📝 SummarXiv

Abstract

The Mg I 12.32 {\mu}m line is highly sensitive to magnetic fields due to its long wavelength, making it a promising tool for precise solar-magnetic-field measurements. The formation of this line is significantly influenced by nonlocal thermodynamic equilibrium (NLTE) effects. Previous studies have shown that the Mg I 12.32 {\mu}m line exhibits different behaviors in various regions of the Sun. This study focuses on the peak intensity of the Mg I 12.32 {\mu}m line to analyze its relationship with the physical parameters of the solar atmosphere and its formation mechanism. We employed the Rybicki-Hummer (RH) 1.5D radiative transfer code to synthesize the Stokes profiles of the Mg I 12.32 {\mu}m line based on a three-dimensional solar atmospheric model of a sunspot and its surrounding quiet Sun. By computing Rxi{\Delta}xi, where Rxi is the average response function and {\Delta}xi is the difference in physical parameters between the two models being compared, we identified the atmospheric height and physical parameters that most significantly influence the normalized peak intensity in the quiet Sun and the active region, respectively. In analyzing the synthesized Stokes profiles, we found two key features: (1) in the quiet Sun, the normalized peak intensity is strong at the centers of the granules and weakens in the intergranular lanes; (2) in the sunspot umbra, the normalized peak intensity is generally weak, with only a few areas showing evident emission. Through the analysis of the response functions, we identified the causes of these differences. In addition, we discussed the mechanisms through which these physical parameters influence the normalized peak intensity.