| タイトル | A mechanism for magnetospheric substorms |
| 本文（外部サイト） | http://hdl.handle.net/2060/19960000800 |
| 著者（英） | Erickson, G. M.; Heinemann, M. |
| 著者所属（英） | Boston Univ. |
| 発行日 | 1994-01-01 |
| 言語 | eng |
| 内容記述 | Energy-principle analysis performed on two-dimensional, self-consistent solutions for magnetospheric convection indicates that the magnetosphere is unstable to isobaric (yet still frozen-in) fluctuations of plasma-sheet flux tubes. Normally, pdV work associated with compression maintains stability of the inward/outward oscillating normal mode. However, if Earth's ionosphere can provide sufficient mass flux, isobaric expansion of flux tubes can occur. The growth of a field-aligned potential drop in the near-Earth, midnight portion of the plasma sheet, associated with upward field-aligned currents responsible for the Harang discontinuity, redistributes plasma along field lines in a manner that destabilizes the normal mode. The growth of this unstable mode results in an out-of-equilibrium situation near the inner edge. When this occurs over a downtail extent comparable to the half-thickness of the plasma sheet, collapse ensues and forces thinning of the plasma sheet whereby conditions favorable to reconnection occur. This scenario for substorm onset is consistent with observed upward fluxes of ions, parallel potential drops, and observations of substorm onset. These observations include near Earth onset, pseudobreakups, the substorm current wedge, and local variations of plasma-sheet thickness. |
| NASA分類 | GEOPHYSICS |
| レポートNO | 96N10800
NASA-CR-199342
NAS 1.26:199342 |
| 権利 | No Copyright |
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