Simulating convective clouds with sustained supercooled liquid water down to −37.5°C using a spectral microphysics model

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Spectral (Bin) microphysics coupled with a Mesoscale Model (MM5). Part I: Model description and first results (2005, methodology): “These dynamical and microphysical effects of aerosols on cloud development were also found in simulations with the two-dimensional HUCM as well.”
A two-moment cloud microphysics parameterization for mixed-phase clouds. Part 1: Model description (2006, unknown): “and � ¼ 0:462 for maritime conditions ( Khain et al, 2001 ).”
Global indirect aerosol effects: a review (2004, unknown): “This hypothesis was conﬁrmed by a modeling study with a cloud resolving model by Khain et al. (2001) who showed that aircraft observations of highly supercooled water in deep convective clouds can only be reproduced if large concentrations of small droplets exist but not if the cloud is rather…”
Notes on state-of-the-art investigations of aerosol effects on precipitation: a critical review (2009, methodology): “As it was shown by Rosenfeld and Woodley (2000), Khain et al (2001), Khain and Pokrovsky (2004) and Khain et al (2008a), the strong atmospheric instability and high AP concentration typical of these clouds lead to the formation of a significant amount of ice crystals by homogeneous freezing.”