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arXiv 1105.0953astro-ph.SR
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日震对2011年2月15日X2 .2太阳耀斑的响应

Helioseismic response to X2.2 solar flare of February 15, 2011

Alexander G. Kosovichev

摘要:

2011年2月15日的X2.2级太阳耀斑产生了一次强烈的日震事件,这是太阳动力学天文台(SDO)的HMI仪器观测到的太阳光球对耀斑影响的日震响应。脉冲激发的声波形成了一个紧凑的波包,穿过太阳内部,在表面上表现为扩展的波波纹。观测到初始耀斑撞击的形式是多普勒速度、视线磁场和连续强度的紧凑和快速变化。这些变化形成了典型的双带耀斑结构,并被认为与高能粒子加热低层大气的热和流体动力学效应有关。对SDO/HMI和来自Ramaty高能太阳光谱成像仪(RHESSI)的X射线数据的分析表明,日震波是在硬X射线(50-100 keV)脉冲之前观测到的,由早期脉冲阶段的光球撞击引发的,并且可能与相对低能电子(~6-50 keV)和热通量传输的大气加热有关。在日震波出现之前,撞击造成了太阳黑子半影的短暂运动。研究发现,日震波阵面穿过太阳黑子时振幅较低,且相对于黑子外的阵面有明显的延迟。这些观测结果为研究耀斑对光球的影响和利用耀斑激发的波进行太阳黑子地震学研究开辟了新的前景。

英文摘要:

The X2.2-class solar flare of February 15, 2011, produced a powerful sunquake event, representing a helioseismic response to the flare impact in the solar photosphere, which was observed with the HMI instrument on the Solar Dynamics Observatory (SDO). The impulsively excited acoustic waves formed a compact wavepacket traveling through the solar interior and appearing on the surface as expanding wave ripples. The initial flare impacts were observed in the form of compact and rapid variations of the Doppler velocity, line-of-sight magnetic field and continuum intensity. These variations formed a typical two-ribbon flare structure, and are believed to be associated with thermal and hydrodynamic effects of high-energy particles heating the lower atmosphere. The analysis of the SDO/HMI and X-ray data from the Ramaty High Energy Solar Spectroscopic Imager (RHESSI) shows that the helioseismic waves were initiated by the photospheric impact in the early impulsive phase, observed prior to the hard X-ray (50-100 keV) impulse, and were probably associated with atmospheric heating by relatively low-energy electrons (~6-50 keV) and heat flux transport. The impact caused a short motion in the sunspot penumbra prior to the appearance of the helioseismic wave. It is found that the helioseismic wave front traveling through a sunspot had a lower amplitude and was significantly delayed relative to the front traveling outside the spot. These observations open new perspectives for studying the flare photospheric impacts and for using the flare-excited waves for sunspot seismology.

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