论文标题
低分辨率地面光谱法的精制矫正吸收校正:O2 A波段中的分辨率和径向速度效应,用于外部球星和K I发射线
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
论文作者
论文摘要
光谱观测的矫正矫正是通过标准恒星进行的,这些恒星在时间上观察到,并通过理论上的矫治吸收模型在时间上观察到,或者与科学靶标一起观察到的空气量,或者最近在重要性上生长。当解决牙沟线解析时,即在光谱解决能力大于10000大约10000时,两种方法都可以正常工作,并且足以促进在较低分辨率下检测光谱特征。但是,有意义的定量分析还需要可靠的线强度恢复。在这里,我们显示了分子O2的Fraunhofer A频段表明,在较低的光谱分辨率下,标准的校矫正方法在此中失败了,作为一般问题的一个例子。可能会出现恢复通量的多普勒转移依赖性误差,在极端情况下,该错误可能超过50%,具体取决于目标光谱特征的线形状。讨论了两种应用:在地球模拟气氛的反射光中恢复O2波段,将来可能会使用轨道轨道的星光射线和地面极大的望远镜来促进。以及在Nova后V4332 SGR中恢复K I线的固有比率,以追踪发射区域的光学深度,以使用当前的仪器来体现相关性。我们展示了如何通过使用高分辨率大气传输建模来依赖radial速度偏移,光谱分辨率和目标线路型功能的误差的校正函数,该函数必须用于单个情况。
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.