4.7 Article

A dynamic classification-based long short-term memory network model for daily streamflow forecasting in different climate regions

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ECOLOGICAL INDICATORS
卷 148, 期 -, 页码 -

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ELSEVIER
DOI: 10.1016/j.ecolind.2023.110092

关键词

Dynamic classification; Long short-term memory networks; Streamflow forecasting; Box-Cox method

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Daily streamflow forecasting is crucial for ecological processes, stream ecology, and decision-making. This study proposes an integrated modelling approach that combines a dynamic classification method with LSTM models to improve streamflow forecasting considering different flow regimes. The performance of these models is compared to traditional LSTM models using data from 8 stations in different climate regions. Results indicate that the proposed models outperform traditional LSTM models, with the DC-B-LSTM model performing better in arid areas.
Daily streamflow forecasting is a major determinant of ecological processes in running waters, healthy stream ecology and surrounding environment, and accurate streamflow forecasting provides a powerful foundation for ecological assessment, management, and decision-making. Recently, data-driven models for different flow re-gimes have shown excellent potential in streamflow forecasting. However, the boundaries between different flow regimes were selected arbitrarily without considering the changes in boundaries that often occur over time in the real world. Therefore, in this paper, an integrated modelling approach that couples a dynamic classification method with a long short-term memory networks (LSTM) model without data transformation (the DC-LSTM model) and an LSTM with Box-Cox data transformation (the DC-B-LSTM model) is developed to improve the performance of streamflow forecasting considering different flow regimes. The boundaries of dynamic classifi-cation are dynamic changing interval values of related hydrological variables improved from traditional clas-sification method just using static single-variable threshold, so dynamic classification can more fully explore the relationship and information of hydrological data. The performance of both the DC-LSTM and DC-B-LSTM models is compared to that of the LSTM model without data classification (the traditional LSTM model) and with data classification using a traditional static method (the C-LSTM model) based on data from 8 stations within 4 river basins in different climate regions in the United States. The results show that both the DC-LSTM and DC-B-LSTM models out-perform the traditional LSTM models (with or without static data classification) for all river basins considered. Furthermore, the DC-B-LSTM model displays better performance than the DC-LSTM model in arid areas.

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