氧酸核化的温度,湿度和电离作用
Birte Rörup1, Xu-Cheng He1,2, Jiali Shen1,3
1Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki Helsinki Finland xh346@cam.ac.uk.
概括
氧酸驱动海洋和极地大气中的新粒子形成. 温度影响中性核化,而离子诱导的核化不那么敏感,这表明中性途径主导粒子形成.
科学领域:
- 大气化学 大气化学
- 气溶科学 气溶科学
- 气候科学 气候科学
背景情况:
- 氧酸对于海洋和极地大气中的新粒子形成至关重要.
- 了解它们在不同条件下的核化机制对于全球模拟至关重要.
研究的目的:
- 研究温度,电离和湿度对氧酸核形成的影响.
- 确定不同大气区域的主导核化路径.
主要方法:
- 使用CERN的CLOUD (宇宙外泄水滴) 室进行实验测量.
- 采用动态建模来模拟不同条件下的核化过程.
主要成果:
- 离子诱导的粒子形成对温度变化不敏感.
- 中性粒子形成率在较低的温度下显著增加 (-10°C vs +10°C).
- 电离只能在非常高的酸度下增强粒子形成,这种度在海洋大气中很少见.
结论:
- 中性核化途径可能是酸在上层热带层的主导途径.
- 氧酸核化在很大程度上不受典型的相对湿度范围 (2%-80%) 的影响.
- 氧酸核化是海洋和极地边界层中核化的主要机制.
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