Provenance of Aerosol Black Carbon over Northeast Indian Ocean and South China Sea and Implications for Oceanic Black Carbon Cycling
Xiaofei Geng, Jordahna Haig, Boji Lin, Chongguo Tian, Sanyuan Zhu, Zhineng Cheng, Yupeng Yuan, Yan Zhang, Junyi Liu, Mei Zheng, Jun Li, Guangcai Zhong, Shizhen Zhao, Michael I. Bird, Gan Zhang
Abstract
Aerosol black carbon (BC) is a short-lived climate pollutant. The poorly constrained provenance of tropical marine aerosol BC hinders the mechanistic understanding of extreme climate events and oceanic carbon cycling. Here, we collected PM 2.5 samples during research cruise NORC2016-10 through South China Sea (SCS) and Northeast Indian Ocean (NEIO) and measured the dual-carbon isotope compositions (δ 13 C– Δ 14 C) of BC using hydrogen pyrolysis technique. Aerosol BC exhibits six different δ 13 C− Δ 14 C isotopic spaces (i.e., isotope provinces). Liquid fossil fuel combustion, from shipping emissions and adjacent land, is the predominant source of BC over isotope provinces “SCS close to Chinese Mainland” (53.5%), “Malacca Strait” (53.4%), and “Open NEIO” (40.7%). C 3 biomass burning is the major contributor to BC over isotope provinces “NEIO close to Southeast Asia” (55.8%), “Open NEIO” (41.3%), and “Open SCS” (40.0%). Coal combustion and C 4 biomass burning show higher contributions to BC over “Sunda Strait” and “Open SCS” than the others. Overall, NEIO near the Bay of Bengal, Malacca Strait, and north SCS are three hot spots of fossil fuel-derived BC; the first two areas are also hot spots of biomass-derived BC. The comparable δ 13 C– Δ 14 C between BC in aerosol and dissolved BC in surface seawater may suggest atmospheric BC deposition as a potential source of oceanic dissolved BC.