在厘米尺度上全息测量不均的云混合
Matthew J Beals1, Jacob P Fugal2, Raymond A Shaw3
1Atmospheric Sciences Program, Michigan Technological University, Houghton, MI 49931, USA.
概括
云层中的流会导致云层与空气之间的过渡. 空中全息成像显示滴子大小分布在局部波动, 但保持一致的平均直径.
科学领域:
- 大气科学
- 云物理
- 流情况
背景情况:
- 云的光学特性和降水量取决于流混合.
- 混合可以导致均的蒸发或选择性的滴水消失.
研究的目的:
- 在小乱的尺度上可视化云的空间结构和滴滴大小分布.
- 观察云对空气的反应和混合.
主要方法:
- 使用空中全息成像.
- 分析的重点是消散 (<1厘米).
主要成果:
- 流云呈现不均的现象,有明显的云层空气过渡.
- 当地滴滴密度发生显著波动.
- 尽管有波动,但平均液滴直径几乎保持不变.
结论:
- 云层清晰的空气接口持续到非常小的尺度.
- 滴水蒸发的动态是复杂的,并且取决于规模.
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