Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/31862
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dc.contributor.authorNagar, Anju-
dc.contributor.authorMishra, S D-
dc.contributor.authorVijay, S K-
dc.date.accessioned2015-07-29T12:51:53Z-
dc.date.available2015-07-29T12:51:53Z-
dc.date.issued2015-06-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/31862-
dc.description78-87en_US
dc.description.abstractThis paper aims to investigate the relationship between propagation parameter M(3000)F2 and F2-layer critical frequency (foF2) during 2006-2010. Data from three low latitude stations, namely Jicamarca (12ºS, 283ºE), Kwajalein (09ºN, 167ºE) and Madimbo (22ºS, 031ºE) for the months of January (winter) and July (summer) during 2006-2010 are used for the study. It is found that the daily values of M(3000)F2 cannot be estimated from foF2 using a simple linear equation. It is concluded that that two procedures (day-to-day and hour-to-hour) do not give different results and the correlation coefficients between the daily values of M(3000)F2 and foF2 are generally lower than 0.6 and could be positive or negative.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.relation.ispartof94.20.Bb; 94.20.dj; 96.60.Q-en_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJRSP Vol.44(2) [June 2015]en_US
dc.subjectRadio propagationen_US
dc.subjectIonosphereen_US
dc.subjectF2-layer critical frequencyen_US
dc.subjectPropagation factor M(3000)F2en_US
dc.subjectLow solar activityen_US
dc.titleCorrelation of foF2 and M(3000)F2 over low latitude stations during low solar activity perioden_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.44(2) [June 2015]

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