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    On Estimating Wind Velocity Using an Upward-Looking ADCP

    Source: Journal of Atmospheric and Oceanic Technology:;2001:;volume( 018 ):;issue: 005::page 791
    Author:
    Marmorino, George O.
    ,
    Hallock, Zachariah R.
    DOI: 10.1175/1520-0426(2001)018<0791:OEWVUA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A new set of measurements made using an upward-looking broadband acoustic Doppler current profiler (ADCP) is analyzed for ?surface velocity,? which previous investigations suggest is related to wind velocity. In the present case, use of a shallow instrument depth and 1-m-depth resolution are shown to yield both a surface return, identified by a maximum in backscatter intensity (similar to previous studies), and a subsequent return that corresponds to a maximum in speed. These returns have speeds (measured relative to the 2-m-depth current) that increase to a peak of 0.7?0.8 m s?1 at a wind speed of 4?5 m s?1 and decrease for higher wind speeds, a behavior similar to that found by Nakajima et al., who made ADCP measurements using the same incidence angle (20°) as in the present study. A new finding is that the return having maximum speed yields a direction that better approximates the wind direction (a mean difference of about 5°) over the range of wind speeds sampled (up to 17 m s?1). Suggestions are made for future investigations.
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      On Estimating Wind Velocity Using an Upward-Looking ADCP

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4154489
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    contributor authorMarmorino, George O.
    contributor authorHallock, Zachariah R.
    date accessioned2017-06-09T14:23:33Z
    date available2017-06-09T14:23:33Z
    date copyright2001/05/01
    date issued2001
    identifier issn0739-0572
    identifier otherams-1848.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154489
    description abstractA new set of measurements made using an upward-looking broadband acoustic Doppler current profiler (ADCP) is analyzed for ?surface velocity,? which previous investigations suggest is related to wind velocity. In the present case, use of a shallow instrument depth and 1-m-depth resolution are shown to yield both a surface return, identified by a maximum in backscatter intensity (similar to previous studies), and a subsequent return that corresponds to a maximum in speed. These returns have speeds (measured relative to the 2-m-depth current) that increase to a peak of 0.7?0.8 m s?1 at a wind speed of 4?5 m s?1 and decrease for higher wind speeds, a behavior similar to that found by Nakajima et al., who made ADCP measurements using the same incidence angle (20°) as in the present study. A new finding is that the return having maximum speed yields a direction that better approximates the wind direction (a mean difference of about 5°) over the range of wind speeds sampled (up to 17 m s?1). Suggestions are made for future investigations.
    publisherAmerican Meteorological Society
    titleOn Estimating Wind Velocity Using an Upward-Looking ADCP
    typeJournal Paper
    journal volume18
    journal issue5
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(2001)018<0791:OEWVUA>2.0.CO;2
    journal fristpage791
    journal lastpage798
    treeJournal of Atmospheric and Oceanic Technology:;2001:;volume( 018 ):;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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