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通过来自野火驱动雷暴的大型气溶颗粒的增强辐射冷却
Yaowei Li1, John A Dykema1, David A Peterson2
1School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA.
Science advances
|December 10, 2025
概括
野火会产生烟 (pyroCb) 云,将烟雾送高到大气层. 这些大型烟雾颗粒导致显著的辐射冷却,气候模型可能低估了这种效应.
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:
- 大规模的野火会产生pyrocumulonimbus (pyroCb) 云,将烟雾气溶注入上层热层和下层平流层 (UT/LS).
- 由于有限的直接测量,人们对pyroCb烟雾气溶的辐射效应知之甚少.
- 烟雾气溶持续数月,影响气候和大气辐射平衡.
研究的目的:
- 在现场展示飞机对老化pyroCb烟雾气溶的测量结果.
- 解决从新鲜到老化的气溶演变中的观察差距.
- 为了量化大型pyroCb烟雾颗粒的辐射效应.
主要方法:
- 在现场飞机测量了5天的pyroCb烟雾气溶.
- 气溶颗粒大小分布和组成的分析.
- 基于测量的气溶特性计算辐射效应.
主要成果:
- 抽取的pyroCb烟雾含有异常大的气溶颗粒 (直径500-600nm).
- 这些大颗粒是通过UT/LS的云处理和凝结而形成的.
- 大颗粒增加了30-36%的外发辐射,增强了大气辐射冷却.
结论:
- 与典型的烟雾相比,PyroCb烟雾气溶具有不同的特性 (更大的颗粒大小).
- 目前的气候模型可能低估了pyroCb烟雾的冷却效应,因为粒子大小小小.
- 对pyroCb气溶属性的准确表示对于改善气候预测至关重要,特别是随着野火频率的增加.
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