本文已被：浏览 793次 下载 1352次
中文摘要: 1996年8月3—5日河北省西南部地区出现了特大暴雨过程。此次特大暴雨，主要是9608号台风登陆后减弱为低气压西北上，副热带高压加强西进，低层从东北部有弱冷空气扩散南下，在暴雨区域形成湿斜压锋区，触发不稳定能量释放，致使台风低压北方形成3个中尺度对流云团所致。
中文关键词: 中尺度对流云团，台风低压，湿斜压锋区
Abstract:The torrential rain had happened in the southwest of Hebei province on August 3-5 in 1996.This torrential rain was resulted from the interaction of the landed typhoon 9608 low,subtropical high and weak cold air from northeast.Because of cold air diffused toward the typhoon low,the wet baroclinic front was generated.Then,three mesoscale convective cloud cluster were generated,developed at the north of typhoon low.
文章编号： 中图分类号： 文献标志码：
基金项目:
| Author Name | Affiliation |
引用文本：
杜青文,张迎新,1997.“96.8”特大暴雨的中尺度对流云团特征[J].气象,23(10):39-43.
,1997.Mesoscale Convective Cloud Cluster Analysis of the Torrential Rain in August 1996[J].Meteor Mon,23(10):39-43.
杜青文,张迎新,1997.“96.8”特大暴雨的中尺度对流云团特征[J].气象,23(10):39-43.
,1997.Mesoscale Convective Cloud Cluster Analysis of the Torrential Rain in August 1996[J].Meteor Mon,23(10):39-43.