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Deciphering the seasonal dynamics of multifaceted aerosol-ozone interplay: Implications for air quality management in Eastern China.
Li, Yasong; Wang, Tijian; Wang, Qin'geng; Li, Mengmeng; Qu, Yawei; Wu, Hao; Fan, Jiachen; Shao, Min; Xie, Min.
Affiliation
  • Li Y; School of the Environment, Nanjing University, Nanjing 210023, China.
  • Wang T; School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China. Electronic address: tjwang@nju.edu.cn.
  • Wang Q; School of the Environment, Nanjing University, Nanjing 210023, China.
  • Li M; School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China.
  • Qu Y; College of Intelligent Science and Control Engineering, Jinling Institute of Technology, Nanjing 211112, China.
  • Wu H; Key Laboratory of Transportation Meteorology of China Meteorological Administration, Nanjing Joint Institute for Atmospheric Sciences, Nanjing, China.
  • Fan J; School of the Environment, Nanjing University, Nanjing 210023, China.
  • Shao M; School of Environment, Nanjing Normal University, Nanjing 210046, China.
  • Xie M; School of Environment, Nanjing Normal University, Nanjing 210046, China.
Sci Total Environ ; 946: 174327, 2024 Oct 10.
Article in En | MEDLINE | ID: mdl-38955271
ABSTRACT
We employed an enhanced WRF-Chem to investigate the discrete mechanisms of aerosol-radiation-feedback (ARF), extinction-photochemistry (AEP), and heterogeneous-reactions (AHR) across different seasons in eastern China, aiming to assess the synergistic effects arising from the simultaneous operation of multiple processes on O3 and PM2.5. Our findings demonstrated that ARF fostered the accumulation of pollutants and moisture, initiating two distinct feedback mechanisms concerning O3. The elevation in the NO/NO2 ratio amplified O3 consumption. Increased near-surface moisture diminished upper-level cloud formation, thereby enhancing photolysis rates and O3 photochemical production. The pronounced impact of heightened NO/NO2 on O3 led to a decrease of 0.1-2.7 ppb. When decoupled from ARF, AEP led to a more significant reduction in photolysis rates, resulting in declines in both O3 and PM2.5, except for an anomalous increase observed in summer, with O3 increasing by 1.6 ppb and PM2.5 by 2.5 µg m-3. The heterogeneous absorption of hydroxides in spring, autumn, and winter predominantly governed the AHR-induced variation of O3, leading to a decrease in O3 by 0.7-1 ppb. Conversely, O3 variations in summer were primarily dictated by O3-sensitive chemistry, with heterogeneous absorption of NOy catalyzing a decrease of 2.4 ppb in O3. Furthermore, AHR accentuated PM2.5 by facilitating the formation of fine sulfates and ammonium while impeding nitrate formation. In summer, the collective impact of ARF, AEP, and AHR (ALL) led to a substantial reduction of 6.2 ppb in O3, alleviating the secondary oxidation of PM2.5 and leading to a decrease of 0.3 µg m-3 in PM2.5. Conversely, albeit aerosol substantially depleted O3 by 0.4-4 ppb through their interactions except for summer, aerosol feedback on PM2.5 was more pronounced, resulting in a significant increase of 1.7-6.1 µg m-3 in PM2.5. Our study underscored the seasonal disparities in the ramifications of multifaceted aerosol-ozone interplay on air quality.
Key words

Full text: 1 Collection: 01-internacional Database: MEDLINE Language: En Journal: Sci Total Environ Year: 2024 Document type: Article Affiliation country: China

Full text: 1 Collection: 01-internacional Database: MEDLINE Language: En Journal: Sci Total Environ Year: 2024 Document type: Article Affiliation country: China