Molecular characteristics, sources and influencing factors of isoprene and monoterpenes secondary organic aerosol tracers in the marine atmosphere over the Arctic Ocean

• Published in: Science of The Total Environment
• Main Authors: Hu, Chengge, Wei, Zexun, Zhan, Haicong, Gu, Weihua, Liu, Hongwei, Chen, Afeng, Jiang, Bei, Yue, Fange, Zhang, Runqi, Fan, Shidong, He, Pengzhen, Leung, M. Y., Wang, Xinming, Xie, Zhouqing
• Format: Report
• Language: English
• Published: ELSEVIER 2022
• Subjects: Environmental Sciences & Ecology; The Arctic Ocean atmosphere; Biogenic secondary organic aerosols; Biogenic secondary organic carbon; Sea ice changes; Environmental Sciences; CHEMICAL-COMPOSITION; SEASONAL-VARIATIONS; ANTHROPOGENIC EMISSIONS; SOA; PHOTOOXIDATION; CHINA; PM2.5; OXIDATION; PRODUCTS; FOREST; Arctic; Arctic Ocean; Gam; Sea ice
• Online Access: http://ir.gig.ac.cn/handle/344008/68347; https://doi.org/10.1016/j.scitotenv.2022.158645

Biogenic secondary organic aerosols (BSOA) are important components of the remote marine atmosphere. However, the response of BSOA changes to sea ice reduction over the Arctic Ocean remains unclear. Here we investigated iso-prene and monoterpenes secondary organic aerosol (SOAI and SOAM) tracers in three years of summer aerosol sam-ples collected from the Arctic Ocean atmosphere. The results indicated that methyltetrols were the most abundant SOAI tracers, while the main oxidation products of monoterpenes varied over the years owing to different aerosol aging. The results of the principal component analysis (PCA)-generalized additive model (GAM) combined with corre-lation analysis suggested that SOAI tracers were mainly generated by the oxidation of isoprene from marine emissions, while SOAM tracers were probably more influenced by terrestrial transport. Estimation of secondary organic carbon (SOC) indicated that monoterpenes oxidation contributed more than isoprene and that sea ice changes had a relatively small effect on biogenic SOC concentration levels. Our study quantified the contribution of influencing factors to the atmospheric concentration of BSOA tracers in the Arctic Ocean, and showed that there were differences in the sources of precursors for different BSOA. Hence, our findings have contributed to a better understanding of the characteristics, sources and formation of SOA in the atmosphere of the Arctic Ocean.