充满烟雾的旋使半球气溶在中层平流层中增加了一倍,并缓冲臭氧层的消耗
Chaoqun Ma1, Hang Su2, Jos Lelieveld3
1Minerva Research Group, Max Planck Institute for Chemistry, 55128 Mainz, Germany.
Science advances
|July 12, 2024
概括
澳大利亚的大型野火将烟雾升到平流层,形成一个充满烟雾的 vortex (SCV). 这种旋出乎意料地增加了臭氧生产,部分抵消了野火烟雾造成的臭氧消耗.
科学领域:
- 大气化学 大气化学
- 气候科学 气候科学
- 气溶科学 气溶科学
背景情况:
- 2019-2020年澳大利亚的大型野火将烟雾注入平流层.
- 这种烟雾在平流层下层造成了严重的臭氧损耗.
研究的目的:
- 为了模拟野火烟雾的轨迹.
- 为了研究烟雾诱导的在平流层化学中的作用.
- 量化对臭氧消耗和平流层气溶分布的影响.
主要方法:
- 计算机模拟烟雾动态的计算机模型.
- 分析平流层中的气溶分布和化学反应.
- 模拟充满烟雾的旋形成及其影响.
主要成果:
- 这项研究成功地模拟了烟雾向中层平流层 (~35公里) 的上升.
- 一个充满烟雾的 (SCV) 被确定为对空气污染物至关重要.
- 在中层平流层中,SCV几乎使南半球的气溶负担翻了一番.
- 中层平流层中的异质化学物质得到了增强,增强了臭氧的产生.
- 臭氧产量补偿了高达70%的平流层下层臭氧损耗.
结论:
- 充满烟雾的旋在平流层气溶的再分配和影响大气化学方面发挥着重要作用.
- 野火对平流层的影响被SCV放大,影响臭氧水平.
- 全球气温的上升可能会导致野火导致的SCV变得更频繁,更具影响力.
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