论文标题
太阳能旋转引起的太阳活性区域10930的同源喷发的MHD模拟
MHD Simulation of Homologous Eruptions from Solar Active Region 10930 Caused by Sunspot Rotation
论文作者
论文摘要
太阳喷发与黑子旋转之间的关系已得到广泛报道,并且需要研究潜在的机制。在这里,我们对数据受限的方法进行了完整的3D MHD模拟,以研究活性区域(AR)NOAA 10930的耀斑爆发的机理,其特征是连续的太阳突动旋转和同源喷发。我们从Hinode/SOT的磁力图作为初始条件重建了潜在的磁场,并通过在底部边界上施加连续的黑子旋转来驱动MHD系统。主要喷发和预先形成的电流板之前的关键磁性结构得出了多个阶段的复杂MHD演化。主要的喷发是通过在AR的两个主要磁性极性之间的主要极性反转线上的预先形成的电流板中的快速重新连接来直接触发的。此外,我们的模拟成功地显示了同源喷发。它与爆发的相对强度,能量释放,X射线和Hα特征和时间间隔的观测值合理。另外,在模拟中首次爆发之前,黑子的旋转角度也接近观察到的值。我们的仿真提供了与许多基于理想的磁通绳绳的理想不稳定性不同的场景,并显示了黑子旋转和磁重新连接在有效产生同源性喷发中的重要性,这是通过持续的能量抑制和冲动的能量释放的重复方式。
The relationship between solar eruption and sunspot rotation has been widely reported, and the underlying mechanism requires to be studied. Here we performed a full 3D MHD simulation of data-constrained approach to study the mechanism of flare eruptions in active region (AR) NOAA 10930, which is characterized by continuous sunspot rotation and homologous eruptions. We reconstructed the potential magnetic field from the magnetogram of Hinode/SOT as the initial condition and drove the MHD system by applying continuous sunspot rotation at the bottom boundary. The key magnetic structure before the major eruptions and the pre-formed current sheet were derived, which is responsible for the complex MHD evolution with multiple stages. The major eruptions were triggered directly by fast reconnection in the pre-formed current sheet above the main polarity inversion line between the two major magnetic polarities of the AR. Furthermore, our simulation shows the homologous eruption successfully. It has reasonable consistence with observations in relative strength, energy release, X-ray and Hα features and time interval of eruptions. In addition, the rotation angle of the sunspot before the first eruption in the simulation is also close to the observed value. Our simulation offers a scenario different from many previous studies based on ideal instabilities of twisted magnetic flux rope, and shows the importance of sunspot rotation and magnetic reconnection in efficiently producing homologous eruptions by continuous energy injection and impulsive energy release in a recurrent way.