1 Lohmann U, Feichter J. Global indirect aerosol effects: A review. Atmos Chem Phys, 2005, 5: 715—737
[2]
2 IPCC. Climate change 2007: The Physical Science Basis. New York: Cambridge University Press, 2007
[3]
3 Yin Y, Levin Z, Reisin T G, et al. The effects of giant cloud condensation nuclei on the development of precipitation in convective clouds — A numerical study. Atmos Res, 2000, 53: 91—116
5 Zhang L, Michelangeli D V, Taylor P A. Influence of aerosol concentration on precipitation formation in low-level warm stratiform clouds. Aerosol Sci, 2006, 37: 203—217
[6]
6 McFiggans G, Artaxo P, Baltensperger U, et al. The effect of physical and chemical aerosol properties on warm cloud droplet activation. Atmos Chem Phys, 2006, 6: 2593—2649
[7]
7 Snider J R, Guibert S, Brenguier J. Aerosol activation in marine stratocumulus clouds: 2. K？hler and parcel theory closure studies. J Geophys Res, 2003, 108(D15): 8629, doi: 10.1029/2002JD002692
[8]
8 Nenes A, Charlson R J, Facchini M C, et al. Can chemical effects on cloud droplet number rival the first indirect effect? Geophys Res Lett, 2002, 29: 1848, doi: 10.1029/2002GL015295
[9]
9 Ervens B, Feingold G, Kreidenweis S M. Influence of water-soluble organic carbon on cloud drop number concentration. J Geophys Res, 2005, 110: D18211, doi: 10.1029/2004JD005634
[10]
10 Zhao C S, Ishizaka Y, Peng D Y. Numerical study on impacts of multi-component aerosols on marine cloud microphysical properties. J Meteor Soc Jap, 2005, 83: 977—986
12 Mircea M, Facchini M C, Decesari S, et al. The influence of the orgnic aerosol component on CCN supersaturation spectra for different aerosol types. Tellus Ser B-Chem Phys Meteorol, 2002, 54: 74—81
[13]
13 Yin Y, Levin Z, Reisin T, et al. Seeding convective clouds with hygroscopic flares: Numerical simulations using a cloud model with detailed microphysics. J Applied Meteor, 1999, 39: 1460—1472
[14]
14 Tang I N, Munkelwitz H R. Water activities, densities, and refractive indices of aqueous sulfates and sodium nitrate droplets of atmospheric importance. J Geophys Res, 1994, 99: 18801—18808
[15]
15 Pruppacher H R, Klett J D. Microphysics of Clouds and Precipitation. Dordrecht: Kluwer Academic Publishers, 1997
[16]
16 Shulman M L, Jacobson M C, Chalson R J, et al. Dissolution behavior and surface tension effects of organic compounds in nucleating cloud droplets. Geophys Res Lett, 1996, 23: 277—280
[17]
17 Ma J Z, Chen Y, Wang W, et al. Strong air pollution causes haze-clouds over China. J Geophys Res, 2010, 115: D18204, doi: 10.1029/2009JD013065
[18]
18 Wang W, Ma J Z, Hatakeyama S, et al. Aircraft measurements of vertical ultrafine particles profiles over Northern China coastal areas during dust storms in 2006. Atmos Environ, 2008, 42: 5715—5720
[19]
19 Pan X L, Yan P, Tang J, et al. Observational study of influence of aerosol hydroscopic growth on scattering coefficient over rural area near Beijing magacity. Atmos Chem Phys, 2009, 9: 7519—7530
[20]
20 Metzger S, Lelieveld J. Reformulating atmospheric aerosol thermodynamics and hygroscopic growth into fog, haze and clouds. Atmos Chem Phys, 2007, 7: 3163—3193
[21]
21 Decesari S, Facchini M C, Fuzzi S, Tagliavini E. Characterization of water-soluble organic compounds in atmospheric aerosol: A new approach. J Geophys Res, 2000, 105: 1481—1489
23 Hobbs P V. Aerosol-Cloud-Climate Interactions. Missouri: Academic Press Inc., 1993
[24]
24 Twomey S. The nuclei of natural cloud formation, Part II: The supersaturation in natural clouds and the variation of cloud droplet concentration. Geofis Pura Appl, 1959, 43: 243—249
28 Fitzgerald J W. Effect of aerosol composition on cloud droplet size distribution: A numerical study. J Atmos Sci, 1974, 31: 1358—1367
[29]
29 Zhao C S, Tie X X, Brassuer G, et al. Aircraft measurements of cloud droplet spectral dispersion and implications for indirect aerosol radiative forcing. Geophys Res Lett, 2006, 33: L16809, doi: 10.1029/2006GL026653
