Volume 43 Issue 9
Oct.  2014
Turn off MathJax
Article Contents

Yan Shunsheng. Boltzmann-temperature model for enhancing precision of Raman detection aerosol extinction coefficient[J]. Infrared and Laser Engineering, 2014, 43(9): 3015-3019.
Citation: Yan Shunsheng. Boltzmann-temperature model for enhancing precision of Raman detection aerosol extinction coefficient[J]. Infrared and Laser Engineering, 2014, 43(9): 3015-3019.

Boltzmann-temperature model for enhancing precision of Raman detection aerosol extinction coefficient

  • Received Date: 2014-01-11
  • Rev Recd Date: 2014-02-10
  • Publish Date: 2014-09-25
  • Standard model atmosphere is usually adopted in Raman lidar aerosol extinction coefficient inversion, but sometimes standard model atmosphere does not match the actual atmospheric density so cause a greater impact on the detection results. In order to reduce the influence to enhance Raman lidar aerosol extinction coefficient inversion precision, a new model which atmospheric density profile was determinated by the Boltzmann energy distribution and tropospheric temperature linear decline law was proposed to replace standard model atmosphere, Theoretical derivation and experiment verify the feasibility of the method, and the result shows that the new model is more consistent with actual atmosphere, so it can reduce the error, it is proposed Raman lidar data processing may use this new model.
  • [1]
    [2] Cheng Xuewu, Yang Guotao, Yang Yong, et al. Na layerand K layer simultaneous observation by lidar [J]. ChineseJournal of Lasers, 2011, 38(2): 0214001. (in Chinese)程学武, 杨国韬, 杨勇, 等. 高空钠层、钾层同时探测的激光雷达[J]. 中国激光, 2011, 38(2): 0214001.
    [3] Cao Kaifa, Zhao Bo, Fang Xin, et al. Fluorescence lidar forremote monitoring of plant[J]. Chinese Optics Letters, 2010,8(2): 130-133.
    [4]
    [5]
    [6] Ansmann A, Riebesel M, Weitkamp C. Measurement ofatmospheric aerosol extinction profiles with a Raman lidar[J]. Opt Lett, 1990, 15: 746-748.
    [7] Whiteman D N, Melfi S H, Ferrare R A. Raman lidarsystem for the measurement of water vapor and aerosols inthe Earth's atmosphere [J]. Appl Opt, 1992, 31(16): 3068-3082.
    [8]
    [9]
    [10] Fernald F G. Analysis of atmosphere lidar observation: somecomments[J]. Appl Opt, 1984, 23(5): 652-653.
    [11] Bo Guangyu, Xie Chenbo, Liu Dong, et al. Opticalproperties of aerosol in planetary boundary layer measuredby Raman lidar at Hefei in summer and autumn[J]. ChineseJ Lasers, 2010, 37(10): 2526-2532. (in Chinese)伯广宇, 谢晨波, 刘东, 等. 拉曼激光雷达探测合肥地区夏秋季边界层气溶胶的光学性质[J]. 中国激光, 2010, 37(10):2526-2532.
    [12]
    [13]
    [14] Hua Dengxin, Song Xiaoquan. Advances in lidar remotesensing techniques [J]. Infrared and Laser Engineering,2008, 37(2): 21-26. (in Chinese)华灯鑫, 宋小全. 先进激光雷达探测技术研究进展[J]. 红外与激光工程, 2008, 37(2): 21-26.
    [15] Ferrare R A, Melfi S H, Whiteman C N, et al. Raman lidarmeasurements of aero-sol extinction and backscatter 1.Methods and comparisons [J]. J Geophys Res, 1998, 103:19663-19672.
    [16]
    [17]
    [18] Hu Shunxing, Wang Xiaobin, Wu Yonghua, et al. Geometricalform factor determination with Raman backscattering signals[J]. Optics Letters, 30(14): 1879-1881.
    [19]
    [20] Xue Datong. Studies of altitude distribution of earth' satmosphere density [J]. Journal of Vacuum Science andTechnology, 2009, 29: 6-7. (in Chinese)薛大同. 对地球大气密度随高度分布规律的讨论[J]. 真空科学与技术学报, 2009, 29: 6-7.
    [21] Sun Jingqun. Laser Atmosphere Detect [M]. Beijing: SciencePress, 1986: 2-3. (in Chinese)孙景群.激光大气探测[M]. 北京: 科学出版社, 1986: 2-3.
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(816) PDF downloads(257) Cited by()

Related
Proportional views

Boltzmann-temperature model for enhancing precision of Raman detection aerosol extinction coefficient

  • 1. Basic Teaching Department,Tangshan College,Tangshan 063000,China

Abstract: Standard model atmosphere is usually adopted in Raman lidar aerosol extinction coefficient inversion, but sometimes standard model atmosphere does not match the actual atmospheric density so cause a greater impact on the detection results. In order to reduce the influence to enhance Raman lidar aerosol extinction coefficient inversion precision, a new model which atmospheric density profile was determinated by the Boltzmann energy distribution and tropospheric temperature linear decline law was proposed to replace standard model atmosphere, Theoretical derivation and experiment verify the feasibility of the method, and the result shows that the new model is more consistent with actual atmosphere, so it can reduce the error, it is proposed Raman lidar data processing may use this new model.

Reference (21)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return