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    Analysis of Discrete Shallow-Water Models on Geodesic Delaunay Grids with C-Type Staggering

    Source: Monthly Weather Review:;2005:;volume( 133 ):;issue: 008::page 2351
    Author:
    Bonaventura, Luca
    ,
    Ringler, Todd
    DOI: 10.1175/MWR2986.1
    Publisher: American Meteorological Society
    Abstract: The properties of C-grid staggered spatial discretizations of the shallow-water equations on regular Delaunay triangulations on the sphere are analyzed. Mass-conserving schemes that also conserve either energy or potential enstrophy are derived, and their features are analogous to those of the C-grid staggered schemes on quadrilateral grids. Results of numerical tests carried out with explicit and semi-implicit time discretizations show that the potential-enstrophy-conserving scheme is able to reproduce correctly the main features of large-scale atmospheric motion and that power spectra for energy and potential enstrophy obtained in long model integrations display a qualitative behavior similar to that predicted by the decaying turbulence theory for the continuous system.
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      Analysis of Discrete Shallow-Water Models on Geodesic Delaunay Grids with C-Type Staggering

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4228991
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    contributor authorBonaventura, Luca
    contributor authorRingler, Todd
    date accessioned2017-06-09T17:27:13Z
    date available2017-06-09T17:27:13Z
    date copyright2005/08/01
    date issued2005
    identifier issn0027-0644
    identifier otherams-85533.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4228991
    description abstractThe properties of C-grid staggered spatial discretizations of the shallow-water equations on regular Delaunay triangulations on the sphere are analyzed. Mass-conserving schemes that also conserve either energy or potential enstrophy are derived, and their features are analogous to those of the C-grid staggered schemes on quadrilateral grids. Results of numerical tests carried out with explicit and semi-implicit time discretizations show that the potential-enstrophy-conserving scheme is able to reproduce correctly the main features of large-scale atmospheric motion and that power spectra for energy and potential enstrophy obtained in long model integrations display a qualitative behavior similar to that predicted by the decaying turbulence theory for the continuous system.
    publisherAmerican Meteorological Society
    titleAnalysis of Discrete Shallow-Water Models on Geodesic Delaunay Grids with C-Type Staggering
    typeJournal Paper
    journal volume133
    journal issue8
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR2986.1
    journal fristpage2351
    journal lastpage2373
    treeMonthly Weather Review:;2005:;volume( 133 ):;issue: 008
    contenttypeFulltext
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