轻度降雨而不是总降雨决定了气溶的湿去除
Wenwen Xia1,2,3, Yong Wang3, Guang J Zhang4
1State Key Laboratory of Numerical Modelling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China.
Environmental science & technology
|October 17, 2024
概括
降水频率,而不是总量,是去除大气气溶的关键. 轻度降水事件有效地清除污染物,影响空气质量和气溶光学深度 (AOD).
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:
- 降水清理是大气污染物的主要吸收源.
- 降水特征 (数量,强度,频率,持续时间) 对气溶去除的相对重要性仍在争论中.
研究的目的:
- 为了确定哪些沉特征对气溶湿去除最为重要.
- 建立关于大气气溶沉积的主要驱动因素的共识.
主要方法:
- 对气溶湿沉积的全球现场观测的分析.
- 修改全球气候模型以改变轻度降水频率.
- 模型结果与相结合模型对比项目第6阶段 (CMIP6) 模拟的比较.
主要成果:
- 降水频率,特别是轻度降水,是气溶清理的主要因素.
- 降低光降落频率导致气溶光学深度 (AOD) 增加.
- 气溶湿沉积模式的变化与轻度降水频率密切相关,而不是总降水量.
结论:
- 由于它们的高频率,轻微降水事件对气候气溶湿沉积比总降水量更为关键.
- 模型模拟和CMIP6模型之间的比较证实了光降水频率在确定AOD和气溶沉积中的主导作用.
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