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dc.contributor.authorAbdu, M. A.-
dc.contributor.authorDe Paula, E. R.-
dc.contributor.authorBatista, I. S.-
dc.contributor.authorReinisch, B. W.-
dc.contributor.authorMatsuoka, M. T.-
dc.contributor.authorCamargo, P. O.-
dc.contributor.authorVeliz, O.-
dc.contributor.authorDenardini, C. M.-
dc.contributor.authorSobral, J. H. A.-
dc.contributor.authorKherani, E. A.-
dc.contributor.authorDe Siqueira, P. M.-
dc.date.accessioned2014-05-27T11:23:35Z-
dc.date.accessioned2016-10-25T18:25:39Z-
dc.date.available2014-05-27T11:23:35Z-
dc.date.available2016-10-25T18:25:39Z-
dc.date.issued2008-07-01-
dc.identifierhttp://dx.doi.org/10.1029/2007JA012844-
dc.identifier.citationJournal of Geophysical Research A: Space Physics, v. 113, n. 7, 2008.-
dc.identifier.issn0148-0227-
dc.identifier.urihttp://hdl.handle.net/11449/70449-
dc.identifier.urihttp://acervodigital.unesp.br/handle/11449/70449-
dc.description.abstractEquatorial F region vertical plasma drifts, spread F and anomaly responses, in the south American longitude sector during the superstorm of 30 October 2003, are analyzed using data from an array of instruments consisting of Digisondes, a VHF radar, GPS TEC and scintillation receivers in Brazil, and a Digisonde and a magnetometer in Jicamarca, Peru. Prompt penetrating eastward electric field of abnormally large intensity drove the F layer plasma up at a velocity ∼1200 ms -1 during post dusk hours in the eastern sector over Brazil. The equatorial anomaly was intensified and expanded poleward while the development of spread F/plasma bubble irregularities and GPS signal scintillations were weaker than their quiet time intensity. Significantly weaker F region response over Jicamarca presented a striking difference in the intensity of prompt penetration electric field between Peru and eastern longitudes of Brazil. The enhanced post dusk sector vertical drift over Brazil is attributed to electro-dynamics effects arising energetic particle precipitation in the South Atlantic Magnetic Anomaly (SAMA). These extraordinary results and their longitudinal differences are presented and discussed in this paper. Copyright 2008 by the American Geophysical Union.en
dc.language.isoeng-
dc.sourceScopus-
dc.titleAbnormal evening vertical plasma drift and effects on ESF and EIA over Brazil-South Atlantic sector during the 30 October 2003 superstormen
dc.typeoutro-
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)-
dc.contributor.institutionInstituto Nacional de Pesquisas Espaciais (INPE)-
dc.contributor.institutionUniversidade Federal do Rio Grande do Sul (UFRGS)-
dc.contributor.institutionUniversity of Massachusetts-
dc.contributor.institutionJicamarca Radio Observatory (JRO)-
dc.description.affiliationUniversidade Estadual Paulista, Presidente Prudente, São Paulo-
dc.description.affiliationInstituto Nacional de Pesquisas Espaciais, Ave dos Astronautas 1758, 122245 970 Sao Jose dos Campos, Sao Paolo-
dc.description.affiliationDepartment of Cartography São Paolo State University 305 Centro Educacional, Rua Roberto Simonson, 19060-900 Presidente Prudente, SP-
dc.description.affiliationUniversidade Federal de Rio Grande do Sul Instituto de Geociencias 9500-UFRGS, Rua Bento Gonzales, Porto Alegre, RS-
dc.description.affiliationEnvironmental, Earth and Atmospheric Sciences Department Center for Atmospheric Research University of Massachusetts, 600 Suffolk Street, Lowell, MA 01854-
dc.description.affiliationJicamarca Radio Observatory IGP, P.B. 1306, Lima 13-
dc.description.affiliationUnespUniversidade Estadual Paulista, Presidente Prudente, São Paulo-
dc.identifier.doi10.1029/2007JA012844-
dc.rights.accessRightsAcesso restrito-
dc.relation.ispartofJournal of Geophysical Research A: Space Physics-
dc.identifier.scopus2-s2.0-67649129170-
Appears in Collections:Artigos, TCCs, Teses e Dissertações da Unesp

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