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在雅加达洪水事件中观察到的降雨微物理特征
Findy Renggono1, Sopia Lestari2,3, Halda Aditya Belgaman4
1National Research and Innovation Agency, South Tangerang, 15310, Indonesia. findy.renggono@brin.go.id.
Scientific reports
|September 30, 2025
概括
大雅加达经历了洪水的增加,这项研究分析了严重洪水事件期间的降雨特征. 结果揭示了不同的降雨类型和下降大小,对于理解洪水动态至关重要.
科学领域:
- 大气科学 大气科学
- 水文学的水文学
- 气象学 天气学
背景情况:
- 自2019年以来,大雅加达地区的洪水事件显著增加.
- 关于这些洪水事件期间降雨的物理特征的研究有限.
研究的目的:
- 为了调查雅加达三次严重洪水事件期间降雨量下降大小分布.
- 分析和分类降雨特征 (层状,对流,混合) 以及它们与洪水事件的关系.
主要方法:
- 利用了自动气象站和激光降雨监测器数据.
- 纳入了2019年12月至2022年10月的ERA5再分析数据集.
- 分析了降雨量下降大小分布和分类降雨类型.
主要成果:
- 在这三个洪水事件中,在低地和山区均观察到直径高达4毫米的雨滴.
- 与低地相比,山区的雨滴大小的频率更高.
- 案例1在低地出现了长时间的层状降雨,与严重的洪水相吻合,可能与高湿度收和负垂直速度有关.
结论:
- 降雨特征,包括降雨大小分布和类型 (层状,对流,混合),在洪水事件和地理区域 (低地与山地) 之间有所不同.
- 正如在案例1中所观察到的,长时间的分层降雨是导致雅加达严重洪水的一个重要因素.
- 了解这些降雨动态对于改善该地区的洪水预测和缓解策略至关重要.
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