Particle precipitation in the South Atlantic anomaly deduced from VLF propagation path measurements

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dc.contributor.authorGough M.P.
dc.date.accessioned2024-03-13T01:48:02Z
dc.date.available2024-03-13T01:48:02Z
dc.date.issued1975
dc.description.abstractThe VLF propagation path NWC to Sao Paulo, Brazil, passes through both the Brazilian and South African Anomalies. Particle produced ionization in the South African Anomaly is identified by its expected poststorm continuation up to 3-4 days. By comparing it with another mid-latitude path outside the anomaly it is shown that there is no D-region enhancement in the South African Anomaly. Any ionization enhancement in the Brazilian Anomaly should increase to a new level just after a major magnetic storm but no evidence for such VLF effects could be found. © 1975.
dc.description.firstpage1379
dc.description.issuenumber10
dc.description.lastpage1383
dc.description.volume37
dc.identifier.doi10.1016/0021-9169(75)90132-4
dc.identifier.issn0021-9169
dc.identifier.urihttps://dspace.mackenzie.br/handle/10899/38095
dc.relation.ispartofJournal of Atmospheric and Terrestrial Physics
dc.rightsAcesso Restrito
dc.titleParticle precipitation in the South Atlantic anomaly deduced from VLF propagation path measurements
dc.typeArtigo
local.scopus.citations5
local.scopus.eid2-s2.0-33745517792
local.scopus.updated2024-05-01
local.scopus.urlhttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=33745517792&origin=inward
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