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    Comments “On the Use of the DuFort-Frankel Finite-Difference Approximation for Simulation of Diffusion in Geophysical Fluids” 

    Source: Journal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 004:;page 658
    Author(s): O'Brien, James J.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    The Non-Linear Response of a Two-Layer, Baroclinic Ocean to a Stationary, Axially-Symmetric Hurricane. Part II. Upwelling and Mixing Induced by Momentum Transfer 

    Source: Journal of the Atmospheric Sciences:;1967:;Volume( 024 ):;issue: 002:;page 208
    Author(s): O'Brien, James J.
    Publisher: American Meteorological Society
    Abstract: This paper is a continuation of a theoretical description of upwelling and mixing induced in a stratified, rotating, two-layer ocean by momentum transfer from an intense, stationary, axially-symmetric atmospheric vortex. ...
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    Comments on “The Over-Relaxation Factor in the Numerical Solution of the Omega Equation” 

    Source: Monthly Weather Review:;1968:;volume( 096 ):;issue: 002:;page 99
    Author(s): O'BRIEN, JAMES J.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available.
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    Alternative Solutions to the Classical Vertical Velocity Problem 

    Source: Journal of Applied Meteorology:;1970:;volume( 009 ):;issue: 002:;page 197
    Author(s): O'Brien, James J.
    Publisher: American Meteorological Society
    Abstract: The kinematic method for determining vertical velocity ? in pressure coordinates is reviewed. Alternative objective procedures are derived for obtaining ?, and an analytical solution to the pressure-differentiated continuity ...
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    Comment “On the Presentation and Interpretation of Spectra of Large–Scale Disturbances” 

    Source: Monthly Weather Review:;1978:;volume( 106 ):;issue: 008:;page 1204
    Author(s): O'Brien, James J.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    A Note on the Vertical Structure of the Eddy Exchange Coefficient in the Planetary Boundary Layer 

    Source: Journal of the Atmospheric Sciences:;1970:;Volume( 027 ):;issue: 008:;page 1213
    Author(s): O'Brien, James J.
    Publisher: American Meteorological Society
    Abstract: No abstract available
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    On the Initial Condition in Parameter Estimation 

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 011:;page 1361
    Author(s): Yu, Lisan; O'Brien, James J.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    The Non-Linear Response of a Two-Layer, Baroclinic Ocean to a Stationary, Axially-Symmetric Hurricane: Part I. Upwelling Induced by Momentum Transfer 

    Source: Journal of the Atmospheric Sciences:;1967:;Volume( 024 ):;issue: 002:;page 197
    Author(s): O'Brien, James J.; Reid, Robert O.
    Publisher: American Meteorological Society
    Abstract: This study is concerned with the theoretical description of upwelling induced in a stratified, rotating, two-layer ocean by momentum transfer from an intense stationary, axially-symmetric atmospheric vortex. The dynamic ...
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    A Numerical Model of Coastal Upwelling 

    Source: Journal of Physical Oceanography:;1972:;Volume( 002 ):;issue: 001:;page 14
    Author(s): O'Brien, James J.; Hurlburt, H. E.
    Publisher: American Meteorological Society
    Abstract: A wind-driven model of coastal upwelling induced into a stratified, rotating ocean is solved numerically. The circulation is on an f plane and longshore variations are neglected. A multilevel model is derived, but only ...
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    On Upwelling Along a Zonally-Orientated Coastline 

    Source: Journal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 001:;page 125
    Author(s): Kindle, John C.; O'Brien, James J.
    Publisher: American Meteorological Society
    Abstract: A common observation in major coastal upwelling regions is a reversal of the mean longshore current with depth during active upwelling. A numerical model and a simple analytical model applied to a two-layer ocean on a ...
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