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contributor authorLocatelli, John D.
contributor authorMartin, Jonathan E.
contributor authorCastle, Jeffrey A.
contributor authorHobbs, Peter V.
date accessioned2017-06-09T16:10:26Z
date available2017-06-09T16:10:26Z
date copyright1995/09/01
date issued1995
identifier issn0027-0644
identifier otherams-62588.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203496
description abstractFrom 8 to 9 March 1992 cold frontogenesis aloft (CFA), which was associated with the development of a vigorous baroclinic wave, triggered a series of squall lines that produced large hail and several tornadoes as they moved across the central United States. The air lifted by the CFA, which produced the squall lines, was made potentially unstable as a result of the circulation associated with a surface drytrough. This study provides further support for the view that in winter and early spring CFA plays an important role in triggering severe weather in the central United States.
publisherAmerican Meteorological Society
titleStructure and Evolution of Winter Cyclones in the Central United States and Their Effects on the Distribution of Precipitation. Part III: The Development of a Squall Line Associated with Weak Cold Frontogenesis Aloft
typeJournal Paper
journal volume123
journal issue9
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1995)123<2641:SAEOWC>2.0.CO;2
journal fristpage2641
journal lastpage2662
treeMonthly Weather Review:;1995:;volume( 123 ):;issue: 009
contenttypeFulltext


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