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    Relative importance of Terms in the Turbulent-Energy and Momentum Equations as Applied to the Problem of a Surface Roughness Change

    Source: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 008::page 1470
    Author:
    Peterson, Ernest W.
    DOI: 10.1175/1520-0469(1972)029<1470:RIOTIT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: There are four equations which must he satisfied in a description of the flow, in the two-diinensional case, across a change in surface roughness in the neutrally-stable surface boundary layer: the horizontal and vertical momentum equations, the turbulent energy equation, and the continuity equation. Using variations on the Peterson model, the relative magnitudes of the terms in these equations are examined and the wind and shear-stress profiles predicted by each variant model are compared. The following conclusions are made: The horizontal-momentum and turbulent-energy equations are essential in a physically reasonable model of the flow. The vertical-momentum equation is less important since the pressure-gradient term in the horizontal equation of motion is relatively small except near the surface singularity. Neglect of the vertical-motion terms and thus the continuity equation does not alter the major features of the downstream wind and shear-stress profiles.
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      Relative importance of Terms in the Turbulent-Energy and Momentum Equations as Applied to the Problem of a Surface Roughness Change

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4152047
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    contributor authorPeterson, Ernest W.
    date accessioned2017-06-09T14:16:42Z
    date available2017-06-09T14:16:42Z
    date copyright1972/11/01
    date issued1972
    identifier issn0022-4928
    identifier otherams-16281.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152047
    description abstractThere are four equations which must he satisfied in a description of the flow, in the two-diinensional case, across a change in surface roughness in the neutrally-stable surface boundary layer: the horizontal and vertical momentum equations, the turbulent energy equation, and the continuity equation. Using variations on the Peterson model, the relative magnitudes of the terms in these equations are examined and the wind and shear-stress profiles predicted by each variant model are compared. The following conclusions are made: The horizontal-momentum and turbulent-energy equations are essential in a physically reasonable model of the flow. The vertical-momentum equation is less important since the pressure-gradient term in the horizontal equation of motion is relatively small except near the surface singularity. Neglect of the vertical-motion terms and thus the continuity equation does not alter the major features of the downstream wind and shear-stress profiles.
    publisherAmerican Meteorological Society
    titleRelative importance of Terms in the Turbulent-Energy and Momentum Equations as Applied to the Problem of a Surface Roughness Change
    typeJournal Paper
    journal volume29
    journal issue8
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1972)029<1470:RIOTIT>2.0.CO;2
    journal fristpage1470
    journal lastpage1476
    treeJournal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 008
    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