Abstract

Accurate and consistent annual runoff prediction in a region is a hot topic in management, optimization, and monitoring of water resources. A novel prediction model (ESMD-SE-WPD-LSTM) is presented in this study. Firstly, extreme-point symmetric mode decomposition (ESMD) is used to produce several intrinsic mode functions (IMF) and a residual (Res) by decomposing the original runoff series. Secondly, sample entropy (SE) method is employed to measure the complexity of each IMF. Thirdly, wavelet packet decomposition (WPD) is adopted to further decompose the IMF with the maximum SE into several appropriate components. Then long short-term memory (LSTM) model, a deep learning algorithm based recurrent approach, is employed to predict all components. Finally, forecasting results of all components are aggregated to generate the final prediction. The proposed model, which is applied to seven annual series from different areas in China, is evaluated based on four evaluation indexes (R, MAE, MAPE and RMSE). Results indicate that ESMD-SE-WPD-LSTM outperforms other benchmark models in terms of four evaluation indexes. Hence the proposed model can provide higher accuracy and consistency for annual runoff prediction, rendering it an efficient instrument for scientific management and planning of water resources.

Highlights

  • Accurate and consistent annual runoff prediction in regions is a hot topic in the management, optimization, and monitoring of water resources

  • Long-term runoff forecasting plays a critical role in the management and monitoring of water resources

  • To attain a more accurate prediction of annual runoff, this paper presents a hybrid model for long-term runoff prediction, which couples twophase decomposition and LSTM (ESMD-sample entropy (SE)-wavelet packet decomposition (WPD)-LSTM)

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Summary

Methodology

ESMD, proposed by Wang and Li (2013), is a new adaptive data processing method and can be used to analyze a non-stationary and nonlinear signal. (4) Construct p bar differential curves, Lp (p = 1, 2, ⋯ , n) , using the obtained midpoints, and compute the mean curve by L = (L1 + ⋯ Lp )/p. (5) Repeat steps 1-4 on Y − Luntil |L| ≤ θ (θ denotes the permitted error), and the first mode M1 is obtained. (6) Repeat steps 1 to 5 on Y − M1 to obtain M2 , ⋯ , Mn and a residual (R) until (7) Change K within the interval [Kmin , Kmax ] and repeat steps 1 to 6, compute the standard variance σ of Y − R。. The original series can generate a series of intrinsic mode functions (IMF) and a residual (R)

Sample entropy
Model construction
Data description and evaluation indicators
Series decomposition
Sample entropy computation and two-phase decomposition
Number of input variables
Model development
Results and discussion
Experiment 1
Experiment 2
Experiment 3
Comparison of all involved models
Conclusion
Availability of data and materials
METHODS
METHOD

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