“…Recently, HONO photolysis was reported to contribute more strongly to daytime primary OH production than O 3 photolysis, both under urban and rural conditions (Elshorbany et al, 2009a;Sörgel et al, 2011a, respectively). It has been demonstrated that HONO photolysis can be a major OH initiation source under high NO x (e.g., Kleffmann et al, 2007;Elshorbany et al, 2009aElshorbany et al, , 2010aRen et al, 2006;Dusanter et al, 2009) as well as low NO x conditions (e.g., Kleffmann et al, 2005;Elshorbany et al, 2012, Sörgel et al, 2011a. OH radicals constitute the major oxidant of the atmosphere, initiating the removal of most reactive gases (i.e.…”