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    Modelling the Mean Barotropic Circulation in the Bay of Fundy and Gulf of Maine 

    Source: Journal of Physical Oceanography:;1983:;Volume( 013 ):;issue: 005:;page 886
    Author(s): Greenberg, David A.
    Publisher: American Meteorological Society
    Abstract: Two dimensional, nonlinear numerical models are used to study the residual barotropic circulation generated by tides and steady winds in the Bay of Fundy and Gulf of Maine. The first a multi-grid model, is used to examine ...
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    A Diagnostic Finite-Element Ocean Circulation Model in Spherical-Polar Coordinates 

    Source: Journal of Atmospheric and Oceanic Technology:;1998:;volume( 015 ):;issue: 004:;page 942
    Author(s): Greenberg, David A.; Werner, Francisco E.; Lynch, Daniel R.
    Publisher: American Meteorological Society
    Abstract: A spherical-polar 3D, harmonic-in-time, linear finite-element ocean circulation model that allows for spatially arbitrary forcing by winds, density field, and imposed free-surface elevation along open boundaries is presented. ...
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    The Steady-State Barotropic Response of the Gulf of Maine and Adjacent Regions to Surface Wind Stress 

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 005:;page 947
    Author(s): Wright, Daniel G.; Greenberg, David A.; Loder, John W.; Smith, Peter C.
    Publisher: American Meteorological Society
    Abstract: The response of the Gulf of Maine region to steady, spatially uniform wind stress is examined using a linearized numerical model, with the influence of the strong tidal currents in the region included in the bottom stress ...
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