由于台风和污染导致的反应在中度海洋边界层的增强
Shanshan Wang1,2, Qinyi Li3,4,5, Ruifeng Zhang1
1Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP3), Department of Environmental Science and Engineering, Fudan University, Shanghai 200438, China.
National science review
|April 16, 2024
概括
台风通过增加海盐气溶排放,显著增加活性,导致大规模的臭氧破坏. 这凸显了旋风风暴在大气化学和空气质量方面的被忽视的作用.
科学领域:
- 大气化学 大气化学
- 气候科学 气候科学
- 环境科学 环境科学
背景情况:
- 反应性化合物影响大气化学,空气污染和气候.
- 活性的来源包括海盐气溶,海洋活动,极地和火山.
- 台风对反应性水平和来源的影响在很大程度上是未知的.
研究的目的:
- 调查台风在调节活性丰度和来源方面的作用.
- 量化台风引起的活性对臭氧破坏的影响.
- 评估对大气化学和空气质量的影响.
主要方法:
- 在台风影响期间在湖岛对氧化物 (BrO) 的现场观测.
- 在500米以下的海拔上分析 BrO 混合比率.
- 支持使用大气模型模拟进行现场测量.
主要成果:
- 在台风条件下观察到高水平的BrO (平均9.7±4.2 pptv,峰值~26 pptv).
- 台风引起的高风速放大了海盐气溶排放,增加了反应性的释放.
- BrO 的升高与高的 NOx 水平相关,这表明海洋盐气溶中的污染中介释放.
- 观察到的活性的增加导致臭氧破坏增加了约40%.
结论:
- 台风通过海盐气溶激活显著提高反应性水平.
- 污染还可能导致海盐气溶释放出反应性.
- 反应在沿海空气质量和大气氧化能力方面发挥着比以前想象的更为关键的作用.
- 未来的模型应该纳入台风和污染中介的反应性增加.
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