Downstream Water Level Prediction of Reservoir based on Convolutional Neural Network and Long Short-Term Memory Network
Publication: Journal of Water Resources Planning and Management
Volume 147, Issue 9
Abstract
Accurate calculation of power generation output is crucial to the operation and management of reservoir. The calculation of power generation output is related to the downstream water level, which usually is obtained by interpolation of discharge flow. However, the interpolation method has a large error and adversely affects the output calculation, especially for medium and low water head reservoirs. This study explored the relevant factors of the downstream water level and accurately predicted it from historical operational data. The maximal information coefficient and feature combination were used to select feature inputs, and a deep neural network was designed based on a convolutional neural network and a long short-term memory network to predict the downstream water level of a reservoir. To verify the performance of designed model, it was compared with the interpolation method and 4 state-of-the-art prediction methods using 12 validation sets of Gezhouba Reservoir. The experimental results showed that downstream water level obtained by the designed model was closer to the actual water level than was the interpolated water level. Compared with four state-of-the-art prediction methods, the designed method also was very competitive. Finally, the influence of CNNLSTM on power generation output is compared with traditional interpolation method. The comparison results showed that the convolutional neural network–long short-term memory network method reduced the influence of the interpolation method by 92.74% on average.
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Data Availability Statement
Some or all data, models, or code that support the findings of this study are available from the corresponding author upon reasonable request, including the code and model for the downstream water level prediction in the study, and the historical downstream water level data of Gezhouba in 2017.
Acknowledgments
This work is supported by the National Natural Science Foundation of China (Nos. 51979113, U1865202, 51709119, and 51809098) and the National Public Research Institutes for Basic R & D Operating Expenses Special Project (CKSF2017061/SZ) Special thanks are given to the anonymous reviewers and editors for their constructive comments.
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Received: Aug 13, 2020
Accepted: Mar 31, 2021
Published online: Jul 15, 2021
Published in print: Sep 1, 2021
Discussion open until: Dec 15, 2021
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