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arXiv 1802.05028astro-ph.SR
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合成本影闪光的反演:扫描时间对推断大气的影响

Inversions of synthetic umbral flashes: effects of the scanning time on the inferred atmospheres

T. Felipe, H. Socas-Navarro, D. Przybylski

摘要:

使用仪器记录选定波长的窄带图像是太阳观测的常用方法。它们允许通过在每个线位置处用2D图像对斯托克斯轮廓进行采样来扫描谱线,但是需要在谱分辨率和时间节奏之间进行折衷。我们评估的影响,随时间变化的收购不同波长的光谱偏振剖面的反演色球线在阴影闪烁。用MANCHA程序模拟了太阳黑子中非线性波的传播。用NICOLE程序计算了NLTE中Ca Ⅱ 8542 A谱线的合成斯托克斯参数。人工配置文件具有相同的波长覆盖范围和时间的节奏从报告的观测构建和反演。并与原模式进行了比较。推断的大气提供了一个合理的表征的热力学性质的大气在大多数阶段的本影闪光。只有在闪光的早期阶段,当冲击波达到线的形成高度时,斯托克斯轮廓呈现明显的波长偏移和其他虚假变形。这些功能被误解的反演代码,它可以返回不切实际的大气模型从一个很好的拟合斯托克斯配置文件。误导的结果包括闪烁的大气具有强烈的下行流,即使模拟显示在本影闪光期间的上升流,以及磁场强度的大变化。我们的分析验证了反演斯托克斯配置文件通过顺序扫描某些选定的波长的线配置文件,即使在快速变化的事件,如本影闪光的情况下。然而,在闪光的发展阶段的短时间内,反转是不可靠的。

英文摘要:

The use of instruments that record narrow band images at selected wavelengths is a common approach in solar observations. They allow the scanning of a spectral line by sampling the Stokes profiles with 2D images at each line position, but require a compromise between spectral resolution and temporal cadence. We evaluate the impact of the time-dependent acquisition of different wavelengths on the inversion of spectropolarimetric profiles from chromospheric lines during umbral flashes. Simulations of non-linear wave propagation in a sunspot were performed with the code MANCHA. Synthetic Stokes parameters in the Ca II 8542 A line in NLTE were computed for an umbral flash using the code NICOLE. Artificial profiles with the same wavelength coverage and temporal cadence from reported observations were constructed and inverted. The inferred atmospheric stratifications were compared with the original models. The inferred atmospheres provide a reasonable characterization of the thermodynamic properties of the atmosphere during most of the phases of the umbral flash. Only at the early stages of the flash, when the shock wave reaches the formation height of the line, the Stokes profiles present apparent wavelength shifts and other spurious deformations. These features are misinterpreted by the inversion code, which can return unrealistic atmospheric models from a good fit of the Stokes profiles. The misguided results include flashed atmospheres with strong downflows, even though the simulation exhibits upflows during the umbral flash, and large variations in the magnetic field strength. Our analyses validate the inversion of Stokes profiles acquired by sequentially scanning certain selected wavelengths of a line profile, even in the case of rapidly-changing events such as umbral flashes. However, the inversions are unreliable during a short period at the development phase of the flash.

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