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    Three-Dimensional Model Simulations of Tides and Buoyancy Currents along the West Coast of Vancouver Island 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 007:;page 1300
    Author(s): Foreman, Michael G. G.; Thomson, Richard E.
    Publisher: American Meteorological Society
    Abstract: A three-dimensional finite element model is used to calculate the barotropic tides and seasonal buoyancy flows off the western and northern coasts of Vancouver Island. The model buoyancy currents and the harmonics of eight ...
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    Considerations in the Calculation of Vertical Velocity in Three-Dimensional Circulation Models 

    Source: Journal of Atmospheric and Oceanic Technology:;2002:;volume( 019 ):;issue: 012:;page 2063
    Author(s): Luettich, Richard A.; Muccino, Julia C.; Foreman, Michael G. G.
    Publisher: American Meteorological Society
    Abstract: The vertical velocity, w, in three-dimensional circulation models is typically computed from the three-dimensional continuity equation given the free-surface elevation and depth-varying horizontal velocity. This problem ...
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    Stratification and Mean Flow Effects on Diurnal Tidal Currents off Vancouver Island 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 001:;page 15
    Author(s): Cummins, Patrick F.; Masson, Diane; Foreman, Michael G. G.
    Publisher: American Meteorological Society
    Abstract: A series of numerical experiments with a three-dimensional, baroclinic model were conducted to study the influences of density stratification and wind-driven currents on the K1 tide over the continental shelf off Vancouver ...
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    Coastal Oyashio South of Hokkaido, Japan 

    Source: Journal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 007:;page 1477
    Author(s): Kono, Tokihiro; Foreman, Michael; Chandler, Peter; Kashiwai, Makoto
    Publisher: American Meteorological Society
    Abstract: Coastal Oyashio Water (COW), the cold low-salinity water lying along the southeast coast of Hokkaido, sometimes flows into Funka Bay on the southwest coast in winter and spring. Because this water is low in density, a ...
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    On the Influence of Random Wind Stress Errors on the Four-Dimensional, Midlatitude Ocean Inverse Problem 

    Source: Monthly Weather Review:;2009:;volume( 137 ):;issue: 006:;page 1844
    Author(s): Wakamatsu, Tsuyoshi; Foreman, Michael G. G.; Cummins, Patrick F.; Cherniawsky, Josef Y.
    Publisher: American Meteorological Society
    Abstract: The effects of the parameterized wind stress error covariance function on the a priori error covariance of an ocean general circulation model (OGCM) are examined. These effects are diagnosed by computing the projection of ...
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