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    A Finite-Volume Grid Using Multimoments for Geostrophic Adjustment

    Source: Monthly Weather Review:;2006:;volume( 134 ):;issue: 009::page 2515
    Author:
    Xiao, F.
    ,
    Peng, X. D.
    ,
    Shen, X. S.
    DOI: 10.1175/MWR3197.1
    Publisher: American Meteorological Society
    Abstract: This paper presents a novel finite-volume grid that uses not only the volume-integrated average (VIA) like the traditional finite-volume method, but also the surface-integrated average (SIA) as the model variables. The VIA and SIA are generically called ?moments? in the context used here and are carried forward in time separately as the prognostic quantities. With the VIA defined in the control volume while the SIA is on the surface of the control volume, the discretization based on VIA and SIA leads to some new features in the numerical dispersions. A simple formulation using both VIA and SIA for shallow-water equations is presented. The numerical dispersion of the resulting grid, which is denoted as the ?M grid,? is discussed with comparisons to the existing ones.
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      A Finite-Volume Grid Using Multimoments for Geostrophic Adjustment

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4229225
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    • Monthly Weather Review

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    contributor authorXiao, F.
    contributor authorPeng, X. D.
    contributor authorShen, X. S.
    date accessioned2017-06-09T17:27:55Z
    date available2017-06-09T17:27:55Z
    date copyright2006/09/01
    date issued2006
    identifier issn0027-0644
    identifier otherams-85744.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4229225
    description abstractThis paper presents a novel finite-volume grid that uses not only the volume-integrated average (VIA) like the traditional finite-volume method, but also the surface-integrated average (SIA) as the model variables. The VIA and SIA are generically called ?moments? in the context used here and are carried forward in time separately as the prognostic quantities. With the VIA defined in the control volume while the SIA is on the surface of the control volume, the discretization based on VIA and SIA leads to some new features in the numerical dispersions. A simple formulation using both VIA and SIA for shallow-water equations is presented. The numerical dispersion of the resulting grid, which is denoted as the ?M grid,? is discussed with comparisons to the existing ones.
    publisherAmerican Meteorological Society
    titleA Finite-Volume Grid Using Multimoments for Geostrophic Adjustment
    typeJournal Paper
    journal volume134
    journal issue9
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR3197.1
    journal fristpage2515
    journal lastpage2526
    treeMonthly Weather Review:;2006:;volume( 134 ):;issue: 009
    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
    yabeshDSpacePersian