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    Thermal Convection in a Rotating Fluid Annulus. Part I. The Basic Axisymmetric Flow 

    Source: Journal of the Atmospheric Sciences:;1967:;Volume( 024 ):;issue: 002:;page 144
    Author(s): Williams, Gareth P.
    Publisher: American Meteorological Society
    Abstract: The thermally driven motion of a fluid contained in a rotating annulus is investigated by numerical integration of the Navier-Stokes equations as an initial value problem. Four distinct regimes of hydro-dynamical flow can ...
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    Geostrophic Regimes on a Sphere and a Beta Plane 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 012:;page 1237
    Author(s): Williams, Gareth P.
    Publisher: American Meteorological Society
    Abstract: A general geostrophic equation is derived for a shallow layer of fluid on a sphere. This equation encompasses the planetary, intermediate, and quasi-forms of geostrophy and produces their equations directly when the ...
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    Thermal Convection in a Rotating Fluid Annulus: Part 2. Classes of Axisymmetric Flow 

    Source: Journal of the Atmospheric Sciences:;1967:;Volume( 024 ):;issue: 002:;page 162
    Author(s): Williams, Gareth P.
    Publisher: American Meteorological Society
    Abstract: This paper presents the solutions obtained for various axisymmetric thermal convection flows in a rotating annulus. Initially, a solution is obtained for a flow whose interior structure has been observed in detail. A ...
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    The Field Distributions and Balances in a Baroclinic Annulus Wave 

    Source: Monthly Weather Review:;1972:;volume( 100 ):;issue: 001:;page 29
    Author(s): WILLIAMS, GARETH P.
    Publisher: American Meteorological Society
    Abstract: The detailed structure of a steady wave occurring in a rotating annulus of square cross-section and having a free surface is presented. The field distributions are obtained by numerical integration of the three-dimensional ...
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    Thermal Convection in a Rotating Fluid Annulus: Part 3. Suppression of the Frictional Constraint on Lateral Boundaries 

    Source: Journal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 006:;page 1034
    Author(s): Williams, Gareth P.
    Publisher: American Meteorological Society
    Abstract: In certain rotating fluid systems such as the atmosphere, the flow must maintain a zero net torque on the horizontal surface. The character of such flows is sought through numerical integration of the Navier-Stokes equations. ...
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    Friction Term Formulation and Convective Instability in a Shallow Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 005:;page 870
    Author(s): Williams, Gareth P.
    Publisher: American Meteorological Society
    Abstract: The form of the friction terms for a shallow layer of fluid on a sphere is discussed for isotropic and transversely-isotropic fluids. We then examine the nature of convection in a transversely-isotropic fluid and find that ...
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    Planetary Circulations: 1. Barotropic Representation of Jovian and Terrestrial Turbulence 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 008:;page 1399
    Author(s): Williams, Gareth P.
    Publisher: American Meteorological Society
    Abstract: We seek the formative processes of the planetary circulations of Jupiter and Saturn. The study concentrates on examining whether processes known to control the terrestrial circulation, namely, two-dimensional turbulence ...
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    Planetary Circulations: 3. The Terrestrial Quasi-Geostrophic Regime 

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 008:;page 1409
    Author(s): Williams, Gareth P.
    Publisher: American Meteorological Society
    Abstract: The characteristics of the two-level quasi-geostrophic model are evaluated for a wide range of parameters in the terrestrial domain. Flow form is determined primarily by ? (the Coriolis gradient) and by τD, (the time scale ...
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    Planetary Circulations: 2. The Jovian Quasi-Geostrophic Regime 

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 005:;page 932
    Author(s): Williams, Gareth P.
    Publisher: American Meteorological Society
    Abstract: The characteristics of the two-level quasi-geostrophic model are evaluated for a wide range of parameter values in the Jovian domain. The results support the hypothesis that baroclinic instability energizes the circulation ...
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    Geostrophic Regimes, Intermediate Solitary Vortices and Jovian Eddies 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 004:;page 453
    Author(s): Williams, Gareth P.; Yamagata, Toshio
    Publisher: American Meteorological Society
    Abstract: We examine the relevance to Jupiter's atmosphere of the solitary vortices favored at scales intermediate to those of the quasi-geostrophic (QG) and planetary-geostrophic motions. Horizontal divergence plays a crucial role ...
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