What have we missed when studying the impact of aerosols on surface ozone via changing photolysis rates?
ID:2482 View Protection:ATTENDEE Updated Time:2021-06-20 22:27:54 Hits:1847 Poster Presentation

Start Time:2021-07-10 09:05(Asia/Shanghai)

Duration:5min

Session:SP 张贴报告专场 » SP-12主题12、气溶胶与大气环境科学 墙报

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Abstract
Previous studies have emphasized that the decrease in photolysis rate at the surface induced by the light extinction of aerosols could weaken ozone photochemistry and then reduce surface ozone. However, quantitative studies have shown that weakened photochemistry leads to a much greater reduction in the net chemical production of ozone, which does not match the reduction in surface ozone. This suggested that in addition to photochemistry, some other physical processes related to the variation of ozone should also be considered. In this study, the Weather Research and Forecasting with Chemistry (WRF-Chem) model coupled with the ozone source apportionment method was applied to determine the mechanism of ozone reduction induced by aerosols over Central East China (CEC). Our results showed that weakened ozone photochemistry led to a significant reduction in ozone net chemical production, which occurred not only at the surface but also within the lowest several hundred meters in the planetary boundary layer (PBL). Meanwhile, a larger ozone gradient was formed in vertical direction, which led to the high concentrations of ozone aloft being entrained by turbulence from the top of the PBL to the surface and partly counteracting the reduction in surface ozone. In addition, contribution from dry deposition was weakened due to the decrease in surface ozone concentration. The reduction in the ozone’s sink also slowing down the tendency of the decrease in surface ozone. Ozone in the upper layer of the PBL was also reduced, which was induced by much ozone aloft being entrained downward. Therefore, by affecting the photolysis rate, the impact of aerosols was a reduction in ozone not only at the surface but also throughout the entire PBL during the daytime over the CEC in this study. The ozone source apportionment results showed that 41.4%–66.3% of the reduction in surface ozone came from local and adjacent source regions, which suggested that the impact of aerosols on ozone from local and adjacent regions was more significant than that from long-distance regions. The results also suggested that while controlling the concentration of aerosols, simultaneously controlling ozone precursors from local and adjacent source regions is an effective way to suppress the increase in surface ozone over CEC at present.
Keywords
ozone,WRF-Chem,photolysis rates,PM2.5,source apportionment
Speaker
高晋徽
成都信息工程大学

Submission Author
高晋徽 成都信息工程大学
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    Jul 09

    2021

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    Jul 11

    2021

  • May 30 2021

    Abstract Submission Deadline

  • May 30 2021

    Draft paper submission deadline

  • May 30 2021

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  • Jul 10 2021

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  • Jul 11 2021

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青年地学论坛理事会
Organized By
中国科学院地球化学研究所
贵州大学
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