Emission characteristics of CO, NO x , SO 2 and indications of biomass burning observed at a rural site in eastern China

Atmospheric O 3 , CO, SO 2 , and NO y * (NO y * ≈ NO + NO 2 + PAN + organic nitrates + HNO 3 + N 2 O 5 + ⋯) were measured in 1999–2000 at a rural/agricultural site in the Yangtze Delta of China. In this paper we analyze the measurement results to show the emission characteristics of the measured gases and to infer relevant emission ratios. Positive correlations were found between CO and NO y * with a slope (Δ[CO]/Δ[NO y *]) of 36 (ppbv/ppbv) for the winter and nighttime measurements. The ratio is considerably larger than that (≈10 ppbv/ppbv) observed in the industrialized countries. The highest CO/NO y * ratio (30–40 ppbv/ppbv) occurred in September–December 1999 and June 2000. The good correlation between CO and the biomass burning tracer CH 3 Cl and the lack of correlation with the industrial tracer C 2 Cl 4 suggests that the burning of biofuels and crop residues is a major source for the elevated CO and possibly for other trace gases as well. The average SO 2 to NO y * ratio was 1.37 ppbv/ppbv, resulting from the use of relatively high‐sulfur coals in China. The measured SO 2 /NO y * and ΔCO/ΔNO y * were compared with the respective ratios from the current emission inventories for the study region, which indicated a comparable SO 2 /NO x emission ratio but a large discrepancy for CO/NO x . The observed CO to NO y * ratio was more than 3 times the emission ratio derived from the inventories, indicating the need for further improvement of emission estimates for the rural/agricultural regions in China. Additional research will be needed to study the implications of rural emissions to atmospheric chemistry and climate on both regional and global scales.