Westward ionospheric currents over the dip equator during geomagnetic disturbances

Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/6073

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DC Field	Value	Language
dc.contributor.author	Rastogi, R. G	-
dc.date.accessioned	2013-05-30T09:59:48Z	-
dc.date.available	2013-05-30T09:59:48Z	-
dc.date.issued	1975-04	-
dc.identifier.citation	Geophysical Research Letters, Vol. 2, No. 4, pp. 142–145	en
dc.identifier.issn	0094-8276	-
dc.identifier.uri	http://hdl.handle.net/2248/6073	-
dc.description	Open Access	en
dc.description.abstract	During geomagnetic disturbed periods, the q type of sporadic E layer near the dip equator is shown to disappear with maximum error of five minutes during the period when the difference of the geomagnetic H field between the equatorial and non-equatorial station decreases below the night level. These periods are identified with the reversal to westward direction of the electrojet currents at the base of the E region around 100 km level irrespective of the changes in the Sq current system which might be produced by the disturbance.	en
dc.language.iso	en	en
dc.publisher	The American Geophysical Union	en
dc.relation.uri	http://dx.doi.org/10.1029/GL002i004p00142	en
dc.rights	© The American Geophysical Union.	en
dc.title	Westward ionospheric currents over the dip equator during geomagnetic disturbances	en
dc.type	Article	en
Appears in Collections:	IIAP Publications

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