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Interplanetary shock-bow shock interaction: Comparison of a global MHD model and observation

机译:行星际冲击-弓形冲击相互作用:全球MHD模型与观测的比较

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A fast forward shock passing through the bow shock would generate a train of new discontinuities that differ with the distance from the Sun-Earth line. However, interplanetary (IP) shocks are often followed by a rotation of the interplanetary magnetic field (IMF) over a large angle and a presence of this rotation can modify the interaction process. The present paper analyzes in detail one IP shock where data measured by Wind are used as an input to a global BATS-R-US MHD model and the model prediction is compared with Geotail magnetosheath observations. The study is based on three runs of the global MHD model that use different modifications of upstream conditions. We have found that (1) about 45% of IP shocks is followed by a significant IMF rotation within 15 min after the shock ramp; (2) the IMF rotation modifies the dynamics of the magnetospheric response to the IP shock arrival; (3) a train of new discontinuities created by an interaction of the IP shock with bow shock can be identified in MHD simulations as well as in the experimental data; and (4) a new discontinuity is created by the interaction of the IMF rotation with the bow shock. (C) 2014 Published by Elsevier Ltd.
机译:通过弓形冲击的快进冲击会产生一系列新的不连续性,这些不连续性与距太阳地球线的距离不同。但是,行星际(IP)冲击通常伴随着行星际磁场(IMF)在大角度上的旋转,并且这种旋转的存在会改变相互作用过程。本文详细分析了一次IP冲击,其中使用Wind测量的数据作为全球BATS-R-US MHD模型的输入,并将模型预测与Geotail磁石震荡观测结果进行比较。该研究基于使用上游条件的不同修改的全球MHD模型的三个运行。我们发现(1)大约45%的IP冲击后,在冲击斜坡后15分钟内,IMF会明显旋转; (2)IMF旋转改变了磁层对IP冲击到达的响应动力学; (3)可以在MHD模拟以及实验数据中识别出IP冲击与弓形冲击相互作用产生的一系列新的不连续性; (4)IMF旋转与船首冲击的相互作用产生了新的不连续性。 (C)2014由Elsevier Ltd.出版

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