日本地球惑星科学連合2022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-AS11] 大気化学

2022年5月27日(金) 13:45 〜 15:15 201A (幕張メッセ国際会議場)

コンビーナ:内田 里沙(一般財団法人 日本自動車研究所)、コンビーナ:坂本 陽介(京都大学大学院地球環境学堂)、岩本 洋子(広島大学大学院統合生命科学研究科)、コンビーナ:石戸谷 重之(産業技術総合研究所)、座長:松井 仁志(名古屋大学大学院環境学研究科)

14:45 〜 15:00

[AAS11-16] The underappreciated role of anthropogenic sources in atmospheric soluble iron flux to the Southern Ocean

*Mingxu Liu1、Hitoshi Matsui1 (1.Nagoya University)

キーワード:iron oxides, global aerosol simulations, Southern Ocean, anthropogenic activities

The atmospheric deposition of soluble (bioaccessible) iron enhances ocean primary productivity and subsequent atmospheric CO2 sequestration in iron-limited ocean basins, especially the Southern Ocean. While anthropogenic sources have been recently suggested to be important in some northern hemisphere oceans, the role in the Southern Ocean remains ambiguous. In this study, we constrain the atmospheric cycle of anthropogenic iron oxides using new aircraft measurements and global aerosol model simulations. The deposition fluxes of soluble iron from the atmosphere to the Southern Ocean are estimated under present-day and future scenarios. First, by comparing multiple model simulations with the aircraft observations for anthropogenic iron, we show that anthropogenic soluble iron deposition flux to the Southern Ocean could be underestimated by more than a factor of ten in previous modeling estimates. Our improved estimate for the anthropogenic iron budget then enhances its contribution to the soluble iron deposition in the Southern Ocean from about 10% to 60%, implying a dominant role of anthropogenic sources. We predict that anthropogenic soluble iron deposition in the Southern Ocean is reduced substantially (30% to 90%) by the year 2100, and play a major role in the future evolution of atmospheric soluble iron inputs to the Southern Ocean.