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    Evolution of the Subtropical Marine Boundary Layer: Photochemical Ozone Loss

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 016::page 2967
    Author:
    Paluch, I. R.
    ,
    McKeen, S.
    ,
    Lenschow, D. H.
    ,
    Schillawski, R. D.
    ,
    Kok, G. L.
    DOI: 10.1175/1520-0469(1995)052<2967:EOTSMB>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A diurnally averaged ozone decay rate of about 0.11 day?1was observed under partly cloudy sky in the boundary layer over the eastern Atlantic during the second Lagrangian experiment in the Atlantic Stratocumulus Transition Experiment. The observed decay rate can be accounted for by the combined effects of ozone loss through photolysis by UV radiation, reaction With H02 radical, and deposition on the sea surface, and effects of ozone production through photooxidation of carbon monoxide and methane in the presence of nitrogen oxides. The main contributor to the ozone decay is photolysis by UV radiation, but the other sources and sinks also make significant contributions.
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      Evolution of the Subtropical Marine Boundary Layer: Photochemical Ozone Loss

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4157906
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    • Journal of the Atmospheric Sciences

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    contributor authorPaluch, I. R.
    contributor authorMcKeen, S.
    contributor authorLenschow, D. H.
    contributor authorSchillawski, R. D.
    contributor authorKok, G. L.
    date accessioned2017-06-09T14:33:20Z
    date available2017-06-09T14:33:20Z
    date copyright1995/08/01
    date issued1995
    identifier issn0022-4928
    identifier otherams-21554.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157906
    description abstractA diurnally averaged ozone decay rate of about 0.11 day?1was observed under partly cloudy sky in the boundary layer over the eastern Atlantic during the second Lagrangian experiment in the Atlantic Stratocumulus Transition Experiment. The observed decay rate can be accounted for by the combined effects of ozone loss through photolysis by UV radiation, reaction With H02 radical, and deposition on the sea surface, and effects of ozone production through photooxidation of carbon monoxide and methane in the presence of nitrogen oxides. The main contributor to the ozone decay is photolysis by UV radiation, but the other sources and sinks also make significant contributions.
    publisherAmerican Meteorological Society
    titleEvolution of the Subtropical Marine Boundary Layer: Photochemical Ozone Loss
    typeJournal Paper
    journal volume52
    journal issue16
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1995)052<2967:EOTSMB>2.0.CO;2
    journal fristpage2967
    journal lastpage2976
    treeJournal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 016
    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
    yabeshDSpacePersian