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Statistical analysis of severe magnetic fluctuations in the near-Earth plasma sheet observed by THEMIS-E

机译:THEMIS-E观测到的近地等离子体中严重磁起伏的统计分析

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摘要

We statistically analyzed severe magnetic fluctuations in the nightsidenear-Earth plasma sheet at 6–12  (Earth radii; 1  = 6371 km), because they are important for non-magnetohydrodynamics(non-MHD) effects in the magnetotail and are considered to be necessary forcurrent disruption in the inside-out substorm model. We used magnetic fielddata from 2013 and 2014 obtained by the Time History of Events and MacroscaleInteractions during Substorms E (THEMIS-E) satellite (sampling rate: 4 Hz).A total of 1283 severe magnetic fluctuation events were identified thatsatisfied the criteria ∕  0. 5, where and are the standard deviation and the average value of magnetic fieldintensity during the time interval of the local proton gyroperiod, respectively.We found that the occurrence rates of severe fluctuation events are 0.00118,0.00899, and 0.0238 % at 6–8, 8–10, and 10–12 ,respectively, and most events last for no more than 15 s. From theseoccurrence rates, we estimated the possible scale sizes of current disruptionby severe magnetic fluctuations as 3.83  by assuming thatfour substorms with 5 min intervals of current disruption occur every day.The fluctuation events occurred most frequently at the (distance in the geocentric solar magnetospheric coordinate system) close tothe model neutral sheet within 0.2 . Most events occur inassociation with sudden decreases in the auroral electrojet lower (AL) index and magnetic fielddipolarization, indicating that they are related to substorms. Sixty-twopercent of magnetic fluctuation events were accompanied by ion flow withvelocity   100 km s, indicating that the violation of iongyromotion tends to occur during high-speed flow in the near-Earth plasmasheet. The superposed epoch analysis also indicated that the flow speedincreases before the severe magnetic fluctuations. We discuss how both theinside-out and outside-in substorm models can explain this increase in flowspeeds before magnetic fluctuation events.
机译:我们从统计学上分析了6-12点夜间近地等离子板的严重磁波动(地球半径; 1 = 6371 km),因为它们对于磁尾中的非磁流体动力学(非MHD)效应很重要并且被认为是必要的由内而外的亚暴模型中的当前扰动。我们使用了2013年和2014年的事件数据和亚暴E期间大尺度相互作用(THEMIS-E)卫星获得的磁场数据(采样率:4 Hz),共发现1283次严重的磁起伏事件,满足∕> 0的标准.5,其中和是局部质子节肢动物时间间隔内的磁场强度的标准偏差和平均值。我们发现严重波动事件的发生率分别为0.00118,0.00899和0.0238%在6-8 ,8-10和10-12,大多数事件持续的时间不超过15s。从这些发生率中,我们假设每天发生5次最小电流间隔为5 min的四次亚暴,估计由严重的磁波动引起的电流破坏的可能规模为3.83。波动事件最频繁发生在(地心太阳磁层坐标系中的距离)靠近模型中性片0.2。大多数事件与极光电喷较低(AL)指数和磁场双极化的突然下降无关,发生的迹象表明它们与亚暴有关。磁力波动事件的62%伴随着离子流的速度> 100 km s,这表明在近地等离子板中的高速流动过程中倾向于发生离子陀螺运动。叠加的历元分析还表明,在剧烈的电磁波动之前,流速增加了。我们讨论了由内而外和由外而内的亚风暴模型如何解释磁波动事件发生之前流速的这种增加。

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