Articles | Volume 23, issue 12
https://doi.org/10.5194/acp-23-7225-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-23-7225-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Vertical distribution of black carbon and its mixing state in the urban boundary layer in summer
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing, 100029, China
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing, 100029, China
Shandong Lei
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing, 100029, China
University of Chinese Academy of Sciences, Beijing, 100049, China
Yuting Zhang
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing, 100029, China
University of Chinese Academy of Sciences, Beijing, 100049, China
Aodong Du
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing, 100029, China
University of Chinese Academy of Sciences, Beijing, 100049, China
Weijie Yao
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing, 100029, China
University of Chinese Academy of Sciences, Beijing, 100049, China
Guiqian Tang
Institute of Atmospheric Physics, Chinese Academy of Sciences,
Beijing, 100029, China
Tao Wang
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing, 100029, China
Jinyuan Xin
University of Chinese Academy of Sciences, Beijing, 100049, China
Institute of Atmospheric Physics, Chinese Academy of Sciences,
Beijing, 100029, China
Collaborative Innovation Center on Forecast and Evaluation of
Meteorological Disasters, Nanjing University of Information Science and
Technology, Nanjing, 210044, China
Jie Li
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing, 100029, China
University of Chinese Academy of Sciences, Beijing, 100049, China
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing, 100029, China
University of Chinese Academy of Sciences, Beijing, 100049, China
Junji Cao
Institute of Atmospheric Physics, Chinese Academy of Sciences,
Beijing, 100029, China
Zifa Wang
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing, 100029, China
University of Chinese Academy of Sciences, Beijing, 100049, China
Center for Excellence in Regional Atmospheric Environment, Chinese
Academy of Science, Xiamen, 361021, China
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Short summary
We provide the average vertical profiles of black carbon (BC) concentration, size distribution and coating thickness at different times of the day in an urban area based on 112 vertical profiles. In addition, it is found that BC in the residual layer generally has a thicker coating, higher absorption enhancement and hygroscopicity than on the surface. Such aged BC could enter into the boundary layer and influence the BC properties in the early morning.
We provide the average vertical profiles of black carbon (BC) concentration, size distribution...
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