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    The Diurnal Wind Variation in the Lowest 1500 ft in Central Oklahoma. June 1966–May 1967

    Source: Journal of Applied Meteorology:;1973:;volume( 012 ):;issue: 001::page 127
    Author:
    Crawford, Kenneth C.
    ,
    Hudson, Horace R.
    DOI: 10.1175/1520-0450(1973)012<0127:TDWVIT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: One year of wind data from a television tower in northern Oklahoma City has been analyzed an a diurnal basis. The annual mean speeds below the third level at 296 ft are lowest at night and highest during the day, and conversely the speeds up to the seventh level at 1458 ft are lowest during the day and highest at night. Generally, speed changes occur in short time periods shortly after sunrise and near sunset. Resultant wind directions veer most with height between 1700?1000 CST and least during midday. At all levels winds veer with time between 2100 and approximately 1100 CST and then back with time during the remaining hours.
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      The Diurnal Wind Variation in the Lowest 1500 ft in Central Oklahoma. June 1966–May 1967

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4228211
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    contributor authorCrawford, Kenneth C.
    contributor authorHudson, Horace R.
    date accessioned2017-06-09T17:25:00Z
    date available2017-06-09T17:25:00Z
    date copyright1973/02/01
    date issued1973
    identifier issn0021-8952
    identifier otherams-8483.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4228211
    description abstractOne year of wind data from a television tower in northern Oklahoma City has been analyzed an a diurnal basis. The annual mean speeds below the third level at 296 ft are lowest at night and highest during the day, and conversely the speeds up to the seventh level at 1458 ft are lowest during the day and highest at night. Generally, speed changes occur in short time periods shortly after sunrise and near sunset. Resultant wind directions veer most with height between 1700?1000 CST and least during midday. At all levels winds veer with time between 2100 and approximately 1100 CST and then back with time during the remaining hours.
    publisherAmerican Meteorological Society
    titleThe Diurnal Wind Variation in the Lowest 1500 ft in Central Oklahoma. June 1966–May 1967
    typeJournal Paper
    journal volume12
    journal issue1
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1973)012<0127:TDWVIT>2.0.CO;2
    journal fristpage127
    journal lastpage132
    treeJournal of Applied Meteorology:;1973:;volume( 012 ):;issue: 001
    contenttypeFulltext
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