Acta Optica Sinica, Volume. 45, Issue 6, 0601001(2025)

Fluorescence Fluctuation Characteristics Simulation Study of Chromophoric Dissolved Organic Matter under Rough Sea Surface Based on Laser Induced Fluorescence

Beibei Xie1...2,*, Kaijie Ma1, Yingjie Wang1, Wang Gao1, Jiawei Zhao1 and Deming Kong3 |Show fewer author(s)
Author Affiliations
  • 1School of Information Science and Engineering, Yanshan University, Qinhuangdao 066004, Hebei , China
  • 2Key Laboratory of Computer Virtual Technology and System Integration in Hebei Province, Qinhuangdao 066004, Hebei , China
  • 3School of Electrical Engineering, Yanshan University, Qinhuangdao 066004, Hebei , China
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    Figures & Tables(12)
    Simulation results of CDOM fluorescence. (a) Front view; (b) top view
    Simulation results of rough sea surface
    Simulation results of CDOM fluorescence under rough sea surface. (a) Front view; (b) top view
    Sea surface simulation results of different wind directions under wind speed of 9 m/s. (a)‒(c) Wind direction is 0°, t=0, 1, and 2 s; (d)‒(f) wind direction is 90°, t=0, 1, and 2 s
    BRRDFcos θicos θr of each receiving zenith angle is detected along different azimuths under sea surface at 0° wind direction. (a) Azimuth angle of 0°; (b) azimuth angle of 90°; (c) azimuth angle of 180°; (d) azimuth angle of 270°
    BRRDFcos θicos θr of each receiving zenith angle is detected along different azimuths under sea surface at 90° wind direction. (a) Azimuth angle of 0°; (b) azimuth angle of 90°; (c) azimuth angle of 180°; (d) azimuth angle of 270°
    Simulation results of sea surface with different wind speeds. (a)‒(c) Wind speed of 9 m/s, t=0, 1, and 2 s; (d)‒(f) wind speed of 16 m/s, t=0, 1, and 2 s
    BRRDFcos θicos θr simulation results of each received zenith angle under different wind speeds. (a) Wind speed of 9 m/s; (b) wind speed of 16 m/s
    Experimental design. (a) Sea surface slopes up in direction of reception; (b) increase laser incidence angle and receiving zenith angle; (c) sea surface slopes up against receiving direction; (d) increase laser incidence angle and decrease receiving zenith angle
    Experimental results. (a) Simulation results of sea surface sloping up in direction of reception; (b) simulation results of sea surface sloping up against receiving direction
    • Table 1. Simulation parameters of three-dimensional sea surface under typical wind scale

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      Table 1. Simulation parameters of three-dimensional sea surface under typical wind scale

      Wind scaleWind velocity /(m·s-1Lower cut-off frequency /(rad·s-1Upper cut-off frequency /(rad·s-1
      351.25.0
      470.64.0
      590.52.5
      6130.42.0
      7160.31.6
    • Table 2. CDOM absorption coefficient and scattering coefficient of seawater with different wavelengths

      View table

      Table 2. CDOM absorption coefficient and scattering coefficient of seawater with different wavelengths

      Wavelength /nmSeawater
      Absorption coefficient /m-1Scattering coefficient /m-1
      3501.8070.377
      4601.1320.327
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    Beibei Xie, Kaijie Ma, Yingjie Wang, Wang Gao, Jiawei Zhao, Deming Kong. Fluorescence Fluctuation Characteristics Simulation Study of Chromophoric Dissolved Organic Matter under Rough Sea Surface Based on Laser Induced Fluorescence[J]. Acta Optica Sinica, 2025, 45(6): 0601001

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    Paper Information

    Category: Atmospheric Optics and Oceanic Optics

    Received: Jun. 3, 2024

    Accepted: Jul. 16, 2024

    Published Online: Mar. 17, 2025

    The Author Email: Xie Beibei (beibeixie@ysu.edu.cn)

    DOI:10.3788/AOS241125

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