Abrams M C, Gunson M R, Chang A Y, Rinsland C P, Zander R
Appl Opt. 1996 Jun 1;35(16):2774-90. doi: 10.1364/AO.35.002774.
The methodology of spectroscopic remote sensing with high-resolution Fourier-transform spectra obtained from low Earth orbit by the Atmospheric Trace Molecule Spectroscopy (ATMOS) experiment is discussed. During the course of the Atmospheric Laboratory for Applications and Science (ATLAS) shuttle missions (1992-1994) a flexible, yet reproducible, retrieval strategy was developed that culminated in the near-real-time processing of telemetry data into vertical profiles of atmospheric composition during the ATLAS-3 mission. The development, evolution, robustness, and validation of the measurements are presented and assessed with a summary comparison of trace-gas observations within the Antarctic polar vortex in November 1994.
讨论了通过大气痕量分子光谱学(ATMOS)实验从低地球轨道获得高分辨率傅里叶变换光谱进行光谱遥感的方法。在大气应用与科学实验室(ATLAS)航天飞机任务(1992 - 1994年)期间,开发了一种灵活但可重复的反演策略,该策略在ATLAS - 3任务期间最终实现了将遥测数据近实时处理为大气成分垂直剖面。文中介绍并评估了测量的发展、演变、稳健性和验证情况,并对1994年11月南极极涡内痕量气体观测结果进行了总结比较。