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    Acoustic Backscatter from Turbulent Microstructure

    Source: Journal of Atmospheric and Oceanic Technology:;1995:;volume( 012 ):;issue: 002::page 367
    Author:
    Seim, Harvey E.
    ,
    Gregg, Michael C.
    ,
    Miyamoto, R. T.
    DOI: 10.1175/1520-0426(1995)012<0367:ABFTM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Acoustic backscatter has produced spectacular images of internal ocean processes for nearly two decades, but interpretation of the images remains ambiguous because several mechanisms can generate measurable backscatter. The authors present what is thought to be the first simultaneous measurements of calibrated acoustic returns and turbulent microstructure, collected in a set of 20-m-tall billows. The observations are from Admiralty Inlet, a salt-stratified tidal channel near Puget Sound. Scattering due to turbulent microstructure alone is strong enough to explain the measured backscatter at specific sites within the billows. Existing formulations underestimate the strength of acoustic backscatter from turbulent microstructure. Due to a misinterpretation of the high-wavenumber temperature spectrum, some previous formulations underestimate the differential Scattering cross section (σ) when scattering from the viscous-convective subrange. Also, the influence of salinity on refractive-index fluctuations can be as large as or greater than that of temperature when the density stratification is dominated by salinity. Using temperature alone to estimate σ in coastal and estuarine waters may lead to significant underestimates. A simple formulation is derived that takes these two factors into account. Because of high ambient scattering from zooplankton in Admiralty Inlet, the acoustic data are conditionally sampled along modeled profiler trajectories to avoid using bulk statistics. Scalar dissipation is greatest in the bounding surfaces of the billows, consistent with these surfaces producing the most intense scattering. Acoustic backscatter can be used to remotely sense the spatial structure of scalar dissipation in turbulent events where σ due to turbulent microstructure exceeds the background level set by scattering from biology. In lakes and the deep ocean where scattering from zooplankton is expected to be negligible, scattering from microstructure may be the dominant mechanism. The largest uncertainties in the comparison result from the very large difference in sampling volume of the acoustic system and microstructure profiler.
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      Acoustic Backscatter from Turbulent Microstructure

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4145413
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorSeim, Harvey E.
    contributor authorGregg, Michael C.
    contributor authorMiyamoto, R. T.
    date accessioned2017-06-09T13:58:54Z
    date available2017-06-09T13:58:54Z
    date copyright1995/04/01
    date issued1995
    identifier issn0739-0572
    identifier otherams-1031.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145413
    description abstractAcoustic backscatter has produced spectacular images of internal ocean processes for nearly two decades, but interpretation of the images remains ambiguous because several mechanisms can generate measurable backscatter. The authors present what is thought to be the first simultaneous measurements of calibrated acoustic returns and turbulent microstructure, collected in a set of 20-m-tall billows. The observations are from Admiralty Inlet, a salt-stratified tidal channel near Puget Sound. Scattering due to turbulent microstructure alone is strong enough to explain the measured backscatter at specific sites within the billows. Existing formulations underestimate the strength of acoustic backscatter from turbulent microstructure. Due to a misinterpretation of the high-wavenumber temperature spectrum, some previous formulations underestimate the differential Scattering cross section (σ) when scattering from the viscous-convective subrange. Also, the influence of salinity on refractive-index fluctuations can be as large as or greater than that of temperature when the density stratification is dominated by salinity. Using temperature alone to estimate σ in coastal and estuarine waters may lead to significant underestimates. A simple formulation is derived that takes these two factors into account. Because of high ambient scattering from zooplankton in Admiralty Inlet, the acoustic data are conditionally sampled along modeled profiler trajectories to avoid using bulk statistics. Scalar dissipation is greatest in the bounding surfaces of the billows, consistent with these surfaces producing the most intense scattering. Acoustic backscatter can be used to remotely sense the spatial structure of scalar dissipation in turbulent events where σ due to turbulent microstructure exceeds the background level set by scattering from biology. In lakes and the deep ocean where scattering from zooplankton is expected to be negligible, scattering from microstructure may be the dominant mechanism. The largest uncertainties in the comparison result from the very large difference in sampling volume of the acoustic system and microstructure profiler.
    publisherAmerican Meteorological Society
    titleAcoustic Backscatter from Turbulent Microstructure
    typeJournal Paper
    journal volume12
    journal issue2
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1995)012<0367:ABFTM>2.0.CO;2
    journal fristpage367
    journal lastpage380
    treeJournal of Atmospheric and Oceanic Technology:;1995:;volume( 012 ):;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