确定新粒子形成事件对云凝聚核 (CCN) 度的影响
A Casans1, J A Casquero-Vera1, F Rejano2
1Andalusian Institute for Earth System Research IISTA, University of Granada, 18006 Granada, Spain; Department of Applied Physics, University of Granada, 18071 Granada, Spain.
The Science of the total environment
|March 14, 2025
概括
新粒子形成 (NPF) 事件显著影响云凝聚核 (CCN) 度. 一种新的方法量化了NPF.
科学领域:
- 大气科学 大气科学
- 气候科学 气候科学
- 气溶科学 气溶科学
背景情况:
- 大气中的气溶颗粒,作为云凝结核 (CCN),对气候和水文循环至关重要.
- 新粒子形成 (NPF) 事件是CCN的主要来源,但它们的全球影响仍然不确定.
- 目前用于估计NPF的CCN贡献的方法在区分NPF产生的粒子与其他粒子方面存在局限性.
研究的目的:
- 引入和验证一种用于直接估计NPF事件对CCN度的贡献的新方法.
- 为了区分NPF产生的颗粒与背景或运输的气溶.
- 评估该方法在不同大气条件和测量类型中的适用性和局限性.
主要方法:
- 开发了一种方法,重点关注新形成的粒子的最大大小,NPF事件时间,并隔离NPF模式.
- 使用了塞拉内华达站 (SNS) 的尺寸解析CCN测量和多分散CCN测量.
- 将该方法应用于Izaña天文台 (IZO) 的NPF事件,以进行跨站点验证.
主要成果:
- 这种新方法成功地区分了NPF产生的粒子,并且适用于尺寸解析和多分散的CCN数据.
- 平均NPF对CCN的贡献是SNS的6.2±4.8%,IZO的24±25%.
- 在IZO的更高的NPF贡献与更大的颗粒生长和更少的竞争背景气溶有关.
结论:
- 拟议的方法提供了NPF对CCN贡献的直接和可靠估计.
- 在NPF贡献存在显著的变化,受特定事件的特征和现场条件的影响.
- 这些发现增强了对NPF在气溶云相互作用和气候中的作用的理解.
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