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Annales Geophysicae An open-access journal of the European Geosciences Union
Ann. Geophys., 17, 1521-1527, 1999
http://www.ann-geophys.net/17/1521/1999/
doi:10.1007/s00585-999-1521-3
© European Geosciences Union 1999
 
31 Dec 1999
The magnetic field experiment onboard Equator-S and its scientific possibilities
K.-H. Fornacon1, H. U. Auster1, E. Georgescu2,3, W. Baumjohann2, K.-H. Glassmeier1, G. Haerendel2, J. Rustenbach2, and M. Dunlop4 1Institut für Geophysik und Meteorologie der Technischen Universität, D-38106 Braunschweig, Germany
2Max-Planck-Institut für extraterrestrische Physik, D-85740 Garching, Germany
3Institute of Space Sciences, Bucharest, Romania
4Imperial College, London SW7 2BZ, UK
Abstract. The special feature of the ringcore fluxgate magnetometer on Equator-S is the high time and field resolution. The scientific aim of the experiment is the investigation of waves in the 10–100 picotesla range with a time resolution up to 64 Hz. The instrument characteristics and the influence of the spacecraft on the magnetic field measurement will be discussed. The work shows that the applied pre- and inflight calibration techniques are sufficient to suppress spacecraft interferences. The offset in spin axis direction was determined for the first time with an independent field measurement by the Equator-S Electron Drift Instrument. The data presented gives an impression of the accuracy of the measurement.

Key words. Magnetospheric physics (instruments and techniques) · Space plasma physics (instruments and techniques)


Citation: Fornacon, K.-H., Auster, H. U., Georgescu, E., Baumjohann, W., Glassmeier, K.-H., Haerendel, G., Rustenbach, J., and Dunlop, M.: The magnetic field experiment onboard Equator-S and its scientific possibilities, Ann. Geophys., 17, 1521-1527, doi:10.1007/s00585-999-1521-3, 1999.
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