Divergent Impacts of Biomass Burning and Fossil Fuel Combustion Aerosols on Fog‐Cloud Microphysics and Chemistry: Novel Insights From Advanced Aerosol‐Fog Sampling

Author:

Kuang Ye12ORCID,Xu Weiqi3ORCID,Tao Jiangchuan12ORCID,Luo Biao12,Liu Li4ORCID,Xu Hanbin5,Xu Wanyun6ORCID,Xue Biao12,Zhai Miaomiao12,Liu Pengfei7,Sun Yele3ORCID

Affiliation:

1. Institute for Environmental and Climate Research Jinan University Guangzhou China

2. Guangdong‐Hongkong‐Macau Joint Laboratory of Collaborative Innovation for Environmental Quality Jinan University Guangzhou China

3. State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry Institute of Atmospheric Physics Chinese Academy of Sciences Beijing China

4. Key Laboratory of Regional Numerical Weather Prediction Institute of Tropical and Marine Meteorology China Meteorological Administration Guangzhou China

5. Experimental Teaching Center Sun Yat‐Sen University Guangzhou China

6. State Key Laboratory of Severe Weather Key Laboratory for Atmospheric Chemistry Institute of Atmospheric Composition Chinese Academy of Meteorological Sciences Beijing China

7. School of Earth and Atmospheric Sciences Georgia Institute of Technology Atlanta GA USA

Abstract

AbstractActivation of biomass burning aerosols (BBA) and fossil fuel combustion aerosols (FFA) in fogs and clouds significantly impact regional air quality through aqueous chemistry and climate by affecting cloud microphysics. However, we lack direct observations of how these aerosols behave in fogs and clouds. Using a newly developed aerosol‐cloud sampling system, we conducted observations during fog events and found that BBA, despite their high organic content, effectively contributed to super‐micron interstitial aerosols and fog droplets in low supersaturation fogs. In contrast, FFA, predominantly externally mixed organic, did not grow beyond the super‐micron size in fogs due to their near‐hydrophobic nature. Measurements conducted under supersaturations relevant for cloud formation revealed that portions of FFA could serve as cloud condensation nuclei, but only when supersaturation exceeded ∼0.14%. These findings have broad implications for future investigations into the influence of BBA and FFA on fog and cloud chemistry and their interactions with clouds.

Funder

National Natural Science Foundation of China

Special Fund Project for Science and Technology Innovation Strategy of Guangdong Province

Publisher

American Geophysical Union (AGU)

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