Effects of aerosol optical properties on deep convective clouds and radiative forcing

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Implementation of a two‐moment bulk microphysics scheme to the WRF model to investigate aerosol‐cloud interaction (2008, background): “…models promise a valuable approach to investigate the effects of aerosols on cloud development and precipitation [e.g., Khain et al., 2005; Fan et al., 2007a, 2007b, 2008], in which each type of cloud hydrometeors and aerosols is described using size distribution functions containing…”
Formation of highly hygroscopic soot aerosols upon internal mixing with sulfuric acid vapor (2009, background): “(IN), modifying the microphysical and the radiative properties and lifetime of clouds [Andreae and Rosenfeld, 2008; Fan et al., 2008].”
Variability in morphology, hygroscopicity, and optical properties of soot aerosols during atmospheric processing (2008, background): “, atmospheric stabilization and decreasing RH or supersaturation) dominate under heavily polluted conditions (36), whereas the CCN effect is more pronounced in less polluted air or for transported particles in the regional and global atmosphere (37).”