On the center-to-limb variations of the He I 10 830 Å triplet
A. G. M. Pietrow, C. Kuckein, M. Verma, C. Denker, J. C. Trelles Arjona, R. Kamlah, K. Poppenhäger
TL;DR
The paper addresses center-to-limb variations of the He I 10 830 Å triplet in the quiet Sun and its relation to coronal coupling, using high-resolution GRIS+HiFI+ observations across $μ \in [0.1,1.0]$. It employs the HAZEL inversion framework to extract optical depth and Doppler parameters, revealing an increasing opacity toward the limb and a reversed convective signature for the red component, with the blue component effectively absent. The He I CLV is found to be steeper than the nearby continuum, contrasting with the Si I reference line which shows more typical photospheric behavior. The resulting CLV dataset provides a benchmark for radiative-transfer modeling of chromospheric lines and informs interpretations of stellar activity and exoplanet-atmosphere signatures, with the data made publicly available via CDS.
Abstract
We present high-resolution spectroscopic observations of the quiet-Sun center-to-limb variations (CLV) of the He I triplet at 10 830 Å and the nearby Si I 10 827 Å line, observed with GREGOR Infrared Spectrograph (GRIS) and the improved High-resolution Fast Imager (HiFI+). The observations cover the interval $μ= [0.1,\, 1.0]$, where $μ$ is the cosine of the heliocentric angle. At each $μ$-position, the spectra are spatially averaged over 0.02 $μ$, and the resulting CLVs are given both as these averaged data points and as smooth polynomial curves fitted across each wavelength point. The He I spectra were inverted using the HAnle and ZEeman Light (HAZEL) code, showing an increase in optical depth towards the limb and a reversed convective blueshift for the red component, while the blue component was entirely absent. In addition, we find a strong increase in the steepness of the He I CLV compared to that of the nearby continuum. The Si I showed a behavior more typical of photospheric lines, namely shallower CLV, a reduction in width and depth, and a more typical convective blueshift.
