Statistical Study on the Solar Wind Turbulence Spectra Upstream of Mars

Zhuxuan Zou, Yuming Wang, Zhenpeng Su, Long Cheng, Zhiyong Wu, Tielong Zhang, Guoqiang Wang, Sudong Xiao, Yutian Chi, Zonghao Pan, Xinjun Hao, Yiren Li and Kai Liu
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Abstract

We statistically analyze the power spectral density (PSD) of magnetic field turbulence in the upstream solar wind of the Martian bow shock by investigating the data from Tianwen-1 and Mars Atmosphere and Volatile Evolution (MAVEN) during 2021 November 13 and December 31. The spectral indices and break frequencies of these PSDs are automatically identified. According to the profiles of the PSDs, we find that they could be classified into three types: A, B, and C. Only less than a quarter of the events exhibit characteristics similar to the 1 au PSDs (Type A). We observe the energy injection in more than one-third of the events (Type B), and the injected energy usually results in the steeper spectral indices of the dissipation ranges. We find the absence of the dissipation range in over one third of the PSDs (Type C), which is likely due to the dissipation occurring at higher frequencies rather than proton cyclotron resonant frequencies. We also find that the two spacecraft observed different types of PSDs in more than half of the investigated episodes, indicating significant variability upstream of the Martian bow shock. For example, the Type-B PSDs are more often seen by Tianwen-1, which was near the flank of the bow shock, than by MAVEN near the nose. This statistical study demonstrates the complicated turbulent environment of the solar wind upstream of the Martian bow shock.
火星上游太阳风湍流谱的统计研究
利用2021年11月13日和12月31日“天文一号”和火星大气挥发物演化(MAVEN)数据,统计分析了火星弓形激波上游太阳风磁场湍流的功率谱密度(PSD)。自动识别这些psd的频谱指数和断裂频率。根据psd的特征,我们发现它们可以分为三种类型:A、B和c。只有不到四分之一的事件具有与1 au psd相似的特征(A型)。我们在三分之一以上的事件(B型)中观察到能量注入,注入的能量通常导致耗散范围的谱指数更陡。我们发现超过三分之一的psd (C型)没有耗散范围,这可能是由于耗散发生在更高的频率而不是质子回旋加速器共振频率。我们还发现,两个航天器在一半以上的调查事件中观测到不同类型的psd,这表明火星弓形激波上游有显著的变化。例如,b型psd更常被靠近弓形激波侧面的“天文号”(Tianwen-1)看到,而不是被靠近机头的MAVEN看到。这一统计研究证明了火星弓形激波上游太阳风的复杂湍流环境。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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