1999
DOI: 10.1016/s0273-1177(98)00239-7
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Microparticles in the geostationary orbit (GORID experiment)

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Cited by 17 publications
(4 citation statements)
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“…A practically identical twin instrument was operated on board the Galileo spacecraft, which was launched in 1989, and between 1995 and 2003 it was the first Jupiter-orbiting spacecraft (Grün et al 1992a). A third identical instrument (GORID), an engineering model of the Ulysses sensor, was operational in geostationary orbit on the Express telecommunication satellite between 1997 and 2002 (Drolshagen et al 1999). Finally, the Cassini spacecraft, launched in 1997, carries the Cosmic Dust Analyzer (CDA) which is an upgrade of the Ulysses instrument that is equipped with a time-of-flight mass spectrometer ).…”
Section: The Ulysses Dust Instrumentmentioning
confidence: 99%
“…A practically identical twin instrument was operated on board the Galileo spacecraft, which was launched in 1989, and between 1995 and 2003 it was the first Jupiter-orbiting spacecraft (Grün et al 1992a). A third identical instrument (GORID), an engineering model of the Ulysses sensor, was operational in geostationary orbit on the Express telecommunication satellite between 1997 and 2002 (Drolshagen et al 1999). Finally, the Cassini spacecraft, launched in 1997, carries the Cosmic Dust Analyzer (CDA) which is an upgrade of the Ulysses instrument that is equipped with a time-of-flight mass spectrometer ).…”
Section: The Ulysses Dust Instrumentmentioning
confidence: 99%
“…The Cassini spacecraft en route to Saturn crossed the interplanetary space between Jupiter and Saturn after its encounter with Jupiter on 31 December 2000 and before entering the Saturnian system on 1 July 2004, during Saturn Orbit Insertion (SOI). The Cassini spacecraft carries the Cosmic Dust Analyzer (CDA) instrument, successor of the dust instruments on board Ulysses, Galileo, and Gorid [ Grün et al , 1992b, 1992a; Drolshagen et al , 1999]. Like those instruments, CDA is able to determine the impact velocity and mass of the impactors.…”
Section: Introductionmentioning
confidence: 99%
“…doi:10.1016/j.asr.2005.03.060 a few cm); however measurements of micron to mm sized particles are generally obtained from in situ sampling. The meteoroid and debris populations can be investigated by active impact experiments (e.g., the Geostationary Orbit Impact Detector GORID; Drolshagen et al, 1999), or from the analysis of returned spaceflown surfaces. During the last three decades, several surfaces designed to sample the low Earth orbit impact environment have been deployed in space as dedicated experiments, and then returned to Earth to provide a wealth of information on the solid particle populations.…”
Section: Introductionmentioning
confidence: 99%