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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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