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Spatial and seasonal variations of surface ozone formation regime and source attributions in the Guanzhong Basin, China
  • +8
  • Guohui Li,
  • Ruonan Wang,
  • Naifang Bei,
  • Jiarui Wu,
  • Suixin Liu,
  • Lang Liu,
  • Xia Li,
  • Jiaoyang Yu,
  • Min Zuo,
  • Zhenxing Shen,
  • Xuexi Tie
Guohui Li
Institute of Earth Environment, Chinese Academy of Sciences

Corresponding Author:[email protected]

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Ruonan Wang
Institute of Earth Environment, Chinese acdemy of sciences
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Naifang Bei
Xi'an Jiaotong University
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Jiarui Wu
Institute of Earth Environment, Chinese Academy of Sciences
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Suixin Liu
Institute of Earth Environment
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Lang Liu
Institute of Earth Environment, Chinese Academy of Sciences
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Xia Li
Institute of Earth Environment, Chinese Academy of Sciences
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Jiaoyang Yu
Institute of Earth Environment, Chinese Academy of Sciences
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Min Zuo
Institute of Earth Environment, Chinese Academy of Sciences
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Zhenxing Shen
Department of Environmental Science and Engineering, Xiâ¿¿an Jiaotong University, China
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Xuexi Tie
Key Laboratory of Aerosol Chemistry and Physics, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
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Abstract

Rapid increasing industries and city expansions have caused severe air pollution in the Guanzhong Basin (GZB), China in recent decades. Observations reveal that, although implementation of strict mitigation measures since 2014 has considerably reduced particulate matter (PM) pollution, the ozone (O) pollution during the warm season has continuously deteriorated in the basin. Simulations in May and August 2018 have been conducted using the WRF-Chem model to examine spatial and seasonal variations of the O formation regimes as well as source attributions in the GZB. The model generally performs well in simulating meteorological parameters, O, NO, and fine PM against measurements. The identified O formation regimes in cities of the GZB are all VOCs-sensitive in May and become more NO-sensitive in August. Sensitivity studies have shown that the power plants source generally suppresses the Oformation considerably in May and enhances it slightly in August due to its high NO and low VOCs emissions. The residential, transportation and industry sources increase the O concentration in May and August. Moreover, the transportation and industry sources play an increasingly important role in August but opposite for the residential source. The variation of O formation regimes and source attributions from May to August is caused by intensification of solar radiation, which not only promotes photochemical processes, also increases temperature and further enhances biogenic emissions and vertical exchange in the planetary boundary layer. The present study can provide guidelines to devise the effective O abatement strategies suitable for local situations.