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arXiv 1706.05047physics.space-ph
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前震瞬态核内电子的费米加速

Fermi acceleration of electrons inside foreshock transient cores

Terry Z. Liu, San Lu, Vassilis Angelopoulos, Heli Hietala, Lynn B. Wilson

摘要:

最近观察到,地球弓形激波上游的前震瞬变将电子加速到其热能的许多倍。然而,这种加速是如何发生的尚不清楚。使用THEMIS案例研究,我们研究了一个子集的加速事件(247个事件中的31个),在前震瞬变与核心,表现出逐渐的电子能量增加伴随着低背景磁场强度和大幅度的磁波动。利用多个航天器上电子分布和能量增加率的演化,我们认为会聚前震瞬态压缩边界和弓形激波之间的费米加速是观测到的电子加速的原因。然后,我们表明,一维测试粒子模拟的理想费米加速模型在波动的领域规定的意见,可以重现所观察到的电子分布,能量增加率和俯仰角各向同性的演变,为我们的假设提供进一步的支持。因此,费米加速可能是主要的电子加速机制,至少在这一子集的前震瞬态核心。

英文摘要:

Foreshock transients upstream of Earth's bow shock have been recently observed to accelerate electrons to many times their thermal energy. How such acceleration occurs is unknown, however. Using THEMIS case studies, we examine a subset of acceleration events (31 of 247 events) in foreshock transients with cores that exhibit gradual electron energy increases accompanied by low background magnetic field strength and large-amplitude magnetic fluctuations. Using the evolution of electron distributions and the energy increase rates at multiple spacecraft, we suggest that Fermi acceleration between a converging foreshock transient's compressional boundary and the bow shock is responsible for the observed electron acceleration. We then show that a one-dimensional test particle simulation of an ideal Fermi acceleration model in fluctuating fields prescribed by the observations can reproduce the observed evolution of electron distributions, energy increase rate, and pitch-angle isotropy, providing further support for our hypothesis. Thus, Fermi acceleration is likely the principal electron acceleration mechanism in at least this subset of foreshock transient cores.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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