Evaluating the performance of hydrological models with joint multifractal spectra

被引:2
|
作者
Bai, Zhixu [1 ]
Xu, Yue-Ping [2 ]
Pan, Suli [3 ]
Liu, Li [2 ]
Wang, Zixia [2 ]
机构
[1] Wenzhou Univ, Coll Architecture & Civil Engn, Wenzhou 325035, Lucheng, Peoples R China
[2] Zhejiang Univ, Coll Civil Engn & Architecture, Inst Hydrol & Water Resources, Hangzhou, Zhejiang, Peoples R China
[3] Zhejiang Univ Water Resources & Elect Power, Coll Water Conservancy & Environm Engn, Hangzhou, Zhejiang, Peoples R China
基金
浙江省自然科学基金; 中国国家自然科学基金;
关键词
joint multifractal spectra analysis; hydrological model; Nash-Sutcliffe efficiency; hydrological processes; RIVER-BASIN; FLUCTUATION ANALYSIS; FRACTAL ANALYSIS; SOIL-MOISTURE; TIME-SERIES; CROP YIELD; RUNOFF; RAINFALL; PRECIPITATION; REPRESENTATION;
D O I
10.1080/02626667.2022.2114834
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
The investigation of methods to evaluate the performance of hydrological models has never stopped. This study explores an innovative application, called joint multifractal spectra (JMS) analysis. The JMS analysis, which is demonstrated in three typical basins in Zhejiang Province, China, analyses both flood and low-flow periods. JMS is applied to seasonal-decomposed observed and simulated runoff series, thus helping to analyse the rising and the recession processes of discharge, which are unique features of a hydrograph. This is achieved by using q exponents to magnify or shrink the relative magnitudes of different parts. The joint multifractal spectra revealed many details of modelling, like the evaluation of recession process modelling. Given its versatility, the JMS analysis has great potential for its applications in hydrological modelling.
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页码:1771 / 1789
页数:19
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