首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Fast tailward flows in the plasma sheet boundary layer during a substorm on 9 March 2008: THEMIS observations
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Fast tailward flows in the plasma sheet boundary layer during a substorm on 9 March 2008: THEMIS observations

机译:THEMIS观测结果,在2008年3月9日的一次亚暴期间,血浆片边界层中快速向后流动:

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Tailward flows in the plasma sheet boundary layer (PSBL) were observed simultaneously by the five Time History of Events and Macroscale Interactions during Substorms (THEMIS) probes at down-tail distances X ~ 7.6 to ~17.6 R_E for ~10 min during an interval of successive substorm intensification in a storm time on 9 March 2008. The flows first occurred close to Earth and then propagated along the magnetic field lines in the PSBL with a speed of ~150-350 km s~(-1). We show that the occurrence of tailward flows is highly dependent on proximity to the plasma sheet boundary. Higher speeds occurred in the outer part of the PSBL, while either lower tailward speeds (or even earthward flows) were seen in the inner part of the PSBL. The tailward flow occurrence increased during magnetotail stretching and decreased or ceased during magnetic field dipolarizations. These PSBL tailward flows near the Earth can be understood as an outflow of the earthward flows that essentially empty the central plasma sheet. The tailward flows along the field line filled the void left behind by the dipolarization front.
机译:通过5个事件的时间历史和亚暴期间的宏观相互作用(THEMIS)探针,在距离X〜7.6到〜17.6 R_E的向下尾部距离〜10 min内,同时观察到了血浆片边界层(PSBL)的尾流,历时10分钟。在2008年3月9日的一次暴风雨中连续出现次暴雨。气流首先出现在地球附近,然后沿PSBL中的磁力线传播,速度约为150-350 km s〜(-1)。我们表明,向后流动的发生高度依赖于等离子体板边界的接近度。 PSBL的外部出现了较高的速度,而PSBL的内部则出现了较低的向后速度(甚至向地面流动)。向后流动的发生在磁尾拉伸期间增加,而在磁场双极化期间减少或停止。这些靠近地球的PSBL向后流动可理解为基本上使中央等离子板排空的向地流的流出。沿着磁力线的向后流动充满了双极化前沿留下的空隙。

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