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    Baroclinic Instability of the Zonal Wind: Part III 

    Source: Journal of the Atmospheric Sciences:;1964:;Volume( 021 ):;issue: 006:;page 603
    Author(s): Miles, John W.
    Publisher: American Meteorological Society
    Abstract: A zonal-wind configuration in which wind speed is proportional to pressure-altitude and stability is proportional to the square of the density is posed. A solution to the eigenvalue problem governing the stability of this ...
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    Baroclinic Instability of the Zonal Wind: Part II 

    Source: Journal of the Atmospheric Sciences:;1964:;Volume( 021 ):;issue: 005:;page 500
    Author(s): Miles, John W.
    Publisher: American Meteorological Society
    Abstract: An approximate solution of the eigenvalue problem governing the stability of the zonal wind with respect to small disturbances of long wavelength is developed for profiles with strong, positive-definite vertical shear. It ...
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    A Note on Charney's Model of Zonal–Wind Instability 

    Source: Journal of the Atmospheric Sciences:;1964:;Volume( 021 ):;issue: 004:;page 451
    Author(s): Miles, John W.
    Publisher: American Meteorological Society
    Abstract: Abstract not available.
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    On Tidal Damping in Laplace's Global Ocean 

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 002:;page 377
    Author(s): Miles, John W.
    Publisher: American Meteorological Society
    Abstract: Laplace's tidal equations are augmented by dissipation in a bottom boundary layer that is intermediate in character between those of Ekman and Stokes. Laplace's tidal equation for a global ocean remains second-order and ...
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    Comments on “Stratified Flow Over Extended Obstacles and its Application to Topographical Effect on Vertical Wind Shear” 

    Source: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 004:;page 772
    Author(s): Miles, John W.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    On Solitary Rossby Waves 

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 007:;page 1236
    Author(s): Miles, John W.
    Publisher: American Meteorological Society
    Abstract: A variational principle and an associated integral invariant are constructed for two-dimensional (non-divergent) waves of permanent form in a Rossby ?-plane. A solitary-wave solution is obtained, and it is shown that the ...
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    Solitary Wave Evolution Over a Gradual Slope with Turbulent Friction 

    Source: Journal of Physical Oceanography:;1983:;Volume( 013 ):;issue: 003:;page 551
    Author(s): Miles, John W.
    Publisher: American Meteorological Society
    Abstract: A solitary wave of amplitude a evolving in water of depth d over a bottom of gradual slope δ and turbulent friction coefficient Cf is found to have the asymptotic (as d ?0) relative amplitude a/d = α1 = 15α/4Cf α1<αb where ...
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