论文标题
对不均匀的低太阳风的三维模拟
Three-dimensional simulations of the inhomogeneous Low Solar Wind
论文作者
论文摘要
在不久的将来,帕克太阳能探测器将使太阳能电晕和太阳能风之间的过渡的动态和性质进行严格的测试。最流行的机制旨在解释新生太阳风的动力学,包括其加热和加速度,是磁性水力动力学(MHD)湍流。以前的大多数模型都集中在非线性级联反复及其反射的相互作用引起的非线性级联反应,但忽略了可能与太阳能冠状血浆的垂直结构相关的效果,尽管有大量证据。在本文中,我们首次通过3D MHD数值模拟了垂直结构化的太阳电晕和太阳风的动力学,从低电晕到15 R_SUN。我们发现,背景结构对MHD湍流的演变具有强大的影响,比垂直均匀的情况更快。在时间尺度上,与非线性时间短,与相混合相关的线性效应导致1/F垂直能谱。随着湍流级联反应的发展,我们观察到一个垂直(平行)能量谱,其功率定律指数为-3/2或-5/3(-2),垂直磁场比速度频谱更陡峭,并且具有强大的负残留能量。我们得出的结论是,湍流很可能是由驱动的横向扭结波的自幕产生的,以前称为“单位扰动”,这可能代表原始太阳风中的主要非线性能量级联通道。
In the near future, Parker Solar Probe will put theories about the dynamics and nature of the transition between the solar corona and the solar wind to stringent tests. The most popular mechanism aimed to explain the dynamics of the nascent solar wind, including its heating and acceleration is magnetohydrodynamic (MHD) turbulence. Most of the previous models focus on nonlinear cascade induced by interactions of outgoing Alfvén waves and their reflections, ignoring effects that might be related to perpendicular structuring of the solar coronal plasma, despite overwhelming evidence for it. In this paper, for the first time, we analyse through 3D MHD numerical simulations the dynamics of the perpendicularly structured solar corona and solar wind, from the low corona to 15 R_Sun. We find that background structuring has a strong effect on the evolution of MHD turbulence, on much faster time scales than in the perpendicularly homogeneous case. On time scales shorter than nonlinear times, linear effects related to phase mixing result in a 1/f perpendicular energy spectrum. As the turbulent cascade develops, we observe a perpendicular (parallel) energy spectrum with the power law index of -3/2 or -5/3 (-2), a steeper perpendicular magnetic field than velocity spectrum, and a strong build-up of negative residual energy. We conclude that the turbulence is most probably generated by the self-cascade of the driven transverse kink waves, referred to previously as `uniturbulence', which might represent the dominant nonlinear energy cascade channel in the pristine solar wind.