Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/3025
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dc.contributor.authorRamesh, K. B-
dc.contributor.authorSastri, J. H-
dc.date.accessioned2008-08-05T07:53:14Z-
dc.date.available2008-08-05T07:53:14Z-
dc.date.issued1995-06-
dc.identifier.citationAnnales Geophysicae-Atmospheres Hydrospheres and Space Sciences, Vol. 13, No. 6, pp. 633 - 640en
dc.identifier.issn0992-7689-
dc.identifier.urihttp://hdl.handle.net/2248/3025-
dc.description.abstractMeasurements of the changes in phase path of F-region reflections at normal incidence at Kodaikanal (77°28'E, 10°14'N, dip 3°N) from February 1991 to February 1993 are used to determine the variation of the equatorial evening F-region vertical drifts (Vz) with season, solar and magnetic activity. It is found that on average, at Kodaikanal, the post-sunset peak in Vz (Vzp) is higher in equinox and local winter months than in local summer. The day-to-day variability in Vzp is highest in summer and lowest in winter. This seasonal trend persists even on magnetically quiet days (Ap≤14). Vzp is found to increase with 10.7 cm solar flux in all three seasons but tends to saturate for large flux values (>230 units) during local summer and winter months. Magnetic activity [represented by Ap as well as the time-weighted accumulations of ap and ap(τ)] does not seem to have any statistically significant effect on Vzp, except during equinoctial months of moderate solar activity, when Vzp decreases as magnetic activity increases.en
dc.format.extent3894 bytes-
dc.format.mimetypeapplication/pdf-
dc.language.isoenen
dc.publisherEuropean Geophysical Societyen
dc.subjectEquatorial Ionosphereen
dc.subjectIonospheric of Regionen
dc.subjectVertical Driften
dc.subjectSolar Cycleen
dc.subjectSeasonal Variationen
dc.subjectGeomagnetic Activityen
dc.subjectIndiaen
dc.subjectAsiaen
dc.titleSolar cycle and seasonal variations in F-region vertical drifts over Kodaikanal, Indiaen
dc.typeArticleen
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