| 2002年6月13日重庆区域大暴雨分析 |
| |
| 引用本文： | 王中,周毅.2002年6月13日重庆区域大暴雨分析[J].气象,2004,30(5):30-32. |
| |
| 作者姓名： | 王中 周毅 |
| |
| 作者单位： | 重庆市气象台,401147 |
| |
| 摘 要： | 通过对重庆西部“6 1 3”区域大暴雨的分析 ,发现此次天气过程是一次典型的高原涡与西南涡耦合 ,结合地面弱冷空气条件下产生的 ,同时对ECMWF和T2 1 3数值预报产品进行了简要的分析 ,发现ECMWF和T2 1 3的形势预报能力都比较好 ,但T2 1 3的部分物理量要素和降水量预报能力还有待提高。
|
| 关 键 词： | 耦合 区域大暴雨 数值预报 |
Analysis of Heavy Rainfall Event on June 13th in Chongqing |
| |
| Wang Zhong,Zhou Yi.Analysis of Heavy Rainfall Event on June 13th in Chongqing[J].Meteorological Monthly,2004,30(5):30-32. |
| |
| Authors: | Wang Zhong Zhou Yi |
| |
| Abstract: | An analysis of a heavy rainfall event over the west of Chongqing on June 13th , 2002 is made. It is shown that the event resulted in a typical coupling of plateau vortex and southwest vortex, in addition the influence of the weak cold air. And it is shown that the general circulation forecast capability of the models of ECMWF and T213 is relatively high, however, part of physical elements products of T213 models and its precipitation forecast should be improved. |
| |
| Keywords: | plateau vortex heavy rainfall event numerical forecast |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
| 点击此处可从《气象》浏览原始摘要信息 |
| 点击此处可从《气象》下载免费的PDF全文 |
|
