Trapped energetic electrons in the magnetosphere of Ganymede

被引:15
作者
Eviatar, A
Williams, DJ
Paranicas, C
McEntire, RW
Mauk, BH
Kivelson, MG
机构
[1] Tel Aviv Univ, Raymond & Beverly Sackler Fac Exact Sci, Dept Geophys & Planetary Sci, IL-69978 Tel Aviv, Israel
[2] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD 20742 USA
[3] Univ Calif Los Angeles, Inst Geophys, Los Angeles, CA 90024 USA
[4] Univ Calif Los Angeles, Dept Earth & Space Sci, Los Angeles, CA 90024 USA
关键词
D O I
10.1029/1999JA900450
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
On May 7, 1997, the Galileo orbiter flew through the magnetosphere of Ganymede and crossed flux tubes connected at both ends to the satellite. Energetic electrons, observed during this encounter by mea,ns of the Energetic Particle Detector on board Galileo, showed double loss cones and "butterfly" type pitch angle distributions, as has been noted in past publications. In addition, as the spacecraft flew toward Ganymede, both the shape and magnitude of the spectrum changed. The intensities decreased, with the greatest depletion observed at the lowest energies, and the monotonic slope characteristic of the Jovian environment was replaced by a rollover of the spectrum at the low-energy end. The spectra lead us to infer a strongly energy-dependent injection efficiency into the trapping region. As on previous encounters, the pitch angle distributions confirmed the position of the magnetopause as indicated by the magnetometer measurements, but the spectra remained Jovian until the trapping region was reached. Various physical mechanisms capable of generating the observed spectra and pitch angle distributions, including downstream reconnection insertion followed by magnetic gradient drift and absorption of the lowest-energy electrons by Ganymede and injection from Jovian flux tubes upstream are assessed.
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收藏
页码:5547 / 5553
页数:7
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