Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/3816
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dc.contributor.authorSastri, J. H-
dc.date.accessioned2008-09-23T11:26:57Z-
dc.date.available2008-09-23T11:26:57Z-
dc.date.issued1986-05-
dc.identifier.citationSolar Physics, Vol. 105, No. 1, pp. 191 - 196en
dc.identifier.issn0038-0938 (Print) 1573-093X (Online)-
dc.identifier.urihttp://hdl.handle.net/2248/3816-
dc.description.abstractAs a sequel to the recent identification of the high-speed stream as the candidate structure in the solar wind at 1 AU that is primarily responsible for the geomagnetic disturbances occasionally noticed after 'disparition brusques' (DBs) of solar filaments (Sastri et al., 1985), it is reported here that the streams, inferred to be recurrent in an earlier study, were consistently preceded by a stream interface, as expected of corotating streams. This observation substantiates the role of corotating streams of coronal hole origin in the apparent link between DBs and geomagnetic activity, and strengthens the view that DBs are not a unique source of geomagnetic activity.en
dc.language.isoenen
dc.publisherSpringeren
dc.relation.urihttp://dx.doi.org/10.1007/BF00156386en
dc.subjectGeomagnetismen
dc.subjectMagnetic Stormsen
dc.subjectSolar Terrestrial Interactionsen
dc.subjectField Strengthen
dc.subjectFilamentsen
dc.subjectProton Energyen
dc.subjectTemporal Distributionen
dc.titleDisappearing solar filaments and geomagnetic activityen
dc.typeArticleen
Appears in Collections:IIAP Publications

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