Modification of the Power Spectral Density of Magnetic Field Fluctuations by Quasi-perpendicular Interplanetary Shocks

Byeongseon Park, Alexander Pitňa, Jana Šafránková and Zdeněk Němeček
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Abstract

We investigate the role of interplanetary (IP) shocks in solar wind turbulence using observations of Solar Orbiter, Parker Solar Probe, and Wind. Employing statistical analysis of quasi-perpendicular fast forward (FF) and fast reverse (FR) shocks, we revisit evolution of magnetic field turbulence across IP shocks. Our previous work indicates that the spectral properties of magnetic fluctuations are statistically conserved across different types of IP shocks, except FR shocks in the transition range of frequencies. We focus on the spectral index in the transition range ( ) using 1 minute sliding windows at 10 s intervals to probe the turbulent dissipation near shocks. We address the influence of key turbulence parameters, particularly cross helicity (σc) and fluctuation amplitude (σB), on . Our results demonstrate (1) an immediate change in across the shock with no evidence for further gradual or asymptotic evolution over extended intervals, and this implies that shock universally serves as a thin boundary separating two turbulence states; (2) the dominant factor forming the steepness of is σc, rather than σB; and (3) the statistically shallower downstream of FR shocks results from a systematic reduction in σc across shocks. These findings suggest that the observed spectral modification is primarily governed by changes in turbulence Alfvénicity, not directly by dissipation processes related to the shock, and can be commonly observed toward extensive heliospheric distances.
准垂直行星际冲击对磁场波动功率谱密度的修正
利用太阳轨道器、帕克太阳探测器和wind的观测资料,研究了行星际激波在太阳风湍流中的作用。利用准垂直快进(FF)和快逆(FR)冲击的统计分析,我们重新审视了IP冲击中磁场湍流的演变。我们之前的工作表明,在不同类型的激波中,磁波动的频谱特性在统计上是守恒的,除了频率过渡范围内的FR激波。我们使用间隔10 s的1分钟滑动窗来探测激波附近的湍流耗散,重点研究了过渡范围()内的谱指数。我们讨论了关键的湍流参数,特别是交叉螺旋度(σc)和波动幅度(σB)对湍流的影响。我们的研究结果表明:(1)激波宽度的直接变化,没有证据表明在较长的时间间隔内会进一步逐渐或渐近演变,这意味着激波通常充当分隔两种湍流状态的薄边界;(2)形成陡度的主导因素是σc,而不是σB;(3)统计上较浅的FR冲击下游是由于冲击间σc的系统性降低造成的。这些发现表明,观测到的光谱变化主要是由湍流的变化所控制的,而不是直接由与激波有关的耗散过程所控制的,并且可以在广泛的日球层距离上观测到。
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