Multifractal description of streamflow and suspended sediment concentration data from Indian river basins

被引:17
作者
Adarsh, S. [1 ]
Dharan, Drisya S. [1 ]
Nandhu, A. R. [1 ]
Vishnu, B. Anand [1 ]
Mohan, Vysakh K. [1 ]
Watorek, M. [2 ,3 ]
机构
[1] TKM Coll Engn, Kollam, Kerala, India
[2] Polish Acad Sci, Inst Nucl Phys, Complex Syst Theory Dept, Ul Radzikowskiego 152, PL-31342 Krakow, Poland
[3] Cracow Univ Technol, Fac Comp Sci & Telecommun, Ul Warszawska 24, PL-31155 Krakow, Poland
关键词
Streamflow; Multifractal; Sediment; Persistence; Correlation; DETRENDED FLUCTUATION ANALYSIS; CROSS-CORRELATION ANALYSIS; PEARL RIVER; TIME-SERIES; RAINFALL; TEMPERATURE; RECORDS; FLOWS;
D O I
10.1007/s11600-020-00407-2
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
This study investigated the multifractality of streamflow data of 192 stations located in 13 river basins in India using the multifractal detrended fluctuation analysis (MF-DFA). The streamflow datasets of different river basins displayed multifractality and long-term persistence with a mean exponent of 0.585. The streamflow records of Krishna basin displayed least persistence and that of Godavari basin displayed strongest multifractality and complexity. Subsequently, the streamflow-sediment links of five major river basins were evaluated using the novel multifractal cross-correlation analysis (MFCCA) method of cross-correlation studies. The results showed that the joint persistence of streamflow and total suspended sediments (TSS) is approximately the mean of the persistence of individual series. The streamflow displayed higher persistence than TSS in 60% of the stations while in majority of stations of Godavari basin the trend was opposite. The annual cross-correlation is higher than seasonal cross-correlation in majority of stations but at these time scales strength of their association differs with river basin.
引用
收藏
页码:519 / 535
页数:17
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