Leveraging historic streamflow and weather data with deep learning for enhanced streamflow predictions

Christiaan Schutte, M. van der Laan, B. J. van der Merwe
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Abstract

Streamflow information is crucial for effectively managing water resources. The declining number of active gauging stations in many rivers is a global concern, necessitating the need for reliable streamflow estimates. Deep learning techniques offer potential solutions, but their application in southern Africa remains largely underexplored. To fill this gap, this study evaluated the predictive performance of gated recurrent unit (GRU) and long short-term memory (LSTM) networks using two headwater catchments of the Steelpoort River, South Africa, as case studies. The model inputs included rainfall, maximum, and minimum temperature, as well as past streamflow, which was utilized in an autoregressive sense. The inclusion of streamflow in this way allowed for the incorporation of simulated streamflow values into the look-back window for predicting the streamflow of the testing set. Two modifications were required to the GRU and LSTM architectures to ensure physically consistent predictions, including a change in the activation function of the GRU/LSTM cells in the final hidden layer, and a non-negative constraint that was used in the dense layer. Models trained using commercial weather station data produced reliable streamflow estimates, while moderately accurate predictions were obtained using freely available gridded weather data.
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利用历史数据和天气数据进行深度学习,增强对流量的预测能力
溪流信息对于有效管理水资源至关重要。许多河流的有效测量站数量不断减少,这是一个全球关注的问题,因此有必要进行可靠的流量估算。深度学习技术提供了潜在的解决方案,但其在南部非洲的应用在很大程度上仍未得到充分探索。为了填补这一空白,本研究以南非钢波特河的两个上游集水区为案例,评估了门控递归单元(GRU)和长短期记忆(LSTM)网络的预测性能。模型输入包括降雨量、最高气温和最低气温,以及过去的溪流流量,并在自回归意义上加以利用。通过这种方式,可以将模拟流量值纳入预测测试集流量的回溯窗口。为了确保预测结果的物理一致性,需要对 GRU 和 LSTM 架构进行两处修改,包括改变 GRU/LSTM 单元在最终隐藏层中的激活函数,以及在密集层中使用非负约束。使用商业气象站数据训练的模型可得出可靠的流量估计值,而使用免费提供的网格气象数据则可获得中等精度的预测值。
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