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    Representativeness of Wind Observations at Airports

    Source: Bulletin of the American Meteorological Society:;1980:;volume( 061 ):;issue: 009::page 962
    Author:
    Wieringa, J.
    DOI: 10.1175/1520-0477(1980)061<0962:ROWOAA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Wind information for use at airports can be called representative if it provides an optimal estimate of wind variations to be expected over the runway. It is shown that a single anemometer at a nonideal but reasonable location will usually provide adequate observational data to allow such a representative wind estimate after proper correction and data handling. It follows from the properties of the surface wind field and of the instruments used to measure it that aeronautical wind averaging periods should be at least 2 min for mean winds and at least 5 s for gusts. Small-scale obstacle effects and measuring height variations can be dealt with by an objective exposure correction model. It is shown that the aggregate wind estimation error cannot be less than 10% because of the influence of spatial distance and reporting time lag. The employment of additional anemometers appears justified only by large-scale terrain influences such as mountains or sea breeze-inducing coastlines.
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      Representativeness of Wind Observations at Airports

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    contributor authorWieringa, J.
    date accessioned2017-06-09T14:39:53Z
    date available2017-06-09T14:39:53Z
    date copyright1980/09/01
    date issued1980
    identifier issn0003-0007
    identifier otherams-23952.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4160570
    description abstractWind information for use at airports can be called representative if it provides an optimal estimate of wind variations to be expected over the runway. It is shown that a single anemometer at a nonideal but reasonable location will usually provide adequate observational data to allow such a representative wind estimate after proper correction and data handling. It follows from the properties of the surface wind field and of the instruments used to measure it that aeronautical wind averaging periods should be at least 2 min for mean winds and at least 5 s for gusts. Small-scale obstacle effects and measuring height variations can be dealt with by an objective exposure correction model. It is shown that the aggregate wind estimation error cannot be less than 10% because of the influence of spatial distance and reporting time lag. The employment of additional anemometers appears justified only by large-scale terrain influences such as mountains or sea breeze-inducing coastlines.
    publisherAmerican Meteorological Society
    titleRepresentativeness of Wind Observations at Airports
    typeJournal Paper
    journal volume61
    journal issue9
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1980)061<0962:ROWOAA>2.0.CO;2
    journal fristpage962
    journal lastpage971
    treeBulletin of the American Meteorological Society:;1980:;volume( 061 ):;issue: 009
    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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