Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/37637
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dc.contributor.authorAgrawal, S P-
dc.contributor.authorSingh, R L-
dc.date.accessioned2016-11-25T10:54:13Z-
dc.date.available2016-11-25T10:54:13Z-
dc.date.issued1976-12-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/37637-
dc.description330-332en_US
dc.description.abstractUsing the hourly neutron monitor data for the present solar cycle, the characteristics of all the Forbush decreases (FDs) have been studied. Statistically, the rigidity spectral exponent is found to be 0·8 ± 0·2. It is seen that most of the FDs occur in coincidence with sudden storm commencements and the largest FDs are produced by solar flares occurring near the central meridian. These results are discussed in terms of earlier observations.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJRSP Vol.05(4) [December 1976]en_US
dc.titleForbush Decrease & Geomagnetic Storms in relation to Varying Interplanetary Parametersen_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.05(4) [December 1976]

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