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    Parallel Conservative Scheme for Solving the Shallow-Water Equations 

    Source: Monthly Weather Review:;1993:;volume( 121 ):;issue: 001:;page 305
    Author(s): Neta, B.; Lustman, L.
    Publisher: American Meteorological Society
    Abstract: To improve the simulation of nonlinear aspects of the flow over steep topography, a potential enstrophy-and energy-conserving finite-difference scheme for the shallow-water equations was derived by Arakawa and Lamb. Here ...
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    Influence of Linear Depth Variation on Poincaré, Kelvin, and Rossby Waves 

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 007:;page 929
    Author(s): Staniforth, A. N.; Williams, R. T.; Neta, B.
    Publisher: American Meteorological Society
    Abstract: Exact solutions to the linearized shallow-water equations in a channel with linear depth variation and a mean flow are obtained in terms of confluent hypergeometric functions. These solutions are the generalization to ...
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    A Perfectly Matched Layer Approach to the Linearized Shallow Water Equations Models 

    Source: Monthly Weather Review:;2004:;volume( 132 ):;issue: 006:;page 1369
    Author(s): Navon, I. M.; Neta, B.; Hussaini, M. Y.
    Publisher: American Meteorological Society
    Abstract: A limited-area model of linearized shallow water equations (SWE) on an f plane for a rectangular domain is considered. The rectangular domain is extended to include the so-called perfectly matched layer (PML) as an absorbing ...
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