[1] Rossow W B, Walker A W, Gardner L C. Comparison of ISCCP and other cloud amounts ［J］. J. Climate, 1993, 6: 2394-2418.
[2] Rossow W B, Schiffer R A. Advances in understanding clouds from ISCCP ［J］. Bull. Amer. Meteor. Soc., 1999, 80: 2261-2287.
[3] Hahn C J, Warren S G, London J. Climatological Data for Clouds over the Globe from Surface Observations ［R］. Oak Ridge National Laboratory Tech. Rep. ORNL/CDIAC-72 NDP-026A, Oak Ridge, TN, 1994.
[5] Hahn C J, Rossow W B, Warren S G. ISCCP cloud properties associated with standard cloud types identified in individual surface observations ［J］. J. Climate, 2001, 14: 11-28.
[6] Hartmann D L, Ockert-Bell M E, Michelsen M L. The effect of cloud type on earth’s energy balance: Global analysis ［J］. J. Climate, 1992, 5: 1281-1304.
[7] Wang Zhien, Sassen K. Cloud type and macrophysical property retrieval using multiple remote sensors ［J］. Journal of Applied Meteorology, 2001, 40: 1665-1682.
[9] Comstock J M, Ackerman T P. Ground-based lidar and radar remote sensing of tropical cirrus clouds at Nauru Island: Cloud statistics and radiative impacts ［J］. J. Geophys. Res., 2002, 107(D23): 4714.
[10] Devara P C S, Raj P E, Dani K K, et al. Mobile lidar profiling of tropical aerosols and clouds ［J］. J. Atmos. Ocean. Tech., 2008, 25: 1288-1295.
[11] Sakai T, Nagai T, Nakazato M, 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.
