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    Semigeostrophic Theory 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 016:;page 1770
    Author(s): Schubert, Wayne H.
    Publisher: American Meteorological Society
    Abstract: The geopotential tendency form of semigeostrophic theory is derived and compared with the potential vorticity form. The tendency form is compact and particularly convenient for non-Boussinesq, nonuniform potential vorticity flows.
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    Experiments with Lilly's Cloud-Topped Mixed Layer Model 

    Source: Journal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 003:;page 436
    Author(s): Schubert, Wayne H.
    Publisher: American Meteorological Society
    Abstract: Lilly's model of a horizontally homogeneous cloud-topped mixed layer is studied. The model is closed by taking a weighted (weighting factor or entrainment parameter k) average of Lilly's maximum and minimum entrainment ...
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    EDITORIAL 

    Source: Monthly Weather Review:;1999:;volume( 127 ):;issue: 001:;page 3
    Author(s): Schubert, Wayne H.
    Publisher: American Meteorological Society
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    Procedures Governing Peer Review in AMS Journals 

    Source: Journal of the Atmospheric Sciences:;1999:;Volume( 056 ):;issue: 001:;page 3
    Author(s): Schubert, Wayne H.
    Publisher: American Meteorological Society
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    Procedures Governing Peer Review in AMS Journals 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 001:;page 3
    Author(s): Schubert, Wayne H.
    Publisher: American Meteorological Society
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    Semigeostrophic Theory on the Hemisphere 

    Source: Journal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 012:;page 1449
    Author(s): Magnusdottir, Gudrun; Schubert, Wayne H.
    Publisher: American Meteorological Society
    Abstract: This paper presents the combined isentropic and spherical geostrophic coordinate version of semigeostrophic theory. This is accomplished by first proposing a spherical coordinate generalization of the geostrophic momentum ...
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    Vorticity Coordinates, Transformed Primitive Equations, and a Canonical Form for Balanced Models 

    Source: Journal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 022:;page 3309
    Author(s): Schubert, Wayne H.; Magnusdottir, Gudrun
    Publisher: American Meteorological Society
    Abstract: A potential pseudodensity principle is derived for the quasi-static primitive equations on the sphere. An important step in the derivation of this principle is the introduction of ?vorticity coordinates??that is, new ...
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    Analytical Predictions for Zonally Symmetric Equilibrium States of the Stratospheric Polar Vortex 

    Source: Journal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 018:;page 2709
    Author(s): Prieto, Ricardo; Schubert, Wayne H.
    Publisher: American Meteorological Society
    Abstract: Equilibrium states of initially barotropically unstable polar vortices are predicted using two different approaches: minimum enstrophy and maximum entropy theories, which have been extended to include flows evolving on the ...
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    The Generalization of Semigeostrophic Theory to the β-Plane 

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 014:;page 1714
    Author(s): Magnusdottir, Gudrun; Schubert, Wayne H.
    Publisher: American Meteorological Society
    Abstract: We develop here the isentropic?geostrophic coordinate version of semigeostrophic theory on a midlatitude ?-plane. This approach results in a simple mathematical form in which the horizontal ageostrophic velocities are ...
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    Publication Trends in American Meteorological Society Technical Journals 

    Source: Bulletin of the American Meteorological Society:;1989:;volume( 070 ):;issue: 005:;page 476
    Author(s): Johnson, Richard H.; Schubert, Wayne H.
    Publisher: American Meteorological Society
    Abstract: Some statistical measures of growth of American Meteorological Society technical journals have been compiled. A general upward trend in total number of articles, pages, and an increase (nearly doubling during the past 20 ...
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