全可压缩3D MHD模拟太阳风

Takuma Matsumoto
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引用次数: 15

摘要

确定日冕的加热机制和太阳风的驱动机制是理解太阳物理学的关键挑战。采用全三维可压缩磁流体动力学(MHD)模拟方法,对开放区域上方快速太阳风的加热机制进行了区分。我们的模拟描述了Alfvenic波的演化,其中包括从光球层到27个太阳半径($R_\odot$)距离的可压缩效应。由于阿尔芬波的耗散,热日冕和快速太阳风同时重现。由于包含了过渡区和低层大气,我们首次通过进行全三维可压缩MHD模拟得出了太阳质量损失率。根据以往的太阳风模型,确定了Alfven湍流是太阳风加速区($s>1.3 R_\odot$)的主要加热机制。此外,激波形成和相混合在下过渡区($s<1.03R_\odot$)以下也很重要。
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Full compressible 3D MHD simulation of solar wind
Identifying the heating mechanisms of the solar corona and the driving mechanisms of solar wind are key challenges in understanding solar physics. A full three-dimensional compressible magnetohydrodynamic (MHD) simulation was conducted to distinguish between the heating mechanisms in the fast solar wind above the open field region. Our simulation describes the evolution of the Alfvenic waves, which includes the compressible effects from the photosphere to the heliospheric distance $s$ of 27 solar radii ($R_\odot$). The hot corona and fast solar wind were reproduced simultaneously due to the dissipation of the Alfven waves. The inclusion of the transition region and lower atmosphere enabled us to derive the solar mass loss rate for the first time by performing a full three-dimensional compressible MHD simulation. The Alfven turbulence was determined to be the dominant heating mechanism in the solar wind acceleration region ($s>1.3 R_\odot$), as suggested by previous solar wind models. In addition, shock formation and phase mixing are important below the lower transition region ($s<1.03R_\odot$) as well.
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