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    Open-Ocean Modeling as an Inverse Problem: The Primitive Equations 

    Source: Monthly Weather Review:;1994:;volume( 122 ):;issue: 006:;page 1326
    Author(s): Bennett, Andrew F.; Chua, Boon S.
    Publisher: American Meteorological Society
    Abstract: The ill-posedness of regional primitive equation models is examined, using a regional shallow-water model. The ill-posedness is resolved by reformulation as a least-squares inverse problem, in the sense that the Euler-Lagrange ...
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    Generalized Inverse of a Reduced Gravity Primitive Equation Ocean Model and Tropical Atmosphere–Ocean Data 

    Source: Monthly Weather Review:;2000:;volume( 128 ):;issue: 006:;page 1757
    Author(s): Ngodock, Hans E.; Chua, Boon S.; Bennett, Andrew F.
    Publisher: American Meteorological Society
    Abstract: A nonlinear 2½-layer reduced gravity primitive equations (PE) ocean model is used to assimilate sea surface temperature (SST) data from the Tropical Atmosphere?Ocean (TAO) moored buoys in the tropical Pacific. The aim of ...
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    Generalized Inversion of Tropical Atmosphere–Ocean (TAO) Data and a Coupled Model of the Tropical Pacific. Part II: The 1995–96 La Niña and 1997–98 El Niño 

    Source: Journal of Climate:;2000:;volume( 013 ):;issue: 015:;page 2770
    Author(s): Bennett, Andrew F.; Chua, Boon S.; Harrison, D. Ed; McPhaden, Michael J.
    Publisher: American Meteorological Society
    Abstract: The investigation of the consequences of trying to blend tropical Pacific observations from the Tropical Atmosphere?Ocean (TAO) array into the dynamical framework of an intermediate coupled ocean?atmosphere model is ...
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    Generalized Inversion of Tropical Atmosphere–Ocean Data and a Coupled Model of the Tropical Pacific 

    Source: Journal of Climate:;1998:;volume( 011 ):;issue: 007:;page 1768
    Author(s): Bennett, Andrew F.; Chua, Boon S.; Harrison, D. Ed; McPhaden, Michael J.
    Publisher: American Meteorological Society
    Abstract: It is hypothesized that the circulation of the tropical Pacific Ocean and atmosphere satisfies the equations of a simple coupled model to within errors having specified covariances, and that the Tropical Atmosphere?Ocean ...
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