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SolarWind Discontinuity Interaction with the Bow Shock: Current Density Growth and Dawn-Dusk Asymmetry

机译:SolarWind不连续性与弓形激波的相互作用:电流密度增长和黎明-黄昏不对称性

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摘要

The solar wind is filled with various magnetic field fluctuations,and one of the most widespread types of such fluctuations is solar wind discontinuities.They are rapid highamplitude magnetic field rotations sharing properties of nonlinear Alfvén waves and plane plasma slabs.They are believed to play an important role in the interaction of the solar wind with the Earth's magnetosphere.Most studies of solar wind discontinuities are based on observations in pristine solar wind,often by solar wind monitors at L1.However,before interacting with the Earth's magnetosphere,solar wind discontinuities cross the bow shock and can change their properties.In this study,we investigate the transformation of discontinuities due to the bow shock crossing.We compiled a set of 100 high-amplitude (> 3 nT) discontinuities observed by ARTEMIS in the upstream of the bow shock and by THEMIS in the downstream from the bow shock crossing (in the Earth's magnetosheath).Comparison of discontinuity properties in the solar wind and magnetosheath demonstrates discontinuity thinning and current density increase in the magnetosheath.Although all considered solar wind discontinuities mostly resemble rotational discontinuities,in the magnetosheath they start having properties of tangential discontinuities.We reveal a clear dawn-dusk asymmetry of discontinuity properties that are likely related to the asymmetry of the ion foreshock. We discuss how solar wind discontinuity transformation at the bow shock crossing can alter their interaction with the Earth's magnetosphere.
机译:太阳风充满了各种磁场波动,而这种波动最普遍的类型之一是太阳风不连续性。它们是快速的高振幅磁场旋转,具有非线性阿尔芬波和平面等离子体板的特性。它们被认为在太阳风与地球磁层的相互作用中起着重要作用。大多数关于太阳风不连续性的研究都是基于对原始太阳风的观测,通常是通过L1的太阳风监测器。然而,在与地球磁层相互作用之前,太阳风的不连续性会越过弓形激波并改变其性质。在这项研究中,我们研究了由于弓形激波交叉引起的不连续性的转变。我们编制了一组 100 个高振幅 (> 3 nT) 不连续性,这些不连续性由 ARTEMIS 在弓形激波的上游和 THEMIS 在弓形激波交叉口下游(在地球磁鞘中)观察到。太阳风和磁鞘中不连续性的比较表明,磁鞘中的不连续性变薄和电流密度增加。尽管所有被认为的太阳风不连续性大多类似于旋转不连续性,但在磁鞘中,它们开始具有切向不连续性的性质。我们揭示了不连续性的明显黎明-黄昏不对称性,这可能与离子前震的不对称性有关。我们讨论了弓形激波交叉处的太阳风不连续性转换如何改变它们与地球磁层的相互作用。

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