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    Relevance of a Tuning-Fork Effect for Temperature Measurements with the Gill Solent HS Ultrasonic Anemometer–Thermometer

    Source: Journal of Atmospheric and Oceanic Technology:;2001:;volume( 018 ):;issue: 008::page 1367
    Author:
    Siebert, Holger
    ,
    Muschinski, Andreas
    DOI: 10.1175/1520-0426(2001)018<1367:ROATFE>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The performance of a new type of sonic anemometer?thermometer (called a sonic), the Solent-Research HS, manufactured by Gill Instruments, Lymington, United Kingdom, was investigated. Measurements of the three wind-velocity components u, ?, w, and temperature T were taken in the laboratory under quiet conditions and in the field at wind speeds of about 10 m s?1. The power spectra of u, ?, w, and T measured in the laboratory follow a ?5/3 power law at moderate frequencies. At frequencies higher than u/l (here u is the mean wind speed along a given path of length l), there is a roll-off in all spectra, an expected effect caused by the spatial averaging along the finite pathlength. Over the bandwidth of fs/2 = 50 Hz, the standard deviations due to uncorrelated noise amount to 0.02 m s?1 for u, ?, and w and to 0.02 K for T. In the field, the spectra of u, ?, and w show a clean ?5/3 power law, except for a flattening at frequencies larger than 30 Hz. The ratio of the spectra of the transverse and longitudinal velocity components was close to 4/3, the ratio predicted by classical theory for isotropic turbulence. The T spectra measured in the field were severely contaminated at frequencies larger than about 5 Hz. Closer inspection of the T time series revealed amplitude-modulated artifacts. These artifacts were presumed to be the result of oscillations of the sonic's pathlengths induced by oscillations of the tower, which was exposed to a turbulently changing wind. The artifacts were reproduced in the laboratory by controlled blows on the sonic's attachment. The mechanical oscillations, which the authors refer to as the tuning-fork effect, were measured with a strain gauge attached to the sonic. The tuning-fork effect was observed simultaneously and independently in the strain-gauge measurements and as artifacts in the temperature time series.
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      Relevance of a Tuning-Fork Effect for Temperature Measurements with the Gill Solent HS Ultrasonic Anemometer–Thermometer

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155000
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    contributor authorSiebert, Holger
    contributor authorMuschinski, Andreas
    date accessioned2017-06-09T14:25:17Z
    date available2017-06-09T14:25:17Z
    date copyright2001/08/01
    date issued2001
    identifier issn0739-0572
    identifier otherams-1894.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155000
    description abstractThe performance of a new type of sonic anemometer?thermometer (called a sonic), the Solent-Research HS, manufactured by Gill Instruments, Lymington, United Kingdom, was investigated. Measurements of the three wind-velocity components u, ?, w, and temperature T were taken in the laboratory under quiet conditions and in the field at wind speeds of about 10 m s?1. The power spectra of u, ?, w, and T measured in the laboratory follow a ?5/3 power law at moderate frequencies. At frequencies higher than u/l (here u is the mean wind speed along a given path of length l), there is a roll-off in all spectra, an expected effect caused by the spatial averaging along the finite pathlength. Over the bandwidth of fs/2 = 50 Hz, the standard deviations due to uncorrelated noise amount to 0.02 m s?1 for u, ?, and w and to 0.02 K for T. In the field, the spectra of u, ?, and w show a clean ?5/3 power law, except for a flattening at frequencies larger than 30 Hz. The ratio of the spectra of the transverse and longitudinal velocity components was close to 4/3, the ratio predicted by classical theory for isotropic turbulence. The T spectra measured in the field were severely contaminated at frequencies larger than about 5 Hz. Closer inspection of the T time series revealed amplitude-modulated artifacts. These artifacts were presumed to be the result of oscillations of the sonic's pathlengths induced by oscillations of the tower, which was exposed to a turbulently changing wind. The artifacts were reproduced in the laboratory by controlled blows on the sonic's attachment. The mechanical oscillations, which the authors refer to as the tuning-fork effect, were measured with a strain gauge attached to the sonic. The tuning-fork effect was observed simultaneously and independently in the strain-gauge measurements and as artifacts in the temperature time series.
    publisherAmerican Meteorological Society
    titleRelevance of a Tuning-Fork Effect for Temperature Measurements with the Gill Solent HS Ultrasonic Anemometer–Thermometer
    typeJournal Paper
    journal volume18
    journal issue8
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(2001)018<1367:ROATFE>2.0.CO;2
    journal fristpage1367
    journal lastpage1376
    treeJournal of Atmospheric and Oceanic Technology:;2001:;volume( 018 ):;issue: 008
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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