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利用ARTEMIS数据绘制月球尾流电势结构

Mapping the Lunar Wake Potential Structure With ARTEMIS Data.

作者信息

Xu Shaosui, Poppe Andrew R, Halekas Jasper S, Mitchell David L, McFadden James P, Harada Yuki

机构信息

Space Sciences Laboratory, University of California, Berkeley, CA, USA.

Department of Physics and Astronomy, University of Iowa, Iowa City, IA, USA.

出版信息

J Geophys Res Space Phys. 2019 May;124(5):3360-3377. doi: 10.1029/2019ja026536. Epub 2019 Apr 23.

Abstract

The refilling of the lunar wake is relatively well explained by the theory of 1-D plasma expansion into a vacuum; however, the field-aligned wake potential is not a directly measured quantity, and thus, a statistical analysis of wake potentials at high altitudes has not been previously performed. In this study, we obtain the wake potential by comparing the field-aligned electron distributions inside and outside of the lunar wake measured by the two probes of the Acceleration, Reconnection, Turbulence, and Electrodynamics of Moon's Interaction with the Sun (ARTEMIS) mission. The derived potentials from ARTEMIS data vary with solar wind electron temperature and bulk flow velocity as the theory predicts. We also expand the 1-D plasma theory to 2-D in the plane of the interplanetary magnetic field and the solar wind velocity to examine how a tilted interplanetary magnetic field affects the wake potential structure. As the expansion time for the two sides of the wake differs, a wake potential asymmetry is developed in our model. This asymmetry is confirmed by the data-derived wake potentials. Moreover, ambipolar electric fields are obtained from both the modeled and data-derived wake potentials and show good agreement. Lastly, we examine the effects of the solar wind strahl-electron population on the wake potential structure, which appears to cause a net potential difference across the lunar shadow. This may imply that the disturbance of the wake plasma expansion extends farther outside the wake than previous plasma-expansion theories have predicted.

摘要

月球尾迹的再填充现象可以用一维等离子体向真空膨胀的理论较好地解释;然而,场向尾迹电势并非直接测量的量,因此此前尚未对高海拔处的尾迹电势进行统计分析。在本研究中,我们通过比较由月球与太阳相互作用的加速、重联、湍流及电动力学(ARTEMIS)任务的两个探测器测量的月球尾迹内外的场向电子分布来获得尾迹电势。从ARTEMIS数据推导得出的电势如理论预测的那样随太阳风电子温度和整体流速而变化。我们还将一维等离子体理论扩展到行星际磁场和太阳风速度平面内的二维情况,以研究倾斜的行星际磁场如何影响尾迹电势结构。由于尾迹两侧的膨胀时间不同,我们的模型中产生了尾迹电势不对称性。这种不对称性在由数据推导得出的尾迹电势中得到了证实。此外,从模型和数据推导得出的尾迹电势中都获得了双极电场,且二者吻合良好。最后,我们研究了太阳风散逸层电子群体对尾迹电势结构的影响, 这似乎会在月球阴影区产生净电势差。这可能意味着尾迹等离子体膨胀的扰动在尾迹外的延伸范围比之前的等离子体膨胀理论所预测的更远。

相似文献

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Mapping the Lunar Wake Potential Structure With ARTEMIS Data.利用ARTEMIS数据绘制月球尾流电势结构
J Geophys Res Space Phys. 2019 May;124(5):3360-3377. doi: 10.1029/2019ja026536. Epub 2019 Apr 23.
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