[1]钟利华,李仲怡,李勇,等.西江流域台风暴雨面雨量分布特征及天气概念模型[J].气象研究与应用,2017,38(03):13-22.
　Zhong Li-hua,Li Zhong-yi,Li Yong,et al.Areal rainfall distribution characteristics of typhoon torrential rain and weather concept model of Xijiang basin[J].Journal of Meteorological Research and Application,2017,38(03):13-22.
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西江流域台风暴雨面雨量分布特征及天气概念模型()
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气象研究与应用[ISSN:1673-8411/CN:45-1356/P]

卷:
第38卷
期数:
2017年03期
页码:
13-22
栏目:
天气气候
出版日期:
2017-09-30

文章信息/Info

Title:
Areal rainfall distribution characteristics of typhoon torrential rain and weather concept model of Xijiang basin
作者:
钟利华;  李仲怡;  李勇;  罗小莉;  史彩霞
广西区气象服务中心, 南宁 530022
Author(s):
Zhong Li-hua;  Li Zhong-yi;  Li Yong;  Luo Xiao-li;  Shi Cai-xia
Guangxi Meteorological Service Centre, Nanning 530022
关键词:
西江流域; 台风; 暴雨面雨量; 分布特征; 概念模型
Keywords:
Xijiang basin; typhoon; rainstorm areal rainfall; distribution characteristic; concept model
分类号:
P46
摘要:
通过对1971-2015年登陆华南的台风与西江流域暴雨落区的关联分析，将造成西江流域暴雨的台风按路径分为四类，对每类路径的台风暴雨时空分布特征进行分析研究；通过对台风暴雨典型个例合成分析，建立各类路径台风暴雨天气概念模型。结果表明：（1）西江流域台风暴雨出现在每年6-11月，8月最多，11月最少，6月、9月以Ⅱ类路径为主，7月Ⅱ类、Ⅲ类和Ⅳ类路径较多，8月以Ⅳ类路径为主，10月、11月以Ⅰ类路径为主；（2）Ⅰ类路径台风暴雨集中出现在郁江干流，Ⅱ类路径在黔浔江河段和郁江干流，Ⅲ类路径在红水河河段、黔浔江河段和郁江干流、桂江干流，Ⅳ类路径在红水河河段；（3）Ⅰ、Ⅱ类路径台风暴雨强度最强，范围较大，Ⅲ类路径台风暴雨范围最大，强度较Ⅰ、Ⅱ类稍弱，Ⅳ类路径台风暴雨范围和强度都比其他类型要小（弱）.
Abstract:
Based on the correlation analysis of Xijiang river basin rainstorm falling area and typhoon landing in south China during 1971-2015, the typhoon were divided into four categories according to the path of rainstorm in Xijiang river basin. The spatial and temporal characteristics were studied and the weather concept models of all kinds of typhoon rainstorm were established by the synthetic analysis of classic examples. The results show that: (1) the Xijiang river basin typhoon torrential rain mainly appeared during June ~ November with the most in August and least in November. June and September are given priority to rainstorm of Ⅱ class path, Ⅱ, Ⅲ and Ⅳ class path is more July, and August is given priority to ones of Ⅳ class path, the rainstorm of October and November are mainly the ones of Ⅰ class path; (2) typeⅠfocus in main stream of Yu river, type Ⅱ happens in main stream Qianxun river and Yu river, type Ⅲ appears in Hongshui river, Qianxun river and mian sreams of Yu river and Gui river, type Ⅳ occurred in Hongshui river; (3) the intensity of type Ⅰand Ⅱrainstorm is the strongest and the range is rather large while the type Ⅲ has the largest raining area but weaker intensity. By contrast, the type Ⅳhas the weaker intensity and smaller range.

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备注/Memo

备注/Memo:
收稿日期:2017-01-29。
基金项目:广西科学研究与技术开发计划项目（桂科攻1598017-15）。
作者简介:钟利华(1962-),女,广西恭城人,主要从事天气预报研究与服务.E-mail:1427962612@qq.com.
更新日期/Last Update: 1900-01-01