Simulation and forecasting of streamflows using machine learning models coupled with base flow separation

被引:195
作者
Tongal, Hakan [1 ]
Booij, Martijn J. [2 ]
机构
[1] Suleyman Demirel Univ, Engn Fac, Dept Civil Engn, TR-32260 Isparta, Turkey
[2] Univ Twente, Fac Engn Technol, Dept Water Engn & Management, Enschede, Netherlands
关键词
Simulation; Forecasting; Base flow separation; Support vector regression; Artificial neural networks; Random forest; ARTIFICIAL NEURAL-NETWORK; SUPPORT VECTOR REGRESSION; RAINFALL-RUNOFF MODEL; SINGULAR-SPECTRUM ANALYSIS; TIME-SERIES PREDICTION; 3 MOUNTAINOUS BASINS; CLIMATE-CHANGE; RIVER-BASIN; WAVELET TRANSFORM; HYBRID APPROACH;
D O I
10.1016/j.jhydrol.2018.07.004
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Efficient simulation of rainfall-runoff relationships is one of the most complex problems owing to the high number of interrelated hydrological processes. It is well-known that machine learning models could fail in simulating streamflows from only meteorological variables in the absence of antecedent streamflow values. The main reason for this could be low and lagged relationships between streamflow and meteorological variables. To overcome this inefficiency, for the first time, we developed a simulation framework by coupling a base flow separation method to three machine learning methods. It was demonstrated that separating streamflow into different components such as base flow and surface flow can be useful for improving simulation and forecasting capabilities of machine learning models. We simulated streamflow in four rivers in the United States with Support Vector Regression (SVR), Artificial Neural Networks (ANNs) and Random Forest (RF) as a function of precipitation (P), temperature (T) and potential evapotranspiration (PET). We concluded that the base flow separation method improved the simulation performances of the machine learning models to a certain degree. Apart from the simulation scheme, we also employed a forecasting scheme by using the antecedent observed discharge values in addition to P, T, and PET. We discussed performances of models in simulation and forecasting of streamflow regarding model types, input structures and catchment dynamics in detail.
引用
收藏
页码:266 / 282
页数:17
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