Improvement of model simulation for summer PM2.5 and O3 through coupling with two new potential HONO sources in the North China Plain

被引:1
作者
Zhao, Xiaoxi [1 ,2 ,3 ]
Song, Min [2 ,4 ]
Zhao, Xiujuan [3 ]
Xue, Chaoyang [2 ,5 ]
Liu, Pengfei [2 ]
Ye, Can [2 ,6 ]
He, Xiaowei [2 ,7 ]
Mu, Yujing [2 ,7 ]
Hu, Bo [1 ,7 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, Key Lab Atmospher Environm & Extreme Meteorol, Beijing 100029, Peoples R China
[2] Chinese Acad Sci, Res Ctr Ecoenvironm Sci, Beijing 100085, Peoples R China
[3] Chinese Meteorol Adm, Inst Urban Meteorol, Beijing 100089, Peoples R China
[4] Shandong Jianzhu Univ, Sch Municipal & Environm Engn, Jinan 250101, Peoples R China
[5] Max Planck Inst Chem, D-55128 Mainz, Germany
[6] Tiangong Univ, Sch Environm Sci & Engn, Tianjin 300387, Peoples R China
[7] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
基金
中国国家自然科学基金;
关键词
Fine particulate matter (PM2.5); Secondary inorganic aerosol (SIA); Secondary organic aerosol (SOA); Ozone (O-3); WRF-Chem model; Potential HONO source; NITROUS-ACID HONO; AEROSOL FORMATION; ORGANIC-COMPOUNDS; EMISSIONS; CHEMISTRY; IMPACTS; OH; PREDICTIONS; NITRATE; OZONE;
D O I
10.1016/j.scitotenv.2024.175168
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A large fraction of fine particulate matter (PM2.5) and ozone (O-3) in the troposphere originates from secondary formation through photochemical processes, which remarkably contributes to the deterioration of regional air quality in China. The photochemical reactions initiated by hydroxyl radicals (OH) play vital roles in secondary PM2.5 and O-3 formation. In contrast, the OH levels in polluted areas are underestimated by current chemical transport models (CTMs) because of the strongly unknown daytime sources of tropospheric nitric acid (HONO), which has been recognized as the dominant source of primary OH in polluted areas of China. In this study, the atmospheric HONO levels at two urban sites were found to be significantly underestimated by the WRF-Chem model based on available information on HONO sources. The HONO levels could be well reproduced by the WRF-Chem model after incorporating two new potential HONO sources from the photochemical reactions of NOx, as proposed in our previous study based on chamber experiment results. Comparing the simulations with available information of HONO sources, the simulated levels of atmospheric OH, secondary inorganic and organic aerosols (SIA and SOA), PM2.5 and daily maximum 8-h average (MDA8) O-3 were evidently elevated or were closer to the observations over the North China Plain (NCP), with elevation percentages of 0.48-20.1 %, and a decrement percentage of -5.79 % for pNO(3)(-). Additionally, the compensating errors in modeling PM2.5 and the gap in MDA8 O-3 levels between observation and simulation in 2 + 26 cities became evidently smaller. The results of this study indicated that the empirical parameterization of two new potential HONO sources through photochemical reactions of NOx improved the model performance in modeling PM2.5 and O-3 by narrowing the gap in daytime HONO levels between simulation and observation, although their detailed chemical mechanisms are still unknown and should be further investigated and explicitly parameterized.
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页数:10
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