[1] Li Gang, Tan Yanke, Li Chongyin, et al. The distribution characteristics of total ozone and its relationship with stratospheric temperature during boreal winter in the recent 30 years[J]. Chinese Journal of Geophysics, 2015, 58(5): 1475-1491.
[2] Luo Yuhan, Liu Wenqing, Bian Lingen, et al. The retrieval of ozone column densities by passive differential optical absorption spectroscopy during summer at Zhongshan station, Antarctic[J]. Spectroscopy and Spectral Analysi, 2011, 31(2): 456-460.
[4] Farman J C, Gardiner B G, Shanklin J D. Large losses of total ozone in Antarctica reveal seasonal CIOx/NOx interaction[J]. Nature, 1985, 315: 207-210.
[5] Yan Huanhuan, Wang Weihe, Zhang Xingying, et al. Ozone column retrieved from GF-5 satellite environmental trace gas monitoring instrument[J]. Aerospace Shanghai, 2019, 36(Sup 2): 199-203.
[6] Rozanov V V, Diebel D, Spurr R J D, et al. GOMETRAN: A radiative transfer model for the satellite project GOME, the plane-parallel version[J]. Journal of Geophysical Research: Atmospheres, 1997, 102(D14): 16683-16695.
[7] Burrows J P, Holzle E, Goede A P H, et al. SCIAMACHY-scanning imaging absorption spectrometer for atmospheric chartography[J]. Acta Astronautica, 1995, 35(7): 445-451.
[8] Nett H, Frerick J, Paulsen T, et al. The atmospheric instruments and their applications: GOMOS, MIPAS and SCIAMACHY[J]. ESA Bulletin, 2001, 106: 77-87.
[9] Compernolle S, Verhoelst T, Pinardi G, et al. Validation of Aura-OMI QA4ECV NO2 climate data records with ground-based DOAS networks: the role of measurement and comparison uncertainties[J]. Atmospheric Chemistry and Physics, 2020, 20(13): 8017-8045.
[10] Xue R B, Wang S S, Li D R, et al. Spatio-temporal variations in NO2 and SO2 over Shanghai and Chongming Eco-Island measured by ozone monitoring instrument (OMI) during 2008-2017[J]. Journal of Cleaner Production, 2020, 258: 120563.
[11] Xie B, Zhang H, Wang Z L, et al. A modeling study of effective radiative forcing and climate response due to tropospheric ozone[J]. Advances in Atmospheric Sciences, 2016, 33(7): 819-828.
[12] Shikwambana L, Mhangara P, Mbatha N. Trend analysis and first time observations of sulphur dioxide and nitrogen dioxide in South Africa using TROPOMI/Sentinel-5 P data[J]. International Journal of Applied Earth Observation and Geoinformation, 2020,91: 102130.
[13] Katerina G, Maria E K, Tijl V, et al. TROPOMI/S5P total ozone column data: Global ground-based validation and consistency with other satellite missions[J]. Atmospheric Measurement Techniques, 2019, 12(10): 5263-5287.
[14] Cheng L X, Tao J H, Valks P, et al. NO2 retrieval from the environmental trace gases monitoring instrument (EMI): Preliminary results and intercomparison with OMI and TROPOMI[J]. Remote Sensing, 2019, 11(24): 3017.
[15] Liu Li, Zheng Xiangdong, Chen Shu, et al. Validation study of FY-3A-TOU total ozone using ground-based data[J]. Chinese Journal of Space Science, 2015, 35(6): 696-706.
[16] Wang Weihe, Zhang Xingying, An Xingqin, et al. Analysis for retrieval and validation results of FY-3 total ozone unit (TOU)[J]. Chinese Science Bulletin, 2010, 55(17): 1726-1733.
[17] Veefkind J P, Johan F H, Ellen J B, et al. Total ozone from the ozone monitoring instrument (OMI) using the DOAS technique[J]. IEEE Transactions on Geoscience and Remote Sensing, 2006, 44(5): 1239-1244.
[18] Bogumil K, Orphal J, Homann T, et al. Measurements of molecular absorption spectra with the SCIAMACHY preflight model: instrument characterization and reference data for atmospheric remote-sensing in the 230-2380 nm region[J]. Journal of Photochemistry and Photobiology A: Chemistry, 2003, 157(2-3): 167-184.
[19] Platt U, Stutz J. Differential Optical Absorption Spectroscopy[M]. Physics of Earth and Space Environments. Berlin, Heidelberg: Springer Berlin Heidelberg, 2008: 135-174.
