抄録
A new method to estimate the spatial structure of the moving magnetohydrodynamic (MHD) system is presented. We integrate the Faraday's induction equation, [Formula Omitted], assuming that the system is one-dimensional. The spatial gradient direction, along which the integration is made, is determined by minimizing the residue of the integrated Faraday's equation against the observed magnetic field. This new method can be regarded as an extension of the conventional magnetic minimum variance method. Sample data analyses using this new method for magnetotail events are also presented.
本文言語 | 英語 |
---|---|
ページ(範囲) | 603-614 |
ページ数 | 12 |
ジャーナル | Journal of geomagnetism and geoelectricity |
巻 | 48 |
号 | 42496 |
DOI | |
出版ステータス | 出版済み - 1996 |
外部発表 | はい |
!!!All Science Journal Classification (ASJC) codes
- 環境科学(全般)
- 地球惑星科学(全般)