Acta Optica Sinica, Volume. 38, Issue 12, 1228003(2018)

Influence of Ultraviolet Wavelength Selection on Detection Performance of All-Day Water Vapor Raman Lidar

Dongchen Shi*, Dengxin Hua*, Bo Huang, Ning Lei, and Fei Gao
Author Affiliations
  • School of Mechanical and Precision Instrument Engineering, Xi'an University of Technology, Xi'an, Shaanxi 710048, China
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    Figures & Tables(12)
    Spectrum of atmospheric backscattering signal
    Raman backscattering coefficients of N2 and H2O with excitation wavelengths of 354.7 nm and 266.0 nm
    (a) Extinction coefficient profiles and atmospheric transmissivity in standard atmosphere model, and (b) product between Raman backscattering coefficient and atmospheric transmissivity when excitation wavelengths are 354.7 nm and 266.0 nm
    (a) Ozone absorption coefficients for two kinds of ultraviolet wavelengths; (b) diurnal variation rule of ozone hourly concentrated in Xi’an main city
    (a) Ozone absorption of atmospheric two-way transmissivity during daytime and nighttime; (b) product between Raman backscattering coefficient and atmospheric transmissivity at 266.0 nm and 354.7 nm bands when ozone attenuation is considered
    (a) Polychromator at 54.7 nm; (b) polychromator at 266.0 nm
    Solar illumination spectra along normal directions on top of atmospheric layer and surface of earth
    Atmospheric backscattering ratio Rb for standard atmospheric model and cloud model
    (a) Clear and (b) cloudy daytime signal-to-noise ratio of N2 and H2O of two ultraviolet wavelengths
    • Table 1. Vibration Raman frequency shift, Raman central wavelength, and backscattering cross section of O2, N2, and H2O with excitation wavelengths of 354.7 nm and 266.0 nm

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      Table 1. Vibration Raman frequency shift, Raman central wavelength, and backscattering cross section of O2, N2, and H2O with excitation wavelengths of 354.7 nm and 266.0 nm

      Molecule kRaman frequency shift /cm-1Raman central wavelength /nm(λ354.7k) /(cm2·sr-1)(λ266.0k) /(cm2·sr-1)
      Excitation wavelength 354.7 nmExcitation wavelength 266.0 nm
      O21555375.8277.52.25×10-301.24×10-29
      N22331386.7283.62.8×10-309.68×10-30
      H2O3652407.8294.66.2×10-32.28×10-29
    • Table 2. Sun irradiation background noises at 266.0 nm and 354.7 nm of all Raman channels of Raman lidar

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      Table 2. Sun irradiation background noises at 266.0 nm and 354.7 nm of all Raman channels of Raman lidar

      Raman channel kSb(λ266.0k) /(W·m-2·nm-1)Sb(λ354.7k) /(W·m-2·nm-1)Pb(λ266.0k) /(10-14 J)Pb(λ354.7k) /(10-8 J)
      O200.455101.069
      N21.46×10-190.468501.100
      H2O1.6×10-60.88493.7572.078
    • Table 3. Parameters of 354.7 nm and 266.0 nm Raman lidar system

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      Table 3. Parameters of 354.7 nm and 266.0 nm Raman lidar system

      Wave range of transmission and receiving system /nmNd∶YAG laserPulse energy /mJPulse repetition frequency /HzPulse width /nsDetectorQuantum efficiency /%
      354.7Injection-seeded5001010Hamamatsu R389626
      266.0Injection-seeded1501010Hamamatsu R389629
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    Dongchen Shi, Dengxin Hua, Bo Huang, Ning Lei, Fei Gao. Influence of Ultraviolet Wavelength Selection on Detection Performance of All-Day Water Vapor Raman Lidar[J]. Acta Optica Sinica, 2018, 38(12): 1228003

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    Paper Information

    Category: Remote Sensing and Sensors

    Received: May. 22, 2018

    Accepted: Jul. 30, 2018

    Published Online: May. 10, 2019

    The Author Email:

    DOI:10.3788/AOS201838.1228003

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