负责缅甸海岸海上-陆上雨水对比的机制
Pushpaleela Ancy1, Hamza Varikoden2, Chethalan Anthony Babu1
1Department of Atmospheric Sciences, Cochin University of Science and Technology, Kochi, 682 016, India.
The Science of the total environment
|January 21, 2026
概括
季风降雨模式在缅甸西海岸沿海和陆地之间有很大差异. 海上降雨在晚上和早上达到峰值,而陆上降雨在下午和晚上达到峰值,这是由不同的大气过程驱动的.
科学领域:
- 气象学 天气学
- 大气科学 大气科学
- 气候科学 气候科学
背景情况:
- 白天降雨周期是季风变化的关键因素,特别是在具有重要的地理特征的地区,如缅甸西海岸 (WCM).
- 的地形和陆海对比度极大地影响了该地区的降雨模式.
研究的目的:
- 分析WCM上昼间降雨模式的空间和时间特征.
- 根据时间和位置 (海上与陆上) 将白天降雨分为不同的模式.
- 确定不同降雨模式的潜在大气驱动因素.
主要方法:
- 利用了22年的TRMM 3B42 V7降水数据和ERA5再分析数据.
- 选定的降雨天,最大降雨量超过3mm/h.
- 根据每日最大的时间 (上午,下午,晚上,夜间) 和位置 (海上,陆上) 将降雨量分为八种模式.
主要成果:
- 在海上和陆上降雨制度之间存在着明确的区别.
- 海上降雨主要以早晨和夜间的高峰为特征,由海洋动态 (汇聚,,湿度) 驱动.
- 陆地降雨在下午和晚上最强,与表面加热引起的不稳定性有关,而早晨/夜间陆地降雨是动态控制的.
结论:
- 离岸降雨制度始终受到大规模动态过程的控制.
- 陆上降雨模式表现出变化,热力学不稳定性导致下午/晚上峰值,动态强迫控制早晨/夜间峰值.
- 区分陆海影响对于改善昼间降雨模型和预测季风极端在WCM中至关重要.
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