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contributor authorWeaver, John F.
contributor authorToth, James J.
date accessioned2017-06-09T14:43:48Z
date available2017-06-09T14:43:48Z
date copyright1990/06/01
date issued1990
identifier issn0882-8156
identifier otherams-2541.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162190
description abstractConditions leading up to an outbreak of severe hailstorms in northeast Colorado are examined using satellite and surface data. A persistent mesoscale ridge of surface-high pressure, caused by outflow from a mesoscale- convective system, is seen to coincide with the occurrence of large hail which was confined to a narrow band extending nearly parallel to the Front Range of the Rocky Mountains. The development of the mesoscale ridge during its most intense stages is documented using a procedure that yields an approximate streamfunction for the surface geostrophic wind. Unlike alternatives over sloping terrain, this method is quick and can be adjusted to minimize the error over a limited portion of the analysis area.
publisherAmerican Meteorological Society
titleThe Use of Satellite Imagery and Surface Pressure-Gradient Analysis Modified for Sloping Terrain to Analyze the Mesoscale Events Preceding the Severe Hailstorms of 2 August 1986
typeJournal Paper
journal volume5
journal issue2
journal titleWeather and Forecasting
identifier doi10.1175/1520-0434(1990)005<0279:TUOSIA>2.0.CO;2
journal fristpage279
journal lastpage298
treeWeather and Forecasting:;1990:;volume( 005 ):;issue: 002
contenttypeFulltext


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