在城市环境中,气溶混合状态,新粒子形成和云滴数量度
Sabin Kasparoglu1, Nicholas Meskhidze2, Markus D Petters3
1Department of Marine, Earth, and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USA; Air Quality Research Center, University of California, Davis, Davis, CA 95616, USA.
The Science of the total environment
|August 14, 2024
概括
人类产生的气溶通过改变云凝结核来影响云形成. TRACER实验揭示了气溶的特性及其对云滴数量度的影响,显示风向的变化.
科学领域:
- 大气化学 大气化学
- 云物理 云物理
- 气溶科学 气溶科学
背景情况:
- 人类产生的气溶被假设能影响对流性降水.
- 气溶作为云凝聚核 (CCN),影响云的特性.
研究的目的:
- 综合来自TRACER实验的气溶尺寸分布和高度测量结果.
- 研究气溶特性与云凝聚核 (CCN) 和云滴数度 (CDNC) 之间的关系.
主要方法:
- 测量气溶尺寸分布和低和湿度对15至250nm之间的粒子.
- 分析气溶混合状态和湿透模式.
- 亚亚巴特地块模型模拟来导出CCN和CDNC.
主要成果:
- 气溶是外部混合的,几乎有两个组成部分的描述 (更多的和更少的湿透模式).
- 湿度可视性参数没有显著的尺寸依赖性,但根据风力行业而异.
- 日间循环表明二次有机气溶凝结;观察到新的粒子形成事件.
- CCN和CDNC显示了由风力部门影响的2-3倍的动态范围.
结论:
- 气溶的特性,特别是湿度,有很大的差异,影响云液滴的形成.
- 风向在确定气溶成分及其对CDNC的后续影响方面发挥着至关重要的作用.
- 新粒子形成和随后的混合影响气溶特性和云特性.
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