[1] [1] G. L. Schuster, M. Vaughan, D. Macdonnell et al.. Comparison of CALIPSO aerosol optical depth retrievals to AERONET measurements, and a climatology for the lidar ratio of dust[J]. Atmos. Chem. Phys. Discuss., 2012, 12(5): 11641～11697

[2] [2] A. K. Srivastava, S. N. Tripathi, S. Dey et al.. Inferring aerosol types over the Indo-Gangetic Basin from ground based sunphotometer measurements[J]. Atmospheric Research, 2012, 109-110: 64～75

[3] [3] A. Pietruczuk, J. Podgórski. The lidar ratio derived from sun-photometer measurements at Belsk Geophysical Observatory[J]. Acta Geophysica, 2009, 57(2): 476～493

[4] [4] J. Raut, P. Chazette. Retrieval of aerosol complex refractive index from a synergy between lidar, sunphotometer and in situ measurements during LISAIR experiment[J]. Atmos. Chem. Phys. Discuss., 2007, 7(1): 2797～2815

[5] [5] F. Mao, W. Gong, Z. Zhu et al.. The ground-based lidar combined with sunphotometer for aerosol optical depth retrieval[C]. SPIE, 2008, 7145: 71452R

[6] [6] Y. Sasano, E. V. Browell, S. Ismail. Error caused by using a constant extinction/backscattering ratio in the lidar solution[J]. Appl. Opt., 1985, 24(22): 3929～3932

[7] [7] F. G. Fernald. Analysis of atmospheric lidar observations[J]. Appl. Opt., 1984, 23(5): 652～653

[8] [8] V. A. Kovalev, M. P. Bristow. Compensational three-wavelength differential-absorption lidar technique for reducing the influence of differential scattering on ozone-concentration measurements[J]. Appl. Opt., 1996, 35(24): 4790～4797

[9] [9] Wang Xiangchuan, Rao Ruizhong. Lidar ratios for atmospheric aerosol and cloud particles[J]. Chinese J. Lasers, 2005, 32(10): 1321～1325

[10] [10] S. J. Doherty, T. L. Anderson, R. J. Charlson. Measurement of the lidar ratio for atmospheric aerosols with a 180° backscatter nephelometer[J]. Appl. Opt., 1999, 38(9): 1823～1832

[11] [11] J. D. Spinhirne, J. A. Reagan, B. M. Herman. Vertical distribution of aerosol extinction cross section and inference of aerosol imaginary index in the troposphere by lidar technique[J]. J. Appl. Met., 1980, 19(4): 426～438

[12] [12] S. Otto, E. Bierwirth, B. Weinzierl et al.. Solar radiative effects of a Saharan dust plume observed during SAMUM assuming spheroidal model particles[J]. Tellus B, 2009, 61(1): 270～296

[13] [13] F. Dulac, P. Chazette. Airborne study of a multi-layer aerosol structure in the eastern Mediterranean observed with the airborne polarized lidar ALEX during a STAAARTE campaign (7 June 1997)[J]. Atmos. Chem. Phys., 2003, 3(5): 1817～1831

[14] [14] C. Cattrall, J. Reagan, K. Thome et al.. Variability of aerosol and spectral lidar and backscatter and extinction ratios of key aerosol types derived from selected Aerosol Robotic Network locations[J]. J. Geophysical Research, 2005, 110(D10): D10S11

[15] [15] Anders Angstrm. The parameters of atmospheric turbidity[J]. Tellus, 1964, 16(1): 64～75

[16] [16] B. N. Holben, T. I. E. I. Slutsker, D. Tar et al.. AERONET: a federated instrument network and data archive for aerosol characterization[J]. 1998, 66(1): 1～16

[17] [17] Z. Liu, A. Omar, Y. Hu et al.. CALIOP Algorithm Theoretical Basis Document, Part 3: Scene Classification Algorithms[R]. NASA Langley Reseach Center Doc. PC-SCI-202, 2005. 1～56

[18] [18] Wu Mingquan, Niu Zheng, Qiao Yuliang et al.. Aerosol types and its affecting factors over Beijing: based on MODIS data[J]. J. Geo-Information Science, 2009, 11(4): 541～548

[19] [19] Cao Xianjie, Zhang Lei, Li Xia et al.. Analyses on aerosol absorption and scattering properties in Zhangye region[J]. Plateau Meteorology, 2010, 29(5): 1246～1253

[20] [20] Wu Dexia, Liu Jianguo, Lu Yihuai et al.. Observation of black carbon aerosol during Beijing Olympic Games[J]. J. Atmospheric and Environmental Optics, 2009, 4(4): 300～306

[21] [21] Rao Jiawang, Ma Ronghua, Duan Hongtao et al.. Aerosol optical thickness of the atmospheric aerosol over Taihu Lake and its features: results of in-site measurements[J]. Environmental Science & Technology, 2012, 33(7): 2158～2164