“…Atmospheric surface measurements of gas phase oxides of nitrogen, NO3, HONO, and HNO 3 and airborne measurements of HNO3 in precipitation at cloud base and in selected urban plumes are at variance with values predicted by gas phase photochemical models. In particular, homogeneous odd nitrogen reaction schemes (see compilations by Baulch et al [1980] and Hampson [1980]) are unable to resolve (1) low nocturnal measurements of NO 3 at rural and urban sites in Europe and the United States [Noxon et al, 1978[Noxon et al, , 1980Platt et al, 1979Platt et al, , 1980aPlatt et al, , b, 1981, (2) the buildup of HONO throughout the night in the Los Angeles area [Platt et al, 1980b], (3) the formation of HNO 3 in warm frontal clouds over the Ohio River Valley [Lazrus et al, 1983] and the increase of NO 3-in a case of a fair-weather cumulus cloud [Leaitch et al, 1982], and (4) the formation of HNO3 within plumes and in the Los Angeles Basin [Parungo and Pueschel, 1980;Van Valin et al, 1981;Richards, 1983]. In all these cases, heterogeneous reactions between oxides of nitrogren and atmospheric particles are proposed as one explanation for these observations.…”