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  1. 115 理学系研究科・理学部
  2. 06 地球惑星科学専攻
  3. 1150610 学術雑誌論文
  1. 0 資料タイプ別
  2. 10 学術雑誌論文
  3. 014 自然科学

Kelvin-Helmholtz Instability at the Magnetospheric Boundary : Dependence on the Magnetosheath Sonic Mach Number

http://hdl.handle.net/2261/38131
http://hdl.handle.net/2261/38131
0bfd5793-68e6-4e2e-9ce2-de13382f3c91
名前 / ファイル ライセンス アクション
JGR_A094_NA07_10655.pdf JGR_A094_NA07_10655.pdf (2.2 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2010-11-18
タイトル
タイトル Kelvin-Helmholtz Instability at the Magnetospheric Boundary : Dependence on the Magnetosheath Sonic Mach Number
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
著者 Miura, Akira

× Miura, Akira

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Miura, Akira

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著者所属
著者所属 Department of Earth and Planetary Physics, University of Tokyo
抄録
内容記述タイプ Abstract
内容記述 It has recently been demonstrated, by means of a two-dimensional MHD simulation, that a finite thick velocity shear layer with super-Alfvénic velocity jump at the magnetospheric boundary is unstable to the Kelvin-Helmholtz (K-H) instability no matter how large the magnetosheath sonic Mach number (MS ); a result suggesting that the tail flank boundary of the magnetosphere is unstable to the K-H instability. In order to investigate this consequence further, the dependence of the development of the K-H instability on MS is studied in detail. For all magnetosheath sonic Mach numbers a velocity boundary layer is formed by the instability inside of the magnetopause, and it becomes wider for a smaller magnetosheath sonic Mach number. A flow vortex is excited at the inner edge of the velocity boundary layer for all sonic Mach numbers, and the magnetopause boundary is more highly nonlinearly corrugated by the instability for a smaller sonic Mach number. The net energy and momentum flux densities into the magnetosphere are calculated just prior to the saturation stage; for 1.0 < MS < 3.0 the energy flux density into the magnetosphere is approximated by 0.054 MS ρ0 CS ³/2 = 0.045V 0 p0 (where ρ0 is the unperturbed magnetosheath plasma density, p0 is the unperturbed magnetosheath pressure, V 0 is the unperturbed magnetosheath flow velocity, and CS is the magnetosheath sound speed), and the momentum flux density into the magnetosphere or the tangential (shearing) stress at the boundary is approximated by 0.083p0. The anomalous viscosity by the instability decreases in the absolute magnitude with increasing MS ; this result suggests that the dayside (except the subsolar region) and the dawn-dusk magnetopauses, where the magnetosheath flow remains subsonic, are the most viscous parts of the boundary, although the tail flanks are also found to be viscous enough for the viscous interaction. The structure of the weak shock in the magnetosheath developed from the K-H instability and the asymptotic eigenmode structure of the instability are elucidated. The relevance of the simulation results to the viscous interaction and a ULF wave generation is finally discussed.
書誌情報 Journal of geophysical research. A

巻 97, 号 7, p. 10655-10675, 発行日 1992-07
ISSN
収録物識別子タイプ ISSN
収録物識別子 01480227
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA10819721
DOI
識別子タイプ DOI
関連識別子 info:doi/10.1029/92JA00791
権利
権利情報 copyright 1992 by the American Geophysical Union
日本十進分類法
主題Scheme NDC
主題 450
出版者
出版者 American Geophysical Union
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