• Journal of Atmospheric and Environmental Optics
  • Vol. 19, Issue 6, 624 (2024)
JI Fangli1,2,*, ZHAO Xin1, SI Fuqi1, ZHOU Haijin1..., QIAN Yuanyuan1,2 and YANG Taiping1,2|Show fewer author(s)
Author Affiliations
  • 1Key Laboratory of Environmental Optics and Technology, Anhui Institute of Optics and Fine Mechanics, HFIPS,Chinese Academy of Sciences, Hefei 230031, China
  • 2University of Science and Technology of China, Hefei 230026, China
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    DOI: 10.3969/j.issn.1673-6141.2024.06.002 Cite this Article
    Fangli JI, Xin ZHAO, Fuqi SI, Haijin ZHOU, Yuanyuan QIAN, Taiping YANG. Research on DOAS algorithm based on discrete wavelength[J]. Journal of Atmospheric and Environmental Optics, 2024, 19(6): 624 Copy Citation Text show less
    DW-DOAS algorithm data processing flow chart
    Fig. 1. DW-DOAS algorithm data processing flow chart
    [in Chinese]
    Fig. 2. [in Chinese]
    Fitting results of DW-DOAS and DOAS retrieving NO2 SCD when select different FWHM on January 1, 2019.(a) 1 nm; (b) 2 nm; (c) 3 nm; (d) 4 nm
    Fig. 3. Fitting results of DW-DOAS and DOAS retrieving NO2 SCD when select different FWHM on January 1, 2019.(a) 1 nm; (b) 2 nm; (c) 3 nm; (d) 4 nm
    NO2 absorption cross section (solid line) and selected central wavelength (dashed line) for ground data
    Fig. 4. NO2 absorption cross section (solid line) and selected central wavelength (dashed line) for ground data
    Fitting results of DW-DOAS and DOAS retrieving NO2 SCD when select different elevation from January 1 to March 31, 2019. (a) 5°; (b) 10°; (c) 20°; (d)30°
    Fig. 5. Fitting results of DW-DOAS and DOAS retrieving NO2 SCD when select different elevation from January 1 to March 31, 2019. (a) 5°; (b) 10°; (c) 20°; (d)30°
    NO2 absorption cross section (solid line) and selected central wavelength (dashed line) for EMI data
    Fig. 6. NO2 absorption cross section (solid line) and selected central wavelength (dashed line) for EMI data
    NO2 SCD retrieved by DOAS (a) and corresponding by DW-DOAS (b) for one orbit of 6 January 2019, and the relative differences (c) between them
    Fig. 7. NO2 SCD retrieved by DOAS (a) and corresponding by DW-DOAS (b) for one orbit of 6 January 2019, and the relative differences (c) between them
    Fitting results of DW-DOAS and DOAS retrieving NO2 SCD for one orbit of 6 January 2019
    Fig. 8. Fitting results of DW-DOAS and DOAS retrieving NO2 SCD for one orbit of 6 January 2019
    NO2 SCD retrieved by DOAS (a) and corresponding by DW-DOAS (b) for all orbits of 6 January 2019, and the relative differences (c) between them
    Fig. 9. NO2 SCD retrieved by DOAS (a) and corresponding by DW-DOAS (b) for all orbits of 6 January 2019, and the relative differences (c) between them
    Different algorithms

    The appearance of

    wavelength

    Polynomial degreeFitting parametersWavelength calibration
    DOASContinuous5NO2, O3, O4, H2O, RingBefore fit
    DW-DOASDispersed2NO2, O3, O4, H2O, RingNo
    Table 1. NO2 SCD retrieval details for DOAS and DW-DOAS
    Elevation angle/(o)CorrelationAverage relative error/%Mean absolute differenceRoot mean square error
    50.9986.77.51 × 10155.07 × 1015
    100.9996.66.54 × 10155.34 × 1015
    200.9994.24.56 × 10153.21 × 1015
    300.9993.61.12 × 10159.92 × 1014
    Table 2. The results of retrieving NO2 SCD at elevation angles of 5°,10°,20°and 30°
    Fangli JI, Xin ZHAO, Fuqi SI, Haijin ZHOU, Yuanyuan QIAN, Taiping YANG. Research on DOAS algorithm based on discrete wavelength[J]. Journal of Atmospheric and Environmental Optics, 2024, 19(6): 624
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