日本地球惑星科学連合2024年大会

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セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS09] 大気化学

2024年5月27日(月) 10:45 〜 12:15 104 (幕張メッセ国際会議場)

コンビーナ:入江 仁士(千葉大学環境リモートセンシング研究センター)、中山 智喜(長崎大学 大学院水産・環境科学総合研究科)、石戸谷 重之(産業技術総合研究所)、江波 進一(国立大学法人筑波大学)、座長:宮川 拓真(国立研究開発法人 海洋研究開発機構)

11:00 〜 11:15

[AAS09-08] Seasonal variations and sources of brown carbon in the Asian outflow: co-analyses on the optical properties and organic tracers

*朱 春茂1宮川 拓真1竹谷 文一1、Bhagawati Kunwar2、Dhananjay Deshmukh2河村 公隆2金谷 有剛1 (1.海洋研究開発機構、2.中部大学)

キーワード:ブラウンカーボンエアロゾル、光吸収特性、有機トレーサー、バイオマス燃焼

Light-absorbing organic aerosols (brown carbon, BrC) significantly impact climate, yet their detailed chemistry remains unclear. This study delves into the seasonal variations of optical properties of BrC and the relations with organic tracersat Fukue Island, a site in the Asian outflow region, from November 2019 to November 2020. In the study, we collected PM2.5 aerosols, analyzed their light absorption properties (water and methanol extracts), and quantified major organic components (organic carbon, water-soluble organic carbon, organic tracers). We found that the absorption coefficient of BrC exhibit distinct seasonal variations, peaking during winter-spring when influenced by air masses carrying emissions from Asian sources. Water-soluble BrC formation shows a strong correlation with a specific marker for fossil fuel combustion, phthalic acid, suggesting its significant influence during these seasons. Biomass burning emissions, as indicated by another marker, levoglucosan, contribute to BrC formation, particularly in spring. A distinct fraction of BrC, soluble in methanol, is more prevalent in summer, hinting at potential contributions from additional sources such as local biogenic emissions present in air masses from this period. This study sheds light on the seasonal dynamics and diverse sources of BrC in the Asian outflow region, even under generally clean atmospheric conditions. Our findings highlight the role of both anthropogenic and biogenic precursors, as well as potentially unique formation processes occurring in less polluted environments. This knowledge contributes to a better understanding of the complex factors influencing BrC formation and its implications for regional climate and air quality.