火山灰的冰核形成极大地改变了云的特性
Lin Lin1, Xiaohong Liu1, Xi Zhao1
1Department of Atmospheric Sciences, Texas A&M University, College Station, TX, USA.
Science advances
|May 9, 2025
概括
火山灰 (VA) 通过促进冰核形成,显著改变云,导致较少,较大的冰晶. 这一发现影响了我们对气溶-冰云相互作用和潜在的气候地质工程的理解.
科学领域:
- 大气科学 大气科学
- 云物理 云物理
- 气候科学 气候科学
背景情况:
- 云层中冰晶的形成极大地影响了大气的特性和全球气候.
- 众所周知,火山灰 (VA) 在实验室实验中有效地核化冰,但其在大气中的作用尚不清楚.
研究的目的:
- 调查火山灰对大气冰晶形成和云特性的影响.
- 为火山灰在大气中异质冰核形成中的作用提供证据.
主要方法:
- 在火山爆发后对云特性进行卫星测量的分析.
- 富含灰和缺乏灰的喷发后的变化比较.
- 云微物理模拟以支持拟议的冰形成机制.
主要成果:
- 在富含灰的火山爆发后,观察到雪花云的突然变化:冰晶数量减少,冰晶大小增加,雪花云的发生增加.
- 在没有灰的喷发后没有检测到任何显著的变化,突出显示了火山灰的作用.
- 模拟证实,火山灰抑制了同质结,有利于异质核形成.
结论:
- 火山灰在大气中起到异质冰核的作用,改变状云的形成.
- 这种机制通过抑制同质结导致更少,更大的冰晶.
- 这些发现增强了对气溶与冰云相互作用的理解,并表明了云地质工程的潜力.
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