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    Demonstration of a Cut-Cell Representation of 3D Orography for Studies of Atmospheric Flows over Very Steep Hills

    Source: Monthly Weather Review:;2011:;volume( 140 ):;issue: 002::page 411
    Author:
    Lock, Sarah-Jane
    ,
    Bitzer, Heinz-Werner
    ,
    Coals, Alison
    ,
    Gadian, Alan
    ,
    Mobbs, Stephen
    DOI: 10.1175/MWR-D-11-00069.1
    Publisher: American Meteorological Society
    Abstract: dvances in computing are enabling atmospheric models to operate at increasingly fine resolution, giving rise to more variations in the underlying orography being captured by the model grid. Consequently, high-resolution models must overcome the problems associated with traditional terrain-following approaches of spurious winds and instabilities generated in the vicinity of steep and complex terrain.Cut-cell representations of orography present atmospheric models with an alternative to terrain-following vertical coordinates. This work explores the capabilities of a cut-cell representation of orography for idealized orographically forced flows. The orographic surface is represented within the model by continuous piecewise bilinear surfaces that intersect the regular Cartesian grid creating cut cells. An approximate finite-volume method for use with advection-form governing equations is implemented to solve flows through the resulting irregularly shaped grid boxes.Comparison with a benchmark orographic test case for nonhydrostatic flow shows very good results. Further tests demonstrate the cut-cell method for flow around 3D isolated hills and stably resolving flows over very steep orography.
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      Demonstration of a Cut-Cell Representation of 3D Orography for Studies of Atmospheric Flows over Very Steep Hills

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4229669
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    contributor authorLock, Sarah-Jane
    contributor authorBitzer, Heinz-Werner
    contributor authorCoals, Alison
    contributor authorGadian, Alan
    contributor authorMobbs, Stephen
    date accessioned2017-06-09T17:29:16Z
    date available2017-06-09T17:29:16Z
    date copyright2012/02/01
    date issued2011
    identifier issn0027-0644
    identifier otherams-86143.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4229669
    description abstractdvances in computing are enabling atmospheric models to operate at increasingly fine resolution, giving rise to more variations in the underlying orography being captured by the model grid. Consequently, high-resolution models must overcome the problems associated with traditional terrain-following approaches of spurious winds and instabilities generated in the vicinity of steep and complex terrain.Cut-cell representations of orography present atmospheric models with an alternative to terrain-following vertical coordinates. This work explores the capabilities of a cut-cell representation of orography for idealized orographically forced flows. The orographic surface is represented within the model by continuous piecewise bilinear surfaces that intersect the regular Cartesian grid creating cut cells. An approximate finite-volume method for use with advection-form governing equations is implemented to solve flows through the resulting irregularly shaped grid boxes.Comparison with a benchmark orographic test case for nonhydrostatic flow shows very good results. Further tests demonstrate the cut-cell method for flow around 3D isolated hills and stably resolving flows over very steep orography.
    publisherAmerican Meteorological Society
    titleDemonstration of a Cut-Cell Representation of 3D Orography for Studies of Atmospheric Flows over Very Steep Hills
    typeJournal Paper
    journal volume140
    journal issue2
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR-D-11-00069.1
    journal fristpage411
    journal lastpage424
    treeMonthly Weather Review:;2011:;volume( 140 ):;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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