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    The Nonlinear Forcing of Large-Scale Internal Gravity Waves by Stratified Shear Instability 

    Source: Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 005:;page 653
    Author(s): Scinocca, J. F.; Ford, R.
    Publisher: American Meteorological Society
    Abstract: The forcing of large-scale internal gravity waves by shear-unstable stratified free shear layers is investigated. The gravity wave forcing mechanism considered arises from the nonlinear interaction of unstable modes of ...
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    Secondary Cyclogenesis—Comparison of Observations and Theory 

    Source: Monthly Weather Review:;1990:;volume( 118 ):;issue: 002:;page 427
    Author(s): Ford, R. Paul; Moore, G. W. Kent
    Publisher: American Meteorological Society
    Abstract: A case study of a small-scale polar front cyclone observed during the Canadian Atlantic Storms Program (CASP) is presented. The cyclone forms along an essentially two-dimensional front, which is in approximate thermal wind ...
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    A Nonhydrostatic Finite-Element Model for Three-Dimensional Stratified Oceanic Flows. Part II: Model Validation 

    Source: Monthly Weather Review:;2004:;volume( 132 ):;issue: 012:;page 2832
    Author(s): Ford, R.; Pain, C. C.; Piggott, M. D.; Goddard, A. J. H.; de Oliveira, C. R. E.; Umpleby, A. P.
    Publisher: American Meteorological Society
    Abstract: A three-dimensional nonhydrostatic ocean model that utilizes finite-element discretizations on structured or unstructured meshes has been formulated. In the current part of this work a first step in the validation of this ...
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    A Nonhydrostatic Finite-Element Model for Three-Dimensional Stratified Oceanic Flows. Part I: Model Formulation 

    Source: Monthly Weather Review:;2004:;volume( 132 ):;issue: 012:;page 2816
    Author(s): Ford, R.; Pain, C. C.; Piggott, M. D.; Goddard, A. J. H.; de Oliveira, C. R. E.; Umpleby, A. P.
    Publisher: American Meteorological Society
    Abstract: The vast majority of advanced numerical ocean models in use today, while performing extremely well, especially for certain classes of problem, do not necessarily take full advantage of current trends in numerical analysis ...
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