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contributor authorRao, V. V. M. Jagannadha
contributor authorBabu, A. Narendra
contributor authorRao, S. Vijaya Bhaskara
contributor authorRao, D. Narayana
date accessioned2017-06-09T16:48:05Z
date available2017-06-09T16:48:05Z
date copyright2007/01/01
date issued2007
identifier issn1558-8424
identifier otherams-74375.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4216593
description abstractUnique facility of measuring vertical winds using Indian mesosphere?stratosphere?troposphere (MST) radar along with horizontal winds enables the study of the atmospheric circulation over Gadanki, India. Several important features are noted while analyzing the wind field. A tropical easterly jet stream of 35 m s?1 strength is seen around 16 km during monsoon season. Relatively strong jetlike northward motion (southerlies) of 5?7 m s?1 is seen around 14 km during winter months. These two maxima in zonal and meridional wind patterns, even though they differ in strength greatly, occur in two contrasting seasons. Downward motion combined with upper-level northward and lower-level southward motion observed during winter in normal years indicates the signature of tropical Hadley circulation over the study region. During the 1997/98 El Niño event, however, an anomalous pattern of winds is seen and Hadley circulation is observed to be weakened.
publisherAmerican Meteorological Society
titleAnomalous Wind Circulation Observed during 1997/98 El Niño Using Indian MST Radar
typeJournal Paper
journal volume46
journal issue1
journal titleJournal of Applied Meteorology and Climatology
identifier doi10.1175/JAM2443.1
journal fristpage112
journal lastpage119
treeJournal of Applied Meteorology and Climatology:;2007:;volume( 046 ):;issue: 001
contenttypeFulltext


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