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arXiv 2408.01591astro-ph.SRphysics.space-ph
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均匀与连续分层大气中的磁流体力学(MHD)波

MHD waves in homogeneous and continuously stratified atmospheres

Paul S. Cally, Thomas J. Bogdan

AI总结:

本文系统梳理线性理想MHD波理论并推广至重力分层大气,重点分析波模转换、精确解及WKBJ和射线方法,并讨论其对太阳大气加热的意义。

摘要:

本文阐述了线性、理想磁流体力学(MHD)波(慢波、Alfvén波和快波)的基本方程、概念与模式,并将其推广至重力分层大气。研究特别关注波模转换,即全局波在穿过特定大气层时,其局部行为从一种模式转变为另一种模式。文中探讨了可获得的精确解,并介绍了程函方法——WKBJ与射线理论。尽管重点在于该主题的理论基础,但仍详细讨论了快/慢波及快/Alfvén波转换对太阳大气加热的意义。

英文摘要:

The basic equations, concepts, and modes of linear, ideal, MHD waves -- slow, Alfvén and fast -- are set out and generalised to gravitationally-stratified atmospheres. Particular attention is devoted to mode conversion, wherein the local behavior of a global wave changes from one mode to another in passing through particular atmospheric layers. Exact solutions are explored where available. Eikonal methods -- WKBJ and ray theory -- are described. Although our emphasis is on the theoretical underpinning of the subject, the solar atmospheric heating implications of fast/slow and fast/Alfvén conversions are discussed in detail.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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