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    An Adaptive Multimoment Global Model on a Cubed Sphere

    Source: Monthly Weather Review:;2010:;volume( 139 ):;issue: 002::page 523
    Author:
    Chen, Chungang
    ,
    Xiao, Feng
    ,
    Li, Xingliang
    DOI: 10.1175/2010MWR3365.1
    Publisher: American Meteorological Society
    Abstract: An adaptive global shallow-water model is proposed on cubed-sphere grid using the multimoment finite volume scheme and the Berger?Oliger adaptive mesh refinement (AMR) algorithm that was originally designed for a Cartesian grid. On each patch of the cubed-sphere grid, the curvilinear coordinates are constructed in a way that the Berger?Oliger algorithm can be applied directly. Moreover, an algorithm to transfer data across neighboring patches is proposed to establish a practical integrated framework for global AMR computation on the cubed-sphere grid. The multimoment finite volume scheme is adopted as the fluid solver and is essentially beneficial to the implementation of AMR on the cubed-sphere grid. The multimoment interpolation based on both volume-integrated average (VIA) and point value (PV) provides the compact reconstruction that makes the present scheme very attractive not only in dealing with the artificial boundaries between different patches but also in the coarse?fine interpolations required in the AMR computations. The single-cell-based reconstruction avoids involving more than two nesting levels during interpolations. The reconstruction profile of constrained interpolation profile?conservative semi-Lagrangian scheme with third-order polynomial function (CIP-CSL3) is adopted where the slope parameter provides a flexible and convenient switching to get the desired numerical properties, such as high-order (fourth order) accuracy, monotonicity, and positive definiteness. Numerical experiments with typical benchmark tests for both advection equation and shallow-water equations are carried out to evaluate the proposed model. The numerical errors and the corresponding CPU times of numerical experiments on uniform and adaptive meshes verify the performance of the proposed model. Compared to the uniformly refined grid, the AMR technique is able to achieve the similar numerical accuracy with less computational cost.
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      An Adaptive Multimoment Global Model on a Cubed Sphere

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4213206
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    • Monthly Weather Review

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    contributor authorChen, Chungang
    contributor authorXiao, Feng
    contributor authorLi, Xingliang
    date accessioned2017-06-09T16:38:07Z
    date available2017-06-09T16:38:07Z
    date copyright2011/02/01
    date issued2010
    identifier issn0027-0644
    identifier otherams-71326.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4213206
    description abstractAn adaptive global shallow-water model is proposed on cubed-sphere grid using the multimoment finite volume scheme and the Berger?Oliger adaptive mesh refinement (AMR) algorithm that was originally designed for a Cartesian grid. On each patch of the cubed-sphere grid, the curvilinear coordinates are constructed in a way that the Berger?Oliger algorithm can be applied directly. Moreover, an algorithm to transfer data across neighboring patches is proposed to establish a practical integrated framework for global AMR computation on the cubed-sphere grid. The multimoment finite volume scheme is adopted as the fluid solver and is essentially beneficial to the implementation of AMR on the cubed-sphere grid. The multimoment interpolation based on both volume-integrated average (VIA) and point value (PV) provides the compact reconstruction that makes the present scheme very attractive not only in dealing with the artificial boundaries between different patches but also in the coarse?fine interpolations required in the AMR computations. The single-cell-based reconstruction avoids involving more than two nesting levels during interpolations. The reconstruction profile of constrained interpolation profile?conservative semi-Lagrangian scheme with third-order polynomial function (CIP-CSL3) is adopted where the slope parameter provides a flexible and convenient switching to get the desired numerical properties, such as high-order (fourth order) accuracy, monotonicity, and positive definiteness. Numerical experiments with typical benchmark tests for both advection equation and shallow-water equations are carried out to evaluate the proposed model. The numerical errors and the corresponding CPU times of numerical experiments on uniform and adaptive meshes verify the performance of the proposed model. Compared to the uniformly refined grid, the AMR technique is able to achieve the similar numerical accuracy with less computational cost.
    publisherAmerican Meteorological Society
    titleAn Adaptive Multimoment Global Model on a Cubed Sphere
    typeJournal Paper
    journal volume139
    journal issue2
    journal titleMonthly Weather Review
    identifier doi10.1175/2010MWR3365.1
    journal fristpage523
    journal lastpage548
    treeMonthly Weather Review:;2010:;volume( 139 ):;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
    yabeshDSpacePersian