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    Observing Turbulence with a Modified Acoustic Doppler Current Profiler

    Source: Journal of Atmospheric and Oceanic Technology:;1994:;volume( 011 ):;issue: 006::page 1592
    Author:
    Gargett, Ann E.
    DOI: 10.1175/1520-0426(1994)011<1592:OTWAMA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: This paper describes hardware and software modifications to a commercial incoherent acoustic Doppler current profiler that allow it to be used as a survey tool for measurement of turbulent velocity fields associated with coastal flows. The unambiguous measurement of vertical velocity, which is the heart of the modified system, can be used to provide quantitative estimates of turbulent kinetic energy E, as well as the spatial scales at which it resides and the rate ? at which it is dissipated. Provided that beam velocities are recorded directly, estimates of Reynolds stresses made from paired slant beams can be corrected for errors due to interbeam differences in bias error. With addition of a towed CTD, a direct measurement of buoyancy flux can be made. Although discussed here for an incoherent Doppler used in vigorous coastal turbulence, recent advances in coded-pulse Doppler sonars should enable use of most of these techniques in the lower-signal environment of the deep ocean, if a sufficiently stable platform can be provided.
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      Observing Turbulence with a Modified Acoustic Doppler Current Profiler

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4233516
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    contributor authorGargett, Ann E.
    date accessioned2017-06-09T17:40:38Z
    date available2017-06-09T17:40:38Z
    date copyright1994/12/01
    date issued1994
    identifier issn0739-0572
    identifier otherams-997.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4233516
    description abstractThis paper describes hardware and software modifications to a commercial incoherent acoustic Doppler current profiler that allow it to be used as a survey tool for measurement of turbulent velocity fields associated with coastal flows. The unambiguous measurement of vertical velocity, which is the heart of the modified system, can be used to provide quantitative estimates of turbulent kinetic energy E, as well as the spatial scales at which it resides and the rate ? at which it is dissipated. Provided that beam velocities are recorded directly, estimates of Reynolds stresses made from paired slant beams can be corrected for errors due to interbeam differences in bias error. With addition of a towed CTD, a direct measurement of buoyancy flux can be made. Although discussed here for an incoherent Doppler used in vigorous coastal turbulence, recent advances in coded-pulse Doppler sonars should enable use of most of these techniques in the lower-signal environment of the deep ocean, if a sufficiently stable platform can be provided.
    publisherAmerican Meteorological Society
    titleObserving Turbulence with a Modified Acoustic Doppler Current Profiler
    typeJournal Paper
    journal volume11
    journal issue6
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1994)011<1592:OTWAMA>2.0.CO;2
    journal fristpage1592
    journal lastpage1610
    treeJournal of Atmospheric and Oceanic Technology:;1994:;volume( 011 ):;issue: 006
    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