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    An Ocean Refractometer: Resolving Millimeter-Scale Turbulent Density Fluctuations via the Refractive Index

    Source: Journal of Atmospheric and Oceanic Technology:;2006:;volume( 023 ):;issue: 001::page 121
    Author:
    Alford, Matthew H.
    ,
    Gerdt, David W.
    ,
    Adkins, Charles M.
    DOI: 10.1175/JTECH1830.1
    Publisher: American Meteorological Society
    Abstract: A fiberoptic sensor has been constructed to measure oceanic density fluctuations via their refractive index signature. The resolution (?z = 1 mm, ?t = 0.2 ms) and precision (?n < 10?8, ?? = 3.4 ? 10?5 kg m?3) of the device are far better than other methods and are sufficient to resolve the entire turbulent spectrum. Spectra show the salinity Batchelor rolloff at levels undetectable via conductivity measurements. However, the low-wavenumber portion of the spectrum occupied by the turbulent inertial subrange (≈1 m?1 cm scales) is marred by noise resulting from fiber motion in response to turbulent velocity fluctuations. The technique is described, and the first ocean measurements are reported.
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      An Ocean Refractometer: Resolving Millimeter-Scale Turbulent Density Fluctuations via the Refractive Index

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4227526
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorAlford, Matthew H.
    contributor authorGerdt, David W.
    contributor authorAdkins, Charles M.
    date accessioned2017-06-09T17:23:02Z
    date available2017-06-09T17:23:02Z
    date copyright2006/01/01
    date issued2006
    identifier issn0739-0572
    identifier otherams-84214.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4227526
    description abstractA fiberoptic sensor has been constructed to measure oceanic density fluctuations via their refractive index signature. The resolution (?z = 1 mm, ?t = 0.2 ms) and precision (?n < 10?8, ?? = 3.4 ? 10?5 kg m?3) of the device are far better than other methods and are sufficient to resolve the entire turbulent spectrum. Spectra show the salinity Batchelor rolloff at levels undetectable via conductivity measurements. However, the low-wavenumber portion of the spectrum occupied by the turbulent inertial subrange (≈1 m?1 cm scales) is marred by noise resulting from fiber motion in response to turbulent velocity fluctuations. The technique is described, and the first ocean measurements are reported.
    publisherAmerican Meteorological Society
    titleAn Ocean Refractometer: Resolving Millimeter-Scale Turbulent Density Fluctuations via the Refractive Index
    typeJournal Paper
    journal volume23
    journal issue1
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/JTECH1830.1
    journal fristpage121
    journal lastpage137
    treeJournal of Atmospheric and Oceanic Technology:;2006:;volume( 023 ):;issue: 001
    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