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    The Dynamics of Low-Frequency Variability in a Simple Model of the Global Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 003:;page 429
    Author(s): Robinson, Walter A.
    Publisher: American Meteorological Society
    Abstract: We examine the dynamics of low-frequency variability in a simple global model with zonally homogeneous boundary conditions. Low-frequency structure comprises trains of nearly equivalent barotropic Rossby waves with weak ...
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    Analysis of LIMS Data by Potential vorticity Inversion 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 016:;page 2319
    Author(s): Robinson, Walter A.
    Publisher: American Meteorological Society
    Abstract: The invertibility of potential vorticity is used to investigate how flows in the middle atmosphere are determined. The distribution of potential vorticity associated with an observed flow is computed. The inversion problem, ...
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    Irreversible Wave–Mean Flow Interactions in a Mechanistic Model of the Stratosphere 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 022:;page 3413
    Author(s): Robinson, Walter A.
    Publisher: American Meteorological Society
    Abstract: A wave-1 minor warming is simulated in a mechanistic, global, primitive equation model. The modification of the zonal flow by the rearrangement of potential vorticity on a middle stratospheric isentrope is compared in a ...
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    Mechanisms of Low-Frequency Variability in a Simple Model with Orography 

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 006:;page 878
    Author(s): Robinson, Walter A.
    Publisher: American Meteorological Society
    Abstract: Mechanisms of low-frequency variability are examined in an extended run of a two-level nonlinear global model with a single isolated mountain. The presence of the mountain modifies the low-frequency behavior, compared with ...
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    Comments on “Horizontal Divergence Associated with Zonally Isolated Jet Streams” 

    Source: Journal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 012:;page 1760
    Author(s): Robinson, Walter A.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Eddy Feedbacks on the Zonal Index and Eddy–Zonal Flow Interactions Induced by Zonal Flow Transience 

    Source: Journal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 017:;page 2553
    Author(s): Robinson, Walter A.
    Publisher: American Meteorological Society
    Abstract: A mechanistic approach is used to determine the nature and frequency dependence of transient eddy feedbacks on zonally symmetric low-frequency variability. The zonal momentum of a simple though fully nonlinear atmospheric ...
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    Two Applications of Potential Vorticity Thinking 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 011:;page 1554
    Author(s): Robinson, Walter A.
    Publisher: American Meteorological Society
    Abstract: Reasoning in terms of potential vorticity provides physical explanations for the dissipative destabilization of external Rossby waves and for the acceleration of the zonal mean jet during baroclinic life cycles. Both ...
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    Does Eddy Feedback Sustain Variability in the Zonal Index? 

    Source: Journal of the Atmospheric Sciences:;1996:;Volume( 053 ):;issue: 023:;page 3556
    Author(s): Robinson, Walter A.
    Publisher: American Meteorological Society
    Abstract: The dynamics of variability in the zonal index are studied using a simple circulation model. Results from simulations with differing drag suggest that variability in the zonal index involves a positive feedback from transient ...
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    A Baroclinic Mechanism for the Eddy Feedback on the Zonal Index 

    Source: Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 003:;page 415
    Author(s): Robinson, Walter A.
    Publisher: American Meteorological Society
    Abstract: A baroclinic mechanism for the positive eddy feedback on the zonal index is proposed. The author considers the quasigeostrophic response of the zonally averaged flow to forcing by baroclinic eddies. The transient response ...
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    On the Self-Maintenance of Midlatitude Jets 

    Source: Journal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 008:;page 2109
    Author(s): Robinson, Walter A.
    Publisher: American Meteorological Society
    Abstract: In this paper an atmospheric jet is considered self-maintaining if the overall effect of baroclinic eddies is to preserve or enhance its westerly shear with height. Observations suggest that the wintertime jets in Earth?s ...
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