Raman lidar for measurement of tropospheric water vapor

被引:0
作者
Shang Z. [1 ,2 ]
Xie C. [1 ]
Zhong Z. [1 ]
Wang B. [1 ]
Wang Z. [1 ]
Zhao M. [1 ]
Tan M. [1 ,2 ]
Liu D. [1 ]
Wang Y. [1 ,2 ]
机构
[1] Key Laboratory of Atmospheric Composition and Optical Radiation, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei
[2] University of Science and Technology of China, Hefei
来源
Hongwai yu Jiguang Gongcheng/Infrared and Laser Engineering | 2016年 / 45卷 / 12期
关键词
Photoelectric detection; Raman lidar; Troposphere; Water vapor mixing ratio;
D O I
10.3788/IRLA201645.1211003
中图分类号
学科分类号
摘要
The content of water vapor in atmosphere is very little, but it is the most active molecule in atmosphere. The volume ratio of moisture to air was about 0.1%-4% and most part water vapor concentration in the troposphere. The influences of atmospheric attenuation become more serious along with the development of the optics-electron detecting technology. The water vapor in the atmosphere was the main factor and uncertain parameter to affect atmospheric attenuation. Infradred wavelengths was commonly used in photoelectric detection, but water vapor makes great effect on the radiation absorption due to its high concentration. Raman lidar has become the useful advantaged tools to measure water vapor. The system structure and specifications of Raman lidar developed by introduced. The measurement results show that this lidar can take measurements of water vapor over 8 km height at night and water vapor in boundary layer in day time as well as the tropospheric aerosol in day and night continuously. The obtained results are better consistent with radiosonde data in terms of the water vapor, which assures the reliability and availability of the Raman lidar for water vapor observation. © 2016, Editorial Board of Journal of Infrared and Laser Engineering. All right reserved.
引用
收藏
页数:6
相关论文
共 14 条
[1]  
Song Z., Applied Atmospheric Optics, (1990)
[2]  
Arnold T., Herry R., Estimating effects of temperature and moisture on in the dame unstable boundary layer for visible, infrared, ratio, and millimeter wavelengths, SPIE, 1668, pp. 465-476, (1992)
[3]  
Zhou X., Tao S., Yao K., Advanced Atmospheric Physics, (1990)
[4]  
Shine K.P., Sinha A., Sensitivity of the Earth's climate to height-dependent changes in the water vapor mixing ratio, Nature, 354, 6352, pp. 382-384, (1991)
[5]  
Nott G.J., Duck T.J., Doly J.G., Et al., A remotely operated lidar for aerosol, temperature, and water vapor profiling in the high Arctic, Journal of Atmospheric and Oceanic Technology, 29, 2, pp. 221-234, (2012)
[6]  
Wang H., Hua D., Wang Y., Et al., Design and analysis of new spectroscopic system of Raman lidar for detection of atmospheric water vapor, Acta Phys Sin, 62, 12, (2013)
[7]  
Wang Y., Gao F., Zhu C., Et al., Raman lidar for atmospheric temperature, humidity and aerosols up to troposphere Height, Acta Optica Sinica, 35, 3, (2015)
[8]  
Li T., Chen S., Zhang Y., Et al., Simulation of water vapor multiple wavelengths lidar echo signals and error analysis, Chinese Journal of Lasers, 42, 2, (2015)
[9]  
Xie C., Zhou J., Yue G., Et al., New mobile Raman lidar for measurement of tropospheric water vapor, Acta Optica Sinica, 26, 9, pp. 1281-1286, (2006)
[10]  
Xie C., Zhou J., Yue G., Et al., Mobile lidar system for measuring tropospheric aerosol and water vapor, Infrared and Laser Engineering, 36, 3, pp. 365-368, (2007)