嘉陵江流域降水量时空分布特征
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:Temporal and Spatial Distribution of Precipitation in Jialingjiang River Basin
  • 作者:贺成民 ; 陈元芳 ; 孙夏利
  • 英文作者:HE Cheng-min;CHEN Yuan-fang;SUN Xia-li;College of Hydrology and Water Resources, Hohai University;Hydrology and Water Resources Investigation Bureau of Shaanxi Province;The Experimental Teaching Center of Water Conservancy Projects, Hohai University;
  • 关键词:嘉陵江流域 ; 降水量 ; 时空分布 ; 小波分析 ; Mann-Kendall法
  • 英文关键词:Jialingjiang River Basin;;precipitation;;temporal and spatial distribution;;wavelet analysis;;Mann-Kendall method
  • 中文刊名:SDNY
  • 英文刊名:Water Resources and Power
  • 机构:河海大学水文水资源学院;陕西省水文水资源勘测局;河海大学水利工程实验教学中心;
  • 出版日期:2019-06-25
  • 出版单位:水电能源科学
  • 年:2019
  • 期:v.37;No.226
  • 基金:国家自然科学基金项目(51479061)
  • 语种:中文;
  • 页:SDNY201906002
  • 页数:4
  • CN:06
  • ISSN:42-1231/TK
  • 分类号:11-14
摘要
利用嘉陵江流域9个气象站点1961~2018年共58年实测降水资料,选用Morlet小波分析方法研究流域降水序列的多时间尺度,同时对降水数据做Mann-Kendall非参数检验,并结合GIS空间分析技术,探讨了嘉陵江流域降水量年际变化特征、降水变化时间周期及空间分布特征。结果表明,嘉陵江流域58年的年平均降水量为954.1mm,并以3.9mm/10a的速率减少,在1984年突变最明显,降水由丰变枯;降水变化存在4个主周期,分别为32、14、8、3年,且周期波动强度依次由强到弱变化;受季风因素影响,流域降水地域性差异较为明显,由西北至东南方向呈逐渐上升趋势;只有达县和沙坪坝两区降水量呈增长趋势,增加倾向率分别为14.1、15.1mm/10a,其余地区降水量均有不同程度的降低,所以东南地区偏涝。
        Using 58-years measured rainfall data from 9 meteorological stations in the Jialingjiang River Basin,Morlet wavelet analysis method was used to study the multi-time scale of the rainfall sequence in the basin.At the same time,the Mann-Kendall nonparametric test was carried out on the rainfall data,and the GIS spatial analysis technique was used to discuss the inter-annual variation characteristics of precipitation,time period of precipitation change and spatial distribution characteristics in the Jialingjiang River Basin.The results show that the 58-years average annual precipitation in the Jialingjiang River Basin is 954.1 mm,which decreases at a rate of 3.9 mm/10 a.There is a significant mutation in 1984,and the precipitation changed from high to low.There are four main periods of precipitation change,which are 32,14,8 and 3 a,and the intensity of cyclical fluctuations changes from strong to weak.Affected by the monsoon factor,the regional differences in precipitation of the basin are more obvious,appearing agradual upward trend from northwest to southeast.Regionally,only the precipitation in Daxian County and Shapingba County showed an increasing trend with 14.1 mm/10 aand 15.1 mm/10 a,respectively.The precipitation in other areas decreased in varying degrees,so the southeast region was waterlogged.
引文
[1]杨忠英.嘉陵江20世纪90年代以来径流量锐减现象分析[J].四川水利,2004(5):20-22.
    [2]陈桂亚,Derek Clarke.气候变化对嘉陵江流域水资源量的影响分析[J].长江科学院院报,2007,24(4):14-18.
    [3]王文圣,丁晶,李跃清.水文小波分析[M].北京:化学工业出版社,2005.
    [4]许家琦,舒红.降水数据空间插值的时间尺度效应[J].测绘信息与工程,2009,34(3):29-30.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700