2009
DOI: 10.1016/j.asr.2009.01.037
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Variation of ionospheric total electron content in Indian low latitude region of the equatorial anomaly during May 2007–April 2008

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Cited by 58 publications
(36 citation statements)
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“…It is also challenging to model the low-latitude ionosphere with relevant accuracy (Sridharan et al 1994;Kumar and Singh 2009;Aggarwal 2011). TEC is an important ionospheric parameter which is defined as the total number of electrons present within a cross-section 1 m 2 along the integrated path from the satellite to the receiver.…”
Section: Introductionmentioning
confidence: 99%
“…It is also challenging to model the low-latitude ionosphere with relevant accuracy (Sridharan et al 1994;Kumar and Singh 2009;Aggarwal 2011). TEC is an important ionospheric parameter which is defined as the total number of electrons present within a cross-section 1 m 2 along the integrated path from the satellite to the receiver.…”
Section: Introductionmentioning
confidence: 99%
“…Rama Rao et al [6] [39] and Venkatesh et al [26] reported that the EEJ shows a clear seasonal behavior with stronger electrojet strength during equinoctial months over Indian equatorial and low latitude sectors. Kumar et al [81] found the EIA crest in TEC is maximum in equinox months constitute due to EEJ strength. The research of Rama Rao et al [39] reported that the positions of the EIA crest and its [26] found (r = 0.53) over the Brazilian region; Rama Rao et al [39] found (r = 0.62), Bagiya et al [44] found (r = 0.71) and Venkatesh et al [26] found (r = 0.51) in the Indian region stations.…”
Section: Dependence Of Gps-tec On Eej Strengthmentioning
confidence: 99%
“…edge of the equatorial ionization anomaly) in the ionosphere or presence of some irregularities like spread F or plasma bubbles at the time of whistler observations. Kumar and Singh (2009) using GPS based measurements showed that Varanasi is situated at the edge to equatorial ionization anomaly region. We have also checked our GPS scintillation data for any possibility of observation of some ionospheric irregularities or plasma bubbles and found that some weak ionospheric irregularities were present at the time The ionospheric and other parameters derived from whistler measurements compare well with direct rocket and satellite measurements (Park et al, 1978;Singh et al, 1998;Chauhan and Singh, 2010;Kumar et al, 2012).…”
Section: Whistler-lightning Connectionsmentioning
confidence: 99%