地球磁层黄昏侧翼区的低杂波和孤波

IF 4.6 Q2 MATERIALS SCIENCE, BIOMATERIALS
Neetasha Arya, Amar Kakad
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引用次数: 0

摘要

各种航天器任务在磁层顶附近探测到了各种等离子体波。在本文中,我们利用磁层多尺度(MMS)飞行任务提供的高分辨率数据,介绍了在地球磁层黄昏侧翼区域同时观测到的较低混合波和离子孤波的新情况。所有四个 MMS 航天器在从地球磁层到磁鞘的穿越过程中都持续观测到了这种波的活动。我们的分析表明,由低混合漂移不稳定性驱动的低混合漂移波与密度梯度相关。此外,分析表明,整个离子群都会漂移,从而驱动离子孤波。研究发现,这些波在地球磁层黄昏侧翼区域的粒子加热中起着至关重要的作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Lower hybrid and solitary waves in dusk flank region of the Earth’s magnetosphere
A variety of plasma waves have been detected in the vicinity of the magnetopause by various spacecraft missions. In this paper, utilizing high-resolution data from the Magnetospheric Multiscale (MMS) mission, we present new observations of simultaneous lower hybrid and ion solitary waves in the dusk flank region of Earth’s magnetosphere. All four MMS spacecraft consistently observed this wave activity during their traversal from Earth’s magnetosphere to the magnetosheath. Our analysis suggests that the lower hybrid drift waves, driven by lower-hybrid drift instability, were observed in correlation with density gradients. Furthermore, the analysis indicates that the entire ion bulk population drifts, which drives ion solitary waves. It is found that these waves play a crucial role in particle heating in the dusk flank region of Earth’s magnetosphere.
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来源期刊
ACS Applied Bio Materials
ACS Applied Bio Materials Chemistry-Chemistry (all)
CiteScore
9.40
自引率
2.10%
发文量
464
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