• Acta Optica Sinica
  • Vol. 38, Issue 5, 0501001 (2018)
Qi Zhao1、2, Chaolong Cui、*, Honghua Huang1, Wenyue Zhu1, and Ruizhong Rao1、2
Author Affiliations
  • 1 Key Laboratory of Atmospheric Optics, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei, Anhui 230031, China
  • 2 School of Environmental Science and Optoelectronic Technology, University of Science and Technology of China, Hefei, Anhui 230026, China
  • 2 Science Island Branch of Graduate School, University of Science and Technology of China, Hefei, Anhui 230031, China
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    DOI: 10.3788/AOS201838.0501001 Cite this Article Set citation alerts
    Qi Zhao, Chaolong Cui, Honghua Huang, Wenyue Zhu, Ruizhong Rao. Effect of Inner Scale on Measurement Results of Residual Turbulent Scintillation Lidar[J]. Acta Optica Sinica, 2018, 38(5): 0501001 Copy Citation Text show less
    Influences of inner scale and length on Cn2 using two atmospheric turbulence spectrum models. (a) Modified Hill spectrum; (b) Rytov improved model
    Fig. 1. Influences of inner scale and length on Cn2 using two atmospheric turbulence spectrum models. (a) Modified Hill spectrum; (b) Rytov improved model
    Comparison of Cn2 calculated by modified Hill spectrum under different inner scales and Kolmogorov spectrum. (a) Experimental result of all day when L=1020 m; (b) enlarged experimental result in 18:00/19:15 when L=1020 m; (c) experimental result of all day when L=2040 m; (d) enlarged experimental result in 18:00/19:15 when L=2040 m
    Fig. 2. Comparison of Cn2 calculated by modified Hill spectrum under different inner scales and Kolmogorov spectrum. (a) Experimental result of all day when L=1020 m; (b) enlarged experimental result in 18:00/19:15 when L=1020 m; (c) experimental result of all day when L=2040 m; (d) enlarged experimental result in 18:00/19:15 when L=2040 m
    Comparison of Cn2 calculated by Rytov improved model under different inner scales and Kolmogorov spectrum. (a) Experimental result of all day when L=1020 m; (b) enlarged experimental result in 18:00/19:15 when L=1020 m; (c) experimental result of all day when L=2040 m; (d) enlarged experimental result in 18:00/19:15 when L=2040 m
    Fig. 3. Comparison of Cn2 calculated by Rytov improved model under different inner scales and Kolmogorov spectrum. (a) Experimental result of all day when L=1020 m; (b) enlarged experimental result in 18:00/19:15 when L=1020 m; (c) experimental result of all day when L=2040 m; (d) enlarged experimental result in 18:00/19:15 when L=2040 m
    L /ml0 /mmAVGBIASMAEMRE /%
    10201-14.8770.0500.0490.330
    13-14.577-0.2500.2511.692
    20401-14.8360.0040.0030.021
    13-14.718-0.1140.1140.775
    Table 1. Statistical analysis for lg Cn2 of finite inner scale and not considering inner scale using modified Hill spectrum
    L /ml0 /mmAVGBIASMAEMRE /%
    10201-15.3690.5420.5423.655
    13-14.812-0.0150.0150.101
    20401-15.3540.5220.5223.399
    13-15.0310.1990.1981.317
    Table 2. Statistical analysis for lg Cn2 of finite inner scale and not considering inner scale using Rytov improved model
    Qi Zhao, Chaolong Cui, Honghua Huang, Wenyue Zhu, Ruizhong Rao. Effect of Inner Scale on Measurement Results of Residual Turbulent Scintillation Lidar[J]. Acta Optica Sinica, 2018, 38(5): 0501001
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