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    A Microstructure Instrument for Profiling Oceanic Turbulence in Coastal Bottom Boundary Layers

    Source: Journal of Atmospheric and Oceanic Technology:;1987:;volume( 004 ):;issue: 002::page 288
    Author:
    Dewey, Richard K.
    ,
    Crawford, William R.
    ,
    Gargett, Ann E.
    ,
    Oakey, Neil S.
    DOI: 10.1175/1520-0426(1987)004<0288:AMIFPO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A free-falling instrument has been built to measure temperature, salinity and turbulent shear from near surface to within 15 cm of the ocean bottom. A probe guard mounted at the lower end of the instrument protects sensitive shear and temperature sensors from bottom sediments. The noise level in the shear signal corresponds to a dissipation rate of 3.0 ? 10?7 W m?3, with vibrations of the probe guard providing the largest component of the noise. The signals are transmitted through a neutrally buoyant line to the ship where they are displayed in real time and recorded for later analysis. The profiling technique is capable of 20 profiles per hour through 50 m of water. Simultaneous profiles of turbulent microstructure and density can now be consistently obtained through the entire water column.
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      A Microstructure Instrument for Profiling Oceanic Turbulence in Coastal Bottom Boundary Layers

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4166178
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorDewey, Richard K.
    contributor authorCrawford, William R.
    contributor authorGargett, Ann E.
    contributor authorOakey, Neil S.
    date accessioned2017-06-09T14:53:20Z
    date available2017-06-09T14:53:20Z
    date copyright1987/06/01
    date issued1987
    identifier issn0739-0572
    identifier otherams-290.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4166178
    description abstractA free-falling instrument has been built to measure temperature, salinity and turbulent shear from near surface to within 15 cm of the ocean bottom. A probe guard mounted at the lower end of the instrument protects sensitive shear and temperature sensors from bottom sediments. The noise level in the shear signal corresponds to a dissipation rate of 3.0 ? 10?7 W m?3, with vibrations of the probe guard providing the largest component of the noise. The signals are transmitted through a neutrally buoyant line to the ship where they are displayed in real time and recorded for later analysis. The profiling technique is capable of 20 profiles per hour through 50 m of water. Simultaneous profiles of turbulent microstructure and density can now be consistently obtained through the entire water column.
    publisherAmerican Meteorological Society
    titleA Microstructure Instrument for Profiling Oceanic Turbulence in Coastal Bottom Boundary Layers
    typeJournal Paper
    journal volume4
    journal issue2
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1987)004<0288:AMIFPO>2.0.CO;2
    journal fristpage288
    journal lastpage297
    treeJournal of Atmospheric and Oceanic Technology:;1987:;volume( 004 ):;issue: 002
    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