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Satellite depiction of the evolution of a West African squall cluster

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dc.creatorFernández Rojas, Walter
dc.date.accessioned2023-10-30T16:05:03Z
dc.date.available2023-10-30T16:05:03Z
dc.date.issued1989
dc.description.abstractWest African squall lines or disturbance lines have been studied by several investigators (e.g., Hamilton and Archbold 1945; Eldridge 1957; Fortune 1980; Fernandez 1982a, 1982b) and their climatological aspects are, in general, well known (Aspliden et al. 1976). The squall line is found to be the leading portion of a propagating disturbance, namely the squall cluster, which consists of the squall line (a line of cumulonimbus clouds) and the cloud shield (anvil cloud) that trails behind it. This paper uses METEOSAT imagery to investigate the evolution of an unusually persistent squall cluster.es
dc.description.procedenceUCR::Vicerrectoría de Investigación::Unidades de Investigación::Ciencias Básicas::Centro de Investigaciones Geofísicas (CIGEFI)es
dc.description.procedenceUCR::Vicerrectoría de Docencia::Ciencias Básicas::Facultad de Ciencias::Escuela de Físicaes
dc.identifier.citationhttps://rmets.onlinelibrary.wiley.com/doi/10.1002/j.1477-8696.1989.tb06967.x
dc.identifier.doihttps://doi.org/10.1002/j.1477-8696.1989.tb06967.x
dc.identifier.issn1477-8696
dc.identifier.urihttps://hdl.handle.net/10669/90250
dc.language.isoeng
dc.rightsacceso embargado
dc.sourceWeather, vol.44 (1), pp.29-33es
dc.subjectMETEOROLOGICAL SATELLITESes
dc.subjectEVOLUTIONes
dc.subjectSQUALLes
dc.subjectSTORMSes
dc.subjectWEST AFRICAes
dc.titleSatellite depiction of the evolution of a West African squall clusteres
dc.typeartículo originales

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