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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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    Upwelling Circulation on the Oregon Continental Shelf. Part II: Simulations and Comparisons with Observations 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 008:;page 1867
    Author(s): Federiuk, J.; Allen, J. S.
    Publisher: American Meteorological Society
    Abstract: Sixty-day simulations of flow on the Oregon continental shelf are performed using the Blumberg and Mellor sigma coordinate, primitive equation model. The model is two-dimensional (an across-shelf section) with high spatial ...
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    Upwelling Circulation on the Oregon Continental Shelf. Part I: Response to Idealized Forcing 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 008:;page 1843
    Author(s): Allen, J. S.; Newberger, P. A.; Federiuk, J.
    Publisher: American Meteorological Society
    Abstract: Time-dependent upwelling on the Oregon continental shelf is studied with a two-dimensional approximation, that is, spatial variations across-shelf and with depth, using the Blumberg?Mellor, finite-difference, stratified, ...
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