Statistical study of thin current sheet evolution around substorm onset
Open Access
- 13 May 2004
- journal article
- magnetospheric physics
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 109 (A5)
Abstract
The spatial distribution of current sheet thinning in the substorm growth phase is examined statistically using Geotail data. The current density is calculated from the ion and electron velocity moments. It is found that the current sheet becomes thin before the onset mainly on the Earthward side of the initial near‐Earth neutral line (NENL) position and becomes less than 0.5 RE on average. However, on the tailward side of the NENL position, the current sheet becomes thin only after the onset. This result implies that the NENL forms at or near the tailward edge of the thin current sheet. An intense current sheet is formed in the center of the plasma sheet on average, but the largest current density is temporarily observed in the off‐neutral sheet region, indicating the formation of a double‐peaked current sheet. The current carriers becomes mainly electrons in the thin current sheet under the existence of the ambipolar electric field directed toward the neutral sheet.Keywords
This publication has 60 references indexed in Scilit:
- Evolution of the thin current sheet in a substorm observed by GeotailJournal of Geophysical Research, 2003
- Current sheet flapping motion and structure observed by ClusterGeophysical Research Letters, 2003
- Cluster observation of a bifurcated current sheetGeophysical Research Letters, 2003
- Fast flow during current sheet thinningGeophysical Research Letters, 2002
- Substorm dipolarization and recoveryJournal of Geophysical Research, 1999
- Two‐dimensional HaIl‐MHD simulation of current sheet dynamics during substorm growth phaseJournal of Geophysical Research, 1997
- A statistical survey of the central plasma sheetJournal of Geophysical Research, 1994
- Characteristics of ion flow in the quiet state of the inner plasma sheetGeophysical Research Letters, 1993
- Current carriers in the near‐Earth cross‐tail current sheet during substorm growth phaseGeophysical Research Letters, 1990
- The lower‐hybrid‐drift instability as a source of anomalous resistivity for magnetic field line reconnectionGeophysical Research Letters, 1977