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    Open-Channel Flow and Turbulence Measurement by High-Resolution Doppler Sonar

    Source: Journal of Atmospheric and Oceanic Technology:;1994:;volume( 011 ):;issue: 005::page 1295
    Author:
    Lhermitte, R.
    ,
    Lemmin, U.
    DOI: 10.1175/1520-0426(1994)011<1295:OCFATM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Measurements of water velocity and turbulence in a water flume using a Doppler sonar operating at 1 MHz are presented. Analysis of the results shows that the instrument qualifies as a very useful tool for nonintrusive and accurate measurement of vertical profiles of water horizontal velocity u and vertical velocity w as well as water turbulence parameters including the ?u?w? Reynold's stress component. The water circulating in the flume is well filtered, so that the backscattering signal relates primarily to temperature microstructure occurring at ?/2, with ?=0.15 cm being the sonar wavelength. Quantitative measurements of backscattering intensity show that the backscattering signal disappears if the water turbulence intensity is below a certain value. This relates to the fact that the high-wavenumber end of the temperature turbulence spectrum no longer reaches the ?/2 scale. Application of the method to measurement of oceanic turbulence is discussed.
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      Open-Channel Flow and Turbulence Measurement by High-Resolution Doppler Sonar

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4233250
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    contributor authorLhermitte, R.
    contributor authorLemmin, U.
    date accessioned2017-06-09T17:40:06Z
    date available2017-06-09T17:40:06Z
    date copyright1994/10/01
    date issued1994
    identifier issn0739-0572
    identifier otherams-973.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4233250
    description abstractMeasurements of water velocity and turbulence in a water flume using a Doppler sonar operating at 1 MHz are presented. Analysis of the results shows that the instrument qualifies as a very useful tool for nonintrusive and accurate measurement of vertical profiles of water horizontal velocity u and vertical velocity w as well as water turbulence parameters including the ?u?w? Reynold's stress component. The water circulating in the flume is well filtered, so that the backscattering signal relates primarily to temperature microstructure occurring at ?/2, with ?=0.15 cm being the sonar wavelength. Quantitative measurements of backscattering intensity show that the backscattering signal disappears if the water turbulence intensity is below a certain value. This relates to the fact that the high-wavenumber end of the temperature turbulence spectrum no longer reaches the ?/2 scale. Application of the method to measurement of oceanic turbulence is discussed.
    publisherAmerican Meteorological Society
    titleOpen-Channel Flow and Turbulence Measurement by High-Resolution Doppler Sonar
    typeJournal Paper
    journal volume11
    journal issue5
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1994)011<1295:OCFATM>2.0.CO;2
    journal fristpage1295
    journal lastpage1308
    treeJournal of Atmospheric and Oceanic Technology:;1994:;volume( 011 ):;issue: 005
    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
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