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    Vertical Ozone Distribution in the Lower Troposphere Near an Urban Pollution Complex

    Source: Journal of Applied Meteorology:;1968:;volume( 007 ):;issue: 002::page 252
    Author:
    Lea, Duane A.
    DOI: 10.1175/1520-0450(1968)007<0252:VODITL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Balloon-borne chemiluminescent ozonesondes frequently reveal high ozone amounts in the lowest kilometer over Point Mugu, Calif. The most severe cases, at least, are presumably associated with influx of smoggy pollution from the nearby Los Angeles Basin. Surprisingly, the soundings show a pronounced tendency for maximum ozone to occur above the base of the low-level temperature inversion. A possible explanation might involve lifting of Los Angeles pollutant into the inversion by convection and orography, followed by modification enroute to Point Mugu by differential erosion and differential advection. From the persistence of observed ozone maxima in the soundings, the semipermanent temperature inversion over coastal southern California appears to be an effective reservoir for atmospheric ozone. It seems likely that ozone stored therein can at times reach the surface and contribute to localized pollution.
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      Vertical Ozone Distribution in the Lower Troposphere Near an Urban Pollution Complex

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4218889
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    contributor authorLea, Duane A.
    date accessioned2017-06-09T16:54:59Z
    date available2017-06-09T16:54:59Z
    date copyright1968/04/01
    date issued1968
    identifier issn0021-8952
    identifier otherams-7644.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4218889
    description abstractBalloon-borne chemiluminescent ozonesondes frequently reveal high ozone amounts in the lowest kilometer over Point Mugu, Calif. The most severe cases, at least, are presumably associated with influx of smoggy pollution from the nearby Los Angeles Basin. Surprisingly, the soundings show a pronounced tendency for maximum ozone to occur above the base of the low-level temperature inversion. A possible explanation might involve lifting of Los Angeles pollutant into the inversion by convection and orography, followed by modification enroute to Point Mugu by differential erosion and differential advection. From the persistence of observed ozone maxima in the soundings, the semipermanent temperature inversion over coastal southern California appears to be an effective reservoir for atmospheric ozone. It seems likely that ozone stored therein can at times reach the surface and contribute to localized pollution.
    publisherAmerican Meteorological Society
    titleVertical Ozone Distribution in the Lower Troposphere Near an Urban Pollution Complex
    typeJournal Paper
    journal volume7
    journal issue2
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1968)007<0252:VODITL>2.0.CO;2
    journal fristpage252
    journal lastpage267
    treeJournal of Applied Meteorology:;1968:;volume( 007 ):;issue: 002
    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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