首页> 外文期刊>The Astrophysical journal >Disappearance of Anisotropic Intermittency in Large-amplitude MHD Turbulence and Its Comparison with Small-amplitude MHD Turbulence
【24h】

Disappearance of Anisotropic Intermittency in Large-amplitude MHD Turbulence and Its Comparison with Small-amplitude MHD Turbulence

机译:大振幅MHD湍流中各向异性间歇性的消失及其与小振幅MHD湍流的比较

获取原文
           

摘要

Multi-order structure functions in the solar wind are reported to display a monofractal scaling when sampled parallel to the local magnetic field and a multifractal scaling when measured perpendicularly. Whether and to what extent will the scaling anisotropy be weakened by the enhancement of turbulence amplitude relative to the background magnetic strength? In this study, based on two runs of the magnetohydrodynamic (MHD) turbulence simulation with different relative levels of turbulence amplitude, we investigate and compare the scaling of multi-order magnetic structure functions and magnetic probability distribution functions (PDFs) as well as their dependence on the direction of the local field. The numerical results show that for the case of large-amplitude MHD turbulence, the multi-order structure functions display a multifractal scaling at all angles to the local magnetic field, with PDFs deviating significantly from the Gaussian distribution and a flatness larger than 3 at all angles. In contrast, for the case of small-amplitude MHD turbulence, the multi-order structure functions and PDFs have different features in the quasi-parallel and quasi-perpendicular directions: a monofractal scaling and Gaussian-like distribution in the former, and a conversion of a monofractal scaling and Gaussian-like distribution into a multifractal scaling and non-Gaussian tail distribution in the latter. These results hint that when intermittencies are abundant and intense, the multifractal scaling in the structure functions can appear even if it is in the quasi-parallel direction; otherwise, the monofractal scaling in the structure functions remains even if it is in the quasi-perpendicular direction.
机译:据报道,太阳风中的多阶结构函数在平行于局部磁场采样时显示出单分形标度,而在垂直测量时显示出多分形标度。湍流幅度相对于本底磁场强度的增强是否会减小缩放各向异性?在何种程度上减弱缩放各向异性?在这项研究中,基于两次运行的磁流体动力学(MHD)湍流模拟,湍流振幅的相对水平不同,我们研究并比较了多阶磁结构函数和磁概率分布函数(PDF)的缩放比例及其相关性在当地领域的方向。数值结果表明,对于大振幅MHD湍流,多级结构函数在与局部磁场的所有角度上均显示出多重分形比例,PDF明显偏离了高斯分布,并且平坦度均大于3角度。相比之下,对于小振幅MHD湍流,多阶结构函数和PDF在准平行和准垂直方向上具有不同的特征:单分形缩放和高斯分布在前者,以及转换将单分形标度和高斯样分布分解为后者的多分形标度和非高斯尾分布。这些结果表明,当间歇性很强且剧烈时,即使在准平行方向上,结构函数中的多重分形标度也会出现。否则,即使在准垂直方向上,结构函数中的单形缩放也保持不变。

著录项

获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号