A coupled model of nonlinear dynamical system and deep learning for multi-step ahead daily runoff prediction for data scarce regions

被引:0
|
作者
Qian, Longxia [1 ,2 ]
Hu, Wei [1 ]
Zhao, Yong [3 ]
Hong, Mei [4 ]
Fan, Linlin [5 ]
机构
[1] Nanjing Univ Posts & Telecommun, Sch Sci, Nanjing 210023, Peoples R China
[2] China Meteorol Adm, Key Lab High Impact Weather Special, Changsha 410073, Peoples R China
[3] Minist Water Resources, Key Lab Water Safety Beijing Tianjin Hebei Reg, Beijing 100038, Peoples R China
[4] Natl Univ Def Technol, Coll Meteorol & Oceanog, Changsha 410073, Peoples R China
[5] Changjiang River Sci Res Inst, Agr Water Conservancy Dept, Wuhan 430010, Peoples R China
基金
中国国家自然科学基金;
关键词
Data scarce regions; Multi-step ahead forecasting; Nonlinear dynamics; Spatiotemporal information fusion; Attention mechanism; ARTIFICIAL NEURAL-NETWORK; RIVER FLOW;
D O I
10.1016/j.jhydrol.2024.132640
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Multi-step ahead streamflow forecasting is crucial for effective water resources planning and management in data scarce regions. This paper develops a coupled model named CNN-LSTM-Self-attention-Anticipated Learning Machine (CLS-ALM), which is based on nonlinear dynamical systems and deep learning techniques. First, the CLS-ALM model establishes a learnable parameter to effectively concatenate and fuse feature vectors by the Convolutional Neural Networks-Long Short-Term Memory (CNN-LSTM) module and the transformer module. Second, the model generates sampled nondelay attractors for high-dimensional feature vectors. ALM learns the mapping from sampled nondelay attractors of high-dimensional feature vectors to the delay attractor of the target variable. This process is referred to as the spatial-temporal information-transformation (STI) equation. This allows for the extension of target variable in the temporal dimension and the completion of predictions. Third, the model extends one-day-ahead forecasting to multi-day-ahead forecasting. For one-day-ahead prediction, at the four stations of USGS 01013500, USGS 01031500, USGS 01047000, and USGS 01030500, the R-value of CLS-ALM exceeds 0.9, especially at the USGS 01013500 station, where its R-value exceeds 0.98. When the number of training samples is 700, and the lead-time is 3 days, the NSE value of CLS-ALM is 393.88 %, 55.44%, and 181.63% higher than that of ALM, CL-S, and CL, respectively. When the lead-time is 5 days, the NSE value of CLS-ALM is 306.45 %, 304.77 %, and 1162.37 % higher than that of ALM, CL-S, and CL, respectively. At the USGS 01030500 station, when the lead-time is 7 days, the R value of CLS-ALM is 3.55 %, 25.06 %, and 6.64 % higher than that of ALM, CL-S, and CL, respectively. Therefore, the CLS-ALM can adeptly integrate and harnesses the spatiotemporal information embedded in short-term high-dimensional data, mitigating the constraints imposed by the limited sample length.
引用
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页数:23
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