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arXiv 1806.09574astro-ph.SR
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太阳耀斑多线程流体动力学模拟中非局域热力学平衡效应的高效计算

Efficient Calculation of Non-Local Thermodynamic Equilibrium Effects in Multithreaded Hydrodynamic Simulations of Solar Flares

Jeffrey W. Reep, Stephen J. Bradshaw, Nicholas A. Crump, Harry P. Warren

摘要:

了解太阳色球层的动力学对于了解太阳大气层的能量传输至关重要。色球层在许多波长下都是光学厚度,并由非局部热力学平衡(NLTE)描述,使得很难解释观测结果。此外,有相当多的证据表明,大气层是膨胀的,目前的仪器不足以解决小规模的功能。在耀斑中,很可能需要多线程模型来描述加热。NLTE效应和多线程建模的结合需要计算上苛刻的计算,这促使开发一种可以有效处理两者的模型。我们描述了一个求解器的实现在一个流体动力学代码的氢水平的人口,近似NLTE的解决方案。我们推导出一个准确的电子密度在整个大气中,其中包括非平衡电离的影响,氦和金属。我们展示了对流体动力学模拟的影响,这些模拟用于使用后处理辐射转移代码来合成光变曲线。我们证明了这个模型的实用性IRIS观测的一个小耀斑。我们表明,在镁II,C II和O I的多普勒频移可以解释与多线程模型的循环进行电子束加热,只要NLTE效应进行治疗。然而,强度与观测值并不匹配,这是由于对初始大气的假设。我们简要地展示了如何改变初始大气可以大大改变线的轮廓,因此导出量,并建议它应该调整到耀斑前的观测。

英文摘要:

Understanding the dynamics of the solar chromosphere is crucial to understanding energy transport across the solar atmosphere. The chromosphere is optically thick at many wavelengths and described by non-local thermodynamic equilibrium (NLTE), making it difficult to interpret observations. Furthermore, there is considerable evidence that the atmosphere is filamented, and that current instruments do not sufficiently resolve small scale features. In flares, it is likely that multithreaded models are required to describe the heating. The combination of NLTE effects and multithreaded modeling requires computationally demanding calculations, which has motivated the development of a model that can efficiently treat both. We describe the implementation of a solver in a hydrodynamic code for the hydrogen level populations that approximates the NLTE solutions. We derive an accurate electron density across the atmosphere, that includes the effects of non-equilibrium ionization for helium and metals. We show the effects on hydrodynamic simulations, which are used to synthesize light curves using a post-processing radiative transfer code. We demonstrate the utility of this model on IRIS observations of a small flare. We show that the Doppler shifts in Mg II, C II, and O I can be explained with a multithreaded model of loops subjected to electron beam heating, so long as NLTE effects are treated. The intensities, however, do not match observed values very well, which is due to assumptions about the initial atmosphere. We briefly show how altering the initial atmosphere can drastically alter line profiles, and therefore derived quantities, and suggest that it should be tuned to pre-flare observations.

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