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contributor authorBONNER, WILLIAM D.
contributor authorWINNINGHOFF, FRANK
date accessioned2017-06-09T15:59:03Z
date available2017-06-09T15:59:03Z
date copyright1969/07/01
date issued1969
identifier issn0027-0644
identifier otherams-58099.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198508
description abstractTIROS-VII and -VIII photographs are used to study synoptic and mesoscale cloud patterns during 6 days with strong southerly flow in the Central United States. Cases with nocturnal thunderstorms show a tendency for thunderstorms to occur in the downstream portion of the jet. Through advection of moisture and turbulent breakdown of the nocturnal inversion, the low-level jet plays an important role both in the formation of stratus and in its manner of dissipation. Longitudinal cumulus cloud bands with spacing of 10 to 15 km occur with slightly superadiabatic lapse rates and moderate wind shear in agreement with theoretical results by Kuo.
publisherAmerican Meteorological Society
titleSATELLITE STUDIES OF CLOUDS AND CLOUD BANDS NEAR THE LOW-LEVEL JET
typeJournal Paper
journal volume97
journal issue7
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1969)097<0490:SSOCAC>2.3.CO;2
journal fristpage490
journal lastpage500
treeMonthly Weather Review:;1969:;volume( 097 ):;issue: 007
contenttypeFulltext


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