2000
DOI: 10.1029/1999ja000244
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Global Positioning System measurements of the ionospheric zonal apparent velocity at Cachoeira Paulista in Brazil

Abstract: Abstract.Ionospheric irregularities and their zonal apparent drift were studied using Global Positioning System (GPS) measurements at Cachoeira Paulista (22.41øS, 45.00øW, -26 ø dip angle) in Brazil during November 6-19, 1998. Radio scintillations at the GPS L1 frequency (1.575 GHz) were monitored using four GPS

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Cited by 78 publications
(134 citation statements)
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“…5a). We have selected the period of 22:00-24:00 LT because throughout this time the scintillation-producing irregularities can be considered for practical purposes to drift at comparable velocities with the background plasma (Kil et al, 2000(Kil et al, , 2002Engavale et al, 2005). Before 22:00 LT, due to the presence of perturbation electric fields associated with the Rayleigh-Taylor instability, the irregularities are still growing and the values of V zonal may present great variability Engavale et al, 2005), whereas after 24:00 LT the scintillation-producing irregularities start to decay faster by cross-field diffusion (Basu et al, 1978).…”
Section: Ionospheric Irregularity Zonal Drift Velocitiesmentioning
confidence: 99%
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“…5a). We have selected the period of 22:00-24:00 LT because throughout this time the scintillation-producing irregularities can be considered for practical purposes to drift at comparable velocities with the background plasma (Kil et al, 2000(Kil et al, , 2002Engavale et al, 2005). Before 22:00 LT, due to the presence of perturbation electric fields associated with the Rayleigh-Taylor instability, the irregularities are still growing and the values of V zonal may present great variability Engavale et al, 2005), whereas after 24:00 LT the scintillation-producing irregularities start to decay faster by cross-field diffusion (Basu et al, 1978).…”
Section: Ionospheric Irregularity Zonal Drift Velocitiesmentioning
confidence: 99%
“…In the South American sector, the zonal drift of scintillationproducing irregularities has been studied in the last few decades through the detection of VHF geostationary satellite signals (Abdu et al, 1985;Basu et al, 1996;de Paula et al, 2010), from UHF geosynchronous satellite measurements Sheehan and Valladares, 2004), and through an L-band GPS-spaced antenna system (Kil et al, 2000(Kil et al, , 2002Ledvina et al, 2004;Kintner et al, 2004;Muella et al, 2013Muella et al, , 2014. Basu et al (1996) estimated the zonal drift of the kilometer-scale irregularities causing VHF scintillations above the equatorial site of Ancón (MLAT 1.46 • N) in Peru and at the low-latitude station of Agua Verde (MLAT 11.3 • S) in Chile.…”
Section: Introductionmentioning
confidence: 99%
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“…20,2011 corresponds to a decrease in the carrier to noise ratio of GPS signal down to 16.5 dB, which can be caused by ionospheric scintillation. The signal can be degraded by more than 20 dB for strong scintillation (Kil et al 2000).…”
Section: Effects Of Non-uniform Pseudorange Error For One Satellitementioning
confidence: 99%
“…[25] Works about GPS scintillations in Sã o Luís and Cachoeira Paulista make only brief comments about storm effects [e.g, Kil et al, 2000;Rodrigues et al, 2004]. BONELLI: GPS SCINTILLATION 6 of 9 S09D05 W W W. ag u .…”
mentioning
confidence: 99%