[1] Rosenfeld D. Aerosols, clouds, and climate［J］. Science, 2006, 312(5778): 1323-1324.

[2] Finlayson-Pitts B J, Pitts J N. Chemistry of the upper and lower atmosphere: Theory, experiments, and applications［M］. San Diego: Academic Press, 1999.

[3] Huebert B J, Bates T, Russell P B, et al. An overview of ACE-Asia: Strategies for quantifying the relationships between Asian aerosol and their climatic impacts［J］. Journal of Geophysical Research, 2003, 108(D23): 8633.

[4] Ramanathan V, Crutzen P J, Kiehl J T, et al. Aerosols, climate, and the hydrological cycle［J］. Science, 2001, 294(5549): 2119-2124.

[5] 吴丰成. 基于车载差分吸收光谱技术的城市大气污染物探测研究［D］. 合肥: 中国科学院安徽光学精密机械研究所, 2013.

    Wu Fengcheng. Observations of distribution and emission for air pollution in urban area by mobile differential optical absorption spectroscopy［D］. Hefei: Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, 2013.

[6] 李 菲, 邓雪娇, 谭浩波. 微量振荡天平法与激光散射单粒子法在气溶胶观测中的对比试验研究［J］. 热带气象学报, 2015, 31(4): 497-504.

    Li Fei, Deng Xuejiao, Tan Haobo. Comparative study of tapered element oscillating microbalance technology and principle of single particle laser scattering used in measuring aerosol loading［J］. Journal of Tropical Meteorology, 2015, 31(4): 497-504.

[7] Dubovik O, Holben B, Eck T F. Variability of absorption and optical properties of key aerosol types observed in worldwide locations［J］. Journal of the Atmospheric Sciences, 2002, 59(3): 590-608.

[8] Ancellet G, Francois R. Compact airborne lidar for tropospheric ozone: Description and field measurements［J］. Applied Optics, 1998, 37(24): 5509-5521.

[9] Wagner T, Dix B, Friedeburg C V. MAX-DOAS O4 measurements: A new technique to derive information on atmospheric aerosols - Principles and information content［J］. Journal of Geophysical Research, 2004, 109(D22): D22205.

[10] Wagner T, Beirle S, Deutschmann T. Three-dimensional simulation of the Ring effect in observations of scattered sun light using Monte Carlo radiative transfer models［J］. Atmospheric Measurement Techniques, 2009, 2(1): 113-124.

[11] Wagner T, Deutschmann T, Platt U. Determination of aerosol properties from MAX-DOAS observations of the Ring effect［J］. Atmospheric Measurement Techniques, 2009, 2(2): 495-512.

[12] Ortega I, Coburn S. The CU 2-D-MAX-DOAS instrument - Part 2: Raman scattering probability measurements and retrieval of aerosol optical properties［J］. Atmospheric Measurement Techniques, 2016, 9(8): 3893-3910.

[13] 裴 显, 李 昂, 谢品华. 基于Monte Carlo大气辐射传输模型的Ring效应模拟［J］. 大气与环境光学学报, 2013, 8(5): 354-363.

    Pei Xian, Li Ang, Xie Pinhua. Ring effect simulation based on Monte Carlo atmospheric radiative transfer model［J］. Journal of atmospheric and Environment Optics, 2013, 8(5): 354-363.

[14] Wang Y, Li A, Xie P H. A rapid method to derive horizontal distributions of trace gases and aerosols near the surface using multi-axis differential optical absorption spectroscopy［J］. Atmospheric Measurement Techniques, 2014, 7(6): 1663-1680.

[15] 吴丰成, 谢品华, 李 昂, 等. 基于多轴差分吸收光谱技术的查找表法反演气溶胶消光廓线研究［J］. 光学学报, 2013, 33(6): 0601002.

    Wu Fengcheng, Xie Pinhua, Li Ang, et al. Research of aerosol extinction inverted with look-up table method based on muti-axis differential optical absorption spectroscopy［J］. Acta Optica Sinica, 2013, 33(6): 0601002.

[16] 牟福生, 谢品华, 李 昂, 等. 基于MAX-DOAS观测大气Ring效应的气溶胶消光廓线反演［J］. 光学学报, 2015, 35(11): 1101001.

    Mou Fusheng, Xie Pinhua, Li Ang, et al. Retrieval of aerosol profile based on the Ring effect observed by MAX-DOAS［J］. Acta Optica Sinica, 2015, 35(11): 1101001.

[17] Fayt C, van Roozendael M. WinDOAS 2.1 software user manual［A/OL］.［2016-06-03］. http: ∥www.oma.be/BIRA-IASB/Molecules/BrO/WinDOAS-SUM-210b.pdf.

[18] Vandaele A C, Hermans C. Measurements of the NO2 absorption cross-sections from 42000 cm-1 to 10000 cm-1 (238-1000 nm) at 220 K and 294 K［J］. Journal of Quantitative Spectroscopy and Radiative Transfer, 1998, 59(3/5): 171-184.

[19] Bogumil K, Orphal J, Homann T. Measurements of molecular absorption spectra with the SCIAMACHY pre-flight 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.

[20] Meller R, Moortgat G K. Temperature dependence of the absorption cross sections of formaldehyde between 223 and 323 K in the wavelength range 225-375 nm［J］. Journal of Geophysical Research Atmospheres, 2000, 105(D6): 7089-7101.