A comparison of G-band brightness as a proxy-magnetometer in various magnetic configurations
Malay Shukla, Sneha Pandit, Nitin Yadav
TL;DR
The study addresses whether centering G-band filters at 430.4 nm improves detection of small-scale solar magnetic fields compared with the traditional 430.5 nm setting. It combines realistic 3D MHD simulations with RH 1.5D spectral synthesis to generate synthetic G-band images across quiet-Sun and plage environments, applying Gaussian spectral broadening to emulate instrument filters. The results show that 430.4 nm yields higher intensity contrast, particularly for narrowband filters, due to higher formation heights and enhanced CH-opacity sensitivity in magnetized regions, though some strong-field areas can appear darker due to heating balance and Wilson depression effects. The findings suggest 430.4 nm as a promising alternative for high-contrast magnetic diagnostics, with potential applications to stellar contexts, while highlighting the need for further work on instrumental effects and spectropolarimetric capabilities.
Abstract
We investigate the diagnostic potential of the G-band at 430.4 nm for probing small-scale magnetic fields in the solar photosphere. Combining three-dimensional MHD simulations from the MURaM code and spectral synthesis via the RH 1.5D code, we evaluate the intensity contrast in the G-band filtergrams by comparing the filter centered at 430.4 nm in comparison to the conventional 430.5 nm. Our results show that filtergrams centered at 430.4 nm provide higher contrast across varying magnetic environments, particularly at narrow filter widths. This enhancement arises from its slightly higher formation height and greater sensitivity to temperature variations in magnetized regions. These findings indicate that G-band filtergrams centered at 430.4 nm show enhanced diagnostic potential under the assumptions of the present modeling. The obtained results are also relevant and suggest potential applications in stellar contexts, where molecular bands are often used as proxies for magnetic activity.
