Weather Forecasting on Parallel Architectures

Abstract Global forecasting at the National Meteorological Center is performed using a spherical harmonics spectral model. The model is used in global data assimilation, and in the aviation and medium range forecast production suites. In this presentation, the major numerical and physical aspects of the model are highlighted, and parallelization considerations are analyzed and applied to three parallel computer architectures. The first parallelization is on a parallel vector processor shared memory platform such as Cray YMP or C90. The other two are on distributed memory platforms: a data parallel implementation on Connection Machines and a single program multiple data (SPMD) adaptation to a Cray T3D machine.

[1]  R. Lindzen Turbulence and stress owing to gravity wave and tidal breakdown , 1981 .

[2]  Patrick H. Worley,et al.  Parallelizing the spectral transform method. Part II , 1992, Concurr. Pract. Exp..

[3]  H. Kuo Further Studies of the Parameterization of the Influence of Cumulus Convection on Large-Scale Flow , 1974 .

[4]  Piers J. Sellers,et al.  A Global Climatology of Albedo, Roughness Length and Stomatal Resistance for Atmospheric General Circulation Models as Represented by the Simple Biosphere Model (SiB) , 1989 .

[5]  William Bourke,et al.  A multi-level spectral model. I. Formulation and hemispheric integrations , 1974 .

[6]  H. L. Penman Natural evaporation from open water, bare soil and grass , 1948, Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences.

[7]  E. Kessler On the distribution and continuity of water substance in atmospheric circulations , 1969 .

[8]  H. Charnock Wind stress on a water surface , 1955 .

[9]  W. Daniel Hillis,et al.  Data parallel algorithms , 1986, CACM.

[10]  S. Orszag Transform method for the calculation of vector-coupled sums: Application to the spectral form of the vorticity equation , 1970 .

[11]  H. Kuo On Formation and Intensification of Tropical Cyclones Through Latent Heat Release by Cumulus Convection , 1965 .

[12]  William Gropp,et al.  Parallel Scalability of the Spectral Transform Method , 1991, PPSC.

[13]  Remo Guidieri Res , 1995, RES: Anthropology and Aesthetics.

[14]  Eugenia Kalnay,et al.  The effect of a gravity wave drag parameterization scheme on GLA fourth order GCM forecasts , 1986 .

[15]  Joseph G. Sela,et al.  The NMC spectral model , 1982 .

[16]  Patrick H. Worley,et al.  Parallelizing the Spectral Transform Method , 1992, The Sixth Distributed Memory Computing Conference, 1991. Proceedings.

[17]  Paul B. Anderson,et al.  Massive Parallization of NMC's Spectral Model , 1994, J. Parallel Distributed Comput..

[18]  Joseph Sela,et al.  Spectral Modeling at the National Meteorological Center , 1980 .

[19]  Stephen B. Fels,et al.  An efficient, accurate algorithm for calculating CO2 15 μm band cooling rates , 1981 .

[20]  H. Pan,et al.  A Simple Parameterization Scheme of Evapotranspiration over Land for the NMC Medium-Range Forecast Model , 1990 .

[21]  Boris Katz,et al.  Recent Changes Implemented into the Global Forecast System at NMC , 1991 .

[22]  C. Leith Atmospheric Predictability and Two-Dimensional Turbulence , 1971 .

[23]  J. Hansen,et al.  A parameterization for the absorption of solar radiation in the earth's atmosphere , 1974 .