EGU24-6995, updated on 08 Mar 2024
https://doi.org/10.5194/egusphere-egu24-6995
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Microphysical complexity of black carbon particles restricts their warming potential

Jianfei Peng2, Xiao-Feng Huang1, Yan Peng1, Jing Wei1, Xiao-Yu Lin1, Meng-Xue Tang1, Yong Cheng1, Zhengyu Men2, Tiange Fang2, Jinsheng Zhang2, Ling-Yan He1, Chao Liu3, Li-Ming Cao1, Hongjun Mao2, John H. Seinfeld4, and Yuan Wang5
Jianfei Peng et al.
  • 1Laboratory of Atmospheric Observation Supersite, School of Environment and Energy, Peking University Shenzhen Graduate School, Shenzhen, China
  • 2Tianjin Key Laboratory of Urban Transport Emission Research & State Environmental Protection Key Laboratory of Urban Ambient Air Particulate Matter Pollution Prevention and Control, College of Environmental Science and Engineering, Nankai University, Tian
  • 3Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science & Technology, Nanjing, China
  • 4Divisions of Chemistry and Chemical Engineering and Engineering and Applied Science, California Institute of Technology, Pasadena, CA, USA.
  • 5Department of Earth System Science, Stanford University, Stanford, California, USA

Black carbon (BC) strongly absorbs solar radiation, but its warming effect on climate is poorly quantified. A key challenge is to accurately assess BC light absorption after BC is mixed with non-BC components. However, there has consistently been a large observation-modeling gap in BC light absorption estimation, reflecting the insufficient understanding of realistic BC complexity. Here, we conduct comprehensive in situ measurements of BC single-particle microphysics, e.g., size, coating amounts, density, and shape, along with optical closure calculation. Specifically, the observed particle-to-particle heterogeneities in size and coating and the non-spherical BC shape only explain the lower observed BC absorption by ∼20% and ∼30%, respectively. A remaining gap for fully aged spherical BC-containing particles is related to the off-center BC-core position. The global climate model assessment shows that fully accounting for the observed BC complexity in the aerosol microphysical representation reduces the global BC direct radiative forcing by up to 23%.

How to cite: Peng, J., Huang, X.-F., Peng, Y., Wei, J., Lin, X.-Y., Tang, M.-X., Cheng, Y., Men, Z., Fang, T., Zhang, J., He, L.-Y., Liu, C., Cao, L.-M., Mao, H., Seinfeld, J. H., and Wang, Y.: Microphysical complexity of black carbon particles restricts their warming potential, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-6995, https://doi.org/10.5194/egusphere-egu24-6995, 2024.