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Large-Scale Structure and Dynamics of the Magnetotails of Mercury, Earth, Jupiter and Saturn

机译:汞,地球,木星和土星的磁链的大型结构和动力学

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Spacecraft observations have established that all known planets with an internal magnetic field, as part of their interaction with the solar wind, possess well-developed magnetic tails, stretching vast distances on the nightside of the planets. In this review paper we focus on the magnetotails of Mercury, Earth, Jupiter and Saturn, four planets which possess well-developed tails and which have been visited by several spacecraft over the years. The fundamental physical processes of reconnection, convection, and charged particle acceleration are common to the magnetic tails of Mercury, Earth, Jupiter and Saturn. The great differences in solar wind conditions, planetary rotation rates, internal plasma sources, ionospheric properties, and physical dimensions from Mercury’s small magnetosphere to the giant magnetospheres of Jupiter and Saturn provide an outstanding opportunity to extend our understanding of the influence of such factors on basic processes. In this review article, we study the four planetary environments of Mercury, Earth, Jupiter and Saturn, comparing their common features and contrasting their unique dynamics.
机译:航天器的观测结果表明,所有已知的具有内部磁场的行星,在与太阳风相互作用的过程中,都具有发达的磁尾,这些磁尾在行星的夜侧延伸很宽的距离。在这篇评论文章中,我们重点关注水星,地球,木星和土星的磁尾翼,这四个行星具有发达的尾巴,并且多年来已被几艘航天器访问过。重新连接,对流和带电粒子加速的基本物理过程是水星,地球,木星和土星的磁尾所共有的。从水星的小磁层到木星和土星的巨大磁层,太阳风条件,行星自转速度,内部等离子体源,电离层性质以及物理尺寸的巨大差异为扩展我们对这些因素对基本影响的理解提供了绝佳的机会。流程。在这篇评论文章中,我们研究了水星,地球,木星和土星的四个行星环境,比较了它们的共同特征并对比了它们的独特动力。

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