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    Mechanisms and Parameterizations of Geostrophic Adjustment and a Variational Approach to Balanced Flow 

    Source: Journal of the Atmospheric Sciences:;1992:;Volume( 049 ):;issue: 013:;page 1144
    Author(s): Vallis, Geoffrey K.
    Publisher: American Meteorological Society
    Abstract: Geostrophic balance is shown to be the minimum energy state, for a given linear potential vorticity field, for small deviations of the height field around a resting state, in the shallow-water equations. This includes (but ...
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    On the Spectral Integration of the Quasi-Geostrophic Equations for Doubly-Periodic and Channel Flow 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 001:;page 95
    Author(s): Vallis, Geoffrey K.
    Publisher: American Meteorological Society
    Abstract: The spectral integration of the quasi-geostrophic equations is reexamined for simple boundary conditions in Cartesian geometry. For doubly-periodic flow, it is shown that the mean shear must be constant in time or its ...
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    On the Predictability of Quasi-Geostrophic Flow: The Effects of Beta and Baroclinicity 

    Source: Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 001:;page 10
    Author(s): Vallis, Geoffrey K.
    Publisher: American Meteorological Society
    Abstract: The equilibrium statistics and predictability properties of one- and two-layer quasi-geostrophic flow are examined with the aid of a numerical model. The effect of beta in one-layer flow is to slow the transfer of energy ...
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    Large-Scale Circulation and Production of Stratification: Effects of Wind, Geometry, and Diffusion 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 005:;page 933
    Author(s): Vallis, Geoffrey K.
    Publisher: American Meteorological Society
    Abstract: The combined effects of wind, geometry, and diffusion on the stratification and circulation of the ocean are explored by numerical and analytical methods. In particular, the production of deep stratification in a simply ...
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    Correlation Dimensions of Primitive Equation and Balanced Models 

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 015:;page 2556
    Author(s): Sundermeyer, Miles; Vallis, Geoffrey K.
    Publisher: American Meteorological Society
    Abstract: Low-order primitive equation and balanced models are compared by evaluating the correlation dimension of each over a range of Rossby numbers. The models are the nine-component primitive equation model of Lorenz and the ...
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    The Role of Bottom Vortex Stretching on the Path of the North Atlantic Western Boundary Current and on the Northern Recirculation Gyre 

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 008:;page 2053
    Author(s): Zhang, Rong; Vallis, Geoffrey K.
    Publisher: American Meteorological Society
    Abstract: The mechanisms affecting the path of the depth-integrated North Atlantic western boundary current and the formation of the northern recirculation gyre are investigated using a hierarchy of models, namely, a robust diagnostic ...
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    Ocean Heat Uptake in Eddying and Non-Eddying Ocean Circulation Models in a Warming Climate 

    Source: Journal of Physical Oceanography:;2013:;Volume( 043 ):;issue: 010:;page 2211
    Author(s): Zhang, Yu; Vallis, Geoffrey K.
    Publisher: American Meteorological Society
    Abstract: cean heat uptake is explored with non-eddying (2°), eddy-permitting (0.25°), and eddy-resolving (0.125°) ocean circulation models in a domain representing the Atlantic basin connected to a southern circumpolar channel with ...
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    Meridional Energy Transport in the Coupled Atmosphere–Ocean System: Compensation and Partitioning 

    Source: Journal of Climate:;2013:;volume( 026 ):;issue: 018:;page 7151
    Author(s): Farneti, Riccardo; Vallis, Geoffrey K.
    Publisher: American Meteorological Society
    Abstract: he variability and compensation of the meridional energy transport in the atmosphere and ocean are examined with the state-of-the-art GFDL Climate Model, version 2.1 (CM2.1), and the GFDL Intermediate Complexity Coupled ...
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    Impact of Great Salinity Anomalies on the Low-Frequency Variability of the North Atlantic Climate 

    Source: Journal of Climate:;2006:;volume( 019 ):;issue: 003:;page 470
    Author(s): Zhang, Rong; Vallis, Geoffrey K.
    Publisher: American Meteorological Society
    Abstract: In this paper, it is shown that coherent large-scale low-frequency variabilities in the North Atlantic Ocean?that is, the variations of thermohaline circulation, deep western boundary current, northern recirculation gyre, ...
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    The Role of Criticality on the Horizontal and Vertical Scales of Extratropical Eddies in a Dry GCM 

    Source: Journal of the Atmospheric Sciences:;2014:;Volume( 071 ):;issue: 007:;page 2300
    Author(s): Chai, Junyi; Vallis, Geoffrey K.
    Publisher: American Meteorological Society
    Abstract: his paper discusses the sensitivity of the horizontal and vertical scales of extratropical eddies when criticality is varied in a dry, primitive-equation, general circulation model. Criticality is a measure of extratropical ...
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