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Deng Pan, Zhang Tianshu, Chen Wei, Liu Yang. Lidar measurement for atmospheric density and temperature in middle atmosphere over Hefei[J]. Infrared and Laser Engineering, 2017, 46(7): 730003-0730003(6). doi: 10.3788/IRLA201746.0730003
Citation: Deng Pan, Zhang Tianshu, Chen Wei, Liu Yang. Lidar measurement for atmospheric density and temperature in middle atmosphere over Hefei[J]. Infrared and Laser Engineering, 2017, 46(7): 730003-0730003(6). doi: 10.3788/IRLA201746.0730003
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Lidar measurement for atmospheric density and temperature in middle atmosphere over Hefei

doi: 10.3788/IRLA201746.0730003
  • 1.

    Anhui Institute of Optics and Fine Mechanics,Chinese Academy of Sciences,Hefei 230031,China;

  • 2.

    University of Science and Technology of China,Hefei 230036,China;

  • 3.

    State Key Laboratory of Pulsed Power Laser Technology(Electronic Engineering Institute),Hefei 230037,China

  • Received Date: 2016-11-04
  • Rev Recd Date: 2016-12-08
  • Publish Date: 2017-07-25
  • In order to study the distributed situation of the middle atmosphere, a self-developed Rayleigh scattering lidar used to remote sensing in the altitude range 25-40 km was introduced, which was located at Hefei(31.90 N; 117.170 E), China. Rayleigh scattering lidar with 532 nm wavelength made the measurements of atmospheric density and temperature. The results obtained by Rayleigh scattering lidar were compared with the data provided by NRLMSISE-00 Atmosphere Model to prove the Rayleigh scattering lidar system performance and the reliability of the data processing method. Through comparison and analysis of the result data, it can be found that the density ratio of Rayleigh scattering lidar to NRLMSISE-00 Atmosphere Model is from 0.99 to 1.03, and the temperature biases between Rayleigh scattering lidar and NRLMSISE-00 Atmosphere Model are about 2.8 K from 25 km to 40 km. Especially under the altitude 38 km, the temperature biases is about 1.6 K. These results indicate that atmospheric density and temperature profiles obtained by Rayleigh lidar show the coincident distribution with the data of NRLMSISE-00 Atmosphere Model over the altitudes of 25 km to 40 km, and the Rayleigh scattering lidar can represent the distribution of the atmospheric density and temperature between the altitude 25 km and 40 km over Hefei.
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    [2] Liu Dong, Yang Yongying, Zhou Yudi, et al. High spectral resolution lidar for atmosphere remote sensing:a review[J]. Infrared and Laser Engineering, 2015, 44(9):2535-2546. (in Chinese)刘东, 杨甬英, 周雨迪, 等. 大气遥感高光谱分辨率激光雷达研究进展[J]. 红外与激光工程, 2015, 44(9):2535-2546.
    [3] Mariche V V N, MatVienko G G, Tikhomiro V A A, et al. Evaluation of the capability of Lidar placed onboard an orbital platform to measure the atmospheric density profiles[C]//Proceedings of SPIE, 2014, 9292:92925L.
    [4] Alain Hauchecorne, Marie-Lise Chanin. Density and temperature profiles obtained by lidar between 35 and 75 km[J]. Geophysical Research Letters, 1980, 7(8):565-668.
    [5] Robert L McKenzie. A method of atmospheric density measurements during space shuttle entry using ultraviolet-laser Rayleigh scattering[Z]. US:NASA Technical Memorandum, 1988.
    [6] Chen W N, Tsao C C, Nee J B. Rayleigh 1idar temperature measurements in the upper troposphere and lower stratosphere[J]. Journal of Atmospheric and Solar-Terrestrial Physics, 2004, 66:39-49.
    [7] Dai Yongjiang. Laser and Infrared Sounds Principle[M]. Beijing:National Defense Industry Press, 2012:271-272. (in Chinese)戴永江. 激光与红外探测原理[M]. 北京:国防工业出版社,2012:271-272.
    [8] Barnett J J, Corney M. Middle Atmospheric Reference Model Derived from Satellite Data[M]. US:International Council of Scientific Unions Middle Atmosphere Program, 1985, 16:47-85.
    [9] Weitkamp C. Lidar Range-Resolve Optical Remote Sensing of the Atmosphere[M]. Germany:Springer Science and Business Media, 2005:6-12.
    [10] Liu Xiaoqin. The Na-T-A lidar system and its observation of sodium density and atmospheric temperature[D]. Hefei:Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, 2006. (in Chinese)刘小勤. Na-T-A激光雷达系统及钠层密度和大气温度探测研究[D]. 合肥:中国科学院安徽光学精密机械研究所, 2006.
    [11] Tang Lei, Wu Haibin, Sun Dongsong, et al. Analysis of system accuracy for Rayleigh backscattering Doppler wind lidar[J]. Infrared and Laser Engineering, 2014, 43(11):3570-3576. (in Chinese)唐磊, 吴海滨, 孙东松, 等. 瑞利散射多普勒测风激光雷达系统误差分析[J]. 红外与激光工程, 2014, 43(11):3570-3576.
    [12] Wang Guocheng, Dou Xiankang, Xia Haiyun, et al. Performance of a Rayleigh Doppler lidar for middle atmosphere wind measurement[J]. Infrared and Laser Engineering, 2012, 41(9):2351-2357.
    [13] Picone J M, Hedin A E, Drob D P, et al. NRLMSISE-00 empirical model of the atmosphere:Statistical comparisons and scientific issues[J]. J Geophys Res, 2002, 107:1468-1483.
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Lidar measurement for atmospheric density and temperature in middle atmosphere over Hefei

doi: 10.3788/IRLA201746.0730003
  • 1. Anhui Institute of Optics and Fine Mechanics,Chinese Academy of Sciences,Hefei 230031,China;
  • 2. University of Science and Technology of China,Hefei 230036,China;
  • 3. State Key Laboratory of Pulsed Power Laser Technology(Electronic Engineering Institute),Hefei 230037,China
  • Received Date: 2016-11-04
  • Rev Recd Date: 2016-12-08
  • Publish Date: 2017-07-25

Abstract: In order to study the distributed situation of the middle atmosphere, a self-developed Rayleigh scattering lidar used to remote sensing in the altitude range 25-40 km was introduced, which was located at Hefei(31.90 N; 117.170 E), China. Rayleigh scattering lidar with 532 nm wavelength made the measurements of atmospheric density and temperature. The results obtained by Rayleigh scattering lidar were compared with the data provided by NRLMSISE-00 Atmosphere Model to prove the Rayleigh scattering lidar system performance and the reliability of the data processing method. Through comparison and analysis of the result data, it can be found that the density ratio of Rayleigh scattering lidar to NRLMSISE-00 Atmosphere Model is from 0.99 to 1.03, and the temperature biases between Rayleigh scattering lidar and NRLMSISE-00 Atmosphere Model are about 2.8 K from 25 km to 40 km. Especially under the altitude 38 km, the temperature biases is about 1.6 K. These results indicate that atmospheric density and temperature profiles obtained by Rayleigh lidar show the coincident distribution with the data of NRLMSISE-00 Atmosphere Model over the altitudes of 25 km to 40 km, and the Rayleigh scattering lidar can represent the distribution of the atmospheric density and temperature between the altitude 25 km and 40 km over Hefei.

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