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    Numerical Weather Prediction 

    Source: Bulletin of the American Meteorological Society:;1978:;volume( 059 ):;issue: 001:;page 5
    Author(s): Shuman, Frederick G.
    Publisher: American Meteorological Society
    Abstract: This article is addressed to the layman with a science education. It is thus not addressed specifically to the meteorologist, but it contains certain information about the weather services, and the impact of numerical ...
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    Nominations to the Grade of Fellows Are Open 

    Source: Bulletin of the American Meteorological Society:;1975:;volume( 056 ):;issue: 001:;page 45
    Author(s): Shuman, Frederick G.
    Publisher: American Meteorological Society
    Abstract: tract
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    On Certain Truncation Errors Associated with Spherical Coordinates 

    Source: Journal of Applied Meteorology:;1970:;volume( 009 ):;issue: 004:;page 564
    Author(s): Shuman, Frederick G.
    Publisher: American Meteorological Society
    Abstract: Excessive errors are committed in grids, in which mesh-lengths in the longitudinal direction are preserved in polar regions, if the hydrodynamic equations written in spherical coordinates are directly transformed into ...
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    History of Numerical Weather Prediction at the National Meteorological Center 

    Source: Weather and Forecasting:;1989:;volume( 004 ):;issue: 003:;page 286
    Author(s): Shuman, Frederick G.
    Publisher: American Meteorological Society
    Abstract: The first modern numerical weather prediction (NWP) models were developed for the computer that was announced in 1932 at the Institute for Advanced Study, in Princeton, New Jersey. Within 3 yr three agencies of the United ...
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    NUMERICAL METHODS IN WEATHER PREDICTION: II. SMOOTHING AND FILTERING 

    Source: Monthly Weather Review:;1957:;volume( 085 ):;issue: 011:;page 357
    Author(s): SHUMAN, FREDERICK G.
    Publisher: American Meteorological Society
    Abstract: A method is developed for the design of finite-difference smoothing and filtering operators which meet pre-determined specifications, and which are applicable to automatic computing machinery. The general technique is to ...
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    NUMERICAL METHODS IN WEATHER PREDICTION: I. THE BALANCE EQUATION 

    Source: Monthly Weather Review:;1957:;volume( 085 ):;issue: 010:;page 329
    Author(s): SHUMAN, FREDERICK G.
    Publisher: American Meteorological Society
    Abstract: Two methods of solving the balance equation are outlined. Both methods have been used successfully on a daily operational basis at the Joint Numerical Weather Prediction Unit for a period of more than a year. Solutions ...
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    PREDICTIVE CONSEQUENCES OF CERTAIN PHYSICAL INCONSISTENCIES IN THE GEOSTROPHIC BAROTROPIC MODEL 

    Source: Monthly Weather Review:;1957:;volume( 085 ):;issue: 007:;page 229
    Author(s): SHUMAN, FREDERICK G.
    Publisher: American Meteorological Society
    Abstract: The physical inconsistency of geostrophic flow and small surface pressure tendencies is discussed. The frequently disastrous consequences in conventional geostrophic barotropic predictions are numerically identified by ...
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    Reply 

    Source: Journal of Applied Meteorology:;1970:;volume( 009 ):;issue: 002:;page 316
    Author(s): Shuman, Frederick G.; Hovermale, John
    Publisher: American Meteorological Society
    Abstract: tract
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    NOTE ON THE FORMULATION OF FINITE DIFFERENCE EQUATIONS INCORPORATING A MAP SCALE FACTOR 

    Source: Monthly Weather Review:;1968:;volume( 096 ):;issue: 003:;page 157
    Author(s): SHUMAN, FREDERICK G.; STACKPOLE, JOHN D.
    Publisher: American Meteorological Society
    Abstract: Numerical experimentation with various finite difference formulations of a particular set of differential equations incorporating a map scale factor indicates that the stability of the calculations is as dependent upon the ...
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    DIFFERENCE SYSTEM AND BOUNDARY CONDITIONS FOR THE PRIMITIVE-EQUATION BAROTROPIC FORECAST 

    Source: Monthly Weather Review:;1966:;volume( 094 ):;issue: 005:;page 329
    Author(s): SHUMAN, FREDERICK G.; VANDERMAN, LLOYD W.
    Publisher: American Meteorological Society
    Abstract: A primitive-equation free-surface barotropic model was designed for the tropical belt. By the use of Shuman's difference system, experiments were made to test the effect of both approximate and correct boundary conditions ...
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