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    Measurements of Turbulent Fluxes in Bass Strait

    Source: Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 001::page 28
    Author:
    Antonia, R. A.
    ,
    Chambers, A. J.
    ,
    Rajagopalan, S.
    ,
    Sreenivasan, K. R.
    ,
    Friehe, C. A.
    DOI: 10.1175/1520-0485(1978)008<0028:MOTFIB>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Measurements of turbulent momentum, heat and moisture fluxes have been made in Bass Strait from a stable platform, at a height of approximately 5 m above water. Direct measurements of these fluxes are compared with estimates obtained from spectra of velocity, temperature and humidity fluctuations with the use of the inertial dissipation technique. Directly measured momentum and moisture flux values are in reasonable agreement with inertial dissipation values. The sensible heal flux obtained by the inertial dissipation technique is about twice as large as the directly measured heat flux. The dependence on wind speed of bulk transfer coefficients of momentum, heat and moisture and of variances of velocity and scalar fluctuations is discussed and compared with available data.
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      Measurements of Turbulent Fluxes in Bass Strait

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162598
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    contributor authorAntonia, R. A.
    contributor authorChambers, A. J.
    contributor authorRajagopalan, S.
    contributor authorSreenivasan, K. R.
    contributor authorFriehe, C. A.
    date accessioned2017-06-09T14:44:42Z
    date available2017-06-09T14:44:42Z
    date copyright1978/01/01
    date issued1978
    identifier issn0022-3670
    identifier otherams-25778.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162598
    description abstractMeasurements of turbulent momentum, heat and moisture fluxes have been made in Bass Strait from a stable platform, at a height of approximately 5 m above water. Direct measurements of these fluxes are compared with estimates obtained from spectra of velocity, temperature and humidity fluctuations with the use of the inertial dissipation technique. Directly measured momentum and moisture flux values are in reasonable agreement with inertial dissipation values. The sensible heal flux obtained by the inertial dissipation technique is about twice as large as the directly measured heat flux. The dependence on wind speed of bulk transfer coefficients of momentum, heat and moisture and of variances of velocity and scalar fluctuations is discussed and compared with available data.
    publisherAmerican Meteorological Society
    titleMeasurements of Turbulent Fluxes in Bass Strait
    typeJournal Paper
    journal volume8
    journal issue1
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1978)008<0028:MOTFIB>2.0.CO;2
    journal fristpage28
    journal lastpage37
    treeJournal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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