Jimmy Chi Hung Fung, Shanshan Wang, Golam Sarwar, Alba Badia, Li Zhang, Bin Zhou, Qinyi Li, Carlos A. Cuevas, Qiang Zhang, Alfonso Saiz-Lopez, Xiao Fu, Tao Wang, European Commission, Consejo Superior de Investigaciones Científicas (España), Higher Learning Institutions in Shanghai Municipality, National Science Foundation (US), National Natural Science Foundation of China, Li, Qinyi [0000-0002-5146-5831], Fung, Jimmy [0000-0002-7859-8511], Cuevas, Carlos A. [0000-0002-9251-5460], Saiz-Lopez, A. [0000-0002-0060-1581], Li, Qinyi, Fung, Jimmy, Cuevas, Carlos A., and Saiz-Lopez, A.
21 pags.,11 figs, 1 tab., Air pollution has been a hazard in China over recent decades threatening the health of half a billion people. Much effort has been devoted to mitigating air pollution in China leading to a significant reduction in primary pollutants emissions from 2013 to 2017, while a continuously worsening trend of surface ozone (O3, a secondary pollutant and greenhouse gas) was observed over the same period. Atmospheric oxidation, dominated by daytime reactions involving hydroxyl radicals (OH), is the critical process to convert freshly‐emitted compounds into secondary pollutants, and is underestimated in current models of China's air pollution. Halogens (chlorine, bromine, and iodine) are known to profoundly influence oxidation chemistry in the marine environment; however, their impact on atmospheric oxidation and air pollution in China is unknown. In the present study, we report for the first time that halogens substantially enhance the total atmospheric oxidation capacity in polluted areas of China, typically 10% to 20% (up to 87% in winter) and mainly by significantly increasing OH level. The enhanced oxidation along the coast is driven by oceanic emissions, and that over the inland areas by anthropogenic emission. The extent and seasonality of halogen impact are largely explained by the dynamics of Asian monsoon, location and intensity of halogen emissions, and O3 formation regime. The omission of halogen emissions and chemistry may lead to significant errors in historical re‐assessments and future projections of the evolution of atmospheric oxidation in polluted regions., This study received funding from the European Research Council Executive Agency under the European Union's Horizon 2020 Research and Innovation Programme (Project ERC‐2016‐ COG 726349 CLIMAHAL), and was supported by the Consejo Superior de Investigaciones Científicas (CSIC) of Spain, and The Program for Professor of Special Appointment (Eastern Scholar) at Shanghai Institutions of Higher Learning and Shanghai Thousand Talents Program. The development and maintenance of the WRF‐Chem model are conducted by NOAA/ESRL/GSD in active collaboration with other institutes. Computing resources, support, and data storage were provided by the Climate Simulation Laboratory at NCAR's Computational and Information Systems Laboratory (CISL), sponsored by the NSF. The Fudan team acknowledges the financial support from National Natural Science Foundation of China (41775113). The HKPU team acknowledges financial support from the Hong Kong Research Grants Council (A‐PolyU502/16, T24‐504/17‐N). Data that support the finding of this study can be found at DOI: 10.17632/whz6yk79m4.1 (Li et al., 2020)