Jiangsu Key Laboratory of Atmospheric Environment Monitoring and
Pollution Control, Jiangsu Engineering Technology Research Center of
Environmental Cleaning Materials, Collaborative Innovation Center of
Atmospheric Environment and Equipment Technology, School of Environmental
Science and Engineering, Nanjing University of Information Science &
Technology, Nanjing, Jiangsu, China
Jiangsu Key Laboratory of Atmospheric Environment Monitoring and
Pollution Control, Jiangsu Engineering Technology Research Center of
Environmental Cleaning Materials, Collaborative Innovation Center of
Atmospheric Environment and Equipment Technology, School of Environmental
Science and Engineering, Nanjing University of Information Science &
Technology, Nanjing, Jiangsu, China
Jiangsu Key Laboratory of Atmospheric Environment Monitoring and
Pollution Control, Jiangsu Engineering Technology Research Center of
Environmental Cleaning Materials, Collaborative Innovation Center of
Atmospheric Environment and Equipment Technology, School of Environmental
Science and Engineering, Nanjing University of Information Science &
Technology, Nanjing, Jiangsu, China
Lei Chen
Jiangsu Key Laboratory of Atmospheric Environment Monitoring and
Pollution Control, Jiangsu Engineering Technology Research Center of
Environmental Cleaning Materials, Collaborative Innovation Center of
Atmospheric Environment and Equipment Technology, School of Environmental
Science and Engineering, Nanjing University of Information Science &
Technology, Nanjing, Jiangsu, China
Delong Zhao
Beijing Weather Modification Office, Beijing 100089, China
Deping Ding
Beijing Weather Modification Office, Beijing 100089, China
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Total article views: 3,777 (including HTML, PDF, and XML)
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Total article views: 818 (including HTML, PDF, and XML)
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The black carbon (BC) vertical profile plays a critical role in BC–meteorology interaction, which also influences PM2.5 concentrations. More BC mass was assigned into high altitudes (above 1000 m) in the model, which resulted in a stronger cooling effect near the surface, a larger temperature inversion below 421 m, more reductions in PBLH, and a larger increase in near-surface PM2.5 in the daytime caused by the direct radiative effect of BC.
The black carbon (BC) vertical profile plays a critical role in BC–meteorology interaction,...
