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    Generation and Propagation of 30-Day Waves in a Numerical Model of the Pacific 

    Source: Journal of Physical Oceanography:;1980:;Volume( 010 ):;issue: 008:;page 1168
    Author(s): Cox, Michael D.
    Publisher: American Meteorological Society
    Abstract: A multilevel numerical model is applied to the equatorial Pacific Ocean, driven by long-term averaged, monthly varying winds. In agreement with satellite-observed sea surface temperatures, the solution is unstable at certain ...
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    A Numerical Study of Somali Current Eddies 

    Source: Journal of Physical Oceanography:;1979:;Volume( 009 ):;issue: 002:;page 311
    Author(s): Cox, Michael D.
    Publisher: American Meteorological Society
    Abstract: A three-dimensional numerical ocean model is used to study the transient response of the western boundary region of a tropical ocean to the sudden onset of winds parallel to the boundary. In particular, the behavior of ...
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    An Eddy-Resolving Numerical Model of the Ventilated Thermocline: Time Dependence 

    Source: Journal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 007:;page 1044
    Author(s): Cox, Michael D.
    Publisher: American Meteorological Society
    Abstract: A primitive equation, eddy-resolving numerical model is used to study the inherent time scales of variability in the subtropical ocean, assuming temporally constant surface forcing. Three primary scales arise: mesoscale ...
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    An Eddy Resolving Numerical Model of the Ventilated Thermocline 

    Source: Journal of Physical Oceanography:;1985:;Volume( 015 ):;issue: 010:;page 1312
    Author(s): Cox, Michael D.
    Publisher: American Meteorological Society
    Abstract: A three-dimensional, primitive equation numerical model is used to study the effects of mesoscale eddies within the subtropical thermocline. Solutions are obtained for an ocean bounded by idealized topography are driven ...
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    An Idealized Model of the World Ocean. Part I: The Global-Scale Water Masses 

    Source: Journal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 011:;page 1730
    Author(s): Cox, Michael D.
    Publisher: American Meteorological Society
    Abstract: A primitive equation, three-dimensional numerical model of the ocean, employing idealized versions of the real topography and surface boundary conditions, is used to study the water mass structure of the World Ocean. In ...
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    An Approximate Equation of State for Numerical Models of Ocean Circulation 

    Source: Journal of Physical Oceanography:;1972:;Volume( 002 ):;issue: 004:;page 510
    Author(s): Bryan, Kirk; Cox, Michael D.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    The Circulation of the World Ocean: A Numerical Study. Part I, A Homogeneous Model 

    Source: Journal of Physical Oceanography:;1972:;Volume( 002 ):;issue: 004:;page 319
    Author(s): Bryan, Kirk; Cox, Michael D.
    Publisher: American Meteorological Society
    Abstract: Calculations are carried out for a homogeneous model of the World Ocean. Solutions for the large-scale, wind-driven circulation are obtained by numerical integration with respect to time of a numerical model. The model ...
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    A Nonlinear Model of an Ocean Driven by Wind and Differential Heating: Part II. An Analysis of the Heat, Vorticity and Energy Balance 

    Source: Journal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 006:;page 968
    Author(s): Brain, Kirk; Cox, Michael D.
    Publisher: American Meteorological Society
    Abstract: An analysis is made of the heat and vorticity balance of a numerical model of a baroclinic ocean. The computation is carried out on a three-dimensional grid designed to resolve the thermocline, and the narrow sidewall ...
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    A Nonlinear Model of an Ocean Driven by Wind and Differential Heating: Part I. Description of the Three-Dimensional Velocity and Density Fields 

    Source: Journal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 006:;page 945
    Author(s): Bryan, Kirk; Cox, Michael D.
    Publisher: American Meteorological Society
    Abstract: A numerical experiment is carried out to investigate the circulation of an ocean, driven by a prescribed density gradient and wind stress at the surface. The mathematical formulation includes in one model most of the ...
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    A Numerical Model of the Ventilated Thermocline 

    Source: Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 004:;page 674
    Author(s): Cox, Michael D.; Bryan, Kirk
    Publisher: American Meteorological Society
    Abstract: A steady state numerical solution is found for an idealized, rectangular ocean basin driven by wind and surface buoyancy flux. A three-dimensional primitive equation model is used. In agreement with recent analytical ...
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