“…Previous laboratory studies have shown a large variability of γ N 2 O 5 (0.0002-0.3) depending on the physical characteristics of the substrates (e.g., aerosol surfaces, water droplets, and ice and crystal surfaces), environmental conditions (e.g., acidity, relative humidity, and temperature), and chemical composition of aerosol particles (e.g., nitrate, sulfate, black carbon, and organic coating; Sander et al, 2006;Chang et al, 2011;Anttila et al, 2006;Cosman et al, 2008;Thornton and Abbatt, 2005;McNeill et al, 2006). To reveal the effects of each factor on N 2 O 5 /ClNO 2 chemistry, several parameterizations of γ N 2 O 5 and ø have been proposed during the last decade (Riemer et al, 2003;Evans and Jacob, 2005;Anttila et al, 2006;Davis et al, 2008;Riemer et al, 2009;Griffiths et al, 2009). For example, Bertram and Thornton (2009) constructed a parameterization of γ N 2 O 5 as a function of aerosol liquid water, nitrate, and chloride content based on the measurements of laboratory-generated internally mixed chloride-nitrate particles.…”