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Pressure-driven and ionosphere-driven modes of magnetospheric interchange instability
http://hdl.handle.net/2261/38138
http://hdl.handle.net/2261/38138a27c1a9a-944a-41d5-921e-b4a358371cea
名前 / ファイル | ライセンス | アクション |
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JGR_A114_a02224.pdf (299.0 kB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2016-12-28 | |||||
タイトル | ||||||
タイトル | Pressure-driven and ionosphere-driven modes of magnetospheric interchange instability | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題 | interchange instability | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | MHD instability | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | inner magnetosphere | |||||
主題Scheme | Other | |||||
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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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 | A general stability criterion for magnetospheric interchange instability, which includes an ionospheric destabilizing contribution, is derived for an arbitrary finite-β magnetospheric model satisfying the magnetohydrostatic force balance. The derivation is based on the magnetospheric energy principle. Unperturbed field-aligned currents in finite-β nonaxisymmetric magnetospheric models are assumed to close via diamagnetic currents in the magnetosphere or in the ionosphere. By exploiting the limit of a very large perpendicular wave number and the eikonal representation for the perpendicular plasma displacement, the magnetospheric interchange mode is shown to be compressible. In this limit the kink mode makes no contribution to the change in the magnetospheric potential energy. By using magnetospheric flux coordinates, the explicit form of the magnetospheric potential energy change is calculated for interchange perturbations, which do not bend magnetospheric magnetic fields. For a nonaxisymmetric finite-β magnetospheric model, a combined effect of the pressure gradient and field line curvature, not only in the meridional plane but also in the plane parallel to the longitudinal direction, is responsible for pressure-driven interchange instability. For an axisymmetric, north-south symmetric and low-β magnetospheric model, in which the magnetic field is approximated by a dipole field, the m = 1 or m = 2 ionosphere-driven mode, where m is the azimuthal mode number, has an upper critical equatorial β value for instability in the order of 1. Thus a substantial region of the inner magnetosphere or the near-Earth magnetosphere may be unstable against ionosphere-driven interchange instability caused by a horizontal plasma displacement on the spherical ionospheric surface | |||||
書誌情報 |
Journal of geophysical research. A 巻 114, p. A02224, 発行日 2009-02 |
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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/10.1029/2008JA013663 | |||||
権利 | ||||||
権利情報 | copyright 2009 by the American Geophysical Union | |||||
日本十進分類法 | ||||||
主題 | 450 | |||||
主題Scheme | NDC | |||||
出版者 | ||||||
出版者 | American Geophysical Union |