摘要
本文在分析梅雨期暴雨中尺度水热场特征的基础上,利用Nitta的云谱模式和积云对流参数化方法对暴雨区积云对流对环境水热场的反馈机制进行了诊断研究.结果表明,在暴雨过程中,主要是高云和低云两类云的活动,在对流层中层很少有卷出的积云;积云对流的补偿下沉气流强烈地加热和干燥环境大气,这种加热和干燥效应主要被积云卷出的液态水再蒸发所抵消;同时,在暴雨过程中还可能存在某种不同于积云卷出液态水的蒸发冷却和湿润环境大气的物理机制.
A heavy rainfall case in Chinese Meiyu season is studied with mesoscale experiment data. It is shown that cumulus convection has strong feedback on the mesoscale heat and moisture fields. Nitta's cloud spectrum model is solved and parameterization approach is used to study the mechanism of the heating and drying effects caused by cumulus on the environment. Some interesting results are presented in the paper.
出处
《大气科学》
CSCD
北大核心
1991年第4期36-42,共7页
Chinese Journal of Atmospheric Sciences
关键词
暴雨
积云
对流
反馈机制
水热场
Meiyu heavy rainfall
Cumulus convection
Heat and moisture fields
Feedback effects.
