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    A Fourth-Order-Centered Finite-Volume Scheme for Regular Hexagonal Grids

    Source: Monthly Weather Review:;2007:;volume( 135 ):;issue: 012::page 4030
    Author:
    Miura, Hiroaki
    DOI: 10.1175/2007MWR2075.1
    Publisher: American Meteorological Society
    Abstract: Fourth-order-centered operators on regular hexagonal grids with the ZM-grid arrangement are described. The finite-volume method is used and operators are defined at hexagonal cell centers. The gradient operator is calculated from 12 surrounding cell center scalars. The divergence operator is defined from 12 surrounding cell corner vectors. A linear combination of local or interpolated values generates cell corner values used to calculate the operators. The flux-divergence operator applies the same cell corner values as those used in the gradient and divergence operators. The fourth-order convergence of the gradient and divergence operators is obtained in numerical tests using sufficiently smooth and differentiable test functions. The flux-divergence operator is formally second-order accurate. However, the results from a cone advection test show that the flux-divergence operator performs better than a commonly used second-order flux-divergence operator. Numerical dispersion and phase error are small because mean wind advection is computed with fourth-order accuracy.
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      A Fourth-Order-Centered Finite-Volume Scheme for Regular Hexagonal Grids

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4207571
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    contributor authorMiura, Hiroaki
    date accessioned2017-06-09T16:21:01Z
    date available2017-06-09T16:21:01Z
    date copyright2007/12/01
    date issued2007
    identifier issn0027-0644
    identifier otherams-66255.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4207571
    description abstractFourth-order-centered operators on regular hexagonal grids with the ZM-grid arrangement are described. The finite-volume method is used and operators are defined at hexagonal cell centers. The gradient operator is calculated from 12 surrounding cell center scalars. The divergence operator is defined from 12 surrounding cell corner vectors. A linear combination of local or interpolated values generates cell corner values used to calculate the operators. The flux-divergence operator applies the same cell corner values as those used in the gradient and divergence operators. The fourth-order convergence of the gradient and divergence operators is obtained in numerical tests using sufficiently smooth and differentiable test functions. The flux-divergence operator is formally second-order accurate. However, the results from a cone advection test show that the flux-divergence operator performs better than a commonly used second-order flux-divergence operator. Numerical dispersion and phase error are small because mean wind advection is computed with fourth-order accuracy.
    publisherAmerican Meteorological Society
    titleA Fourth-Order-Centered Finite-Volume Scheme for Regular Hexagonal Grids
    typeJournal Paper
    journal volume135
    journal issue12
    journal titleMonthly Weather Review
    identifier doi10.1175/2007MWR2075.1
    journal fristpage4030
    journal lastpage4037
    treeMonthly Weather Review:;2007:;volume( 135 ):;issue: 012
    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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