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    GATE phase III Mean Synoptic-Scale Radiative Convergence Profiles

    Source: Monthly Weather Review:;1981:;volume( 109 ):;issue: 002::page 371
    Author:
    Ackerman, Steven A.
    ,
    Cox, Stephen K.
    DOI: 10.1175/1520-0493(1981)109<0371:GPIMSS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Tropospheric radiative convergence profiles are derived for an easterly wave composite during Phase III of the GATE. The easterly waves observed during this period were generally well developed. The profiles also represent the magnitudes and the spatial distribution of atmospheric radiative convergence of the Intertropical Convergence Zone in the GATE area. The 12 h mean daytime and nighttime profiles are presented. Cloud-top pressure distributions as a function of wave position are also presented. The results of this research indicate three possible radiative induced mechanisms which contribute to the observed diurnal cycle in large-scale mass convergence: 1) radiative convergence differences between the ITCZ and the surrounding regions; 2) mesoscale radiative convergence differences between clear and cluster regions, and 3) a nighttime upper level tropospheric cooling maximum that is centered one-half a wavelength from the region of maximum convective activity.
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      GATE phase III Mean Synoptic-Scale Radiative Convergence Profiles

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4200420
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    contributor authorAckerman, Steven A.
    contributor authorCox, Stephen K.
    date accessioned2017-06-09T16:03:16Z
    date available2017-06-09T16:03:16Z
    date copyright1981/02/01
    date issued1981
    identifier issn0027-0644
    identifier otherams-59820.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4200420
    description abstractTropospheric radiative convergence profiles are derived for an easterly wave composite during Phase III of the GATE. The easterly waves observed during this period were generally well developed. The profiles also represent the magnitudes and the spatial distribution of atmospheric radiative convergence of the Intertropical Convergence Zone in the GATE area. The 12 h mean daytime and nighttime profiles are presented. Cloud-top pressure distributions as a function of wave position are also presented. The results of this research indicate three possible radiative induced mechanisms which contribute to the observed diurnal cycle in large-scale mass convergence: 1) radiative convergence differences between the ITCZ and the surrounding regions; 2) mesoscale radiative convergence differences between clear and cluster regions, and 3) a nighttime upper level tropospheric cooling maximum that is centered one-half a wavelength from the region of maximum convective activity.
    publisherAmerican Meteorological Society
    titleGATE phase III Mean Synoptic-Scale Radiative Convergence Profiles
    typeJournal Paper
    journal volume109
    journal issue2
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1981)109<0371:GPIMSS>2.0.CO;2
    journal fristpage371
    journal lastpage383
    treeMonthly Weather Review:;1981:;volume( 109 ):;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
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