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arXiv 2602.18100astro-ph.SR
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散射偏振的三维辐射传输建模(部分频率 redistribution)I. 验证及太阳Ca I 4227 Å线的盘中心结果

3D radiative transfer modeling of scattering polarization with partial frequency redistribution I. Verification and disk-center results for the solar Ca I 4227 Å line

Istituto ricerche solari Aldo e Cele Daccò (IRSOL), Faculty of Informatics, Università della Svizzera italiana(瑞士意大利大学信息学院阿尔多和塞莱·达科太阳研究研究所(IRSOL));Euler Institute, Faculty of Informatics, Università della Svizzera italiana(瑞士意大利大学信息学院欧拉研究所);Instituto de Astrofísica de Canarias(加那利群岛天体物理研究所);Departamento de Astrofísica, Universidad de La Laguna(拉帕尔马大学天体物理学系);Astronomical Institute ASCR, Ondřejov(捷克科学院天文研究所奥登焦夫分部);AMCS, KAUST(KAUST应用计算数学中心)

Pietro Benedusi, Simone Riva, Tanausú del Pino Alemán, Gioele Janett, Fabio Riva, Jirí Štepán, Rolf Krause, Javier Trujillo Bueno, Luca Belluzzi

AI总结:

本文通过TRIP软件验证了三维非本地热力学平衡辐射传输模型,研究了部分频率 redistribution和三维大气结构对太阳Ca I 4227 Å线盘中心散射偏振信号的影响。

摘要:

几个强太阳共振线显示出可观察的线性散射偏振信号,具有研究外层太阳大气磁性巨大潜力。准确建模这些信号需要解决极化辐射在综合三维太阳大气模型中的辐射传输(RT)问题,在非局部热力学平衡条件下,考虑部分频率 redistribution(PRD)效应。此问题迄今为止计算上不可行。我们介绍了TRIP软件,这是用于大规模并行求解极化辐射的三维非本地热力学平衡RT问题的新软件,包括散射偏振和PRD。我们旨在验证代码并探索PRD和太阳大气三维结构对散射偏振的联合作用。我们运行TRIP以合成Ca I线在4227 Å的斯托克斯谱,在从辐射磁流体动力学模拟中提取的太阳大气三维模型中。我们高效地解决了由此产生的大规模问题,最大达到4×10^10个自由度,使用最先进的预条件Krylov方法,并利用多达20000个并行CPU。在包括验证测试后,我们发现PRD效应和大气模型详细三维结构的联合影响在谱线翼部产生盘中心散射偏振信号。这些信号对磁场敏感,通过磁光效应,也对体积速度梯度敏感。我们还表明CRD近似低估了盘中心线核信号的振幅。这一成就代表了通过合成和观测数据的定量比较诊断太阳色球和过渡区域磁性的关键步骤。

英文摘要:

Several strong solar resonance lines show observable linear scattering polarization signals, holding a great potential for investigating the magnetism of the outer solar atmosphere. Accurately modeling these signals requires solving the radiative transfer (RT) problem for polarized radiation in comprehensive 3D models of the solar atmosphere, in non-local thermodynamic equilibrium, accounting for partial frequency redistribution (PRD) effects. This problem has so far been computationally inaccessible. We present the first scientific application of TRIP, a novel software for the massively parallel solution of the 3D non-LTE RT problem for polarized radiation, including scattering polarization and PRD. We aim to verify the code and explore the combined action of PRD and the 3D structure of the solar atmosphere on scattering polarization. We run TRIP to synthesize the Stokes profiles of the Ca I line at 4227 Å in a 3D model of the solar atmosphere extracted from a radiation magneto-hydrodynamic simulation. We efficiently solve the resulting large-scale problem, with up to $4 \times 10^{10}$ degrees of freedom, with a state-of-the-art preconditioned Krylov method, using up to 20 thousand parallel CPUs. After including verification tests, we find that the joint impact of PRD effects and the detailed 3D structure of the atmospheric model produce disk-center scattering polarization signals in the line wings. These signals are sensitive to the magnetic field, via magneto-optical effects, and to bulk velocity gradients. We also show that the CRD approximation underestimates the amplitude of disk-center line-core signals. This achievement represents a crucial step forward for diagnosing the magnetism of the solar chromosphere and transition region through the quantitative comparisons of synthetic and observational data.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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