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    On Cloud-Top Determination from Gemini-5

    Source: Journal of the Atmospheric Sciences:;1967:;Volume( 024 ):;issue: 001::page 63
    Author:
    Saiedy, F.
    ,
    Jacobowitz, H.
    ,
    Wark, D. Q.
    DOI: 10.1175/1520-0469(1967)024<0063:OCTDFG>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A hand-held spectrograph-camera has been used by the Gemini-5 astronauts to obtain spectra of sunlight reflected from clouds in the region of the oxygen ?A? band near 7600 Å. The transmittance measurements at selected wavelengths inside the band offered a means of measuring the amount of oxygen in the optical path, and, therefore, the cloud top altitude. Results of the observations are presented, with verification of four cases indicating the validity of the experiment. A method for computing a correction factor, needed to account for the extra absorption inside the cloud, is developed. This method gives the dependences of the correction factor on the solar zenith, viewing and azimuthal angles. Results of computations by this method are compared with earlier results based on the two-streams theory of Schuster.
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      On Cloud-Top Determination from Gemini-5

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4150942
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    contributor authorSaiedy, F.
    contributor authorJacobowitz, H.
    contributor authorWark, D. Q.
    date accessioned2017-06-09T14:14:02Z
    date available2017-06-09T14:14:02Z
    date copyright1967/01/01
    date issued1967
    identifier issn0022-4928
    identifier otherams-15287.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150942
    description abstractA hand-held spectrograph-camera has been used by the Gemini-5 astronauts to obtain spectra of sunlight reflected from clouds in the region of the oxygen ?A? band near 7600 Å. The transmittance measurements at selected wavelengths inside the band offered a means of measuring the amount of oxygen in the optical path, and, therefore, the cloud top altitude. Results of the observations are presented, with verification of four cases indicating the validity of the experiment. A method for computing a correction factor, needed to account for the extra absorption inside the cloud, is developed. This method gives the dependences of the correction factor on the solar zenith, viewing and azimuthal angles. Results of computations by this method are compared with earlier results based on the two-streams theory of Schuster.
    publisherAmerican Meteorological Society
    titleOn Cloud-Top Determination from Gemini-5
    typeJournal Paper
    journal volume24
    journal issue1
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1967)024<0063:OCTDFG>2.0.CO;2
    journal fristpage63
    journal lastpage69
    treeJournal of the Atmospheric Sciences:;1967:;Volume( 024 ):;issue: 001
    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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