Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/36782
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dc.contributor.authorPasricha, K-
dc.contributor.authorReddy, B M-
dc.contributor.authorMitra, A P-
dc.date.accessioned2016-11-04T09:26:02Z-
dc.date.available2016-11-04T09:26:02Z-
dc.date.issued1982-04-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/36782-
dc.description64-70en_US
dc.description.abstractThe morphology of ionospheric scintillation at 327 MHz in the equatorial belt is studied by using the radio telescope at Ootacamund. The scintillation indices deduced from strip chart records are compared with the global nocturnal scintillation model developed by E J Fremouw and C L Rino of Stanford Research Institute [Radio Sci(USA), 8(1973) 213]. While there is hardly any disagreement in the seasonal pattern between the model and the Ooty observations, a significant departure is observed in the diurnal pattern. Instead of a single peak around midnight, as predicted by the model, the observations show a major peak at 2230 hrs LT followed by another minor peak at 0330 hrs LT. However, the most spectacular departure is observed in the solar activity variation. The model predicts steep variation of solar activity while the observations pertaining to low-to-medium solar activity show a trend which is almost independent of solar activity. Morphology of scintillation at other stations in the equatorial belt is briefly brought out for comparing with the Ooty 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.11(2) [April 1982]en_US
dc.titleMorphology of Equatorial Ionospheric Scintillation at 327 MHzen_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.11(2) [April 1982]

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