[特邀报告]登陆台风引起氮沉降增加的机制与影响

登陆台风引起氮沉降增加的机制与影响
编号:3709 稿件编号:1908 访问权限:私有 更新:2023-04-16 20:08:20 浏览:213次 特邀报告

报告开始:2023年05月08日 08:30 (Asia/Shanghai)

报告时间:15min

所在会议:[14A] 14A、气溶胶与大气环境 » [14A-4] 14A-4 气溶胶与大气环境

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摘要
Wet deposition of reactive nitrogen (Nr) induced by typhoons has significant eco-environmental impacts on the oceans, especially under the growing frequency of landfalling typhoons in East Asia. However, little is known about the mechanism of how anthropogenic activities influence the ocean ecosystem by interacting with landfalling typhoons. Based on the Nested Air Quality Prediction Modeling System, the Nr wet deposition induced by landfalling typhoon Hagupit 2020, and the ecological response, were explored. The Nr wet deposition over both the Yellow Sea and the Sea of Japan after landfall was found to have increased by up to 1000 times that of the pre-landfall ocean influenced by the typhoon. This high Nr wet deposition was mainly due to the “pumping effect” mechanism of the typhoon, which is strong uplifts of the typhoon rapidly carried surface air pollutants up to high altitudes from the land, following a large wet deposition through long-range transport towards downwind ocean, finally led to a high-concertation chlorophyll-a bloom. This study improves our understanding of Nr wet deposition induced by landfalling typhoons, and helps in the establishment of effective and active measures and to reveal marine ecology damaged by extremely strong convective weather systems.
关键字
氮沉降
报告人
葛宝珠
研究员 中国科学院大气物理研究所

稿件作者
葛宝珠 中国科学院大气物理研究所
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