Superimposed effects of typical local circulations driven by mountainous topography and aerosol–radiation interaction on heavy haze in the Beijing–Tianjin–Hebei central and southern plains in winter
Yue Peng,Hong Wang,Xiaoye Zhang,Zhaodong Liu,Wenjie Zhang,Siting Li,Chen Han,and Huizheng Che
State Key Laboratory of Severe Weather (LASW) and Key Laboratory of Atmospheric Chemistry of China Meteorological Administration, Chinese Academy of Meteorological Sciences (CAMS), Beijing 100081, China
State Key Laboratory of Severe Weather (LASW) and Key Laboratory of Atmospheric Chemistry of China Meteorological Administration, Chinese Academy of Meteorological Sciences (CAMS), Beijing 100081, China
State Key Laboratory of Severe Weather (LASW) and Key Laboratory of Atmospheric Chemistry of China Meteorological Administration, Chinese Academy of Meteorological Sciences (CAMS), Beijing 100081, China
Center for Excellence in Regional Atmospheric Environment, IUE,
Chinese Academy of Sciences, Xiamen 361021, China
Zhaodong Liu
State Key Laboratory of Severe Weather (LASW) and Key Laboratory of Atmospheric Chemistry of China Meteorological Administration, Chinese Academy of Meteorological Sciences (CAMS), Beijing 100081, China
State Key Laboratory of Severe Weather (LASW) and Key Laboratory of Atmospheric Chemistry of China Meteorological Administration, Chinese Academy of Meteorological Sciences (CAMS), Beijing 100081, China
Siting Li
State Key Laboratory of Severe Weather (LASW) and Key Laboratory of Atmospheric Chemistry of China Meteorological Administration, Chinese Academy of Meteorological Sciences (CAMS), Beijing 100081, China
Chen Han
State Key Laboratory of Severe Weather (LASW) and Key Laboratory of Atmospheric Chemistry of China Meteorological Administration, Chinese Academy of Meteorological Sciences (CAMS), Beijing 100081, China
State Key Laboratory of Severe Weather (LASW) and Key Laboratory of Atmospheric Chemistry of China Meteorological Administration, Chinese Academy of Meteorological Sciences (CAMS), Beijing 100081, China
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This study demonstrates a strong link between local circulation, aerosol–radiation interaction (ARI), and haze pollution. Under the weak weather-scale systems, the typical local circulation driven by mountainous topography is the main cause of pollutant distribution in the Beijing–Tianjin–Hebei region, and the ARI mechanism amplifies this influence of local circulation on pollutants, making haze pollution aggravated by the superposition of both.
This study demonstrates a strong link between local circulation, aerosol–radiation interaction...
