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    A Discontinuous Galerkin Global Shallow Water Model

    Source: Monthly Weather Review:;2005:;volume( 133 ):;issue: 004::page 876
    Author:
    Nair, Ramachandran D.
    ,
    Thomas, Stephen J.
    ,
    Loft, Richard D.
    DOI: 10.1175/MWR2903.1
    Publisher: American Meteorological Society
    Abstract: A discontinuous Galerkin shallow water model on the cubed sphere is developed, thereby extending the transport scheme developed by Nair et al. The continuous flux form nonlinear shallow water equations in curvilinear coordinates are employed. The spatial discretization employs a modal basis set consisting of Legendre polynomials. Fluxes along the element boundaries (internal interfaces) are approximated by a Lax?Friedrichs scheme. A third-order total variation diminishing Runge?Kutta scheme is applied for time integration, without any filter or limiter. Numerical results are reported for the standard shallow water test suite. The numerical solutions are very accurate, there are no spurious oscillations in test case 5, and the model conserves mass to machine precision. Although the scheme does not formally conserve global invariants such as total energy and potential enstrophy, conservation of these quantities is better preserved than in existing finite-volume models.
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      A Discontinuous Galerkin Global Shallow Water Model

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4228898
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    contributor authorNair, Ramachandran D.
    contributor authorThomas, Stephen J.
    contributor authorLoft, Richard D.
    date accessioned2017-06-09T17:26:50Z
    date available2017-06-09T17:26:50Z
    date copyright2005/04/01
    date issued2005
    identifier issn0027-0644
    identifier otherams-85450.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4228898
    description abstractA discontinuous Galerkin shallow water model on the cubed sphere is developed, thereby extending the transport scheme developed by Nair et al. The continuous flux form nonlinear shallow water equations in curvilinear coordinates are employed. The spatial discretization employs a modal basis set consisting of Legendre polynomials. Fluxes along the element boundaries (internal interfaces) are approximated by a Lax?Friedrichs scheme. A third-order total variation diminishing Runge?Kutta scheme is applied for time integration, without any filter or limiter. Numerical results are reported for the standard shallow water test suite. The numerical solutions are very accurate, there are no spurious oscillations in test case 5, and the model conserves mass to machine precision. Although the scheme does not formally conserve global invariants such as total energy and potential enstrophy, conservation of these quantities is better preserved than in existing finite-volume models.
    publisherAmerican Meteorological Society
    titleA Discontinuous Galerkin Global Shallow Water Model
    typeJournal Paper
    journal volume133
    journal issue4
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR2903.1
    journal fristpage876
    journal lastpage888
    treeMonthly Weather Review:;2005:;volume( 133 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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