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Reconstruction of missing groundwater level data by using Long Short-Term Memory (LSTM) deep neural network

机译:使用长短期内存(LSTM)深神经网络重建缺失的地下水位数据

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Monitoring groundwater level (GWL) over long time periods is critical in understanding the variability of groundwater resources in the present context of global changes. However, in Normandy (France) for example, GWLs have only been systematically monitored for similar to 20 to 50 years. This study evaluates Long Short-Term Memory (LSTM) neural network modeling to reconstruct GWLs, fill gaps and extend existing time-series. The approach is illustrated by using available monitoring fluctuations in piezometers implanted in the chalk aquifer in the Normandy region, Northern France. Here GWL data recorded over 50 years at 31 piezometers in northwestern Normandy is employed to perform GWL prediction. To optimize the network performance, the most influential factors that impact the accuracy of prediction are first determined, such as the network architecture, data quantity and quality. The resulting network is adopted to reconstruct measurements in the piezometers step by step with an increment of missing observation time. The approach requires no calibration for the time-lag in data processing and the implementation relies only on the groundwater level fluctuations to retrieve missing data in the targeted piezometers.
机译:长期监测地下水位(GWL)对于理解当前全球变化背景下地下水资源的可变性至关重要。然而,以诺曼底(法国)为例,GWL只被系统监测了20到50年。本研究评估了长短时记忆(LSTM)神经网络模型,以重建GWL,填补空白并扩展现有的时间序列。该方法通过在法国北部诺曼底地区白垩含水层中植入测压计的可用监测波动来说明。本文利用诺曼底西北部31个测压计50年来记录的GWL数据进行GWL预测。为了优化网络性能,首先确定影响预测精度的最主要因素,如网络结构、数据量和质量。所得到的网络被用于以缺失观测时间的增量逐步重建测压计中的测量值。该方法不需要对数据处理中的时间延迟进行校准,实施过程仅依靠地下水位波动来检索目标测压计中缺失的数据。

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