East-west ionospheric drifts at the magnetic equator

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dc.contributor.authorWoodman Pollitt, Ronald Francisco
dc.date.accessioned2018-07-02T16:59:39Z
dc.date.available2018-07-02T16:59:39Z
dc.date.issued1972-01-01
dc.description.abstractA technique has been developed to measure the electromagnetic east-west drift velocity of the F region ionosphere by means of the Jicamarca incoherent scatter radar. Results show a fairly consistent behavior from day to day even during a magnetically disturbed day. Velocities are westward with a maximum of the order of 50 m/sec during the day, and eastward with a maximum of the order of 135 m/sec during the night. They are shown as experimental evidence for the superrotation of the neutral atmosphere at equatorial latitudes, but with a velocity smaller than the values inferred from satellite drag.es_ES
dc.formatapplication/pdfes_ES
dc.identifier.citationWoodman, R. F. (1972). East-west ionospheric drifts at the magnetic equator.==$Space research XII,$==Berlin, East Germany, Akademie-Verlag GmbH, 969-974.es_ES
dc.identifier.urihttp://hdl.handle.net/20.500.12816/1628
dc.language.isoenges_ES
dc.publisherInstituto GeofĂ­sico del PerĂșes_ES
dc.rightsinfo:eu-repo/semantics/restrictedAccesses_ES
dc.subjectIonospherees_ES
dc.subjectF regiones_ES
dc.subjectRadares_ES
dc.subjectDoppler effectes_ES
dc.subjectElectric fieldses_ES
dc.subjectIncoherent scattering radares_ES
dc.subjectIonospheric driftes_ES
dc.subject.ocdehttp://purl.org/pe-repo/ocde/ford#1.05.01es_ES
dc.titleEast-west ionospheric drifts at the magnetic equatores_ES
dc.typeinfo:eu-repo/semantics/conferenceObjectes_ES

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