Vertical ionization drifts in the lower equatorial ionosphere and the meridional current systems

dc.contributor.authorBalsley, B. B
dc.contributor.authorCarter, D. A.
dc.contributor.authorWoodman Pollitt, Ronald Francisco
dc.date.accessioned2018-07-03T11:49:35Z
dc.date.available2018-07-03T11:49:35Z
dc.date.issued1976-03-01
dc.description.abstractRecent radar observations near the magnetic equator show that the electron vertical drift velocity below 200 km is upward during the day and downward at night, in agreement with measurements made at higher heights. The electron vertical drifts are consistent with meridional current theories. According to the theories the ion vertical drifts must be somewhat larger than the electron drifts to produce the predicted current system.
dc.description.peer-reviewPor pares
dc.formatapplication/pdf
dc.identifier.citationBalsley, B., Carter, D., & Woodman, R. F. (1976). Vertical ionization drifts in the lower equatorial ionosphere and the meridional current systems.==$Journal de Geophysical Research, 81$==(7), 1296-1300. https://doi.org/10.1029/JA081i007p01296
dc.identifier.doihttps://doi.org/10.1029/JA081i007p01296
dc.identifier.journalJournal de Geophysical Research
dc.identifier.urihttp://hdl.handle.net/20.500.12816/1648
dc.language.isoeng
dc.publisherAmerican Geophysical Union
dc.relation.ispartofurn:issn:0148-0227
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.subjectRadar
dc.subjectIonosphere
dc.subjectElectrons
dc.subjectElectrodynamics
dc.subject.ocdehttp://purl.org/pe-repo/ocde/ford#1.05.01
dc.titleVertical ionization drifts in the lower equatorial ionosphere and the meridional current systems
dc.typeinfo:eu-repo/semantics/article

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