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    Cup Anemometer Behavior in Turbulent Environments

    Source: Journal of Atmospheric and Oceanic Technology:;1998:;volume( 015 ):;issue: 001::page 5
    Author:
    Kristensen, Leif
    DOI: 10.1175/1520-0426(1998)015<0005:CABITE>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The behavior of the cup anemometer rotor in turbulent atmospheric flow is discussed in terms of a general equation of motion. This equates the rate of change s?? of the rotation rate s? of the rotor to a forcing F(s?, h?, w?), which is proportional to the torque and a function of s? and of the total horizontal and the vertical wind velocity components, h?, and w?, respectively. To determine the so-called overspeeding, it is necessary to carry out first-and second-order perturbation calculations around the response curve obtained in a laminar flow. From this curve, which for the purpose of this paper can be considered linear, five constraints are derived between the first and second partial derivatives of F. These constraints provide sufficient information for deriving an expression for the overspeeding to which four distinctly different biases contribute?one for each of the velocity components and one from the covariance between streamwise velocity components ? and w?. A phenomenological model of F in terms of the response distance ?, the distance constant L, a third instrument length scale ?, and two dimensionless constants ?1 and ?2, defining the angular response, makes it possible to quantify the four terms in the overspeeding expression. It turns out that the most significant bias in the mean wind speed is due to lateral velocity fluctuations. Under certain conditions it may be larger than 10%. It is shown how it is possible to reduce all the other biases to acceptable levels. The bias from the lateral velocity fluctuations can also be suppressed significantly by combining the cup anemometer with a wind vane and using a signal processing technique called the vector wind-run method.
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      Cup Anemometer Behavior in Turbulent Environments

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4148957
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    contributor authorKristensen, Leif
    date accessioned2017-06-09T14:09:31Z
    date available2017-06-09T14:09:31Z
    date copyright1998/02/01
    date issued1998
    identifier issn0739-0572
    identifier otherams-1350.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148957
    description abstractThe behavior of the cup anemometer rotor in turbulent atmospheric flow is discussed in terms of a general equation of motion. This equates the rate of change s?? of the rotation rate s? of the rotor to a forcing F(s?, h?, w?), which is proportional to the torque and a function of s? and of the total horizontal and the vertical wind velocity components, h?, and w?, respectively. To determine the so-called overspeeding, it is necessary to carry out first-and second-order perturbation calculations around the response curve obtained in a laminar flow. From this curve, which for the purpose of this paper can be considered linear, five constraints are derived between the first and second partial derivatives of F. These constraints provide sufficient information for deriving an expression for the overspeeding to which four distinctly different biases contribute?one for each of the velocity components and one from the covariance between streamwise velocity components ? and w?. A phenomenological model of F in terms of the response distance ?, the distance constant L, a third instrument length scale ?, and two dimensionless constants ?1 and ?2, defining the angular response, makes it possible to quantify the four terms in the overspeeding expression. It turns out that the most significant bias in the mean wind speed is due to lateral velocity fluctuations. Under certain conditions it may be larger than 10%. It is shown how it is possible to reduce all the other biases to acceptable levels. The bias from the lateral velocity fluctuations can also be suppressed significantly by combining the cup anemometer with a wind vane and using a signal processing technique called the vector wind-run method.
    publisherAmerican Meteorological Society
    titleCup Anemometer Behavior in Turbulent Environments
    typeJournal Paper
    journal volume15
    journal issue1
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1998)015<0005:CABITE>2.0.CO;2
    journal fristpage5
    journal lastpage17
    treeJournal of Atmospheric and Oceanic Technology:;1998:;volume( 015 ):;issue: 001
    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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