Localized Heating and Dynamics of the Solar Corona due to a Symbiosis of Waves and Reconnection

A. K. Srivastava, Sripan Mondal, Eric R. Priest, Sudheer K. Mishra, David I. Pontin, R.Y. Kwon, Ding Yuan, K. Murawski, Ayumi Asai
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Abstract

The Sun’s outer atmosphere, the corona, is maintained at mega-Kelvin temperatures and fills the heliosphere with a supersonic outflowing wind. The dissipation of magnetic waves and direct electric currents are likely to be the most significant processes for heating the corona, but a lively debate exists on their relative roles. Here, we suggest that the two are often intrinsically linked, since magnetic waves may trigger current dissipation, and impulsive reconnection can launch magnetic waves. We present a study of the first of these processes by using a 2D physics-based numerical simulation using the Adaptive Mesh Refined Versatile Advection Code. Magnetic waves such as fast magnetoacoustic waves are often observed to propagate in the large-scale corona and interact with local magnetic structures. The present numerical simulations show how the propagation of magnetic disturbances toward a null point or separator can lead to the accumulation of the electric currents. Lorentz forces can laterally push and vertically stretch the magnetic fields, forming a current sheet with a strong magnetic field gradient. The magnetic field lines then break and reconnect and so contribute toward coronal heating. Numerical results are presented that support these ideas and support the concept of a symbiosis between waves and reconnection in heating the solar corona.
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由波和重联共生引起的日冕局部加热和动力学
太阳的外层大气,即日冕,保持着超开尔文的温度,并使日球层充满了超音速的外流风。磁波和直接电流的耗散可能是加热日冕最重要的过程,但关于它们的相对作用存在着激烈的争论。在这里,我们认为这两者通常是内在联系的,因为电磁波可能触发电流耗散,而脉冲重联可以发射电磁波。我们通过使用自适应网格精细通用平流代码使用基于二维物理的数值模拟来研究这些过程中的第一个。磁波,如快速磁声波,经常被观测到在大尺度日冕中传播并与局部磁结构相互作用。目前的数值模拟显示了磁扰动如何向零点或分离器的传播可以导致电流的积累。洛伦兹力可以横向推动和垂直拉伸磁场,形成具有强磁场梯度的电流片。然后磁力线断开并重新连接,从而导致日冕加热。给出的数值结果支持这些观点,并支持在加热日冕过程中波和重联之间的共生关系的概念。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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