Probing spectral line asymmetries due to the propagating transverse waves in the solar corona
Ambika Saxena, Vaibhav Pant, Tom Van Doorsselaere, M. Saleem Khan
TL;DR
This work addresses how propagating transverse MHD waves in a density-structured solar corona can imprint spectral line asymmetries. It employs 3D MHD simulations of a polar plume with perpendicular density inhomogeneities and forward models Fe XIII 10749 Å emission to generate synthetic spectra across multiple LOS, analyzed with the BR asymmetry technique. The findings show that transverse waves and uniturbulence produce alternating redward and blueward asymmetries, with amplitudes reaching up to about twenty percent of the peak intensity and secondary peak velocities around 30–40 km s$^{-1}$, propagating with the waves and detectable by DKIST. These results suggest spectral line asymmetries as a diagnostic for identifying transverse wave–induced uniturbulence and, more broadly, for tracing mass and energy transport in the corona.
Abstract
Decades-long studies of asymmetric spectral lines in the solar corona suggest mass and energy transport from lower atmospheric layers to the corona. While slow magnetoacoustic waves and plasma flows are recognized as drivers of these spectral line asymmetries, the role of transverse MHD waves remains largely unexplored. Previous simulations have shown that unidirectionally propagating kink waves, in the presence of perpendicular density inhomogeneities, can produce a turbulence-like phenomenon called ``uniturbulence''. However, the spectroscopic signatures of this effect have not been investigated until now. Due to varying Doppler shifts from the plasma elements with different emissions, we expect to observe signatures of both blueward and redward asymmetries. Past instruments like EIS may have missed these signatures due to resolution limitations, but current instruments like DKIST offer a better opportunity for detection. We conducted 3D MHD simulations of transverse waves in a polar plume with density inhomogeneities and performed forward modeling for the Fe XIII emission line at 10749 Å. Our findings show that transverse waves and uniturbulence induce alternating red and blueward asymmetries, with magnitudes reaching up to 20\% of peak intensity and secondary peak velocities between 30 and 40 km s$^{-1}$, remaining under 100 km s$^{-1}$. These asymmetries propagate with the transverse waves, and even at DKIST resolution, similar signatures can be detected. Our study suggests that spectral line asymmetries can serve as a diagnostic tool for detecting transverse wave-induced uniturbulence.
