2006
DOI: 10.1016/j.pss.2005.10.016
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ICE, the electric field experiment on DEMETER

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Cited by 312 publications
(230 citation statements)
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“…[14] The DEMETER plasma wave instrument (ICE) [Berthelier et al, 2006] was used to detect the VLF (up to 20 kHz) and quasi-static electric field (frequency range 0-1.25 kHz). Langmuir probe [Lebreton et al, 2006] was used to measure electron density and the Magnetic Search Coil (IMSC) instrument [Parrot et al, 2006] for magnetic field measurements.…”
Section: Experiments Resultsmentioning
confidence: 99%
“…[14] The DEMETER plasma wave instrument (ICE) [Berthelier et al, 2006] was used to detect the VLF (up to 20 kHz) and quasi-static electric field (frequency range 0-1.25 kHz). Langmuir probe [Lebreton et al, 2006] was used to measure electron density and the Magnetic Search Coil (IMSC) instrument [Parrot et al, 2006] for magnetic field measurements.…”
Section: Experiments Resultsmentioning
confidence: 99%
“…DEMETER is a French satellite launched at the end of June 2004, and orbiting at an altitude of about 710 km along approximately a circular orbit with an inclination of 98.3 • . We use the waveform of one component of the electric field measurement in the VLF frequency range by the ICE experiment (Berthelier et al, 2006). The waveform is available when the satellite is in the burst mode.…”
Section: Satellite Vlf Data and The Whistler Time Determinationmentioning
confidence: 99%
“…The sensitivities of the electric field antenna onboard DEME-TER satellite are 0.1 µV m −1 Hz −1/2 at 100 Hz (Berthelier et al, 2006) which means when the electric field of incident wave exceeds 1 V m −1 at the altitude of 50 km, the disturbance can be detected by DEMETER satellite. Xiong (2001) has pointed out that when the seismic charge density is 10 −4 -10 −5 C m −2 , the electric field can reach 10 3 -10 4 V m −1 at 50 km altitude in the late pre-seismic stages in a 100 km 2 region.…”
Section: The Electric Field Variations Before Earthquakesmentioning
confidence: 99%