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    Ozone Abundances in the Lower Mesosphere Deduced from Backscattered Solar Radiances

    Source: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 012::page 1987
    Author:
    Frederick, J. E.
    ,
    Hays, P. B.
    ,
    Guenther, B. W.
    ,
    Heath, D. F.
    DOI: 10.1175/1520-0469(1977)034<1987:OAITLM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Backscatter ultraviolet data obtained by the Explorer E satellite imply very large ozone column abundances above 56 km in the tropics during mid-day. The number of molecules in a vertical column decays by a factor of 2?3 after the solar zenith angle exceeds 75° in the evening. An increase of similar magnitude occurs after sunrise. Such behavior implies the presence of a greater source of odd oxygen than is included in current photochemical theories. Ozone profiles deduced between altitudes of 50 and 62 km when the solar zenith angle exceeds 80° are in reasonable agreement with past rocket results.
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      Ozone Abundances in the Lower Mesosphere Deduced from Backscattered Solar Radiances

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4153294
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    • Journal of the Atmospheric Sciences

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    contributor authorFrederick, J. E.
    contributor authorHays, P. B.
    contributor authorGuenther, B. W.
    contributor authorHeath, D. F.
    date accessioned2017-06-09T14:19:54Z
    date available2017-06-09T14:19:54Z
    date copyright1977/12/01
    date issued1977
    identifier issn0022-4928
    identifier otherams-17403.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153294
    description abstractBackscatter ultraviolet data obtained by the Explorer E satellite imply very large ozone column abundances above 56 km in the tropics during mid-day. The number of molecules in a vertical column decays by a factor of 2?3 after the solar zenith angle exceeds 75° in the evening. An increase of similar magnitude occurs after sunrise. Such behavior implies the presence of a greater source of odd oxygen than is included in current photochemical theories. Ozone profiles deduced between altitudes of 50 and 62 km when the solar zenith angle exceeds 80° are in reasonable agreement with past rocket results.
    publisherAmerican Meteorological Society
    titleOzone Abundances in the Lower Mesosphere Deduced from Backscattered Solar Radiances
    typeJournal Paper
    journal volume34
    journal issue12
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1977)034<1987:OAITLM>2.0.CO;2
    journal fristpage1987
    journal lastpage1994
    treeJournal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 012
    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