A Comprehensive Study of a Winter Haze Episode over the Area around Bohai Bay in Northeast China: Insights from Meteorological Elements Observations of Boundary Layer

被引:3
作者
Kang, Boshi [1 ,2 ]
Liu, Chong [3 ,4 ]
Miao, Chuanhai [2 ]
Zhang, Tiening [5 ]
Li, Zonghao [2 ]
Hou, Chang [2 ]
Li, Hongshuo [2 ]
Li, Chenrui [6 ]
Zheng, Yu [4 ]
Che, Huizheng [4 ]
机构
[1] China Meteorol Adm, Inst Atmospher Environm, Shenyang 110000, Peoples R China
[2] Liaoning Meteorol Equipment Support Ctr, Shenyang 110000, Peoples R China
[3] China Meteorol Adm, Earth Syst Modeling & Predict Ctr, Beijing 100081, Peoples R China
[4] Chinese Acad Meteorol Sci, Inst Atmospher Composit & Environm Meteorol, State Key Lab Severe Weather, Beijing 100081, Peoples R China
[5] Liaoning Weather Modificat Off, Shenyang 110000, Peoples R China
[6] Lanzhou Cent Meteorol Observ, Lanzhou 730020, Peoples R China
基金
中国国家自然科学基金;
关键词
haze episode; ground-based observations; wind profile radar; boundary layer; sea breeze; Bohai Bay; Northeast China; AEROSOL-RADIATION FEEDBACK; BEIJING-TIANJIN-HEBEI; EASTERN CHINA; AIR-POLLUTION; OPTICAL-PROPERTIES; REGIONAL HAZE; HEAVY HAZE; IMPACTS; VARIABILITY; PM2.5;
D O I
10.3390/su14095424
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Based on wind profile radar observations, along with high-frequency wave radar data, meteorological data, and air quality monitoring data, we studied a haze episode in Panjin-a coastal city around Bohai Bay in Northeast China-that occurred from 8 to 13 February 2020. The results show that this persistent pollution event was dominated by PM10 and PM2.5 and their mass concentrations were both similar to 120 mu g/m(3) in the mature stage. In the early stage, the southerly sea breeze of similar to 4.5 m/s brought a large amount of moist air from the sea, which provided sufficient water vapor for the condensation and nucleation of pollutants, and thus accelerated the formation of haze. In the whole haze process, a weak updraft first appeared in the boundary layer, according to the vertical profile, contributing to the collision and growth of particulate matter. Vertical turbulence was barely observed in the mature stage, with the haze layer reaching 900 m in its peak, suggesting stable stratification conditions of the atmospheric boundary layer. The explosive growth of pollutant concentrations was about 10 h later than the formation of the stable stratification condition of the boundary layer. The potential source areas of air pollutants were identified by the WRF-FLEXPART model, which showed the significant contribution of local emissions and the transport effect of sea breeze. This study provides insights into the formation mechanism of haze pollution in this area, but the data observed in this campaign are also valuable for numerical modeling.
引用
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页数:16
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