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Multifractal two-scale Cantor set model for slow solar wind turbulence in the outer heliosphere during solar maximum

机译:太阳分形过程中太阳外层慢速太阳风湍流的多重分形两尺度Cantor集模型

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To quantify solar wind turbulence, we consider a generalized two-scale weighted Cantor set with two different scales describing nonuniform distribution of the kinetic energy flux between cascading eddies of various sizes. We examine generalized dimensions and the corresponding multifractal singularity spectrum depending on one probability measure parameter and two rescaling parameters. In particular, we analyse time series of velocities of the slow speed streams of the solar wind measured in situ by Voyager 2 spacecraft in the outer heliosphere during solar maximum at various distances from the Sun: 10, 30, and 65 AU. This allows us to look at the evolution of multifractal intermittent scaling of the solar wind in the distant heliosphere. Namely, it appears that while the degree of multifractality for the solar wind during solar maximum is only weakly correlated with the heliospheric distance, but the multifractal spectrum could substantially be asymmetric in a very distant heliosphere beyond the planetary orbits. Therefore, one could expect that this scaling near the frontiers of the heliosphere should rather be asymmetric. It is worth noting that for the model with two different scaling parameters a better agreement with the solar wind data is obtained, especially for the negative index of the generalized dimensions. Therefore we argue that there is a need to use a two-scale cascade model. Hence we propose this model as a useful tool for analysis of intermittent turbulence in various environments and we hope that our general asymmetric multifractal model could shed more light on the nature of turbulence.
机译:为了量化太阳风的湍流,我们考虑了具有两个不同尺度的广义两尺度加权Cantor集,描述了不同大小的级联涡流之间动能通量的不均匀分布。我们根据一个概率度量参数和两个重缩放参数,检查广义维和相应的多重分形奇异谱。特别是,我们分析了在距离太阳不同距离(分别是10、30和65 AU)的太阳最大值期间,旅行者2号太空船在外太阳圈中由原位测量的太阳风慢速流速度的时间序列。这使我们可以研究遥远太阳圈中太阳风的多重分形间歇缩放的演变。即,看来,虽然在太阳最大值期间太阳风的多重分形程度仅与日球层距离弱相关,但在离行星轨道很远的日球层中,多重分形谱可能基本上是不对称的。因此,可以预料到在日光层边界附近的这种缩放应该是不对称的。值得注意的是,对于具有两个不同缩放参数的模型,可以获得与太阳风数据更好的一致性,尤其是对于广义尺寸的负指标。因此,我们认为有必要使用两尺度级联模型。因此,我们建议将此模型作为分析各种环境中间歇性湍流的有用工具,并希望我们的通用非对称多重分形模型可以为湍流的性质提供更多的启示。

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