Identification of current system associated with a partially reversed equatorial electrojet

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DC Field	Value	Language
dc.contributor.author	James, M.E.
dc.contributor.author	Rastogi, R.G.
dc.contributor.author	Rao, D.R.K.
dc.date.accessioned	2015-05-02T10:50:01Z
dc.date.accessioned	2021-02-12T09:23:46Z	-
dc.date.available	2015-05-02T10:50:01Z
dc.date.available	2021-02-12T09:23:46Z	-
dc.date.issued	1996
dc.identifier.citation	JGG, v.49, p.633-640, 1997.	en_US
dc.identifier.uri	http://localhost:8080/xmlui/handle/123456789/44	-
dc.description.abstract	An abnormality among a series of geomagnetic quiescent days during July 1978 has been identified on 26 July using geomagnetic data from a network of 13 observatories in Indo-Russian longitude belt. This abnormality has been explained by invoking an additional clockwise loop current system centered around 5° dip latitude superimposed on the normal Sq current system centered at 20° dip latitude, thereby shifting the focus of the combined current system to 35° dip latitude. Probable causes of this additional currents in the low-latitude have been discussed.	en_US
dc.language.iso	en	en_US
dc.subject	Equatorial electrojet	en_US
dc.subject	Sq current system	en_US
dc.subject	Geomagnetic quiescent days	en_US
dc.subject	Dip latitude	en_US
dc.title	Identification of current system associated with a partially reversed equatorial electrojet	en_US
dc.type	Article	en_US
dc.identifier.accession	090532
Appears in Collections:	ODA_Reprints

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