海洋预报2011，Vol.28Issue(3)：68-73,6.
一次东风波引起的特大暴雨天气过程分析
The analysis of a rainstorm induced by easterly waves
夏秋萍 1张滨1
作者信息
- 1. 宁波92919部队气象台,浙江,宁波,315020
- 折叠
摘要
Abstract
This paper analyzed the process of heavy rain which happened on July 24 to 27 2010 at southeastern coast of Zhejiang, Wenzhou, Taizhou, Ningbo, Zhoushan et al., and discovered that the continuous heavy rain is caused by the easterly waves. The interaction of Western Subtropicaol High heat convection cloud with the easterly waves and the low vortex induced by wave were also important persistent heavy rain; At the same time, the uplifting effect of the Tiantai Mountain and Kuocang mountain, along with the narrow tube effect at the coastal horn-type Harbour also played an important role. We pointed out that it's a profound easterly wave with big northe-south amplitude, long duration and high height extending up to 200 hPa. The structural features are:low-level trough before the divergence, high-level convergence, after the trough of low level convergence together high-level divergence; wave front sinking motion, upward motion after the wave.关键词
东风波/低涡/暴雨/地形Key words
easterly waves/ vortex/ rainstorm/ terrain分类
天文与地球科学引用本文复制引用
夏秋萍,张滨..一次东风波引起的特大暴雨天气过程分析[J].海洋预报,2011,28(3):68-73,6.
