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    Temperature, Humidity, and Wind Variations During Dissipation of a Low-Level jet

    Source: Journal of Applied Meteorology:;1966:;volume( 005 ):;issue: 001::page 36
    Author:
    Izumi, Yutaka
    ,
    Brown, Henry A.
    DOI: 10.1175/1520-0450(1966)005<0036:THAWVD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The time and height variations of temperature, wind speed, and moisture content observed at the Cedar Hill tower during the dissipation of a low-level jet on the morning of 14 May 1962 are presented and discussed. Three distinct stages of significant variations occur before sunrise at the upper levels of the tower. The three stages art: 1) a period of an abrupt and simultaneous warming and drying; 2) a period of steady temperature, mixing ratio, and wind speed; and 3) a period of pronounced decreases in temperature and wind speed and a marked increase in mixing ratio that occur progressively later with increasing height. It is proposed that these variations are produced by horizontal and vertical advection and by turbulent mixing.
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      Temperature, Humidity, and Wind Variations During Dissipation of a Low-Level jet

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    contributor authorIzumi, Yutaka
    contributor authorBrown, Henry A.
    date accessioned2017-06-09T16:43:03Z
    date available2017-06-09T16:43:03Z
    date copyright1966/02/01
    date issued1966
    identifier issn0021-8952
    identifier otherams-7289.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4214944
    description abstractThe time and height variations of temperature, wind speed, and moisture content observed at the Cedar Hill tower during the dissipation of a low-level jet on the morning of 14 May 1962 are presented and discussed. Three distinct stages of significant variations occur before sunrise at the upper levels of the tower. The three stages art: 1) a period of an abrupt and simultaneous warming and drying; 2) a period of steady temperature, mixing ratio, and wind speed; and 3) a period of pronounced decreases in temperature and wind speed and a marked increase in mixing ratio that occur progressively later with increasing height. It is proposed that these variations are produced by horizontal and vertical advection and by turbulent mixing.
    publisherAmerican Meteorological Society
    titleTemperature, Humidity, and Wind Variations During Dissipation of a Low-Level jet
    typeJournal Paper
    journal volume5
    journal issue1
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1966)005<0036:THAWVD>2.0.CO;2
    journal fristpage36
    journal lastpage42
    treeJournal of Applied Meteorology:;1966:;volume( 005 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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