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    Why Western Boundary Currents in Realistic Oceans are Inviscid: A Link between Form Stress and Bottom Pressure Torques 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 010:;page 2871
    Author(s): Hughes, Chris W.; de Cuevas, Beverly A.
    Publisher: American Meteorological Society
    Abstract: It is shown that wind stress curl is balanced by bottom pressure torque in a zonal integral over any strip wide enough to smooth out the effect of nonlinear terms (typically about 3° of latitude). The derivation is completely ...
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    The Region of Large Sea Surface Height Variability in the Southeast Pacific Ocean 

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 005:;page 1044
    Author(s): Webb, David J.; de Cuevas, Beverly A.
    Publisher: American Meteorological Society
    Abstract: Satellite altimeter observations of sea surface height (SSH) show an extensive triangular region of high variability in the southeastern Pacific. The region is unusual in two ways. First, it appears to have a horizontal ...
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    Improved Advection Schemes for Ocean Models 

    Source: Journal of Atmospheric and Oceanic Technology:;1998:;volume( 015 ):;issue: 005:;page 1171
    Author(s): Webb, David J.; de Cuevas, Beverly A.; Richmond, Catherine S.
    Publisher: American Meteorological Society
    Abstract: Leonard?s widely used QUICK advection scheme is, like the Bryan?Cox?Semtner ocean model, based on a control volume form of the advection equation. Unfortunately, in its normal form it cannot be used with the leapfrog?Euler ...
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    Effective Eddy Diffusivities Inferred from a Point Release Tracer in an Eddy-Resolving Ocean Model 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 004:;page 894
    Author(s): Lee, Mei-Man; Nurser, A. J. George; Coward, Andrew C.; de Cuevas, Beverly A.
    Publisher: American Meteorological Society
    Abstract: This study uses tracer experiments in a global eddy-resolving ocean model to examine two diagnostic methods for inferring effective eddy isopycnic diffusivity from point release tracers. The first method is based on the ...
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    Comments on “Decadal Changes in the North Atlantic and Pacific Meridional Overturning Circulation and Heat Flux” 

    Source: Journal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 009:;page 2104
    Author(s): Saunders, Peter M.; Cunningham, Stuart A.; de Cuevas, Beverly A.; Coward, Andrew C.
    Publisher: American Meteorological Society
    Abstract: It is demonstrated that current level models, both with and without assimilation, generate too shallow an overturning in the North Atlantic (just like their predecessors) because they do not reproduce the descent of plumes ...
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    A Model Analysis of the Behavior of the Mediterranean Water in the North Atlantic 

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 003:;page 764
    Author(s): Jia, Yanli; Coward, Andrew C.; de Cuevas, Beverly A.; Webb, David J.; Drijfhout, Sybren S.
    Publisher: American Meteorological Society
    Abstract: The behavior of the Mediterranean Water in the North Atlantic Ocean sector of a global ocean general circulation model is explored, starting from its entry point at the Strait of Gibraltar. The analysis focuses primarily ...
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    A Multiprocessor Ocean General Circulation Model Using Message Passing 

    Source: Journal of Atmospheric and Oceanic Technology:;1997:;volume( 014 ):;issue: 001:;page 175
    Author(s): Webb, David J.; Coward, Andrew C.; de Cuevas, Beverly A.; Gwilliam, Catherine S.
    Publisher: American Meteorological Society
    Abstract: Numerical models of the ocean are widely used to study the physics, chemistry, and biology of the ocean and its effect on climate. Unfortunately limits in available computer power often restrict the length of model runs ...
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