Modeling Mesoscale Cellular Structures and Drizzle in Marine Stratocumulus. Part II: The Microphysics and Dynamics of the Boundary Region between Open and Closed Cells

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Impacts of cloud microphysics on trade wind cumulus: which cloud microphysics processes contribute to the diversity in a large eddy simulation? (2015, methodology): “Many studies using LES models have been conducted to determine the characteristics of shallow cloud and improve large-scale modeling (e.g., Wang and Feingold 2009; Xue et al. 2008, Savic-Jovcic and Stevens 2008, Yamaguchi and Randall 2012).”
An aircraft case study of the spatial transition from closed to open mesoscale cellular convection over the Southeast Pacific (2010, background): “Cloud resolving model simulations do indeed show that spatial CCN gradients can induce precipitation gradients that lead to closed/open cell cloud morphology gradients10 (Wang and Feingold, 2009).”
Global observations of aerosol‐cloud‐precipitation‐climate interactions (2014, result): “This was shown by both observations [e.g., Stevens et al., 2005] and simulations [e.g., Ackerman et al., 1993;Wang and Feingold, 2009a].”