2002
DOI: 10.1109/tgrs.2002.1006371
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The spinning Astrid-2 satellite used for modeling the Earth's main magnetic field

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Cited by 12 publications
(7 citation statements)
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“…In flight, when the field changes rapidly over the full scale range, the instrument's performance was limited by the 1-2 nT ADC-non-linearities. The Earth's field modelling residuals were less than 5 nT rms , comparing favorably to the Ørsted modelling residuals of 2-3 nT rms , stemming mainly from the non-modelled magnetospheric perturbations (Merayo et al, 2002). Technical information on the instrument's noise and stability performance can be found in this paper and in references therein.…”
Section: Instrument Designmentioning
confidence: 72%
See 1 more Smart Citation
“…In flight, when the field changes rapidly over the full scale range, the instrument's performance was limited by the 1-2 nT ADC-non-linearities. The Earth's field modelling residuals were less than 5 nT rms , comparing favorably to the Ørsted modelling residuals of 2-3 nT rms , stemming mainly from the non-modelled magnetospheric perturbations (Merayo et al, 2002). Technical information on the instrument's noise and stability performance can be found in this paper and in references therein.…”
Section: Instrument Designmentioning
confidence: 72%
“…EMMA data were recently used to ascertain the Weimer 2K ionospheric electric field model (Eriksson et al, 2002). EMMA data have also been used as a complement to the Danish Ørsted satellite for mapping of the geomagnetic field (Merayo et al, 2002). …”
Section: Scientific Objectives and Resultsmentioning
confidence: 99%
“…The fluxgate technology has been improving simultaneously with the techniques of magnetic field sensing and now fluxgates are still the sensors that present the best magnetic properties for the measurement of the geomagnetic field. It has to be taken into account that an increase in the knowledge about the magnetic field of the Earth only can be achieved by means of very fine measurements since actual models of the field already reproduce the contribution of the core, the crust and the ionospheric phenomena to the global field, thanks to the data provided by POGO-Polar Orbiting Geophysical Observation missions (1967–1971), Magsat (1979), Astrid-2 (1998) [ 56 ], SAC-A (1998), Ørsted (1999), Komsat (1999), CHAMP (2000), ST-5 (2006) [ 15 ], etc.…”
Section: Magnetic Sensors For Space Missions the Implementation Of Mmentioning
confidence: 99%
“…Firstly, they are inexpensive, small and lightweight. Secondly, they are robust and complete in the sense that sun sensors and star sensors are vulnerable to occultation 1) . Furthermore, magnetic sensors are applicable to wide-range of body rate.…”
Section: Introductionmentioning
confidence: 99%