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    An Optimal-Control/Adjoint-Equations Approach to Studying the Oceanic General Circulation 

    Source: Journal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 010:;page 1471
    Author(s): Tziperman, Eli; Thacker, William Carlisle
    Publisher: American Meteorological Society
    Abstract: An efficient procedure is presented for analyzing oceanographic observations with the aid of a general circulation model. Poorly known model parameters, such as eddy-mixing coefficients, surface forcing and tracer boundary ...
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    Assimilating XBT Data into HYCOM 

    Source: Journal of Atmospheric and Oceanic Technology:;2002:;volume( 019 ):;issue: 005:;page 709
    Author(s): Thacker, William Carlisle; Esenkov, Oleg Evgenievich
    Publisher: American Meteorological Society
    Abstract: A scheme is presented for assimilating expendable bathythermographic data into HYCOM, an oceanic circulation model featuring a hybrid vertical coordinate. The scheme is fully multivariate, using observations of temperature ...
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    Oceanic Data Analysis Using a General Circulation Model. Part I: Simulations 

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 012:;page 1434
    Author(s): Tziperman, Eli; Thacker, William Carlisle; Long, Robert Bryan; Hwang, Show-Ming
    Publisher: American Meteorological Society
    Abstract: This paper deals with the solution of inverse problems involving complex numerical models of the oceanic general circulation and large datasets. The goal of these inverse problems is to find values for model inputs consistent ...
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    Oceanic Data Analysis Using a General Circulation Model. Part II: A North Atlantic Model 

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 012:;page 1458
    Author(s): Tziperman, Eli; Thacker, William Carlisle; Long, Robert Bryan; Hwang, Show-Ming; Rintoul, Stephen R.
    Publisher: American Meteorological Society
    Abstract: A general circulation model and North Atlantic climatological data of temperature salinity, wind stress, evaporation minus precipitation, and air?sea heat fluxes are used to examine the possibility of solving inverse ...
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