“…Measurement of NO 2 is more difficult and therefore has been an active area of research. Examples of NO 2 measurement techniques used for atmospheric observations include photolysis followed by O 3 chemiluminescence (P‐CL) [ Kley and McFarland , 1980; Ryerson et al , 2000], laser‐induced fluorescence (LIF) [ Matsumi et al , 2001; Matsumoto et al , 2001; Matsumoto and Kajii , 2003; Thornton et al , 2000], differential optical absorption spectroscopy (DOAS) [ Platt et al , 1979], tunable diode laser absorption spectroscopy (TDLAS) [ Fried et al , 1988], and cavity ring‐down spectroscopy (CARDS) [ Evertsen et al , 2002; Kasyutich et al , 2003; Kebabian et al , 2005; Mazurenka et al , 2003]. In P‐CL, NO 2 is photolytically converted to NO, which is measured by O 3 chemiluminescence [ Kley and McFarland , 1980; Ryerson et al , 2000].…”