摘要
本文对1988年6月10日至11日发生在长江中游的一次MCC暴雨过程进行了较细致的天气动力学分析,揭示了该例中的云团特征、环境流场和动力、热力学特征。
A heavy rain in an MCC occurred in the middle reaches of the Changjiang River in the period of June 10—11, 1988 was analyzed in much detail by using the synoptic-dynamic method, exposing the characteristics of the clusters, the environment flow field and the dynamics and thermodynamics of the event.
出处
《南京气象学院学报》
CSCD
1990年第4期508-511,共4页
Journal of Nanjing Institute of Meteorology
