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“98·6”广西特大致洪暴雨过程的中尺度系统概述

The Meso-scale system summarization of Guangxi “98. 6” exceptional flood-producing rainfall process

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【作者】 吴恒强; 高安宁; 梁隽玫;

【Author】 WU Heng-qiang1, GAO An-ning2, LIANG Jun-mei1 (1. Guangxi Research Institute of Meteorology, Nanning 530022, China ; 2. Guangxi Meteorological Observatory, Nanning 530022, China)

【机构】 广西气象研究所; 广西气象台; 广西气象研究所 广西南宁530022; 广西南宁530022; 广西南宁530022;

【摘要】 利用常规天气图和1h雨量图,分析了“98·6”广西特大致洪暴雨过程的环流背景和中尺度系统,指出比常年偏南的西太平洋副热带高压、稳定的乌拉尔阻塞高压和南亚高压是极有利于中尺度系统在广西境内活动的环流背景,锋面上的扰动、西南低涡、西南热低压、西南低空急流等从区外移入广西的中尺度系统和海南岛绕流辐合、东兰和昭平附近的地形性涡旋和辐合等在本地特定地形条件下形成的地方性中尺度系统共同作用下产生了这次特大的致洪暴雨过程。当有利于中尺度系统活动的背景环流发生调整后,降雨过程便告结束。

【Abstract】 Based On Conventional synoptic chart and every othet an hour Precipitation chart, circu- lation background and miso-scal system of guangxi "98.6" exceptional flood-producing rainfall pro- cess was analysed. Result Showed that the background circulation, which was propitious to activi- ty of meso-scale system in Guangxi province, was composed by the south-deflection position of western pacific subtropical high、the stability of Ural block high and southern asian high. meso- scale systems such as frontal disturdance、south-western depression、south-western low-level jet、 south-western thermal depression that moved to guangxi area、and diffractive flow convergence caused by Hainan island, the meso-scale system caused by terrain vortex and convergence near Donglan and Zhaoping, were main cause of this exceptionalrainfall by interplay. The precipitation process was over after the adjustment of background circulation that propitious to activity of meso- scale system.

【关键词】 广西; 致洪暴雨; 中尺度系统;
【Key words】 Guangxi; flood-producing rainfall; meso-scale system;
【基金】 广西自然科学基金资助项目(桂科自9912013)
  • 【文献出处】 广西气象 ,Journal of Guangxi Meteorology , 编辑部邮箱 ,2001年03期
  • 【分类号】P458.121.1
  • 【被引频次】25
  • 【下载频次】73
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