dc.contributorUniversidade Estadual Paulista (Unesp)
dc.date.accessioned2014-05-27T11:17:30Z
dc.date.available2014-05-27T11:17:30Z
dc.date.created2014-05-27T11:17:30Z
dc.date.issued1992-12-01
dc.identifierSouth African Journal of Science, v. 88, n. 9-10, p. 516-524, 1992.
dc.identifier0038-2353
dc.identifierhttp://hdl.handle.net/11449/64330
dc.identifier2-s2.0-0027037385
dc.description.abstractOn 27 March 1991, an isolated thunderstorm passed between the two CSIR Doppler radars, spaced about 45km apart. Both radars simultaneously recorded Doppler data of the storm, and a detailed case study during an 11-min period is presented. Air motions synthesized from these data provide the first three-dimensional display of Doppler-derived wind fields within a multicell storm on the Transvaal Highveld. Regions of high divergence values (10 -2s -1) at low levels were found mostly in close proximity to reflectivity maxima (45-51 dBZ), which is consistent with findings from North America, that gravitational loading by the precipitation plays a key role in the initiation and maintenance of downdraughts. -from Authors
dc.languageeng
dc.relationSouth African Journal of Science
dc.relation1.191
dc.relation0,425
dc.rightsAcesso restrito
dc.sourceScopus
dc.subjectDoppler radar
dc.subjectthunderstorm
dc.subjectwind field
dc.subjectSouth Africa
dc.titleThe first case study of a thunderstorm in South Africa based on dual- Doppler radar observations
dc.typeArtículos de revistas


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