[1] Intergovernmental panel on climate change (IPCC) report,climate change 2001,2007
[3] Yang Ruike,Ma Chunlin,Li Liangchao.Influence of multiple scattering on laser pulse propagation through sand and dust storm[J].Chinese J.Lasers,2007,10(34):1393-1397
[4] Andreas Behrendt,Takuji Nakamura.Calculation of the calibration constant of polarization lidar and its dependency on atmospheric temperature[J].Opt.Express,2002,10(16):805-817
[8] W.N.Chen,C.W.Chiang,J.B.Nee.The lidar ratio and depolarization ratio for cirrus clouds [J].Appl.Opt.,41(30):6470-6497
[9] Kenneth Sassen.The polarization lidar technique for cloud research:a review and current assessment[J].The American Meteorologic Society,1991,72(12):1847-1866
[10] David M.Winker,C.Hosteler,M.Vaughn et al..CALIOP algorithm theoretical basis document.part1: CALIOP instrument,and algorithms overview,September 9,2006:4-26
[11] Chris A.Hostetler,Z.Liu,J.Reagan et al..CALIOP algorithm theoretical basis document,calibration and level 1 data products,7 April 2006:5-64
[12] Franz Immler.A new lidar system for the detection of cloud and aerosol backscatter,depolarization,extinction,and fluorescence[C] .23rd International Laser Radar Converence,2006 Nara Japan
[13] Zhenzhu Wang,Ruli Chi,Bo Liu et al..Depolarization properties of cirrus clouds from polarization lidar measurements over Hefei in spring[J].Chin.Opt.Lett.,2008,6(4):235-237
[14] N.Sugimoto,I.Matsui,A.Shimizu et al..Observation of dust and anthropogenic aerosol plumes in the northwest pacific with a two-wavelength polarization lidar on board the research vessel mirai[J].Geophysica Research Letters,2002,29(19):7-1-7-4
[15] A.Hodzic,H.Chepfer,R.Vauard et al..Comparison of pollution aerosol chemistry-transport model simulations with lidar and sun-photometer observations at SIRTA site[J].J.Geophys.Res.,2004,109,D23201
[16] Gian Paolo Gobbi.Polarization lidar returns from aerosols and thin clouds:a framework for the analysis[J].Appl.Opt.,1998,37(24):5505-5508
[17] T.Sakai,T.Nagai,M.Nakazato et al..Ice clouds and asian dust studied with lidar measurements of particle extinction-to-backscatter ratio,particle depolarization,and water-vapor mixing ratio over Tsukuba[J].Appl.Opt.,2003,42(36):7103-7116
[18] Gian Paolo Gobbi,F.Barnaba,R.Giorgi et al..Altitude-resolved properties of a saharan dust event over the mediterranean[J].Atmospheric Environment,2000,34:5119-5127
[19] A.M.Tafuro,F.Barnaba,F.De Tomasi et al..Saharan dust particle properties central mediterranean[J].Atmospheric Research,2006,81:67-93
[20] Jorg Ackermann.The extinction-to-backscatter ratio of tropospheric aerosol:a numerical study[J].J.Atmospheric and Oceanic Technologhy,1998,15:1043-1050
[21] G.P.Gobbi,F.Barnaba,L.Ammannato.The vertical distribution of aerosols,saharan dust and cirrus clouds in rome (Italy) in the year 2001[J].Atmos.Chem.Phys.,2004,4:351-359
[22] Yu You,G.W.Kattawar,P.Yang et al..Sensitivity of depolarized lidar signals to cloud and aerosol particle properties[J].J.Quantitative Spectroscopy & Radiative Transfer,2006,100:470-482