论文标题

在磁场波动的缩放特性上通过内部地层波动

On the Scaling Properties of Magnetic Field Fluctuations Through the Inner Heliosphere

论文作者

Alberti, Tommaso, Laurenza, Monica, Consolini, Giuseppe, Milillo, Anna, Marcucci, Maria Federica, Carbone, Vincenzo, Bale, Stuart D.

论文摘要

尽管已通过多个空间任务的数据对星际磁场的可变性进行了广泛的原位研究,但新启动的任务提供了高分辨率措施并接近太阳,提供了研究最内在太阳系中多尺度变异性的可能性。在这里,通过Parker太阳能探测测量值,我们研究了在不同的中心距离下太阳风磁场波动的缩放特性。结果表明,在接近0.4 au的距离处有明显的过渡。靠近太阳波动显示了f^-3/2频率谱和常规缩放特性,而对于大于0.4 au波动的距离显示了kolmogorov光谱f^-5/3,并以异常尺度为特征。观察到的湍流的统计特性表明,太阳风磁波动在后期远远构成太阳,显示出典型的湍流行为,并通过间歇性描述,而在早期阶段,当离开太阳能电晕时,观察到了这些特性的崩溃,因此显示出统计的单型全球自我差异。从物理上讲,观察到的崩溃应是由于定期统计的湍流或存在强烈的随机波动,能够取消存在异常缩放所需的相关性。

Although the interplanetary magnetic field variability has been extensively investigated in situ by means of data coming from several space missions, the newly launched missions providing high-resolution measures and approaching the Sun, offer the possibility to study the multiscale variability in the innermost solar system. Here by means of the Parker Solar Probe measurements we investigate the scaling properties of solar wind magnetic field fluctuations at different heliocentric distances. The results show a clear transition at distances close to say 0.4 au. Closer to the Sun fluctuations show a f^-3/2 frequency power spectra and regular scaling properties, while for distances larger than 0.4 au fluctuations show a Kolmogorov spectrum f^-5/3 and are characterized by anomalous scalings. The observed statistical properties of turbulence suggests that the solar wind magnetic fluctuations, in the late stage far form the Sun, show a multifractal behaviour typical of turbulence and described through intermittency, while in the early stage, when leaving the solar corona, a breakdown of these properties are observed, thus showing a statistical monofractal global self-similarity. Physically the breakdown observed close to the Sun should be due either to a turbulence with regular statistics or to the presence of intense stochastic fluctuations able to cancel out correlations necessary for the presence of anomalous scaling.

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