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Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/4686
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dc.contributor.authorRastogi, R. G-
dc.date.accessioned2009-07-30T10:06:15Z-
dc.date.available2009-07-30T10:06:15Z-
dc.date.issued1975-02-
dc.identifier.citationProceedings of Indian Academy of Sciences, Sect. A, Vol. 81, No. 2, pp. 80 - 92en
dc.identifier.issn0253-4142-
dc.identifier.urihttp://hdl.handle.net/2248/4686-
dc.description.abstractExperimental data on daily variations in the geomagnetic field are analyzed for evidence of counterflowing electrojets. In particular, the disappearance of the q type of Es layer (Es-q) and the appearance of blanketing-type Es (Es-b) are investigated. Various findings are reported; among them is the suggestion that the source of the upper (107 km) eastward current is the Sq dynamo current system, and that the lower (100 km) westward current is associated with the lunar current system or due to the electric fields generated by the interaction of the solar wind with the magnetosphere or by various polar substorm processes.en
dc.language.isoenen
dc.publisherIndian Academy of Sciencesen
dc.relation.urihttp://adsabs.harvard.edu/abs/1975InASP..81...80Ren
dc.subjectCounterflowen
dc.subjectDiurnal Variationsen
dc.subjectEquatorial Electrojeten
dc.subjectGeomagnetismen
dc.subjectIonospheric Currentsen
dc.subjectSporadic E Layeren
dc.subjectEarth Magnetosphereen
dc.subjectElectric Fieldsen
dc.subjectIonospheric Driften
dc.subjectLunar Tidesen
dc.subjectMagnetic Fieldsen
dc.subjectPolar Substormsen
dc.titleOn the simultaneous existence of eastward and westward flowing equatorial electrojet currentsen
dc.typeArticleen
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