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    Irregular Grid Finite-Difference Techniques: Simulations of Oscillations in Shallow Circular Basins 

    Source: Journal of Physical Oceanography:;1977:;Volume( 007 ):;issue: 002:;page 284
    Author(s): Thacker, W. C.
    Publisher: American Meteorological Society
    Abstract: Finite-difference techniques for irregular computational grids are presented. Successful simulations of transient normal mode oscillations in shallow circular basins, where analytic solutions are known, demonstrate that ...
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    Source: Journal of Physical Oceanography:;1977:;Volume( 007 ):;issue: 006:;page 933
    Author(s): Thacker, W. C.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Comparison of Finite-Element and Finite-Difference Schemes. Part II: Two-Dimensional Gravity Wave Motion 

    Source: Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 004:;page 680
    Author(s): Thacker, W. C.
    Publisher: American Meteorological Society
    Abstract: Irregular grid finite-difference techniques lead to equations similar to those obtained using finite-element techniques. The simpler finite-difference equations offer the advantage of greater computational economy. The ...
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    Comparison of Finite-Element and Finite-Difference Schemes. Part I: One-Dimensional Gravity Wave Motion 

    Source: Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 004:;page 676
    Author(s): Thacker, W. C.
    Publisher: American Meteorological Society
    Abstract: The finite-element scheme requires more computational expense because it is time-implicit and because it requires a smaller time step than the finite-difference scheme. Simulations of normal mode oscillations reveal that ...
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    Estimating Salinity between 25° and 45°S in the Atlantic Ocean Using Local Regression 

    Source: Journal of Atmospheric and Oceanic Technology:;2008:;volume( 025 ):;issue: 001:;page 114
    Author(s): Thacker, W. C.
    Publisher: American Meteorological Society
    Abstract: The empirical relationship between salinity and temperature in the South Atlantic is quantified with the aid of local regression. To capture the spatial character of the TS relationship, models are fitted to data for each ...
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    A Solvable Model of “Shear Dispersion” 

    Source: Journal of Physical Oceanography:;1976:;Volume( 006 ):;issue: 001:;page 66
    Author(s): Thacker, W. C.
    Publisher: American Meteorological Society
    Abstract: Shear dispersion results from vertical shear of horizontal velocity and vertical mixing, features which cannot be included explicitly in one-layer, vertically integrated models. The parametric description of shear dispersion ...
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    Climatic Fingerprints, Patterns, and Indices 

    Source: Journal of Climate:;1996:;volume( 009 ):;issue: 009:;page 2259
    Author(s): Thacker, W. C.
    Publisher: American Meteorological Society
    Abstract: The purpose of this note is to point out that Hasselmann's optimal fingerprints for detecting climatic change follow from the geometrical interpretation of covariance as an inner product.
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    Climatic Indices, Principal Components, and the Gauss-Markov Theorem 

    Source: Journal of Climate:;1996:;volume( 009 ):;issue: 008:;page 1942
    Author(s): Thacker, W. C.; Lewandowicz, R.
    Publisher: American Meteorological Society
    Abstract: If indices are to be used as the variables predicted by linear statistical models, it is important to be able to recover as much local information as possible from the values forecast for the indices. Here it is shown that ...
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