Influence of dust composition on cloud droplet formation

By J. Kelly, C. Chuang, Anthony S. Wexler. 2006

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On the effect of dust particles on global cloud condensation nuclei and cloud droplet number (2011, background): “…the dust impacts on cloud droplet number assume that dust acts as CCN only when soluble material exists in the particles (and controls its hygroscopicity) [e.g., Hoose et al., 2008b; Kelly et al., 2007; Lee et al., 2009; Manktelow et al., 2010; Pringle et al., 2010a, 2010b; Solomos et al., 2011].”
Aerosol cloud precipitation interactions. Part 1. The nature and sources of cloud-active aerosols (2008, background): “…coated with sulfate, nitrate, chloride, or other soluble salts during atmospheric processing, especially in clouds (Andreae et al., 1986; Talbot et al., 1986; Galy-Lacaux et al., 2001; Yin et al., 2002; Formenti et al., 2003; Trochkine et al., 2003; Kelly et al., 2007; Sullivan et al., 2007a,b).”
A single parameter representation of hygroscopic growth and cloud condensation nucleus activity – Part 2: Including solubility (2008, unknown): “Effects of dissolution kinetics (Asa-Awuku and Nenes, 2007; Kelly et al., 2007) and curvature enhanced solubility (Padro and Nenes, 2007) are not considered by this expression.”