Preprints
https://doi.org/10.5194/egusphere-2024-2654
https://doi.org/10.5194/egusphere-2024-2654
18 Sep 2024
 | 18 Sep 2024
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

Formation of Highly Absorptive Secondary Brown Carbon Through Nighttime Multiphase Chemistry of Biomass Burning Emissions

Ye Kuang, Biao Luo, Shan Huang, Junwen Liu, Weiwei Hu, Yuweng Peng, Duohong Chen, Dingli Yue, Wanyun Xu, Bin Yuan, and Min Shao

Abstract. Biomass burning is a major global source of both primary brown carbon (BrC) and reactive trace gases in the atmosphere, thus exerts significant impacts on global climate and regional atmospheric chemistry. However, a substantial gap remains in our understanding of the nighttime evolution of biomass burning emissions. Here we present prominent nighttime formation of secondary organic aerosol (Night-OA) with strong absorptivity but markedly different spectral dependence from that of primary biomass burning organic aerosols, which was observed during autumn of the Pearl River Delta region of China when biomass burning plumes prevailed. Our results demonstrate that the formation of Night-OA appeared high dependence on both magnitudes of afternoon biomass burning emissions and available oxidants of NO2 and O3. Active nighttime NO3 radical chemistry was characterized by quick O3 depletion and almost zero concentration of NO, and the rapid decrease of NO2 coincident with the quick nitrate formation suggests that the rapid NO2 consumption supplied the NO3 and N2O5 reaction chains. However, the quickest Night-OA formation occurred when nitrate formation ceased and relative humidity reached maximum, and mainly added mass to aerosol water abundant diameter ranges. This co-variation demonstrates that gas-phase and aqueous-phase chemistry of biomass burning precursors likely coordinated to promote the quick nighttime formation of Night-OA. Findings of this study highlight the nighttime darkening of biomass burning plumes through multiphase reactions and the proposed secondary BrC formation mechanisms may have broad implications in climate and air quality effects of biomass burning, such as the interaction between biomass burning plumes with water abundant pyroconvection cloud.

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Ye Kuang, Biao Luo, Shan Huang, Junwen Liu, Weiwei Hu, Yuweng Peng, Duohong Chen, Dingli Yue, Wanyun Xu, Bin Yuan, and Min Shao

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Ye Kuang, Biao Luo, Shan Huang, Junwen Liu, Weiwei Hu, Yuweng Peng, Duohong Chen, Dingli Yue, Wanyun Xu, Bin Yuan, and Min Shao
Ye Kuang, Biao Luo, Shan Huang, Junwen Liu, Weiwei Hu, Yuweng Peng, Duohong Chen, Dingli Yue, Wanyun Xu, Bin Yuan, and Min Shao

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Short summary
This research reveals the potential importance of nighttime NO3 radical chemistry and aerosol water in the rapid formation of secondary brown carbon from biomass burning emissions. The findings enhance our understanding of nighttime biomass burning evolution and its implications for climate and regional air quality, especially regarding interactions with aerosol water and water-rich fogs and clouds.