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    Cup Anemometer Overspeeding

    Source: Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 012::page 1328
    Author:
    Busch, N. E.
    ,
    Kristensen, L.
    DOI: 10.1175/1520-0450(1976)015<1328:CAO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Statistical considerations are applied to a general equation of motion for cup anemometers in a turbulent wind. It is shown that the relative overspeeding ?S/S can be expressed as ?S/S = Ih2 · Js(l0/?s) + cIw2, where Is and Iw are the horizontal and the vertical turbulence intensifies, respectively. The function Js depends on the shape of the spectrum of horizontal turbulent energy, l0 is the distance constant for the anemometer, and ?s is a characteristic length scale of the horizontal turbulence. The constant c is of order unity. If ?s is suitably chosen as the scale of the energy-containing eddies, then Js is satisfactorily approximated by Js = (1 + ?s/l0)?1 in most atmospheric applications.
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      Cup Anemometer Overspeeding

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4232664
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    contributor authorBusch, N. E.
    contributor authorKristensen, L.
    date accessioned2017-06-09T17:38:54Z
    date available2017-06-09T17:38:54Z
    date copyright1976/12/01
    date issued1976
    identifier issn0021-8952
    identifier otherams-9201.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232664
    description abstractStatistical considerations are applied to a general equation of motion for cup anemometers in a turbulent wind. It is shown that the relative overspeeding ?S/S can be expressed as ?S/S = Ih2 · Js(l0/?s) + cIw2, where Is and Iw are the horizontal and the vertical turbulence intensifies, respectively. The function Js depends on the shape of the spectrum of horizontal turbulent energy, l0 is the distance constant for the anemometer, and ?s is a characteristic length scale of the horizontal turbulence. The constant c is of order unity. If ?s is suitably chosen as the scale of the energy-containing eddies, then Js is satisfactorily approximated by Js = (1 + ?s/l0)?1 in most atmospheric applications.
    publisherAmerican Meteorological Society
    titleCup Anemometer Overspeeding
    typeJournal Paper
    journal volume15
    journal issue12
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1976)015<1328:CAO>2.0.CO;2
    journal fristpage1328
    journal lastpage1332
    treeJournal of Applied Meteorology:;1976:;volume( 015 ):;issue: 012
    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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