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    AN INVESTIGATION OF CLOUD DISTRIBUTION FROM SATELLITE INFRARED RADIATION DATA

    Source: Monthly Weather Review:;1971:;volume( 099 ):;issue: 008::page 599
    Author:
    LO, ROBERT C.
    ,
    JOHNSON, DONALD R.
    DOI: 10.1175/1520-0493(1971)099<0599:AIOCDF>2.3.CO;2
    Publisher: American Meteorological Society
    Abstract: A physical-statistical model using Nimbus II MRIR (medium resolution infrared) radiometer channel 2 (10?11 µm) data is formed to estimate cloud cover. In the model, cloud cover is estimated from the probability density distribution of DV2 values defined to be the differences between the earth surface temperatures and the corresponding channel 2 observed equivalent black-body temperatures. For cloud type estimation, channel 1 (6.4?6.9 µm) and channel 2 (10?11 µm) data are used simultaneously in a joint distribution model. Bivariate DV1 and DV2 frequency distributions portray distinct features associated with different cloud patterns from which it was possible to estimate the cloud coverage for different levels in the troposphere. The major limiting factor in estimating cloud coverage in this study was the areal resolution of the MRIR radiometer. The results indicate that a reliable global climatology may be formed, using higher resolution radiometers combined with irradiance information from other spectral intervals.
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      AN INVESTIGATION OF CLOUD DISTRIBUTION FROM SATELLITE INFRARED RADIATION DATA

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4198779
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    • Monthly Weather Review

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    contributor authorLO, ROBERT C.
    contributor authorJOHNSON, DONALD R.
    date accessioned2017-06-09T15:59:43Z
    date available2017-06-09T15:59:43Z
    date copyright1971/08/01
    date issued1971
    identifier issn0027-0644
    identifier otherams-58342.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198779
    description abstractA physical-statistical model using Nimbus II MRIR (medium resolution infrared) radiometer channel 2 (10?11 µm) data is formed to estimate cloud cover. In the model, cloud cover is estimated from the probability density distribution of DV2 values defined to be the differences between the earth surface temperatures and the corresponding channel 2 observed equivalent black-body temperatures. For cloud type estimation, channel 1 (6.4?6.9 µm) and channel 2 (10?11 µm) data are used simultaneously in a joint distribution model. Bivariate DV1 and DV2 frequency distributions portray distinct features associated with different cloud patterns from which it was possible to estimate the cloud coverage for different levels in the troposphere. The major limiting factor in estimating cloud coverage in this study was the areal resolution of the MRIR radiometer. The results indicate that a reliable global climatology may be formed, using higher resolution radiometers combined with irradiance information from other spectral intervals.
    publisherAmerican Meteorological Society
    titleAN INVESTIGATION OF CLOUD DISTRIBUTION FROM SATELLITE INFRARED RADIATION DATA
    typeJournal Paper
    journal volume99
    journal issue8
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1971)099<0599:AIOCDF>2.3.CO;2
    journal fristpage599
    journal lastpage605
    treeMonthly Weather Review:;1971:;volume( 099 ):;issue: 008
    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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