semazzi F., J. H. Qian, and J. S. Scroggs, 1995: A global nonhydrostatic, semi-Lagrangian, atmospheric model without orography. Mon. Wea. Rev., 123, 2534- 2550.
Tomita H., M. Satoh, 2004: A new dynamical framework of nonhydrostatic global model using the icosahedral grid. Fluid Dyn. Res., 34, 357- 400.
Williamson D. L., 2007: The evolution of dynamical cores for global atmospheric models. J. Meteor. Soc. Japan, 85B, 241- 269.
Williamson D. L., J. B. Drake, J. J. Hack, R. Jackob, and P. N. Swarztrauber, 1992: A standard test for numerical approximations to the shallow water equations in spherical geometry. Journal of Computational Physics, 102, 211- 224.
Xue J. S., D. H. Chen, 2008: Design of GRAPES dynamical frame and the experiments. Scientific Design and Application of Numerical Prediction System GRAPES, J. H. Wang, Ed., Science Press, Beijing, 65- 136. (in Chinese)