Simultaneous VHF radar backscatter and ionosonde observations of low-latitude E region

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dc.contributor.author Patra, A.K.
dc.contributor.author Sripathi, S.
dc.contributor.author Rao, P.B.
dc.contributor.author Subbarao, K.S.V.
dc.date.accessioned 2015-08-28T07:16:29Z
dc.date.accessioned 2021-02-12T09:27:51Z
dc.date.available 2015-08-28T07:16:29Z
dc.date.available 2021-02-12T09:27:51Z
dc.date.issued 2005
dc.identifier.citation Annales Geophysicae, v.23, p.773-779, 2005 en_US
dc.identifier.uri http://localhost:8080/xmlui/handle/123456789/297
dc.description.abstract The first results of simultaneous observations made on the low-latitude field-aligned irregularities (FAI) using the MST radar located at Gadanki (13.5° N, 79.2° E, dip 12.5°) and the Es parameters using an ionosonde at a nearby station Sriharikota (13.7° N, 80.1° E, dip 12.6°) are presented. The observations show that while the height of the most intense radar echoes is below the virtual height of Es (h'Es) during daytime, it is found to be either below or above during nighttime. The strength of the FAI is better correlated with the top penetration frequency (ftEs) and the blanketing frequency (fbEs) during the night (r=0.4 in both cases) as compared to the day (r=0.35 and -0.04, respectively). Furthermore, the signal strength of FAI is reasonably correlated with (ftEs-fbEs) during daytime (r=0.59) while very poorly correlated during nighttime (r=0.18). While the radar observations in general appear to have characteristics close to that of mid-latitudes, the relationship of these with the Es parameters are poorer than that of mid-latitudes. The observations reported here, nevertheless, are quite consistent with the expectations based on the gradient drift instability mechanism. en_US
dc.language.iso en en_US
dc.subject Equatorial ionosphere en_US
dc.subject Equatorial electrojet en_US
dc.subject Plasma waves en_US
dc.subject Field-aligned irregularities (FAI) en_US
dc.subject MST radar en_US
dc.subject Ionospheric irregularities en_US
dc.title Simultaneous VHF radar backscatter and ionosonde observations of low-latitude E region en_US
dc.type Article en_US
dc.identifier.accession 090787


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