2014
DOI: 10.5194/angeo-32-91-2014
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Characteristics of equatorial ionization anomaly (EIA) in relation to transionospheric satellite links around the northern crest in the Indian longitude sector

Abstract: Abstract. The poleward gradient of the equatorial ionization anomaly (EIA) introduces more intense propagation effects on transionospheric satellite links in comparison to the equatorward gradient.

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Cited by 16 publications
(19 citation statements)
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References 10 publications
(21 reference statements)
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“…The variations of EIA anomaly crest location and intensity have also been reported in the literature [Huang et al, 1989;Rastogi and Klobuchar, 1990]. Sharp latitudinal variability of TEC in the Indian longitude sector has been reported in Paul et al [2011] and Das et al [2014]. Solar cyclic and seasonal variations of TEC have been reported in various literatures such as Rama Rao et al [1977Rao et al [ , 1985, Vertical TEC (VTEC) prediction models have been developed using measured VTEC with the help of artificial neural network (ANN) based models for 77°E, 88°E, and 121°E longitude in the low-latitude regions for different solar activity periods.…”
Section: Introductionsupporting
confidence: 56%
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“…The variations of EIA anomaly crest location and intensity have also been reported in the literature [Huang et al, 1989;Rastogi and Klobuchar, 1990]. Sharp latitudinal variability of TEC in the Indian longitude sector has been reported in Paul et al [2011] and Das et al [2014]. Solar cyclic and seasonal variations of TEC have been reported in various literatures such as Rama Rao et al [1977Rao et al [ , 1985, Vertical TEC (VTEC) prediction models have been developed using measured VTEC with the help of artificial neural network (ANN) based models for 77°E, 88°E, and 121°E longitude in the low-latitude regions for different solar activity periods.…”
Section: Introductionsupporting
confidence: 56%
“…The EIA in the equatorial region causes sharp latitudinal gradient of TEC. The highly dynamic ionosphere results in large day-to-day TEC variations [Rastogi and Klobuchar, 1990;Klobuchar et al, 2001;Paul et al, 2011;Das et al, 2014]. The variations of EIA anomaly crest location and intensity have also been reported in the literature [Huang et al, 1989;Rastogi and Klobuchar, 1990].…”
Section: Introductionmentioning
confidence: 86%
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“…In contrast, the mid‐latitude ionospheric storm model (ie, the CONUS threat model) was utilized during local daytime, since no significantly large gradient was observed through the Brazilian ionospheric study (see Yoon et al). However, the effects of an equatorial ionospheric anomaly (EIA) that characterizes the daytime equatorial ionosphere all the time with a sharp ionospheric spatial gradient in both the equator‐ward and pole‐ward directions (see Das et al) may still exist. To capture more active ionosphere even in nominal days compared to that in mid‐latitude regions, we assumed that the value of σ vig that bounds nominal ionospheric spatial gradients in low‐latitude regions is twice a σ vig of 4 mm/km in CONUS.…”
Section: Approach I: Worst‐case Epb Threat Assessment and Mitigation mentioning
confidence: 99%
“…Amplitude scintillation observations and cycle slips at Calcutta located in the northern anomaly crest region have been extensively reported in literature [Ray and DasGupta, 2007;Roy and Paul, 2013] and also from locations beyond the northern crest of the EIA [A. Das et al, 2014].…”
Section: Introductionmentioning
confidence: 99%