Relating Intermittency and Inverse Cascade to Stochastic Entropy in Solar Wind Turbulence

M. Stumpo, S. Benella, T. Alberti, O. Pezzi, E. Papini, G. Consolini
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Abstract

Turbulent energy transfer in nearly collisionless plasmas can be conceptualized as a scale-to-scale Langevin process. Hence, the statistics of magnetic field fluctuations can be embedded in the framework of stochastic process theory. In this work, we investigate the statistical properties of the pristine solar wind as observed by Parker Solar Probe by defining the cascade trajectories of magnetic field increments and by estimating the stochastic entropy variation along them. Through the stochastic entropy, we can identify two regimes where fluctuations exhibit contrasting statistical properties. In the inertial range, the entropy production is associated with an increase of the flatness indicating the occurrence of intermittency. Otherwise, trajectories associated with an entropy consumption exhibit global scale invariance. In the transition region toward ion scales, the phenomenology switches: entropy-consuming trajectories exhibit a sudden flatness increase, associated with the presence of small-scale intermittency, while entropy-producing trajectories display a nearly constant flatness. Results are interpreted in terms of physical processes consistent with an accumulation of energy at ion scales.
将太阳风湍流中的间歇性和反级联与随机熵联系起来
近乎无碰撞等离子体中的湍流能量传递可以概念化为尺度到尺度的朗格文过程。因此,磁场波动的统计特性可以嵌入随机过程理论的框架中。在这项工作中,我们通过定义磁场增量的级联轨迹并估算其沿线的随机熵变,研究了帕克太阳探测器观测到的原始太阳风的统计特性。通过随机熵,我们可以识别出波动表现出截然不同统计特性的两个区间。在惯性范围内,熵的产生与平坦度的增加有关,表明出现了间歇性。否则,与熵消耗相关的轨迹会表现出全局尺度不变性。在向离子尺度过渡的区域,现象发生了变化:熵消耗轨迹显示出突然的平坦度增加,这与小尺度间歇性的存在有关,而熵产生轨迹则显示出几乎恒定的平坦度。研究结果从与离子尺度能量积累一致的物理过程角度进行了解释。
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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