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ReportsAmplified Trace Gas Removal in the Troposphere
The degradation of trace gases and pollutants in the troposphere is dominated by their reaction with hydroxyl radicals (OH). The importance of OH rests on its high reactivity, its ubiquitous photochemical production in the sunlit atmosphere, and most importantly on its regeneration in the oxidation chain of the trace gases. In the current understanding, the recycling of OH proceeds through HO2 reacting with NO, thereby forming ozone. A recent field campaign in the Pearl River Delta, China, quantified tropospheric OH and HO2 concentrations and turnover rates by direct measurements. We report that concentrations of OH were three to five times greater than expected, and we propose the existence of a pathway for the regeneration of OH independent of NO, which amplifies the degradation of pollutants without producing ozone.
1 Forschungszentrum Jülich, Institut für Chemie und Dynamik der Geosphäre–2: Troposphäre, 52425 Jülich, Germany.
2 College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China. 3 Research Center for Environmental Changes, Academic Sinica, Taipei, China. 4 Faculty of Science, Ibaraki University, Ibaraki 310-8512, Japan. 5 Research Center for Advanced Science and Technology, University of Tokyo, Tokyo 153-8904, Japan. 6 School of Environmental Science and Technology, Shanghai Jiaotong University, Shanghai 200240, China. * To whom correspondence should be addressed. E-mail: f.rohrer{at}fz-juelich.de (F.R.); yhzhang{at}pku.edu.cn (Y.Z.)
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Science. ISSN 0036-8075 (print), 1095-9203 (online)