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    A Mixed Spectral Finite-Difference 3D Model of Neutral Planetary Boundary-Layer Flow over Topography

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 020::page 3523
    Author:
    Ayotte, Keith W.
    ,
    Taylor, Peter A.
    DOI: 10.1175/1520-0469(1995)052<3523:AMSFDM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A simple three-dimensional linear model of planetary boundary-layer flow is developed based on the Mixed Spectral Finite-Difference model of Beljaars et al. using the full second-order turbulence closure of Launder et al. The model uses a steady-state solution to the fully nonlinear model equations over a horizontally homogeneous surface to specify the zero-order, upwind profiles of mean and turbulent quantities. Due to the complexity of the closure and linearization of the model equations, the authors use an automated method of source code generation to produce both the time-dependent model used to generate the zero-order solution and the 3D model. Model results are presented for flow over a simple isolated hill.
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      A Mixed Spectral Finite-Difference 3D Model of Neutral Planetary Boundary-Layer Flow over Topography

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4157953
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    • Journal of the Atmospheric Sciences

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    contributor authorAyotte, Keith W.
    contributor authorTaylor, Peter A.
    date accessioned2017-06-09T14:33:27Z
    date available2017-06-09T14:33:27Z
    date copyright1995/10/01
    date issued1995
    identifier issn0022-4928
    identifier otherams-21597.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157953
    description abstractA simple three-dimensional linear model of planetary boundary-layer flow is developed based on the Mixed Spectral Finite-Difference model of Beljaars et al. using the full second-order turbulence closure of Launder et al. The model uses a steady-state solution to the fully nonlinear model equations over a horizontally homogeneous surface to specify the zero-order, upwind profiles of mean and turbulent quantities. Due to the complexity of the closure and linearization of the model equations, the authors use an automated method of source code generation to produce both the time-dependent model used to generate the zero-order solution and the 3D model. Model results are presented for flow over a simple isolated hill.
    publisherAmerican Meteorological Society
    titleA Mixed Spectral Finite-Difference 3D Model of Neutral Planetary Boundary-Layer Flow over Topography
    typeJournal Paper
    journal volume52
    journal issue20
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1995)052<3523:AMSFDM>2.0.CO;2
    journal fristpage3523
    journal lastpage3538
    treeJournal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 020
    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