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    A Note on Finite-Difference Influence Functions and the Propagation of Discrete Error 

    Source: Journal of the Atmospheric Sciences:;1963:;Volume( 020 ):;issue: 004:;page 339
    Author(s): Gates, W. Lawrence
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    An Essay on Climate Dynamics 

    Source: Bulletin of the American Meteorological Society:;1976:;volume( 057 ):;issue: 005:;page 542
    Author(s): Gates, W. Lawrence
    Publisher: American Meteorological Society
    Abstract: Following a general survey of the evidence for climatic variation, the dynamical basis of climate and the modeling of climatic change are briefly reviewed. The ability of general circulation models and of climate models ...
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    AMIP: The Atmospheric Model Intercomparison Project 

    Source: Bulletin of the American Meteorological Society:;1992:;volume( 073 ):;issue: 012:;page 1962
    Author(s): Gates, W. Lawrence
    Publisher: American Meteorological Society
    Abstract: The Atmospheric Model Intercomparison Project (AMIP) is an international effort to determine the systematic climate errors of atmospheric models under realistic conditions, and calls for the simulation of the climate of ...
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    METHOD OF NUMERICAL FORECASTING BY JUXTAPOSITION OF ONE-DIMENSIONAL SOLUTIONS, AND ITS APPLICATION TO THE EQUIVALENT BAROTROPIC MODEL 

    Source: Journal of Meteorology:;1953:;volume( 010 ):;issue: 002:;page 149
    Author(s): Gates, W. Lawrence
    Publisher: American Meteorological Society
    Abstract: By juxtaposition of a series of one-dimensional solutions at adjacent latitudes, numerical forecasts may easily and inexpensively be incorporated into forecasting routine. Forecasts for 140 degrees of longitude, for the ...
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    A Numerical Study of Transient Rossby Waves in a Wind-Driven Homogeneous Ocean 

    Source: Journal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 001:;page 3
    Author(s): Gates, W. Lawrence
    Publisher: American Meteorological Society
    Abstract: The primitive hydrostatic equations for a rectangular homogeneous ocean with a free surface on a ?-plane are integrated numerically for 60 days from an initial state of rest and undisturbed depth of 400 m. A zonal wind ...
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    ON THE TRUNCATION ERROR, STABILITY, AND CONVERGENCE OF DIFFERENCE SOLUTIONS OF THE BAROTROPIC VORTICITY EQUATION 

    Source: Journal of Meteorology:;1959:;volume( 016 ):;issue: 005:;page 556
    Author(s): Gates, W. Lawrence
    Publisher: American Meteorological Society
    Abstract: The truncation error, stability and convergence properties of various finite-difference formulations of the one-dimensional barotropic vorticity equation are considered, and analytic solutions of the difference equations ...
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    NOTE ON THE SUPPRESSION OF THE OSCILLATION (WEAK INSTABILITY) OF FIRST-FORWARD-THEN-CENTERED TIME DIFFERENCES IN NUMERICAL INTEGRATION 

    Source: Journal of Meteorology:;1960:;volume( 017 ):;issue: 005:;page 572
    Author(s): Gates, W. Lawrence
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    The January Global Climate Simulated by a Two-Level General Circulation Model: A Comparison with Observation 

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 003:;page 449
    Author(s): Gates, W. Lawrence
    Publisher: American Meteorological Society
    Abstract: The mean global distributions of pressure, temperature, wind, moisture, cloudiness, precipitation, evaporation, and surface heat balance simulated for January by the two-level Mintz-Arakawa atmospheric general circulation ...
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    Analysis of the Mean Forcing Fields Simulated By the Two-level, Mintz-Arakawa Atmospheric Model 

    Source: Monthly Weather Review:;1973:;volume( 101 ):;issue: 005:;page 412
    Author(s): GATES, W. LAWRENCE
    Publisher: American Meteorological Society
    Abstract: The global distributions of the mean January surface wind stress, the net diabatic heating rate, and the net rate of moisture addition as simulated in a 30-day integration with the two-level, Mintz-Arakawa atmospheric ...
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    STATIC STABILITY MEASURES IN THE ATMOSPHERE 

    Source: Journal of Meteorology:;1961:;volume( 018 ):;issue: 004:;page 526
    Author(s): Gates, W. Lawrence
    Publisher: American Meteorological Society
    Abstract: Various measures of static stability in the atmosphere are reviewed and their uses briefly discussed. The mean vertical distribution of nine stability measures is given for 100-mb tropospheric layers and for selected ...
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