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    Boundary-Layer Structure Over Tropical Oceans from TIROS-N Infrared Sounder Observations

    Source: Journal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 007::page 1305
    Author:
    Agarwal, Vijay K.
    ,
    Ashajayanthi, A. V.
    DOI: 10.1175/1520-0450(1983)022<1305:BLSOTO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: It has been shown by simulation studies that the 13.4, 11.1 and 8.3 ?m spectral radiances are sensitive to the moisture distribution within the boundary layer. If the distribution gets significantly perturbed due to some stratification present in the boundary layer, the radiances show a change different from the change expected solely on the basis of change in the total water vapor content of the atmosphere. It has been possible to formulate an index which describes these changes in water vapor distribution in the boundary layer. The calculations have been tested using TIROS-N infrared sounder data for three days in June 1979 over the Arabian Sea for the case of monsoon inversion.
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      Boundary-Layer Structure Over Tropical Oceans from TIROS-N Infrared Sounder Observations

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4145674
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    contributor authorAgarwal, Vijay K.
    contributor authorAshajayanthi, A. V.
    date accessioned2017-06-09T13:59:39Z
    date available2017-06-09T13:59:39Z
    date copyright1983/07/01
    date issued1983
    identifier issn0733-3021
    identifier otherams-10545.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145674
    description abstractIt has been shown by simulation studies that the 13.4, 11.1 and 8.3 ?m spectral radiances are sensitive to the moisture distribution within the boundary layer. If the distribution gets significantly perturbed due to some stratification present in the boundary layer, the radiances show a change different from the change expected solely on the basis of change in the total water vapor content of the atmosphere. It has been possible to formulate an index which describes these changes in water vapor distribution in the boundary layer. The calculations have been tested using TIROS-N infrared sounder data for three days in June 1979 over the Arabian Sea for the case of monsoon inversion.
    publisherAmerican Meteorological Society
    titleBoundary-Layer Structure Over Tropical Oceans from TIROS-N Infrared Sounder Observations
    typeJournal Paper
    journal volume22
    journal issue7
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1983)022<1305:BLSOTO>2.0.CO;2
    journal fristpage1305
    journal lastpage1311
    treeJournal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 007
    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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