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长江下游百年一遇的极值风速分布
引用本文:黄世成,周嘉陵,任健,陈兵,程婷.长江下游百年一遇的极值风速分布[J].应用气象学报,2009,20(4):437-442.
作者姓名:黄世成  周嘉陵  任健  陈兵  程婷
作者单位:1.江苏省气象科学研究所, 南京 210008
基金项目:江苏省自然科学基金重点项目,"十一五"国家科技支撑计划"苏通大桥建设关键技术研究"重点项目"安全减灾技术研究专题" 
摘    要:利用2000-2006年长江下游沿江8个风速、风向观测点与邻近气象站同步对比观测资料和1971—2006年长江下游40个气象站风资料, 依据具99%置信水平的数理重构方案和极值Ⅰ型计算方法, 详细给出长江下游百年一遇风速分布状况。结果表明:长江下游沿江地区百年一遇极值风速为25~38 m/s, 较一般方法上限高3 m/s, 下限低2 m/s; 长江南京—镇江段和南通—崇明段, 是长江下游沿江地区的两个大风区, 百年一遇极值风速不低于29 m/s, 其在入海口附近可达34 m/s以上; 在长江常州—江阴段, 江南、江北对称分布两个风速相对低值区, 百年一遇极值风速为23~24 m/s。该结果充分考虑气象站风速资料和局地风速状况, 是沿江相关工程气象应用的重要补充。

关 键 词:长江下游    置信上限    极值风速
收稿时间:2008-05-19
修稿时间:3/4/2009 12:00:00 AM

Speed Distribution of 100-year Extreme Winds in Lower-reaches of the Yangtze
Huang Shicheng,Zhou Jialing,Ren Jian,Chen Bing and Cheng Ting.Speed Distribution of 100-year Extreme Winds in Lower-reaches of the Yangtze[J].Quarterly Journal of Applied Meteorology,2009,20(4):437-442.
Authors:Huang Shicheng  Zhou Jialing  Ren Jian  Chen Bing and Cheng Ting
Affiliation:1.Jiangsu Institute of Meteorological Science, Nanjing 2100082.Jiangsu Meteorological Observatory, Nanjing 2100083.Jiangsu Provincial Meteorological Bureau, Nanjing 2100084.Jiangsu Climate Center, Nanjing 210008
Abstract:In engineering meteorological application the basic wind speed of 100-year return period is commonly confirmed according to the recommend value of national regulation or China basic wind speed distribute map by the method of interpolation. In order to avoid both the potential hazard in engineering design and the higher cost in construction, which may be caused by the low re solution of the basic wind speed distribute map in low er-reaches of the Yangtze and the lacking of actual wind speed data along the river, eight short-term wind observation points are selected along low er-reaches of the Yangtze, and the observation runs synchronously with their neighboring meteorological stations from 2000 to 2006. So the observation pro gram is set up to meet the demand of engineering constructions along low er-reaches of the Yangtze. The observation points are built by on-side investigation to eliminate the extreme terrain effects and can represent the actual wind of the low er-reaches to the largest extent. At every observation point, it is assured that more than one year of simultaneous observation with its adjacent weather station is carried out, although the observational time for each point is not always homology. Based on the short-term synchronous wind data and the annual maximum wind speeds of 40 weather stations of lower-reaches of the Yangtze from 1971 to 2006, the 99% confidence level logistic reconfiguration scheme and extreme value Ⅰ type calculation procedure are referred also a new wind speed distributive status over lower-reaches of the Yangtze is described in detail. Results indicate that along low er-reaches of the Yangtze the 100-year return period maximum wind speed is 25 to 38 m· s-1 which is 3 m ·s-1 larger than upper limit and 2 m · s-1 smaller than lower limit of the result by the general method. lower-reaches of the Yangtze, two gale regions exist both in the Nanjing-Zhenjiang segment and in the Nantong-Chongming segment, where the 100-year return period maximum wind speed is greater than 29 m ·s-1 and even above 34 m · s-1 near the entrance. It is also found that on both sides of Changzhou-Jiangyin river segment two lower extreme wind speed regions are symmetrical distribution, where the 100-year return period maximum wind speed is about 23 to 24 m· s-1. Fully considering the wind data of weather stations and the local wind speed observation, the results are important supplement for the concerned meteorological application works.
Keywords:lower reaches of the Yangtze  confidence upper limit  extreme wind speed
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