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Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/3711
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dc.contributor.authorSastri, J. H-
dc.date.accessioned2008-09-17T11:57:28Z-
dc.date.available2008-09-17T11:57:28Z-
dc.date.issued1988-12-
dc.identifier.citationAnnales Geophysicae-Atmospheres Hydrospheres and Space Sciences, Vol. 6, No. 6, pp. 635 – 642en
dc.identifier.issn0992-7689-
dc.identifier.urihttp://hdl.handle.net/2248/3711-
dc.descriptionOpen Access-
dc.description.abstractPersistent and significant reductions in the strength of the equatorial electrojet, accompanied by poor development of the equatorial ionization anomaly, are noted to sometimes occur in association with negative ionospheric storms at midlatitude. These events are interpretable as the signatures of equatorial disturbance dynamo electric fields generated by storm-time modifications in global thermospheric circulation in response to high latitude energy inputs. These electric field disturbances do not necessarily follow enhanced geomagnetic activity.en
dc.language.isoenen
dc.publisherEuropean Geosciences Unionen
dc.relation.urihttp://www.ann-geophys.net/volumes_and_issues.htmlen
dc.subjectAtmospheric Electricityen
dc.subjectDynamo Theoryen
dc.subjectEquatorial Atmosphereen
dc.subjectGeomagnetismen
dc.subjectIonospheric Disturbancesen
dc.subjectMagnetic Disturbancesen
dc.subjectEquatorial Electrojeten
dc.subjectF Regionen
dc.subjectIonospheric Stormsen
dc.titleEquatorial electric-fields of ionospheric disturbance dynamo orginen
dc.typeArticleen
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