2001
DOI: 10.1016/s1364-6826(00)00218-2
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Propagation modes of low- and very-low-latitude whistlers

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Cited by 17 publications
(30 citation statements)
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“…The propagation mechanisms of low latitude whistlers have been a subject of controversy over the years. Some researchers have supported non-ducted PL mode of propagation in the presence of negative latitudinal electron density gradient in the ionization (Kumar et al, 2007 and references therein;Singh and Hayakawa, 2001). Recently, based on correlation between observed low-latitude whistlers and lightning activity detected by the World-Wide Lightning Location Network near the conjugate point (geography 9.87°S, 83.59°E) of station Allahabad, India, Gokani et al (2015) have shown a possibility of ducted mode of propagation even for such very low latitude whistlers.…”
Section: Plasmaspheric Remote Sensing Using Whistlersmentioning
confidence: 98%
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“…The propagation mechanisms of low latitude whistlers have been a subject of controversy over the years. Some researchers have supported non-ducted PL mode of propagation in the presence of negative latitudinal electron density gradient in the ionization (Kumar et al, 2007 and references therein;Singh and Hayakawa, 2001). Recently, based on correlation between observed low-latitude whistlers and lightning activity detected by the World-Wide Lightning Location Network near the conjugate point (geography 9.87°S, 83.59°E) of station Allahabad, India, Gokani et al (2015) have shown a possibility of ducted mode of propagation even for such very low latitude whistlers.…”
Section: Plasmaspheric Remote Sensing Using Whistlersmentioning
confidence: 98%
“…At mid (30 o -60 o ) and high (> 60 o ) latitudes both satellite and ground based whistler data have been extensively exploited to probe the plasmasphere. At low latitudes (< 30 o ) whistler data have not been used to determine plasmaspheric parameters, the main reason being that the propagation mechanism of low latitude whistlers cannot be determined from the whistler spectra (Singh and Hayakawa, 2001). This is because the nose frequency of such whistlers is higher than 100 kHz, well above the frequency range of the receiver.…”
Section: Plasmaspheric Remote Sensing Using Whistlersmentioning
confidence: 99%
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