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    Balance Equations Based on Momentum Equations with Global Invariants of Potential Enstrophy and Energy 

    Source: Journal of Physical Oceanography:;1991:;Volume( 021 ):;issue: 002:;page 265
    Author(s): Allen, J. S.
    Publisher: American Meteorological Society
    Abstract: An approximate model for small Rossby number ? that is close to the balance equations (BE) but that is based on approximate momentum equations is formulated for a rotating, continuously stratified fluid governed by the ...
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    Upwelling and Coastal Jets in a Continuously Stratified Ocean 

    Source: Journal of Physical Oceanography:;1973:;Volume( 003 ):;issue: 003:;page 245
    Author(s): Allen, J. S.
    Publisher: American Meteorological Society
    Abstract: A simple, linear, two-dimensional, f-plane model of coastal upwelling in a continuously stratified ocean is investigated. The transient response of the fluid to an impulsively applied alongshore wind stress, the nature of ...
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    Reply 

    Source: Journal of Physical Oceanography:;1975:;Volume( 005 ):;issue: 004:;page 774
    Author(s): Allen, J. S.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Coastal Trapped Waves in a Stratified Ocean 

    Source: Journal of Physical Oceanography:;1975:;Volume( 005 ):;issue: 002:;page 300
    Author(s): Allen, J. S.
    Publisher: American Meteorological Society
    Abstract: A two-layer model is used to study the properties of free coastal trapped waves which propagate over an idealized continental shelf and continental slope bottom topography. With both stratification and depth variations ...
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    Iterated Geostrophic Intermediate Models 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 011:;page 2447
    Author(s): Allen, J. S.
    Publisher: American Meteorological Society
    Abstract: Intermediate models contain physics between that in the primitive equations and that in the quasigeostrophic equations and are capable of representing subinertial frequency motion over O(1) topographic variations typical ...
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    A Simple Model for Stratified Shelf Flow Fields with Bottom Friction 

    Source: Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 007:;page 1200
    Author(s): Allen, J. S.
    Publisher: American Meteorological Society
    Abstract: The effect of bottom friction on the subinertial frequency motion of stratified shelf flow fields is studied in a two-layer f-plane model with idealized shelf and slope bottom topography. Coastal-trapped fire waves and ...
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    Continental Shelf Waves and Alongshore Variations in Bottom Topography and Coastline 

    Source: Journal of Physical Oceanography:;1976:;Volume( 006 ):;issue: 006:;page 864
    Author(s): Allen, J. S.
    Publisher: American Meteorological Society
    Abstract: The effects of alongshore variations in bottom topography and coastline on the wind-stress-forced barotropic motion over a continental shelf and slope are studied. Perturbation methods are used to obtain solutions for ...
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    Some Aspects of the Forced Wave Response of Stratified Coastal Regions 

    Source: Journal of Physical Oceanography:;1976:;Volume( 006 ):;issue: 001:;page 113
    Author(s): Allen, J. S.
    Publisher: American Meteorological Society
    Abstract: A two-layer model with an idealized continental shelf and slope bottom topography is utilized to study some properties of the response of stratified coastal regions to meteorological forcing with variations in the alongshore ...
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    On Forced, Long Continental Shelf Waves On an f-Planc 

    Source: Journal of Physical Oceanography:;1976:;Volume( 006 ):;issue: 004:;page 426
    Author(s): Allen, J. S.
    Publisher: American Meteorological Society
    Abstract: Previous studies of forced, long continental shelf waves on an f-plane have considered motion on the shelf and slope which is driven by an alongshore component of the wind stress, essentially through the suction of fluid ...
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    Model Studies of Near-Inertial Waves in Flow over the Oregon Continental Shelf 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 010:;page 2053
    Author(s): Federiuk, J.; Allen, J. S.
    Publisher: American Meteorological Society
    Abstract: Two-dimensional, primitive equation model studies of wind-forced flow over a continental shelf Show that, under upwelling conditions, high levels of near-inertial wave energy are found in the interior over the shelf. The ...
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