The Radiation Belts of Jupiter and Saturn

E. Roussos, P. Kollmann
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引用次数: 15

Abstract

The era of outer planet orbiters (Galileo, Juno and Cassini) is advancing our understanding of how the radiation belts of Jupiter and Saturn are structured, form and evolve well beyond what had been possible during the age of flyby missions and ground-based observations. The nearly two decades-long datasets of these missions, in the context of detailed and long-term observations of Earth's radiation belts, highlight which of the processes that accelerate particles to relativistic kinetic energies and limit their flux intensity can be considered more universal, and thus key for most extraterrestrial magnetospheres, and which reflect the unique aspects of each planet and its magnetospheric system. In this chapter we focus on the in-situ radiation belt observations in the context of theory, simulations and relevant measurements by Earth-based observatories. We describe both the average state and the time variations of Jupiter's and Saturn's radiation belts and associate them with specific physical processes.
木星和土星的辐射带
外行星轨道飞行器(伽利略号、朱诺号和卡西尼号)的时代正在推进我们对木星和土星辐射带的结构、形成和演变的理解,远远超出了飞越任务和地面观测时代的可能。在对地球辐射带进行详细和长期观测的背景下,这些任务近20年的数据集突出了哪些过程可以将粒子加速到相对论动能并限制其通量强度,从而可以被认为是更普遍的,从而对大多数地外磁层至关重要,并且反映了每个行星及其磁层系统的独特方面。在本章中,我们主要从理论、模拟和地面观测的相关测量三个方面对原位辐射带观测进行了介绍。我们描述了木星和土星辐射带的平均状态和时间变化,并将它们与特定的物理过程联系起来。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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