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arXiv 1503.04141physics.space-ph
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CME内部的冲击:1997 - 2006年的性质综述

Shocks inside CMEs: A Survey of Properties from 1997 to 2006

N. Lugaz, C. J. Farrugia, C. W. Smith, K. Paulson

摘要:

我们报告了1997年至2006年在1天文单位的Wind和ACE测量的49个在日冕物质抛射(CME)内传播的快模前向激波。与典型的日冕物质抛射驱动的冲击相比,这些冲击在不同的上游条件下传播,其中上游Alfv{é}n速度的中值为85 km s $^{-1}$,质子$β= 0.08$和磁场强度为8 nT。这些激波速度很快,平均速度为590 km/s $^{-1}$,但强度较弱,平均阿尔夫{é}尼克马赫数为1.9。它们通常将磁场和密度压缩2-3倍。发现的最极端的上游条件是230 km/s $^{-1}$的快磁音速、0.02的等离子体$β$、740 km/s $^{-1}$的上游太阳风速度和0.5 cm $^{-3}$的密度。在这些复杂事件中,有19个与在Wind探测到地震后12小时内的强烈地磁暴(峰值Dst低于$-100$ nT)有关,15个与地震探测后3至9小时内的风暴时间Dst指数下降超过50 nT有关。我们还将它们与在更典型的上游条件下传播的45个冲击样本进行了比较。我们通过叠加历元分析显示了这些地震的平均性质,并对低$β$区的地震压缩比提出了一些分析考虑。由于大多数这些冲击是在后半部分的日冕物质抛射测量,我们得出结论,大约一半的冲击可能不会保持快速模式的冲击,因为它们通过整个日冕物质抛射传播,由于大的上游和磁音速。

英文摘要:

We report on 49 fast-mode forward shocks propagating inside coronal mass ejections (CMEs) as measured by Wind and ACE at 1 AU from 1997 to 2006. Compared to typical CME-driven shocks, these shocks propagate in different upstream conditions, where the median upstream Alfv{é}n speed is 85 km s$^{-1}$, the proton $β= 0.08$ and the magnetic field strength is 8 nT. These shocks are fast with a median speed of 590 km s$^{-1}$ but weak with a median Alfv{é}nic Mach number of 1.9. They typically compress the magnetic field and density by a factor of 2-3. The most extreme upstream conditions found were a fast magnetosonic speed of 230 km s$^{-1}$, a plasma $β$ of 0.02, upstream solar wind speed of 740 km s$^{-1}$ and density of 0.5 cm$^{-3}$. Nineteen of these complex events were associated with an intense geomagnetic storm (peak Dst under $-100$ nT) within 12 hours of the shock detection at Wind, and fifteen were associated with a drop of the storm-time Dst index of more than 50 nT between 3 and 9 hours after shock detection. We also compare them to a sample of 45 shocks propagating in more typical upstream conditions. We show the average property of these shocks through a superposed epoch analysis, and we present some analytical considerations regarding the compression ratios of shocks in low $β$ regimes. As most of these shocks are measured in the back half of a CME, we conclude that about half the shocks may not remain fast-mode shocks as they propagate through an entire CME due to the large upstream and magnetosonic speeds.

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