[1] [1] Haywood J, Bougher O. Estimates of the direct and indirect radiative forcing due to tropospheric aerosols: a review [J].Rev. Geophys., 2000, 38: 513-543.

[2] [2] Sokolik I N, Winker D, Bergametti G,et al. Introduction to special section on mineral dust: outstanding problems in quantifying the radiative impact of mineral dust [J]. J. Geophys. Res., 2001, 106: 18015-18027.

[3] [3] Martonchik J V, Diner D J. Retrieval of aerosol optical properties from multi-angle satellite imagery [J].IEEE Trans. Geosci. Remote Sens., 1992, 30: 223-230.

[4] [4] King M D, Kaufman Y J, Menzel W P,et al. Remote sensing of cloud, aerosol, and water vapor properties from the moderate resolution imaging spectrometer (MODIS) [J]. IEEE Trans. Geosci. Remote Sens., 1992, 30: 1-27.

[5] [5] Deuze J L, Herman M, Goloub P,et al. Characterization of aerosols over ocean from POLDER/ADEOS-1 [J]. Geophys. Res. Lett., 1999, 26: 1421-1424.

[6] [6] Wang M, Gordon H R. Estimating aerosol optical properties over the oceans with the multiangle imaging spectroradiometers: some preliminary result [J].Appl. Opt., 1994, 33: 4042-4057.

[7] [7] Wang Haoran, Chen Wenzhong. Aerosol optical properties and modeling study in East China Seas [J].Journal of Atmospheric and Environmental Optics, 2013, 8: 179-186(in Chinese).

[8] [8] Han Yongxiang, Xi Xiaoxia, Fang Xiaomin,et al. Dust storm in Asia continent and bio-environment effects in the North Pacific: a case study of the strongest dust event in April 2001 in central Asia [J]. Chinese Science Bulletin, 2005, 50: 2649-2655(in Chinese).

[9] [9] Koren I, Ganor E, Joseph J H. On the relation between size and shape of desert dust aerosol [J].J. Geophys. Res., 2001, 106: 18047-18054.

[10] [10] Okada K, Heintzenberg J, Kai K,et al. Shape of atmospheric mineral particles collected in three Chinese arid-regions [J]. Geophys. Res. Lett., 2001, 28: 3123-3126.

[11] [11] West R A, Doose L R, Eibl A M,et al. Laboratory measurements of mineral dust scattering phase function and linear polarization [J]. J. Geophys. Res., 1997, 102: 16871-16881.

[12] [12] Curtis D B, Meland B, Aycibin M,et al. A laboratory investigation of light scattering from representative components of mineral dust aerosols at a wavelength of 550 nm [J]. J. Geophys. Res., 2008, 113, doi:10.1029/2007JD009387

[13] [13] Kalashnikova O V, Kahn R, Sokolik I N,et al. Ability of multiangle remote sensing observations to identify and distinguish mineral dust types: Optical models and retrievals of optically thick plumes [J]. J. Geophys. Res., 2005, 110, doi:10.1029/2004JD004550.

[14] [14] Mishchenko M I, Travis L D. T-matrix computations of light scattering by large spheroidal particles [J].Opt. Commun., 1994, 109: 16-21.

[15] [15] Yang P, Feng Q, Hong G,et al. Modeling the scattering and radiative properties of nonshpherical dust-like aerosols [J]. J. Aerosol Sci., 2007, 38: 995-1014.

[16] [16] Sun Xianming, Wang Haihua, Liu Wanqiang,et al. Nonspherical model for sand dust storm and its application to the research of light multiple scattering [J]. Acta optica Sinica, 2010, 30(5), 1506-1510(in Chinese).

[17] [17] Wei Xiaodong, Zhang Hua. Analysis of optical properties of nonspherical dust aerosols [J].Acta optica Sinica, 2011, 31(5): 0501002(in Chinese).

[18] [18] Dubovik O, Sinyuk A, Lapyonok T,et al. Application of spheroid models to account for aerosol particle nonsphericity in remote sensing of desert dust [J]. J. Geophys. Res., 2006, 111, doi: 10.1029/ 2005JD006619.

[19] [19] Volten H, Muoz O, Rol E,et al. Scattering matrices of mineral aerosol particles at 441.6 and 632.8 nm [J]. J. Geophys. Res., 2001, 106: 17375-17401.

[20] [20] De Haan J F, Bosma P B, Hovenier J W. The adding method for multiple scattering calculations of polarized light [J].Astron. Astrophys., 1987, 183: 371-391.

[21] [21] Bi L, Yang P, Kattawar G W,et al. Modeling optical properties of mineral aerosol particles by using non-symmetric hexehedra [J]. Appl. Opt., 2010, 49: 334-342.