灞河出山径流序列变化的小波分析  

Wavelet analysis on runoff sequences from mountainous watershed of Bahe River

作　　者：张学真[1] 刘燕[1] 

机构地区：[1]长安大学环境科学与工程学院,陕西西安710054

出　　处：《水资源保护》2006年第3期12-15,共4页Water Resources Protection

基　　金：国家科技部资助项目(2002BA901A43)

摘　　要：以西安地区年降水序列为参照,利用小波分析方法对灞河出山径流序列的周期性变化进行分析。结果表明,西安地区平均年降水序列和灞河出山径流序列存在着多时间尺度周期,并且基本具有同步变化的规律性,反映了人类活动对灞河出山径流序列的周期性影响不大。其中,变化较明显的周期是10 a1、5 a左右时间尺度,水文序列变化的高能量主要集中在较小的时间尺度上。用秩次相关分析法检验得出灞河出山径流序列均存趋势性,用有序聚类分析法分析得出灞河出山径流序列的突变年份是1948年。Taking precipitation sequence in Xi＇an as reference, the periodic variation of runoff from mountainous watershed of Bahe River was analyzed. Results show that both of the reference data and examination data has periodicity of multi-scale of time, and the change rules are almost synchronous, which means that the human activity has Little impact on the periodicity of the runoff sequence, The obvious periodic variation appears in the time scale of 10-year, 15- year or so, The high energy of the variation of hydrologic sequence mostly appears at small time scale, Rank correlation analyses show that all of the runoff sequence change with tendency, and the sudden change appeared in 1948, as concluded by order cluster analysis method.

关 键 词：灞河 径流 周期性 小波分析 

分 类 号：TV121.4[水利工程—水文学及水资源]