Acta Optica Sinica, Volume. 43, Issue 18, 1801001(2023)

Maximum Correlated k-Distribution Optimal Algorithm for Single-Scattering Parameters in Cloudy Atmospheres

Yin Zhang, Shaoshuai Zhang, Hao Yan, Yiwei Fan, Guiyi Zhu, and Junhua Yan*
Author Affiliations
  • Key Laboratory of Space Photoelectric Detection and Perception, Ministry of Industry and Information Technology, Nanjing University of Aeronautics and Astronautics, Nanjing 210016, Jiangsu, China
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    Figures & Tables(17)
    Spectral parameter distribution curves of a cloudy atmosphere under different temperatures, atmospheric pressures, particle effective radii, and water contents. (a) Cloudy atmosphere extinction coefficient; (b) cloudy atmosphere single-scattering albedo; (c) cloudy atmosphere asymmetry factor
    Spectral distribution curves of single-scattering albedo. (a) Cloud single-scattering albedo; (b) cloudy atmosphere single-scattering albedo
    Schematic of the maximal correlated parameter grouping method
    Schematic of solving number of quadrature intervals in each group
    Schematic of the rearrangement of spectral parameters and the solution of average equivalent parameters
    Schematic of average extinction coefficient and processed average extinction coefficient in cloudy areas. (a) Spectral distribution of cloudy average extinction coefficient; (b) cloudy average extinction coefficient in g space;(c) cloudy average extinction coefficient after scaling; (d) average extinction coefficient after scaling in g space
    MRE changing with the increasing interval amount when calculating upwelling radiance for the cloudy atmosphere using different CKD methods. (a) Band b1; (b) band b2; (c) band b3; (d) band b4
    Scheme of the maximal correlated parameter grouping situation in band b3 when number of the quadrature intervals is greater than two
    In band b3, spectrum distribution curves of parameters in a cloudy atmosphere, rearrangement of these parameters and average equivalent parameters in each interval when number of quadrature intervals is eight. (a)(b) Extinction coefficient; (c)(d) asymmetry factor; (e)(f) single-scattering albedo; (g)(h) solar flux density
    • Table 1. Visible and near-infrared surface radiation accounted for the proportion of total upward radiation

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      Table 1. Visible and near-infrared surface radiation accounted for the proportion of total upward radiation

      Cloud typeBase /kmTop /kmCloud extinction coefficient /km-1Optical thicknessProportion
      As2.4003.000128.176.95.4×10-35
      Ns0.1600.66092.646.32.6×10-21
      Sc0.6601.00038.713.29.5×10-7
      Sc0.6600.86038.77.742.7×10-4
      Sc0.6600.76038.73.871.6×10-2
      Sc0.6600.71538.72.121.0×10-1
    • Table 2. Parameters of the cloudy atmosphere scene

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      Table 2. Parameters of the cloudy atmosphere scene

      ParameterContent
      Atmospheric model1976 U.S. standard atmosphere
      Atmospheric altitude range/km0-100
      AbsorberH2O,CO2,CH4,N2O,O3,CO,N2,O2
      Scattering phase function modelH-G model
      Ground temperature /K288
      Ground albedo0.03
      Cloud typeCu
      Altitude range of cloud /km4.02-5.22
      Vertical resolution /km0.04
      Average liquid water content of cloud /(g∙m-30.16
      Average particle effective radius of cloud /μm6.10
    • Table 3. Band setting and the corresponding average atmospheric transmittance

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      Table 3. Band setting and the corresponding average atmospheric transmittance

      Band No.Band range /μmWavenumber range /cm-1Average transmittance
      b12.20-2.404165-45450.8847
      b21.80-1.955125-55550.0293
      b31.50-2.005000-66650.6537
      b42.30-2.60384-43500.4281
    • Table 4. Group and intra-group quadrature weights in band b3 at number of quadrature intervals equaling to eight

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      Table 4. Group and intra-group quadrature weights in band b3 at number of quadrature intervals equaling to eight

      GroupMaximal correlated parameterIntegral weight between groupsQuadrature weight
      1FTOA0.48870.43800.07560.08850.3980
      2ω0.51130.05050.17560.16090.6130
    • Table 5. Experimental design of clouds at different heights

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      Table 5. Experimental design of clouds at different heights

      Scene No.Band numberAltitude range of cloud /km
      1b31.02-2.22
      24.02-5.22
      39.02-10.22
    • Table 6. MRE calculated by different methods in cloud scenes at different altitudes

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      Table 6. MRE calculated by different methods in cloud scenes at different altitudes

      Scene No.MRE of radiance /%
      ΔlogkPCOP-CKDSSP-MCKD
      Average error28.607.311.68
      132.695.300.47
      227.077.534.30
      326.059.100.26
    • Table 7. Experimental design of cloud scenes with different particle effective radii and water content

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      Table 7. Experimental design of cloud scenes with different particle effective radii and water content

      Cloud sceneScene No.Average particle effective radius of cloud /μm

      Average liquid water content of cloud /

      (g∙m-3

      Average cloud extinction coefficient /km-1Standard deviation of cloud extinction coefficient /km-1
      CuS16.100.1645.3821.75
      ScS212.420.2330.2714.32
      S314.720.5257.2037.42
      S416.050.6867.185.60
      AcS513.720.3642.6411.53
      S615.520.5052.0213.32
      S716.020.5858.3717.46
    • Table 8. MRE calculated by different methods in cloud scenes with different optical properties

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      Table 8. MRE calculated by different methods in cloud scenes with different optical properties

      Scene No.MRE of radiance /%
      ΔlogkPCOP-CKDSSP-MCKD
      Average error23.278.855.54
      S127.077.534.30
      S214.683.322.03
      S331.2318.3213.67
      S421.985.793.51
      S516.326.861.54
      S623.898.176.32
      S727.7511.967.44
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    Yin Zhang, Shaoshuai Zhang, Hao Yan, Yiwei Fan, Guiyi Zhu, Junhua Yan. Maximum Correlated k-Distribution Optimal Algorithm for Single-Scattering Parameters in Cloudy Atmospheres[J]. Acta Optica Sinica, 2023, 43(18): 1801001

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    Paper Information

    Category: Atmospheric Optics and Oceanic Optics

    Received: Nov. 22, 2022

    Accepted: Feb. 7, 2023

    Published Online: Sep. 4, 2023

    The Author Email: Yan Junhua (yjh9758@126.com)

    DOI:10.3788/AOS222030

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