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首页> 外文期刊>Journal of atmospheric and solar-terrestrial physics >Geotail spacecraft observations of plasma flow rotations at magnetic field dipolarization in near-tail during substorm expansion
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Geotail spacecraft observations of plasma flow rotations at magnetic field dipolarization in near-tail during substorm expansion

机译:地尾航天器在亚暴扩张过程中近尾磁场双极化时等离子体流旋转的观测

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The magnetic field dipolarization at near-tail is one of the key elements in the substorm phenomena, and it often accompanies the plasma flow in tail in some pattern. In this paper, we present 4 events of dipolarization observed from the Geotail satellite, in which the plasma flow rotates in X-Y plane. We found them out of 30 events, identified for 8 months period while Geotail was in the near-tail plasma sheet region defined by X_(GSE) > -15R_E and |Y_(GSE)| < 10R_E. In some cases of those 4 events we find flow rotations that begin nearly simultaneously with the dipolarization initiation and continues afterward for some time. In the other cases, they even precede the initiation of dipolarization by some minutes and continue throughout the maximum interval of the remaining dipolarization period. These flow rotations reveal no features of bursty bulk flows (BBF) and the speed of flow components is moderate, less than ~300 km/s. Also, flow rotations presented here are distinguished from the previously reported ones which appear only after, and thus presumably caused by, the passage of the earthward BBF (thus seen only well after the initiation of the dipolarization). Overall, we find difficulties and inconsistencies in relating the observed flow rotations at dipolarization to BBF as a possible cause. Based on intuitive ground, instead we suggest an alternative, though tentative, possibility that they may be a manifestation of some near-tail instability during the substorm expansion.
机译:近尾磁场的双极化是亚暴现象中的关键因素之一,它经常以某种形式伴随着尾部的等离子体流。在本文中,我们介绍了从Geotail卫星观测到的4个双极化事件,其中等离子流在X-Y平面中旋转。我们在30个事件中发现了它们,确定了8个月,而Geotail处于由X_(GSE)> -15R_E和| Y_(GSE)|定义的近尾血浆片区域。 <10R_E。在这4个事件的某些情况下,我们发现流动旋转几乎与偶极极化开始同时开始,然后持续一段时间。在其他情况下,它们甚至在引发偶极极化之前几分钟,并在剩余的偶极极化周期的最大间隔内持续。这些流动旋转没有显示出突发性大流量(BBF)的特征,流动分量的速度适中,小于〜300 km / s。另外,此处介绍的流体旋转与先前报道的流体旋转不同,后者仅在向地BBF通过之后才出现,因此大概是由地球BBF的通过引起的(因此只有在双极化开始后才能看到)。总的来说,我们发现在将极化时观察到的流体旋转与BBF相关联方面存在困难和不一致之处是可能的原因。相反,基于直观的观点,我们建议了一种替代方法(虽然是初步的),但可能是亚暴扩张期间一些近尾不稳定的表现。

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