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    The Depth-Dependent Current and Wave Interaction Equations: A Revision 

    Source: Journal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 011:;page 2587
    Author(s): Mellor, George L.
    Publisher: American Meteorological Society
    Abstract: his is a revision of a previous paper dealing with three-dimensional wave-current interactions. It is shown that the continuity and momentum equations in the absence of surface waves can include waves after the addition ...
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    An Equation of State for Numerical Models of Oceans and Estuaries 

    Source: Journal of Atmospheric and Oceanic Technology:;1991:;volume( 008 ):;issue: 004:;page 609
    Author(s): Mellor, George L.
    Publisher: American Meteorological Society
    Abstract: No abstract available
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    Analytic Prediction of the Properties of Stratified Planetary Surface Layers 

    Source: Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 006:;page 1061
    Author(s): Mellor, George L.
    Publisher: American Meteorological Society
    Abstract: By considering the complex of one-point, turbulent moment equations for velocity, pressure and temperature, it appears possible to predict some properties of diabatic, density-stratified planetary layers using empirical ...
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    One-Dimensional, Ocean Surface Layer Modeling: A Problem and a Solution 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 003:;page 790
    Author(s): Mellor, George L.
    Publisher: American Meteorological Society
    Abstract: The first part of this paper is generic; it demonstrates a problem associated with one-dimensional, ocean surface layer model comparisons with ocean observations. Unlike three-dimensional simulations or the real ocean, ...
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    A Comparative Study of Curved Flow and Density-Stratified Flow 

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 007:;page 1278
    Author(s): Mellor, George L.
    Publisher: American Meteorological Society
    Abstract: A semi-empirical theory, used to predict buoyancy effects in a density-stratified and shear-driven flow, is also applied to the case of a boundary layer with curvature. Curved flow data are available and interesting in ...
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    The Gaussian Cloud Model Relations 

    Source: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 002:;page 356
    Author(s): Mellor, George L.
    Publisher: American Meteorological Society
    Abstract: Sommeria and Deardorff (1977) have derived turbulence closure relations which should be important to cloud modeling. To obtain these relations they have hade to invoke some analytical approximations and data from numerical ...
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    CORRIGENDUM 

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 011:;page 2304
    Author(s): Mellor, George L.
    Publisher: American Meteorological Society
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    A Numerical Study of the Variability and the Separation of the Gulf Stream, Induced by Surface Atmospheric Forcing and Lateral Boundary Flows 

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 006:;page 660
    Author(s): Ezer, Tal; Mellor, George L.
    Publisher: American Meteorological Society
    Abstract: A primitive equation regional model is used to study the effects of surface and lateral forcing on the variability and the climatology of the Gulf Stream system. The model is an eddy-resolving, coastal ocean model that ...
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    A Numerical Study of the Mediterranean Sea Circulation 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 006:;page 1384
    Author(s): Zavatarielli, Marco; Mellor, George L.
    Publisher: American Meteorological Society
    Abstract: A primitive equation ocean model that makes use of a curvilinear orthogonal grid and a sigma-coordinate system was used to simulate the Mediterranean Sea The model was forced with monthly climatological values of wind ...
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    A Hierarchy of Turbulence Closure Models for Planetary Boundary Layers 

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 007:;page 1791
    Author(s): Mellor, George L.; Yamada, Tetsuji
    Publisher: American Meteorological Society
    Abstract: Turbulence models centered on hypotheses by Rotta and Kolmogoroff are complex. In the present paper we consider systematic simplifications based on the observation that parameters governing the degree of anisotropy are ...
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