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    A Note on Finite Differencing of the Advection-Diffusion Equation 

    Source: Monthly Weather Review:;1981:;volume( 109 ):;issue: 008:;page 1807
    Author(s): Clancy, R. Michael
    Publisher: American Meteorological Society
    Abstract: The criteria advanced by Fromm (1964) and Roache (1976) as necessary and sufficient conditions for numerical stability of the forward-in-time, centered-in-space finite-difference treatment of the advection-diffusion equation ...
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    Synoptic Forecasting of the Oceanic Mixed Layer Using the Navy's Operational Environmental Data Base: Present Capabilities and Future Applications 

    Source: Bulletin of the American Meteorological Society:;1981:;volume( 062 ):;issue: 006:;page 770
    Author(s): Clancy, R. Michael; Martin, Paul J.
    Publisher: American Meteorological Society
    Abstract: A synoptic forecast model of the oceanic mixed layer has been developed for operational use at the U.S. Navy's Fleet Numerical Oceanography Center (FNOC), Monterey, Calif. The potential success of this model depends ...
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    An Operational Global-Scale Ocean Thermal Analysis System 

    Source: Journal of Atmospheric and Oceanic Technology:;1990:;volume( 007 ):;issue: 002:;page 233
    Author(s): Clancy, R. Michael; Phoebus, Patricia A.; Pollak, Kenneth D.
    Publisher: American Meteorological Society
    Abstract: The Optimum Thermal Interpolation System (OTIS) is an ocean thermal analysis product developed for real-time operational use at the U.S. Navy's Fleet Numerical Oceanography Center. It functions in an analysis-prediction-analysis ...
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    Evaluations of Global Wave Prediction at the Fleet Numerical Meteorology and Oceanography Center 

    Source: Weather and Forecasting:;2005:;volume( 020 ):;issue: 005:;page 745
    Author(s): Rogers, W. Erick; Wittmann, Paul A.; Wang, David W. C.; Clancy, R. Michael; Hsu, Y. Larry
    Publisher: American Meteorological Society
    Abstract: It is a major challenge to determine whether bias in operational global wave predictions is predominately due to the wave model itself (internal error) or due to errors in wind forcing (an external error). Another challenge ...
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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