摘要
本文对珠江三角洲地区1983年9月24日在副热带高压控制下强对流天气发生的物理量场进行分析,发现这次强对流天气是在有利的环境条件下发生的。指出了这次强对流天气的可能触发条件,对今后预报此类强对流天气有重要意义.
In this paper, the physical variant fields of a strongly convective weather process ocurred on 24 September 1983 over the Delta of Pearl River are analysed. It has been found that this strongly convective weather process did occur under some singular enviromental conditions. The possible trigger mechanisms for the convective process have been discussed,which will provide some important criteria for the forecast of strongly convective weather processes.
出处
《中山大学学报论丛》
1994年第5期45-49,共5页
Supplement to the Journal of Sun Yatsen University
关键词
强对流天气
副热带高压
strongly convective weather
subtropical anticyclone