深层对流云与持续超冷的液态水下降到-37.5摄氏度
1Institute of Earth Sciences, the Hebrew University of Jerusalem, Israel. daniel@vms.huji.ac.il
Nature
|June 6, 2000
概括
在深层的对流云中发现了极度超冷的液态水,这对于理解云层过程至关重要. 这些发现显示液态水持续到-37.5°C,影响天气和气候模型.
科学领域:
- 大气科学 大气科学
- 云物理 云物理
- 气象学 天气学
背景情况:
- 高超冷水 (温度低于0°C的液态水) 已知存在于圆云和波浪云中,但在深度对流云中尚未得到充分研究.
- 卫星数据显示,在大陆对流风暴中,极度超冷水的频繁发生.
- 之前的研究缺乏对深度对流云顶部超冷水的现场测量.
研究的目的:
- 报告在现场测量深度对流云中的极度超冷水.
- 在非常低的温度下量化液态水的量和液滴大小.
- 为改善云计算过程模拟和了解气候影响提供数据.
主要方法:
- 在现场测量使用飞机仪器在深度对流云.
- 在零度以下温度下分析凝结水含量和滴滴大小分布.
- 观察从液体到冰的相变,以推断结机制.
主要成果:
- 深层对流云中的大部分凝结水保持液态,温度低至-37.5°C.
- 液态水含量达到1.8g m-3,比之前报道的数量级高出一个数量级.
- 滴滴的中位体径为17微米.
- 冰只在稍微较低的温度下被观察到,这表明了均的结.
结论:
- 深层对流云可以含有大量高超冷液态水.
- 这些发现挑战了关于混合相云过程的现有假设.
- 这些数据对于改善数值天气预报和气候模型至关重要,特别是关于降雨,冰和电气化的数据.
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