Grant W B, Margolis J S, Brothers A M, Tratt D M
Appl Opt. 1987 Aug 1;26(15):3033-42. doi: 10.1364/AO.26.003033.
CO(2) lidars have heretofore been used to measure water vapor concentrations primarily using the 10R(20) line at 10.247 microm, which has a strong overlap with a water vapor absorption line. This paper discusses the use of that line as well as other CO(2) laser lines for which the absorption coefficients are weaker. The literature on measurement of water vapor absorption coefficients using CO(2) lasers is reviewed, and the results from four laboratories are shown to be generally consistent with each other after they are normalized to the same partial pressure, temperature, and ethylene absorption coefficient for the 1P(14) CO(2) laser line; however, the agreement with the Air Force Geophysics Laboratory's HITRAN and FASCOD 2 spectral data tapes is not good either for the water vapor absorption lines or for the water vapor continuum. Demonstration measurements of atmospheric water vapor have been conducted using the Mobile Atmospheric Pollutant Mapping System, a dual CO(2) lidar system using heterodyne detection. Results are discussed for measurements using three sets of laser line pairs covering a wide range of water vapor partial pressures.
迄今为止,二氧化碳激光雷达主要利用10.247微米处的10R(20)谱线来测量水汽浓度,该谱线与一条水汽吸收线有很强的重叠。本文讨论了该谱线以及其他吸收系数较弱的二氧化碳激光谱线的应用。回顾了利用二氧化碳激光测量水汽吸收系数的文献,四个实验室的结果在归一化为1P(14)二氧化碳激光谱线相同的分压、温度和乙烯吸收系数后,总体上相互一致;然而,对于水汽吸收线和水汽连续谱,与空军地球物理实验室的HITRAN和FASCOD 2光谱数据磁带的一致性都不好。利用移动大气污染物测绘系统(一种采用外差探测的双二氧化碳激光雷达系统)进行了大气水汽的示范测量。讨论了使用三组覆盖广泛水汽分压范围的激光线对进行测量的结果。