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    Rossby Wave Frequencies and Group Velocities for Finite Element and Finite Difference Approximations to the Vorticity-Divergence and the Primitive Forms of the Shallow Water Equations

    Source: Monthly Weather Review:;1989:;volume( 117 ):;issue: 007::page 1439
    Author:
    Neta, Beny
    ,
    Williams, R. T.
    DOI: 10.1175/1520-0493(1989)117<1439:RWFAGV>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In this paper Rossby wave frequencies and group velocities are analyzed for various finite element and finite difference approximations to the vorticity-divergence form of the shallow water equations. Also included are finite difference solutions for the primitive equations for the staggered grids B and C from Wajsowicz and for the unstaggered grid A. The results are presented for three ratios between the grid size and the Rossby radius of deformation. The Yortcity-divergence equation schemes give superior solutions to those based on the primitive equations. The best results come from the finite element schemes that use linear basis functions on isosceles triangles and bilinear functions on rectangles. All of the primitive equation finite difference schemes have problems for at least one Rossby deformation-grid size ratio.
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      Rossby Wave Frequencies and Group Velocities for Finite Element and Finite Difference Approximations to the Vorticity-Divergence and the Primitive Forms of the Shallow Water Equations

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4202230
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    • Monthly Weather Review

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    contributor authorNeta, Beny
    contributor authorWilliams, R. T.
    date accessioned2017-06-09T16:07:24Z
    date available2017-06-09T16:07:24Z
    date copyright1989/07/01
    date issued1989
    identifier issn0027-0644
    identifier otherams-61448.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4202230
    description abstractIn this paper Rossby wave frequencies and group velocities are analyzed for various finite element and finite difference approximations to the vorticity-divergence form of the shallow water equations. Also included are finite difference solutions for the primitive equations for the staggered grids B and C from Wajsowicz and for the unstaggered grid A. The results are presented for three ratios between the grid size and the Rossby radius of deformation. The Yortcity-divergence equation schemes give superior solutions to those based on the primitive equations. The best results come from the finite element schemes that use linear basis functions on isosceles triangles and bilinear functions on rectangles. All of the primitive equation finite difference schemes have problems for at least one Rossby deformation-grid size ratio.
    publisherAmerican Meteorological Society
    titleRossby Wave Frequencies and Group Velocities for Finite Element and Finite Difference Approximations to the Vorticity-Divergence and the Primitive Forms of the Shallow Water Equations
    typeJournal Paper
    journal volume117
    journal issue7
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1989)117<1439:RWFAGV>2.0.CO;2
    journal fristpage1439
    journal lastpage1457
    treeMonthly Weather Review:;1989:;volume( 117 ):;issue: 007
    contenttypeFulltext
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