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    Mesoscale Wind Variability below 5 km as Revealed by Sequential High-Resolution Wind Soundings

    Source: Monthly Weather Review:;1979:;volume( 107 ):;issue: 001::page 77
    Author:
    Gage, K. S.
    ,
    Jasperson, W. H.
    DOI: 10.1175/1520-0493(1979)107<0077:MWVBKA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The results of an analysis of the variability of the atmospheric wind field below 5 km is presented for a limited sample of high-resolution wind profiles. The wind was measured by tracking balloons utilizing the Control Data METRAC positioning system installed at St. Cloud, Minnesota. Balloons were launched sequentially 30 min apart for a period of 7 h during the afternoon of 31 March 1976. The wind, averaged over 100 m intervals, was analyzed for temporal variability for lags τ up to 240 min. Temporal variability of the wind at individual altitudes on this day did not support any unique power law. However, when the variability statistics at all levels were combined the averaged variability was consistent with the τ? power law.
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      Mesoscale Wind Variability below 5 km as Revealed by Sequential High-Resolution Wind Soundings

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4199980
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    contributor authorGage, K. S.
    contributor authorJasperson, W. H.
    date accessioned2017-06-09T16:02:19Z
    date available2017-06-09T16:02:19Z
    date copyright1979/01/01
    date issued1979
    identifier issn0027-0644
    identifier otherams-59423.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4199980
    description abstractThe results of an analysis of the variability of the atmospheric wind field below 5 km is presented for a limited sample of high-resolution wind profiles. The wind was measured by tracking balloons utilizing the Control Data METRAC positioning system installed at St. Cloud, Minnesota. Balloons were launched sequentially 30 min apart for a period of 7 h during the afternoon of 31 March 1976. The wind, averaged over 100 m intervals, was analyzed for temporal variability for lags τ up to 240 min. Temporal variability of the wind at individual altitudes on this day did not support any unique power law. However, when the variability statistics at all levels were combined the averaged variability was consistent with the τ? power law.
    publisherAmerican Meteorological Society
    titleMesoscale Wind Variability below 5 km as Revealed by Sequential High-Resolution Wind Soundings
    typeJournal Paper
    journal volume107
    journal issue1
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1979)107<0077:MWVBKA>2.0.CO;2
    journal fristpage77
    journal lastpage86
    treeMonthly Weather Review:;1979:;volume( 107 ):;issue: 001
    contenttypeFulltext
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