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    Large-Scale Eddies in the Unstably Stratified Atmospheric Surface Layer. Part I: Velocity and Temperature Structure

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 024::page 3537
    Author:
    Wilczak, J. M.
    DOI: 10.1175/1520-0469(1984)041<3537:LSEITU>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Ensemble vertical cross sections are derived for the velocity and temperature fields associated with large-scale eddy (LSE) temperature ramp structures in the turbulent, convective atmospheric surface layer. The turbulent fluxes of heat and momentum, as well as the third-order moments that represent the fluxes of vertical and horizontal heat, stress and turbulent kinetic energy are interpreted in terms of the circulations associated with the LSE structures. Heat flux and stress correlation coefficients are related to the phase relationships between vertical velocity, longitudinal velocity, and temperature. In particular, w? and T? are found to be in phase essentially everywhere. In contrast, u? and w? have a height dependent phase lag which leads to specific regions within the LSE structure where the momentum flux is consistently counter-gradient.
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      Large-Scale Eddies in the Unstably Stratified Atmospheric Surface Layer. Part I: Velocity and Temperature Structure

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    contributor authorWilczak, J. M.
    date accessioned2017-06-09T14:25:22Z
    date available2017-06-09T14:25:22Z
    date copyright1984/12/01
    date issued1984
    identifier issn0022-4928
    identifier otherams-18968.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155031
    description abstractEnsemble vertical cross sections are derived for the velocity and temperature fields associated with large-scale eddy (LSE) temperature ramp structures in the turbulent, convective atmospheric surface layer. The turbulent fluxes of heat and momentum, as well as the third-order moments that represent the fluxes of vertical and horizontal heat, stress and turbulent kinetic energy are interpreted in terms of the circulations associated with the LSE structures. Heat flux and stress correlation coefficients are related to the phase relationships between vertical velocity, longitudinal velocity, and temperature. In particular, w? and T? are found to be in phase essentially everywhere. In contrast, u? and w? have a height dependent phase lag which leads to specific regions within the LSE structure where the momentum flux is consistently counter-gradient.
    publisherAmerican Meteorological Society
    titleLarge-Scale Eddies in the Unstably Stratified Atmospheric Surface Layer. Part I: Velocity and Temperature Structure
    typeJournal Paper
    journal volume41
    journal issue24
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1984)041<3537:LSEITU>2.0.CO;2
    journal fristpage3537
    journal lastpage3550
    treeJournal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 024
    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