2012
DOI: 10.5194/amt-5-1-2012
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Identification and localization of layers in the ionosphere using the eikonal and amplitude of radio occultation signals

Abstract: Abstract. By using the CHAllenge Minisatellite Payload (CHAMP) radio occultation (RO) data, a description of different types of the ionospheric impacts on the RO signals at the altitudes 30-90 km of the RO ray perigee is given and compared with the results of measurements obtained earlier in the satellite-to-Earth communication link at frequency 1.5415 GHz. An analytical model is introduced for describing propagation of radio waves in a stratified medium consisting of sectors with spherically symmetric refract… Show more

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Cited by 27 publications
(19 citation statements)
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References 41 publications
(59 reference statements)
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“…We position the phase screen in the plane crossing the Earth's center and perpendicular to the incident rays. The occultation geometry has been discussed in many papers: Vorob'ev and Krasil'nikova (1994), Ware et al (1996), Gorbunov and Lauritsen (2004), Cornman et al (2004), and Pavelyev et al (2012), as well as further references therein. The phase screen has been discussed in Hubbard et al (1978), Woo et al (1980), Gurvich (1984), and Gurvich and Brekhovskikh (2001).…”
Section: -D Models Of Refractivity Fluctuation Spectramentioning
confidence: 99%
“…We position the phase screen in the plane crossing the Earth's center and perpendicular to the incident rays. The occultation geometry has been discussed in many papers: Vorob'ev and Krasil'nikova (1994), Ware et al (1996), Gorbunov and Lauritsen (2004), Cornman et al (2004), and Pavelyev et al (2012), as well as further references therein. The phase screen has been discussed in Hubbard et al (1978), Woo et al (1980), Gurvich (1984), and Gurvich and Brekhovskikh (2001).…”
Section: -D Models Of Refractivity Fluctuation Spectramentioning
confidence: 99%
“…The radio occultation (RO) method employs the highly-stable radio waves transmitted at two GPS frequencies 1 f  1575.42 MHz and 2 f  1227.60 MHz by the GPS satellites and recorded at a GPS receiver onboard low Earth orbiting (LEO) satellite to remote sense the Earth's ionosphere and neutral atmosphere [4,5,10,11,17,[23][24][25][26][27][28][29][30][31][32][33][34][35][36][37][38][39][40][41][42]46,47,[52][53][54][55][56][59][60][61]. When applied to ionospheric investigations the RO method may be considered as a global tool and can be compared with the global Earth-and space-based radio tomography [42,43].…”
Section: Application Of Gps Ro Methods To Study the Atmosphere And Ionmentioning
confidence: 99%
“…The rest of the measurements were done in rural or marine areas, relatively far away from pollution sources. A detailed description of the sites and observations can be found in Gó mez- Amo et al (2012a) for the campaigns carried out in Madrid and El Arenosillo. The observation station at Valencia is described by Estellé s et al (2007).…”
Section: Microtops Observationsmentioning
confidence: 99%
“…The analyses show that a linear interpolation between the consecutive calibrations produces the best results, also during the years without calibrations, against the Brewers The same calibration strategy was adopted also in this study. In addition, the Microtops procedure to improve the data quality suggested by Gó mez-Amo et al (2012a) was also implemented, and only the series of three or five observations within 1 min which display standard deviation of the signals less than 2% and standard deviation of the AOD at 1020 nm less than 0.015 have been used (Gó mez-Amo et al, 2012a).…”
Section: Microtops Calibration and Data Qualitymentioning
confidence: 99%
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