Please use this identifier to cite or link to this item: http://nopr.niscair.res.in/handle/123456789/36249
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dc.contributor.authorBowman, G G-
dc.date.accessioned2016-10-26T09:56:50Z-
dc.date.available2016-10-26T09:56:50Z-
dc.date.issued1990-04-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/36249-
dc.description62-68en_US
dc.description.abstractThe experimental evidence for frontal and non-frontal structures associated with mid-latitude spread-F occurrence is presented and discussed. The evidence suggests that on most occasions frontal travelling ionospheric disturbances (TIDs) are primarily responsible for the recorded spread-F traces. However, at times non-frontal movements are detected due possibly to interference effects from TIDs travelling in different directions, or from the influence of small-scale structures which are also present at these times. At other times large-scale non-frontal "tongues" of ionization (of which the occurrence rate is somewhat uncertain) have also been detected when spread-F traces are observed.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.19(2) [April 1990]en_US
dc.titleFrontal and non-frontal characteristics of mid-latitude spread-F structuresen_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.19(2) [April 1990]

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