Inertial-range Turbulence Anisotropy of the Young Solar Wind from Different Source Regions

Wenshuai Cheng, Ming Xiong, Yiming Jiao, Hao Ran, Liping Yang, Huidong Hu and Rui Wang
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Abstract

We investigate the wavevector and variance anisotropies in the inertial range of the young solar wind observed by the Parker Solar Probe (PSP). Using the first 19 encounters of PSP measurements, we identify the young solar wind from different source regions: coronal hole (CH) interiors, streamers, and low Mach-number boundary layers (LMBLs), i.e., the peripheral region inside CHs. We assess the wavevector anisotropy with the 2D and slab turbulence model for the CH wind and streamer wind and the nearly incompressible MHD turbulence model for the LMBL wind, where Taylor’s hypothesis becomes questionable. Unlike the ∼80% 2D contribution typically reported at 1 au, our results show that only 26% of the inertial range energy is associated with 2D fluctuations in the CH wind, and this fraction increases to 45% in the streamer wind. As a representation of the LMBL wind, similarly, the oblique sub-Alfvénic intervals and near-subsonic intervals are characterized by the dominance of slab fluctuations. All the results suggest that slab fluctuations are more abundant in the young solar wind below 0.3 au than at 1 au. Furthermore, we find a dependence of the variance anisotropy in the inertial range on proton plasma beta βp. The variance anisotropy is the strongest in the LMBL wind with the lowest βp and the weakest in the streamer wind with the highest βp. This contrast can be interpreted as the remnant of fluctuations from the coronal sources.
不同源区年轻太阳风的惯性湍流各向异性
研究了帕克太阳探测器(PSP)观测到的年轻太阳风在惯性范围内的波矢量和方差各向异性。利用前19次PSP测量,我们确定了来自不同来源区域的年轻太阳风:日冕洞(CH)内部,流带和低马赫数边界层(LMBLs),即CHs内部的外围区域。我们用二维和平板湍流模型来评估CH风和拖风的波向各向异性,用几乎不可压缩的MHD湍流模型来评估LMBL风的波向各向异性,在这里泰勒的假设变得有问题。与通常报道的1 au的2D贡献约80%不同,我们的研究结果表明,在CH风中,只有26%的惯性范围能量与2D波动有关,而在拖频风中,这一比例增加到45%。作为LMBL风的表征,同样地,斜亚阿尔夫萨奇区间和近亚音速区间的特点是板波动占主导地位。所有的结果都表明,在0.3 au以下的年轻太阳风中,板块波动比在1 au时更为丰富。此外,我们发现惯性范围内的方差各向异性与质子等离子体β βp有关。各向异性方差在βp最低的LMBL风中最强,在βp最高的拖风中最弱。这种对比可以解释为日冕源波动的残余。
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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