Fundamental Plasma Processes in Saturn's Magnetosphere

Fundamental Plasma Processes in Saturn's Magnetosphere
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土星磁层中的基本等离子体过程

DOI:
10.1007/978-1-4020-9217-6_11
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发表时间:
2009
期刊:
Journal of Geophysical Research: Space Physics
影响因子:
--
通讯作者:
R. Thorne
R. Thorne
中科院分区:
--
文献类型:
--
作者:
B. Mauk;D. Hamilton;T. Hill;G. Hospodarsky;Robert E. Johnson;C. Paranicas;E. Roussos;C. Russell;D. Shemansky;E. Sittler;R. Thorne

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在本章中,我们回顾了控制土星广阔空间环境或磁层的选定基本等离子体过程(有关全球背景,请参阅第 9 章)。写这篇文章的时候,我们对土星磁层的运作及其与地球和木星磁层的关系的理解已经达到了一定程度的成熟。在过去十年左右的时间里,我们对行星磁层的理解发生了爆炸式增长,部分原因是轨道航天器(伽利略号和卡西尼号)以及遥感设备(例如哈勃太空望远镜)的存在。本书和本章的目的是在成功返回并分析大量卡西尼号数据后,评估我们对土星磁层的理解。主要任务的结束为我们提供了一个机会来巩固新旧工作,为继续调查提供指导。
In this chapter, we review selected fundamental plasma processes that control the extensive space environment, or magnetosphere, of Saturn (see Chapter 9, for the global context). This writing occurs at a point in time when some measure of maturity has been achieved in our understanding of the operations of Saturn's magnetosphere and its relationship to those of Earth and Jupiter. Our understanding of planetary magnetospheres has exploded in the past decade or so partly because of the presence of orbiting spacecraft (Galileo and Cassini) as well as remote sensing assets (e.g., Hubble Space Telescope). This book and chapter are intended to take stock of where we are in our understanding of Saturn's magnetosphere following the successful return and analysis of extensive sets of Cassini data. The end of the prime mission provides us with an opportunity to consolidate older and newer work to provide guidance for continuing investigations.
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