Refined Telluric Absorption Correction for Low-Resolution Ground-Based Spectroscopy: Resolution and Radial Velocity Effects in the O2 A-Band for Exoplanets and K I Emission Lines

TL;DR

This paper investigates the limitations of standard telluric correction methods at low spectral resolution, especially for the O2 A-band, and proposes a refined correction approach accounting for resolution and radial velocity effects.

Contribution

It introduces a new method for deriving correction functions using high-resolution atmospheric modeling to improve telluric correction at low spectral resolutions.

Findings

Standard correction fails at R<10000, causing flux errors over 50%.

Correction functions depend on radial velocity, resolution, and line profile.

Application to Earth analogs and K I lines demonstrates improved accuracy.

Abstract

Telluric correction of spectroscopic observations is either performed via standard stars that are observed close in time and airmass along with the science target, or recently growing in importance, by theoretical telluric absorption modeling. Both approaches work fine when the telluric lines are resolved, i.e. at spectral resolving power larger than about 10000, and it is sufficient to facilitate the detection of spectral features at lower resolution. However, a meaningful quantitative analysis requires also a reliable recovery of line strengths. Here, we show for the Fraunhofer A-band of molecular O2 that the standard telluric correction approach fails in this at lower spectral resolutions, as an example for the general problem. Doppler-shift dependent errors of the restored flux may arise, which can amount to more than 50% in extreme cases, depending on the line shapes of the target spectral features. Two applications are discussed: the recovery of the O2-band in the reflected light of an Earth analog atmosphere, as facilitated potentially in the future using an orbiting starshade and a ground-based extremely large telescope; and the recovery of the intrinsic ratio of the K I lines in the post-nova V4332 Sgr tracing the optical depth of the emitting region, to exemplify the relevance using present-day instrumentation. We show how one should derive correction functions for the compensation of the error in dependence of radial velocity shift, spectral resolution and target line-profile function by use of high resolution atmospheric transmission modeling, which has to be solved for the individual case.