Continued development of a cloud droplet formation parameterization for global climate models

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On the effect of dust particles on global cloud condensation nuclei and cloud droplet number (2011, methodology): “For modes following Köhler theory, x = −3/2 [Fountoukis and Nenes, 2005], while for particles following FHH theory, x depends on AFHH and BFHH [Kumar et al.”
Aerosol Properties and Processes: A Path from Field and Laboratory Measurements to Global Climate Models (2007, background): “Activation of aerosol particles to form cloud droplets will be expressed in terms of updraft velocity and the aerosol particle properties (number, size, and hygroscopicity) for all types (Abdul-Razzak and Ghan 2000; Fountoukis and Nenes 2005), so that aerosol indirect effects and the competition bet”
Online coupled regional meteorology chemistry models in Europe: current status and prospects (2013, background): “, 1998; Fountoukis and Nenes, 2007), MESA (Zaveri et al., 2005) and PD-FiTE (Topping et al., 2009, 2012). Zhang et al. (2000) present a comparative evaluation of various inorganic thermodynamic aerosol models that are currently used in 3-D models.”
A New Parameterization of Cloud Droplet Activation Applicable to General Circulation Models (2006, methodology): “Efforts have been underway to apply it to deal with the variations in microphysical parameters, such as mass accommodation coefficients, and are described in a recently published paper (Fountoukis and Nenes 2005).”