Collisionless Shocks: Contemporary State After Three Quarters of a Century of Research

IF 38.5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
M. Gedalin, M. Balikhin, V. Krasnoselskikh
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引用次数: 0

Abstract

The collisionless shock research started in the late 1950s. Since then, plenty of data have been accumulated due to the large number of missions in the heliosphere, providing in situ measurements of the fields and particles. The quality of these measurements has vastly improved, especially in the last two decades. Much more data is available for analysis than is already analyzed. Theoretical studies received a push in 1966, when it was shown that shocks are formed due to the interplay between the nonlinear steepening and dispersive broadening of the magnetic field profile. At present, it is a common point of view that shocks are essentially shaped by the kinetics of ions. So far, we achieved a good semi-quantitative understanding of the ion heating in low-Mach number shocks and the relation of this process to the magnetic profile, and a qualitative understanding of the ion reflection and the nature of the well-structured magnetic field. Rippled and nonstationary quasi-perpendicular shocks have been observed, and theory is being developed.

Abstract Image

无碰撞冲击:四分之三世纪研究后的当代状态
无碰撞冲击研究始于20世纪50年代末。从那时起,由于在日球层进行了大量的任务,积累了大量的数据,提供了对磁场和粒子的现场测量。这些测量的质量有了很大的提高,尤其是在过去的二十年里。可供分析的数据比已经分析的要多得多。理论研究在1966年得到了推动,当时表明冲击是由于磁场剖面的非线性陡增和色散展宽之间的相互作用而形成的。目前,一种普遍的观点认为,冲击本质上是由离子动力学形成的。到目前为止,我们对低马赫数激波中的离子加热及其与磁剖面的关系有了较好的半定量认识,对离子反射和结构良好的磁场的性质有了定性认识。波纹和非平稳的准垂直激波已经被观测到,理论正在发展中。
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来源期刊
Reviews of Geophysics
Reviews of Geophysics 地学-地球化学与地球物理
CiteScore
50.30
自引率
0.80%
发文量
28
审稿时长
12 months
期刊介绍: Geophysics Reviews (ROG) offers comprehensive overviews and syntheses of current research across various domains of the Earth and space sciences. Our goal is to present accessible and engaging reviews that cater to the diverse AGU community. While authorship is typically by invitation, we warmly encourage readers and potential authors to share their suggestions with our editors.
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