Enhancing long short-term memory (LSTM)-based streamflow prediction with a spatially distributed approach

Qiutong Yu, B. Tolson, Hongren Shen, Ming Han, Juliane Mai, Jimmy Lin
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Abstract

Abstract. Deep learning (DL) algorithms have previously demonstrated their effectiveness in streamflow prediction. However, in hydrological time series modelling, the performance of existing DL methods is often bound by limited spatial information, as these data-driven models are typically trained with lumped (spatially aggregated) input data. In this study, we propose a hybrid approach, namely the Spatially Recursive (SR) model, that integrates a lumped long short-term memory (LSTM) network seamlessly with a physics-based hydrological routing simulation for enhanced streamflow prediction. The lumped LSTM was trained on the basin-averaged meteorological and hydrological variables derived from 141 gauged basins located in the Great Lakes region of North America. The SR model involves applying the trained LSTM at the subbasin scale for local streamflow predictions which are then translated to the basin outlet by the hydrological routing model. We evaluated the efficacy of the SR model with respect to predicting streamflow at 224 gauged stations across the Great Lakes region and compared its performance to that of the standalone lumped LSTM model. The results indicate that the SR model achieved performance levels on par with the lumped LSTM in basins used for training the LSTM. Additionally, the SR model was able to predict streamflow more accurately on large basins (e.g., drainage area greater than 2000 km2), underscoring the substantial information loss associated with basin-wise feature aggregation. Furthermore, the SR model outperformed the lumped LSTM when applied to basins that were not part of the LSTM training (i.e., pseudo-ungauged basins). The implication of this study is that the lumped LSTM predictions, especially in large basins and ungauged basins, can be reliably improved by considering spatial heterogeneity at finer resolution via the SR model.
利用空间分布式方法加强基于长短期记忆(LSTM)的河水流量预测
摘要深度学习(DL)算法之前已证明了其在水流预测方面的有效性。然而,在水文时间序列建模中,现有的深度学习方法的性能往往受到有限空间信息的限制,因为这些数据驱动模型通常是用块状(空间聚合)输入数据进行训练的。在本研究中,我们提出了一种混合方法,即空间递归(SR)模型,它将整块长短期记忆(LSTM)网络与基于物理的水文路由模拟无缝集成,以增强对河水流量的预测。整块 LSTM 是根据北美五大湖区 141 个测量流域的流域平均气象和水文变量进行训练的。SR 模型包括在子流域尺度上应用训练有素的 LSTM 进行当地河水流量预测,然后由水文路由模型将其转换到流域出口。我们评估了 SR 模型在预测五大湖区 224 个测站流量方面的功效,并将其性能与独立的整块 LSTM 模型进行了比较。结果表明,在用于训练 LSTM 的流域中,SR 模型达到了与 LSTM 相同的性能水平。此外,SR 模型还能更准确地预测大型流域(例如,流域面积大于 2000 平方公里)的溪流,这说明流域特征聚合会造成大量信息损失。此外,当 SR 模型应用于不属于 LSTM 训练的流域(即伪无测站流域)时,其性能优于 LSTM。这项研究的意义在于,通过 SR 模型在更精细的分辨率上考虑空间异质性,可以可靠地改进 LSTM 的预测结果,尤其是在大型盆地和无测井盆地。
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