观测一个倾斜的水分结构,上流较弱,导致局部大雨
Satoru Yoshida1, Tetsu Sakai2, Tomohiro Nagai2
1Meteorological Research Institute, Tsukuba, Japan. syoshida@met.kishou.go.jp.
Scientific reports
|July 2, 2025
概括
潮湿的低水平喷气 (MLLJs) 燃料大雨. 观察结果显示,MLLJ内部有一个倾斜的,和的水分层,由微弱的上流加厚,有效地为对流系统提供水分.
科学领域:
- 大气科学 大气科学
- 气象学 天气学
- 水文学的水文学
背景情况:
- 中级对流系统 (MCS) 导致局部大雨.
- 了解为MCS提供燃料的水分传输至关重要.
- 低水位潮流 (MLLJs) 是主要的水分来源,但它们的结构和形成机制尚不清楚.
研究的目的:
- 为了研究MLLJs内部的水分结构.
- 了解负责MLLJ水分结构的机制.
- 澄清MLLJ如何对MCS发展和大雨造成影响.
主要方法:
- 在日本西部的九州进行现场观测.
- 使用无线电探测器,水蒸汽激光雷达和多普勒激光雷达.
- 分析了MLLJ的特征和湿度分布.
主要成果:
- 确定了一个不稳定的,和的潮湿层,在MLLJ中垂直延伸.
- 观察到这种潮湿层变厚,稍微倾向于MCSs.
- 在云层底下检测到微弱的上升电流,有助于水分传输和层层加厚.
结论:
- MLLJs具有明显的倾斜,和的潮湿层结构.
- 微弱的上流在通过垂直水分传输来加厚这一层中起作用.
- 这种结构有效地为MCS提供燃料,导致局部大雨事件.
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