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A cloud free vault

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dc.contributor.authorWeaver, John F., author
dc.coverage.spatialColorado
dc.date.accessioned2007-01-03T04:54:44Z
dc.date.available2007-01-03T04:54:44Z
dc.date.issued1975
dc.description.abstractA severe squall line, with several isolated storms near its southernmost end, was observed near Grover, Colorado, on the afternoon of 22 July 73 by the NHRE storm monitoring system. The northern segment of the squall line was oriented parallel to cloud level winds (i.e., northeast-southwest), while the southern segment was aligned north-south. The northern segment developed an extensive cloud free vault intruding into the cloud base above the lifting condensation level (LCL) between the precipitation and the updraft pedestal. No downdraft or gust front was observed from the northern segment. Downdrafts and a gust front characterized by a pressure jump of +3 mb and peak winds of 60 knots were produced by both the southern segment and the isolated storms.
dc.format.mediummasters theses
dc.identifier1975_fall_Weaver.pdf
dc.identifierCCRICIRA100001ETDS
dc.identifier.urihttp://hdl.handle.net/10217/22104
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relation.ispartofPublications
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.subjectNational Hail Research Experiment
dc.subjectoutflow
dc.subjectThunderstorms
dc.subjectMeteorology
dc.subjectCloud physics
dc.titleA cloud free vault
dc.typeText
thesis.degree.disciplineUniversity of Wyoming. Department of Atmospheric Science
thesis.degree.grantorUniversity of Wyoming
thesis.degree.levelMasters
thesis.degree.nameMaster of Science (M.S.)

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