印度中部季风后和冬季雷暴的大气驱动因素
U V Murali Krishna1, Subrata Kumar Das1, Jeni N Victor1
1Atmospheric Research Testbeds, Indian Institute of Tropical Meteorology, Ministry of Earth Sciences, Bhopal 466665, India; Indian Institute of Tropical Meteorology, Ministry of Earth Sciences, Pune 411008, India.
The Science of the total environment
|April 25, 2025
概括
印度的恶劣天气事件正在增加. 这项研究分析了季风后和冬季雷暴,揭示了气候模型至关重要的暴雨的独特驱动机制.
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:
- 严重的天气事件,特别是暴雨,在印度次大陆带来了重大的社会经济挑战.
- 驱动这些强烈降雨事件的确切机制,特别是雷暴,仍然不完全理解.
研究的目的:
- 调查印度中部季风后和冬季雷暴的风暴规模特征和驱动机制.
- 增强对该地区严重天气事件造成的因素的理解.
主要方法:
- 使用C频段多普勒天气雷达数据从博帕尔和重新分析数据.
- 分析了雷达反射率,风暴顶峰高度和失调仪观测.
- 检查了大气中的水蒸气传输和综合条件.
主要成果:
- 季风后和冬季雷暴都表现出强烈的对流 (雷达反射率> 45 dBZ).
- 季风后的雷暴更深 (超过12公里),并与一个中等层面的对流系统相关.
- 冬季雷暴在短时间内表现出极端强度 (158毫米/小时),由水平质量趋同驱动.
结论:
- 季风后雷暴的发展与旋风循环和中热层加湿有关.
- 冬季雷暴的发展主要是由寒冷和温暖,潮湿的空气质量的汇聚驱动的.
- 这些发现对于改善区域气候模型对大雨事件的模拟具有重要意义.
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