期刊
GEOPHYSICAL RESEARCH LETTERS
卷 49, 期 23, 页码 -出版社
AMER GEOPHYSICAL UNION
DOI: 10.1029/2022GL098474
关键词
Ganymede; radiation belt; radiation cavity; magnetic trapping; open-closed field lines; Juno
Based on recent flyby data from the Juno spacecraft and reanalysis of past measurements from the Galileo spacecraft, this study examines the radiation environment around Ganymede, a moon of Jupiter. The study finds that Ganymede is surrounded by a radiation cavity with lower intensities compared to Jupiter. Radiation belts are also present in the core of the cavity, with similar intensity to Jupiter for ions but lower for electrons. The formation of these radiation belts requires processes beyond steady influx and accumulation of particles from Jupiter.
While planetary radiation belts are all embedded within the low energy solar wind, Ganymede is in the unique situation of being surrounded by the energetic particles of Jupiter's magnetosphere. Here we study Ganymede's environment based the recent flyby of Juno, as well as through reanalysis of past measurements from the Galileo spacecraft. We find that Ganymede is surrounded by a radiation cavity with intensities that are lower compared to Jupiter. Particles are lost in the cavity due to absorption by Ganymede that is likely enhanced by scattering. In the core of the cavity we find radiation belts. Their intensities are comparable to Jupiter for ions but lower for electrons. The radiation belts form peaks in phase space density, which indicates that they cannot be produced through steady inward influx and accumulation of Jupiter particles. Other processes are needed such as local acceleration, or time dependent transport and loss processes.
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