Cloud condensation nucleation activity of biomass burning aerosol

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A single parameter representation of hygroscopic growth and cloud condensation nucleus activity – Part 3: Including surfactant partitioning (2012, unknown): “…of several effects, including gradual dissolution of sparingly soluble compounds at high relative humidity (Petters and Kreidenweis, 2008; Petters et al., 2009b), highly non-ideal solution behaviour (Prenni et al., 2007; Petters et al., 2009b), measurement uncertainties related to HTDMA…”
Improvements to an Empirical Parameterization of Heterogeneous Ice Nucleation and Its Comparison with Observations (2013, background): “…show that, whereas many of the fresh biomass-burning plumes from various vegetation types have active IN at temperatures as warm as 2308C (e.g., Petters et al. 2009a; Twohy et al. 2010; Pratt et al. 2011; section 3a), fresh urban fossil-fuel pollution tends not to nucleate much ice (K09).”
Scanning Mobility CCN Analysis—A Method for Fast Measurements of Size-Resolved CCN Distributions and Activation Kinetics (2010, methodology): “These methods provide the CCN concentration across supersaturations and particle sizes, which when coupled with theory, enables the parameterization of composition impacts on cloud droplet formation (Rose et al. 2010; Petters et al. 2009; Dusek et al. 2010; Carrico et al. 2008; Petters and Kreidenwe”