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    Dissipation Measurement with a Moored Instrument in a Swift Tidal Channel

    Source: Journal of Atmospheric and Oceanic Technology:;1999:;volume( 016 ):;issue: 011::page 1499
    Author:
    Lueck, Rolf
    ,
    Huang, Daniel
    DOI: 10.1175/1520-0426(1999)016<1499:DMWAMI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A moored and autonomous instrument that measures velocity and temperature fluctuations in the inertial subrange using shear probes and FP07 thermistors has been deployed in a swift [O(1 m s?1)] tidal channel for eight days. The measured velocity signals are free from body vibrations for frequencies below 16 Hz in flows faster than 0.5 m s?1 and below 8 Hz for slower flows. At lower frequencies, fluctuations of torque on the instrument, due mainly to fluctuations of the ambient current, produce large pitching and rolling motions (≈4° peak) that can easily be reduced by minor mechanical changes. Vibrations at higher frequencies do not scale with flow speed and stem mainly from mechanical structures. The velocity spectrum is free from contamination by body motions between 0.2 and 20 cpm (the inertial subrange), and consistent estimates of the rate of dissipation of kinetic energy are obtained from the spectral levels of vertical and lateral velocity fluctuations within this range.
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      Dissipation Measurement with a Moored Instrument in a Swift Tidal Channel

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4151868
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorLueck, Rolf
    contributor authorHuang, Daniel
    date accessioned2017-06-09T14:16:15Z
    date available2017-06-09T14:16:15Z
    date copyright1999/11/01
    date issued1999
    identifier issn0739-0572
    identifier otherams-1612.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151868
    description abstractA moored and autonomous instrument that measures velocity and temperature fluctuations in the inertial subrange using shear probes and FP07 thermistors has been deployed in a swift [O(1 m s?1)] tidal channel for eight days. The measured velocity signals are free from body vibrations for frequencies below 16 Hz in flows faster than 0.5 m s?1 and below 8 Hz for slower flows. At lower frequencies, fluctuations of torque on the instrument, due mainly to fluctuations of the ambient current, produce large pitching and rolling motions (≈4° peak) that can easily be reduced by minor mechanical changes. Vibrations at higher frequencies do not scale with flow speed and stem mainly from mechanical structures. The velocity spectrum is free from contamination by body motions between 0.2 and 20 cpm (the inertial subrange), and consistent estimates of the rate of dissipation of kinetic energy are obtained from the spectral levels of vertical and lateral velocity fluctuations within this range.
    publisherAmerican Meteorological Society
    titleDissipation Measurement with a Moored Instrument in a Swift Tidal Channel
    typeJournal Paper
    journal volume16
    journal issue11
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1999)016<1499:DMWAMI>2.0.CO;2
    journal fristpage1499
    journal lastpage1505
    treeJournal of Atmospheric and Oceanic Technology:;1999:;volume( 016 ):;issue: 011
    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