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    Conservation and Linear Rossby-Mode Dispersion on the Spherical C Grid

    Source: Monthly Weather Review:;2004:;volume( 132 ):;issue: 002::page 641
    Author:
    Thuburn, John
    ,
    Staniforth, Andrew
    DOI: 10.1175/1520-0493(2004)132<0641:CALRDO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Discretizations of the linearized shallow-water equations on a spherical C grid are considered. Constraints on the schemes' coefficients that ensure conservation of mass, angular momentum, and energy are derived. These results generalize previously published results to the case of nonuniform and rotated grids (but are restricted to the linearized equations). Grids with ? stored at the poles and grids with u and h stored at the poles are both considered. Energy conservation is shown to be problematic for grids with u and h at the poles. It is also shown that an inappropriate averaging of the Coriolis terms leads to a misrepresentation of the Rossby modes with shortest meridional scale. The appropriate averaging is shown to be compatible with the constraints required for conservation, and, indeed, the energy-conserving averaging of the Coriolis terms improves the dispersion properties of Rossby modes.
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      Conservation and Linear Rossby-Mode Dispersion on the Spherical C Grid

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4205327
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    contributor authorThuburn, John
    contributor authorStaniforth, Andrew
    date accessioned2017-06-09T16:15:17Z
    date available2017-06-09T16:15:17Z
    date copyright2004/02/01
    date issued2004
    identifier issn0027-0644
    identifier otherams-64235.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4205327
    description abstractDiscretizations of the linearized shallow-water equations on a spherical C grid are considered. Constraints on the schemes' coefficients that ensure conservation of mass, angular momentum, and energy are derived. These results generalize previously published results to the case of nonuniform and rotated grids (but are restricted to the linearized equations). Grids with ? stored at the poles and grids with u and h stored at the poles are both considered. Energy conservation is shown to be problematic for grids with u and h at the poles. It is also shown that an inappropriate averaging of the Coriolis terms leads to a misrepresentation of the Rossby modes with shortest meridional scale. The appropriate averaging is shown to be compatible with the constraints required for conservation, and, indeed, the energy-conserving averaging of the Coriolis terms improves the dispersion properties of Rossby modes.
    publisherAmerican Meteorological Society
    titleConservation and Linear Rossby-Mode Dispersion on the Spherical C Grid
    typeJournal Paper
    journal volume132
    journal issue2
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(2004)132<0641:CALRDO>2.0.CO;2
    journal fristpage641
    journal lastpage653
    treeMonthly Weather Review:;2004:;volume( 132 ):;issue: 002
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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