Impact of thermal structure of planetary boundary layer on aerosol pollution over urban regions in Northeast China

被引:9
|
作者
Lu, Shuo [1 ]
Li, Xiaolan [2 ,3 ]
Zhao, Tianliang [1 ]
Ma, Yanjun [2 ]
Wang, Yangfeng [2 ]
Zhang, Yunhai [2 ]
Luo, Yuehan [1 ]
Xin, Yushan [1 ]
机构
[1] Nanjing Univ Informat Sci & Technol, Precipitat China Meteorol Adm, PREMIC, Key Lab Aerosol Cloud Precipitat China Meteorol A, Nanjing 210044, Peoples R China
[2] China Meteorol Adm, Inst Atmospher Environm, Shenyang 110166, Peoples R China
[3] Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Atmospher Environm & Equip, Jiangsu Key Lab Atmospher Environm Monitoring & P, Nanjing 210044, Peoples R China
基金
中国国家自然科学基金;
关键词
Aerosol pollution; Planetary boundary layer; Thermal structure; Meteorological factors; Northeast China; PEARL RIVER DELTA; AIR-POLLUTION; PM2.5; CONCENTRATIONS; SYNOPTIC WEATHER; HAZE EVENTS; PLAIN; TRANSPORT; HEIGHT; APPORTIONMENT; SIMULATIONS;
D O I
10.1016/j.apr.2023.101665
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This study investigated the characteristics of aerosol pollution in three provincial capitals (Shenyang, Chang-chun, and Harbin) in Northeast China and the impact of the thermal structure of the planetary boundary layer (PBL) using surface air quality monitoring data and meteorological observations and sounding data from January 1 to January 20, 2020. The number of pollution days in Shenyang, Changchun, and Harbin were 13, 17, and 19, respectively, and the number of heavy pollution days was 4, 3, and 13, respectively. Harbin suffered the heaviest and longest pollution with the smallest diurnal variation between daytime low and nighttime high PM2.5. The atmosphere in Harbin was more stable than that in Shenyang and Changchun, and PM2.5 concentration in the three cities tended to increase with decreasing planetary boundary layer height (PBLH). The lower winter air temperature in Northeast China led to a shallower PBL and weaker ventilation coefficient, which in turn led to an increase in PM2.5 concentration, indicating that air temperature is the key meteorological factor affecting local pollution in Northeast China. The analysis of two typical pollution events showed that a warm advection aloft suppressed the development of the PBL in Shenyang. In contrast, the suppressed effect of warm advection on the PBL was weakened in Harbin, which originally had a low PBLH due to cold weather. Moreover, the daytime convective boundary layer in Harbin developed 1-2 h later than that in Shenyang; the delayed development of PBL during the daytime in Harbin was also conducive to poor air quality.
引用
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页数:10
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