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dc.contributor.authorDhanya, R.
dc.contributor.authorGurubaran, S.
dc.contributor.authorEmperumal, K.
dc.date.accessioned2015-09-15T04:59:00Z
dc.date.accessioned2021-02-12T09:29:22Z-
dc.date.available2015-09-15T04:59:00Z
dc.date.available2021-02-12T09:29:22Z-
dc.date.issued2008
dc.identifier.citationAnnales Geophysicae, v.26, 2459-2470, 2008, doi: 10.5194/angeo-26-2459-2008en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/405-
dc.description.abstractThe spaced antenna medium frequency (MF) radar at Tirunelveli (8.7° N, 77.8° E, geographic; 1.7° N, magnetic dip), the only one of its kind currently operating close to the magnetic equator, has provided an opportunity to investigate the electrodynamical processes related to the equatorial electrojet (EEJ) and their influence on the radar scatterers at medium frequencies in the lower E-region heights (90–98 km). Making use of the full correlation analysis that enables determination of useful geometrical parameters from the ground diffraction pattern, the present work delineates for the first time the characteristics of the radar scatterers during the occurrences of equatorial sporadic E (Esq) and blanketing sporadic E (Esb) noticed in simultaneous ionospheric sounding records at Tirunelveli. The ground magnetometer data provide indirect information on the strength of the EEJ and afternoon reverse EEJ or counterelectrojet (CEJ). The results presented in this work also reveal the height dependence of the radar echo intensity and some of the geometrical parameters at certain times, thus clearly bringing out the complex interplay of various physical processes in the probing region.en_US
dc.language.isoenen_US
dc.subjectEquatorial electrojeten_US
dc.subjectIonospheric irregularitiesen_US
dc.subjectIonospspheric physicsen_US
dc.subjectMF radaren_US
dc.subjectTirunelvelien_US
dc.subjectEEJen_US
dc.titleLower E-region echoes over the magnetic equator as observed by the MF radar at Tirunelveli (8.7° N, 77.8° E) and their relationship to Esq and Esben_US
dc.typeArticleen_US
dc.identifier.accession090902
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