[1] ROSENFELD D. Aerosols, clouds, and climate[J]. Science, 2006, 312: 1323-1324.
[3] RAMANATHAN V, CRUTZEN P J, KIEHL J T, et al. Aerosols, climate, and the hydrological cycle [J]. Science, 2001, 294: 2119-2124.
[4] PLATT U, STUTZ J. Differential optical absorption spectroscopy principles and applications[M]. Berlin: Springer, 2008.
[5] HONNINGER G, FRIEDEBURG C V, PLATT U. Multi axis differential optical absorption spectroscopy (MAX-DOAS)[J]. Atmospheric Chemistry and Physics, 2004, 4: 231-254.
[6] LI Su-wen, WEI Min-hong, DAI Hai-feng. Reconstruction of spatial distributions of industrial emissions based on scaning multi-axis DOAS tomography[J]. Acta Optica Sinica, 2015, 35(4): 0401003.
[7] 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-Atmospheres, 2004, 109(3): 1-19.
[8] FRIE U, BALTINK H K, BEIRLE S. Intercomparison of aerosol extinction profiles retrieved from MAX-DOAS measurements[J]. Atmospheric Measurement Techniques, 2016, 9: 3205-3222.
[9] FRIE U, MONKS P S, REMEDIOS J J. MAX-DOAS O4 measurements: A new technique to derive information on atmospheric aerosols: 2. Modeling studies[J]. Journal of Geophysical Research-Atmospheres, 2006(111): D14203.
[10] WAGNER T, BEIRLE S, BRAUERS T. Inversion of tropospheric profiles of aerosol extinction and HCHO and NO2 mixing ratios from MAX-DOAS observations in Milano during the summer of 2003 and comparison with independent data sets[J]. Atmospheric Measurement Techniques, 2011, 4: 2685-2715.
[11] SCHREIER S F, RICHTER A, WITTROCK F. Estimates of free-tropospheric NO2 and HCHO mixing ratios derived from high-altitude mountain MAX-DOAS observations at midlatitudes and in the tropics[J]. Atmospheric Chemistry and Physics, 2016, 16: 2803-2817.
[12] WANG Y, LAMPEL J, XIE P H. Ground-based MAX-DOAS observations of tropospheric aerosols,NO2, SO2 and HCHO in Wuxi, China, from 2011 to 2014[J]. Atmospheric Chemistry and Physics, 2017, 17: 2189-2215.
[13] VLEMMIX T, HENDRICK F, PINARDI G. MAX-DOAS observations of aerosols, formaldehyde and nitrogen dioxide in the Beijing area: comparison of two profile retrieval approaches [J]. Atmospheric Measurement Techniques, 2015, 8: 941-963.
[14] WU Feng-cheng, XIE Pin-hua, LI Ang. 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.
[15] WANG Yang, LI Ang, XIE Pin-hua. Retrieving vertical profile of aerosol extinction by multi-axis differential optical absorption spectroscopy [J].Acta Physica Sinica, 2013,62(18): 180705.
[16] WANG S S, CUEVAS C A, FRIE U. MAX-DOAS retrieval of aerosol extinction properties in Madrid, Spain [J]. Atmospheric Measurement Techniques, 2016, 9: 5089-5101.
[17] WAGNER T, FRIEDEBURG C V, WENIG M. UV/Vis observations of atmospheric O4 absorptions using direct moon light and zenith scattered sunlight under clear and cloudy sky conditions [J]. Journal of Geophysical Research-Atmospheres, 2002, 107(20): 1-15.
[18] ROZANOV A, ROZANOV V, BUCHWITZ M. SCIATRAN 2.0-A new radiative transfer model for geophysical applications in the 175–2400 nm spectral region[J]. Advances in Space Research, 2005, 36: 1015-1019.
[19] WANG Y, BEIRLE S, LAMPEL J. Validation of OMI, GOME-2A and GOME-2B tropospheric NO2, SO2 and HCHO products using MAX-DOAS observations from 2011 to 2014 in Wuxi, China: investigation of the effects of priori profiles and aerosols on the satellite products[J]. Atmospheric Chemistry and Physics, 2017, 17: 5007-5033.
[20] WANG Yang. Research the technology of the remote sensing of spatial distribution of atmospheric trace gases and aerosols based on passive DOAS method [D].Hefei: Anhui Institute of Optics and Fine Mechanics Chinese Academy of Sciences, 2014.
[21] YU Xing-na, LU Rui, LIU Chao. Seasonal variation of columnar aerosol optical properties and radiative forcing over Beijing, China[J]. Atmospheric Environment, 2017, 166: 340-350.