南京大学学报(自然科学版) ›› 2022, Vol. 58 ›› Issue (5): 766779.doi: 10.13232/j.cnki.jnju.2022.05.003
• • 上一篇
Zhixiao Xu1, Liangbo Qi2, Yuan Wang1()
摘要:
利用中国气象局上海台风所的WARMS高分辨率区域模式研究了上海地区三类主要的暴雨天气(准静止锋雨带型、副高边缘强对流型以及暖区雷暴型)对云微物理和边界层过程的敏感性.结果表明,不同云微物理和边界层参数化方案的组合对强降水中心的位置和强度影响较大,但是对主要雨带及走向影响不大.准静止锋雨带型采用Thompson方案模拟的整体降水量更多,WSM6方案模拟的强降水相关性更好,评分更高;副高边缘强对流型中WSM6?MYJ组合激发上海本地对流的效果更明显,但整个雨带来看Thompson方案更有优势;暖区雷暴型中WSM6?MYJ组合优势明显.总体上,Thompson?YSU组合能够模拟出准静止锋雨带型暴雨中丰富的液水含量和冰相粒子,以及较强的整层抬升作用;WSM6?MYJ组合则在副高边缘强对流型和暖区雷暴型这类型暴雨中刻画了较明显的强对流结构,使得地面降水更为强盛.
中图分类号:
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