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    Angular Distribution of Solar Radiation Reflected from Clouds as Determined from TIROS IV Radiometer Measurements

    Source: Journal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 002::page 323
    Author:
    Ruff, I.
    ,
    Koffler, R.
    ,
    Fritz, S.
    ,
    Winston, J. S.
    ,
    Rao, P. K.
    DOI: 10.1175/1520-0469(1968)025<0323:ADOSRR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The pattern of reflection of solar radiation from clouds as a function of angle is obtained by statistical analysis of observations from the TIROS IV visible radiation channel (0.55?0.75 ?). Readings from the water-vapor window channel (8ndash;12 ?) were used to select cases in which clouds fill the field of view of the sensor. The results show a generally anisotropic reflection pattern, which varies with solar zenith angle. The anisotropy is greatest for large values of solar zenith angle, the main feature in these cases being high intensity values of the radiation reflected at azimuths close to 180° from the sun, and at large zenith angles.
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      Angular Distribution of Solar Radiation Reflected from Clouds as Determined from TIROS IV Radiometer Measurements

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4151089
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    • Journal of the Atmospheric Sciences

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    contributor authorRuff, I.
    contributor authorKoffler, R.
    contributor authorFritz, S.
    contributor authorWinston, J. S.
    contributor authorRao, P. K.
    date accessioned2017-06-09T14:14:21Z
    date available2017-06-09T14:14:21Z
    date copyright1968/03/01
    date issued1968
    identifier issn0022-4928
    identifier otherams-15419.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151089
    description abstractThe pattern of reflection of solar radiation from clouds as a function of angle is obtained by statistical analysis of observations from the TIROS IV visible radiation channel (0.55?0.75 ?). Readings from the water-vapor window channel (8ndash;12 ?) were used to select cases in which clouds fill the field of view of the sensor. The results show a generally anisotropic reflection pattern, which varies with solar zenith angle. The anisotropy is greatest for large values of solar zenith angle, the main feature in these cases being high intensity values of the radiation reflected at azimuths close to 180° from the sun, and at large zenith angles.
    publisherAmerican Meteorological Society
    titleAngular Distribution of Solar Radiation Reflected from Clouds as Determined from TIROS IV Radiometer Measurements
    typeJournal Paper
    journal volume25
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1968)025<0323:ADOSRR>2.0.CO;2
    journal fristpage323
    journal lastpage332
    treeJournal of the Atmospheric Sciences:;1968:;Volume( 025 ):;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
    yabeshDSpacePersian