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    Performance of a Horizontally Scanning Doppler Sonar near Shore

    Source: Journal of Atmospheric and Oceanic Technology:;1993:;volume( 010 ):;issue: 005::page 752
    Author:
    Smith, Jerome A.
    DOI: 10.1175/1520-0426(1993)010<0752:POAHSD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In August 1990, tests were performed to investigate the usefulness of a horizontally scanning Doppler acoustic technique in shallow water. Comparisons of radial velocity estimates from a vertical fan beam versus a horizontally aimed pencil beam indicate no degradation attributable to multiple reflections from the surface and bottom. Further tests, in which ping-to-ping phase-coherent means are examined, indicate negligible stationary backscatter from the bottom. Tests in which the acoustic beams were directed shoreward indicate that an extremely dense bubble cloud formed by plunging breakers produces an impenetrable ?wall? at the breakpoint, at acoustic frequencies near 195 kHz. Useful velocity estimates (one component) are obtainable everywhere seaward of the breakpoint of the incoming surf. The spatially extensive velocity estimates offered by this technique provide enormous potential for the study of horizontal currents and wave-current interactions in shallow water.
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      Performance of a Horizontally Scanning Doppler Sonar near Shore

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4228177
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    contributor authorSmith, Jerome A.
    date accessioned2017-06-09T17:24:54Z
    date available2017-06-09T17:24:54Z
    date copyright1993/10/01
    date issued1993
    identifier issn0739-0572
    identifier otherams-848.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4228177
    description abstractIn August 1990, tests were performed to investigate the usefulness of a horizontally scanning Doppler acoustic technique in shallow water. Comparisons of radial velocity estimates from a vertical fan beam versus a horizontally aimed pencil beam indicate no degradation attributable to multiple reflections from the surface and bottom. Further tests, in which ping-to-ping phase-coherent means are examined, indicate negligible stationary backscatter from the bottom. Tests in which the acoustic beams were directed shoreward indicate that an extremely dense bubble cloud formed by plunging breakers produces an impenetrable ?wall? at the breakpoint, at acoustic frequencies near 195 kHz. Useful velocity estimates (one component) are obtainable everywhere seaward of the breakpoint of the incoming surf. The spatially extensive velocity estimates offered by this technique provide enormous potential for the study of horizontal currents and wave-current interactions in shallow water.
    publisherAmerican Meteorological Society
    titlePerformance of a Horizontally Scanning Doppler Sonar near Shore
    typeJournal Paper
    journal volume10
    journal issue5
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1993)010<0752:POAHSD>2.0.CO;2
    journal fristpage752
    journal lastpage763
    treeJournal of Atmospheric and Oceanic Technology:;1993:;volume( 010 ):;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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