YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Journal of the Atmospheric Sciences
    • View Item
    •   YE&T Library
    • AMS
    • Journal of the Atmospheric Sciences
    • View Item
    • All Fields
    • Source Title
    • Year
    • Publisher
    • Title
    • Subject
    • Author
    • DOI
    • ISBN
    Advanced Search
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Archive

    Spectra of Scalar-Flux and Stress Fluctuations in the Atmospheric Surface Layer

    Source: Journal of the Atmospheric Sciences:;1997:;Volume( 054 ):;issue: 009::page 1277
    Author:
    Tong, Chenning
    DOI: 10.1175/1520-0469(1997)054<1277:SOSFAS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In a turbulent flow, the instantaneous turbulent flux and stress fluctuate in time and space. In large-eddy simulations (LES), the subgrid-scale (SGS) flux and stress are also time and space dependent, and their fluctuations are important in the modeling of SGS turbulence. In the present work, spectra of turbulent scalar-flux (temperature-flux) and stress fluctuations in the atmospheric surface layer are studied both by experiment and analysis. LES data show that horizontal two-dimensional (fourth-order) spectrum of temperature-flux and stress fluctuations peak at a scale comparable to the height from the surface z. The quasi-normal assumption is used to predict the variance and model the spectra of temperature-flux and stress fluctuations. The calculated one-dimensional spectra are in good agreement with experimental results. Under convective conditions, the temperature-flux and stress spectra both have a ??5/3 dependence in the inertial range. The normalized stress spectrum is very close to the vertical velocity spectrum at all wavenumbers for the stability conditions considered, whereas the temperature-flux spectrum peaks at a slightly higher wavenumber and has larger inertial-range values. The two-point coherence of flux and stress fluctuations is also similar to that of the vertical velocity.
    • Download: (159.8Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      Spectra of Scalar-Flux and Stress Fluctuations in the Atmospheric Surface Layer

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4158381
    Collections
    • Journal of the Atmospheric Sciences

    Show full item record

    contributor authorTong, Chenning
    date accessioned2017-06-09T14:34:29Z
    date available2017-06-09T14:34:29Z
    date copyright1997/05/01
    date issued1997
    identifier issn0022-4928
    identifier otherams-21982.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4158381
    description abstractIn a turbulent flow, the instantaneous turbulent flux and stress fluctuate in time and space. In large-eddy simulations (LES), the subgrid-scale (SGS) flux and stress are also time and space dependent, and their fluctuations are important in the modeling of SGS turbulence. In the present work, spectra of turbulent scalar-flux (temperature-flux) and stress fluctuations in the atmospheric surface layer are studied both by experiment and analysis. LES data show that horizontal two-dimensional (fourth-order) spectrum of temperature-flux and stress fluctuations peak at a scale comparable to the height from the surface z. The quasi-normal assumption is used to predict the variance and model the spectra of temperature-flux and stress fluctuations. The calculated one-dimensional spectra are in good agreement with experimental results. Under convective conditions, the temperature-flux and stress spectra both have a ??5/3 dependence in the inertial range. The normalized stress spectrum is very close to the vertical velocity spectrum at all wavenumbers for the stability conditions considered, whereas the temperature-flux spectrum peaks at a slightly higher wavenumber and has larger inertial-range values. The two-point coherence of flux and stress fluctuations is also similar to that of the vertical velocity.
    publisherAmerican Meteorological Society
    titleSpectra of Scalar-Flux and Stress Fluctuations in the Atmospheric Surface Layer
    typeJournal Paper
    journal volume54
    journal issue9
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1997)054<1277:SOSFAS>2.0.CO;2
    journal fristpage1277
    journal lastpage1284
    treeJournal of the Atmospheric Sciences:;1997:;Volume( 054 ):;issue: 009
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian