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arXiv 1504.07541astro-ph.SR
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2011年3月9日X级太阳耀斑的辐射流体动力学模拟和观测

Radiative hydrodynamic modelling and observations of the X-class solar flare on 2011 March 9

Michael B. Kennedy, Ryan O. Milligan, Joel C. Allred, Mihalis Mathioudakis, Francis P. Keenan

摘要:

利用辐射转移和流体动力学模拟程序RADYN研究了太阳大气对非热电子束加热的响应。描述非热电子能量分布的参数的时间演化来自硬X射线观测的一个特定的耀斑,我们比较了建模和观测参数。通过对RHESSI X射线能谱的分析,获得了2011年3月9日发生的X1. 5级太阳耀斑期间非热电子束参数的演化。RADYN耀斑模型允许演化110秒,之后电子束加热结束,然后允许继续演化300秒。模拟耀斑参数进行了比较,从极紫外光谱测定的观测参数。该模型产生了一个比观测到的更热、更密集的耀斑环,也更快地冷却,这表明在耀斑的衰变阶段需要额外的能量输入。在爆炸蒸发阶段,一个高密度的冷物质区域通过日冕向上传播。这种材料经历了温度的快速上升,因为它无法辐射掉所有通过非热电子束和热传导沉积在它上面的能量。耀斑过渡区底部的一个狭窄的高密度($n_{e} \le 10^{15}$ cm $^{-3}$)区域是模式大气中的光学线发射源。在耀斑的整个演化过程中计算了电子的碰撞停止深度,发现低层大气的压缩可能允许电子更远地穿透到耀斑大气中,而不是安静的太阳大气。

英文摘要:

We investigated the response of the solar atmosphere to non-thermal electron beam heating using the radiative transfer and hydrodynamics modelling code RADYN. The temporal evolution of the parameters that describe the non-thermal electron energy distribution were derived from hard X-ray observations of a particular flare, and we compared the modelled and observed parameters. The evolution of the non-thermal electron beam parameters during the X1.5 solar flare on 2011 March 9 were obtained from analysis of RHESSI X-ray spectra. The RADYN flare model was allowed to evolve for 110 seconds, after which the electron beam heating was ended, and was then allowed to continue evolving for a further 300s. The modelled flare parameters were compared to the observed parameters determined from extreme-ultraviolet spectroscopy. The model produced a hotter and denser flare loop than that observed and also cooled more rapidly, suggesting that additional energy input in the decay phase of the flare is required. In the explosive evaporation phase a region of high-density cool material propagated upward through the corona. This material underwent a rapid increase in temperature as it was unable to radiate away all of the energy deposited across it by the non-thermal electron beam and via thermal conduction. A narrow and high-density ($n_{e} \le 10^{15}$ cm$^{-3}$) region at the base of the flare transition region was the source of optical line emission in the model atmosphere. The collision-stopping depth of electrons was calculated throughout the evolution of the flare, and it was found that the compression of the lower atmosphere may permit electrons to penetrate farther into a flaring atmosphere compared to a quiet Sun atmosphere.

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