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    On Janssen’s Model for Surface Wave Generation by a Gusty Wind 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 004:;page 592
    Author(s): Miles, John
    Publisher: American Meteorological Society
    Abstract: Janssen?s model for the effect of gustiness on the mean energy transfer from a turbulent wind to a surface wave is simplified through a Gauss?Hermite approximation to his probability integral. Two examples are considered.
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    On Damped Resonant Interactions 

    Source: Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 010:;page 1677
    Author(s): Miles, John
    Publisher: American Meteorological Society
    Abstract: It is shown that the evolution equations for a triad of weakly damped, resonantly interacting waves are isomorphic to the corresponding equations for undamped waves (and therefore may be integrated in term of elliptic ...
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    Resonantly Forced Rossby Waves 

    Source: Journal of Physical Oceanography:;1985:;Volume( 015 ):;issue: 004:;page 467
    Author(s): Miles, John
    Publisher: American Meteorological Society
    Abstract: A shallow, rotating layer of fluid that supports Rossby waves is subjected to turbulent friction through an Ekman layer at the bottom and is driven by a wave that exerts a shear stress on the upper boundary and for which ...
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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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    Gravity Wave Reflection at a Discontinuity in Bottom Slope 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 008:;page 1870
    Author(s): Miles, John; Zou, Qingping
    Publisher: American Meteorological Society
    Abstract: The one-dimensional reflection of a gravity wave at a discontinuity in bottom slope is calculated from a Green?Liouville (WKB) solution of the mild-slope equation.
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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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