Dual spacecraft observations of lobe magnetic field perturbations before, during and after plasmoid release

Dual spacecraft observations of lobe magnetic field perturbations before, during and after plasmoid release
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双航天器观测等离子体团释放之前、期间和之后的波瓣磁场扰动

DOI:
10.1029/1999gl003606
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发表时间:
1999
影响因子:
5.2
通讯作者:
P. Sutcliffe
P. Sutcliffe
中科院分区:
地球科学1区
文献类型:
--
作者:
J. Slavin;M. Hesse;C. Owen;S. Taguchi;D. Fairfield;R. Lepping;S. Kokubun;T. Mukai;A. Lui;R. R. Anderson;H. Matsumoto;P. Sutcliffe

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本文研究了IMP 8和Geotail于1995年1月29日在一次亚暴期间返回的数据集,该亚暴导致了等离子体团的喷射。这两个航天器(s/c)位于尾部的北叶,都观察到一个移动压缩区(TCR)。我们表明,在这种情况下,双S/C测量可以用来模拟所有三个维度的基本等离子体团,并估计其膨胀率。对于这一事件,等离子体团的尺寸ΔX = 18,ΔY = 30,ΔZ = 10 Re是由IMP 8和Geotail观测确定的。此外,在从IMP 8移动到Geotail所需的1.5分钟内,TCR的振幅增加了1.2倍。使用磁通量守恒模型,这种波瓣压缩的增加意味着下面的等离子体团正在以140公里/秒的速度膨胀。最后,在等离子体团喷射之后,波瓣磁场的重新配置将磁通量管移动到等离子体团后面的尾流中,在那里它们将变得可用于馈送重连区域。
This study examines a data set returned by IMP 8 and Geotail on January 29, 1995 during a substorm which resulted in the ejection of a plasmoid. The two spacecraft (s/c) were situated in the north lobe of the tail and both observed a traveling compression region (TCR). We show that in this instance dual s/c measurements can be used to model all three dimensions of the underlying plasmoid and to estimate its rate of expansion. For this event plasmoid dimensions of ΔX ∼18, ΔY ∼30, and ΔZ ∼10 Re are determined from the IMP 8 and Geotail observations. Furthermore, a factor of ∼2 increase in the amplitude of the TCR occurred in the 1.5 min it took to move from IMP 8 to Geotail. Modeled using conservation of magnetic flux, this increase in lobe compression implies that the underlying plasmoid was expanding at a rate of ∼140 km/s. Finally, a reconfiguration of the lobe magnetic field followed plasmoid ejection which moved magnetic flux tubes into the wake behind the plasmoid where they would become available to feed the reconnection region.