Abstract

Accurate estimation of water table depth dynamics is essential for water resource management, especially in areas where groundwater is overexploited. In recent years, as a data-driven model, artificial neural networks (NNs) have been widely used in hydrological modeling. However, due to the non-stationarity of water table depth data, the performance of NNs in areas of over-exploitation is challenging. Therefore, reducing data noise is an essential step before simulating the water table depth. This research proposed a novel method to model the non-stationary time series data of water table depth through combing the advantages of wavelet analysis and Long Short-Term Memory (LSTM) neural network (NN). A typical groundwater over-exploitation area, Baoding, North China Plain (NCP), was selected as a study area. To reflect the impact of anthropogenic activities, the variables harnessed to develop the model includes temperature, precipitation, evaporation, and some socio-economic data. The results show that decomposing the time series of the water table depth into three sub-temporal components by Meyer wavelets can significantly improve the simulation effect of LSTM on the water table depth. The average NSE (Nash-Sutcliffe efficiency coefficient) value of all the sites increased from 0.432 to 0.819. Additionally, a feedforward neural network (FNN) is used to compare forecasts over 12-months. As expected, wavelet-LSTM outperforms wavelet-FNN. As the prediction time increases, the advantages of wavelet-LSTM become more evident. The wavelet-LSTM is satisfactory for forecasting the water table depth at most in 6 months. Furthermore, the importance of input variables of wavelet-LSTM is analysed by the weights of the model. The results indicate that anthropogenic activities influence the water table depth significantly, especially in the sites close to the Baiyangdian Lake, the largest lake in the North China Plain. This study demonstrates that the wavelet-LSTM model provides an option for water table depth simulation and predicting areas of over-exploitation of groundwater.

Highlights

  • Groundwater, an important water resource, is being overexploited due to the rapid population growth and economy, especially in arid and semi-arid areas

  • This study focuses on combing wavelet analysis with neural networks (NNs) to establish a novel data-driven model for non-stationary time series data of water tables in areas of over-exploitation

  • It may be due to the fact that the water table depth near the lake is strongly affected by the lake

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Summary

Introduction

Groundwater, an important water resource, is being overexploited due to the rapid population growth and economy, especially in arid and semi-arid areas. Physical models, such as MODFLOW (Modular Ground-Water Flow Model) (Xu et al, 2012; Lachaal et al, 2012; Xiang et al, 2020), HYDRUS (Huang et al, 2016), GMS (Groundwater Modeling System) (Roy et al, 2015), have been widely used in groundwater resources evaluation and management. Xiang et al (2020) evaluated the balance between groundwater protection with crop production based on the results of MODFLOW combined with DSSAT (Decision Support System for Agrotechnology Transfer). Maihemuti et al (2021) employed HYDRUS to evaluate the effects of groundwater on plant distribution. These physical models usually require boundary conditions and a large number of hydraulic parameters for calibration. When hydrogeological data is lacking, the data-driven model based on NNs shows advantages

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