Author
Listed:
- Shanghong Zhang
(School of Water Resources and Hydropower Engineering, North China Electric Power University, Beijing 102206, China)
- Hao Wang
(School of Water Resources and Hydropower Engineering, North China Electric Power University, Beijing 102206, China)
- Ruicheng Zhang
(School of Water Resources and Hydropower Engineering, North China Electric Power University, Beijing 102206, China)
- Hua Zhang
(School of Water Resources and Hydropower Engineering, North China Electric Power University, Beijing 102206, China)
- Yang Zhou
(School of Water Resources and Hydropower Engineering, North China Electric Power University, Beijing 102206, China)
Abstract
Hydrothermal conditions are a key indicator influencing the evolution of aquatic ecosystems, closely affecting the physical, chemical, and biological properties of water bodies. The construction of cascaded dams on the main stem of the Yangtze River has altered the natural water temperature regime, impacting the hydrothermal status of the water. Utilizing multi-source remote sensing data from Google Earth Engine to invert river surface water temperatures, a parameter-optimized CNN-LSTM-Attention hybrid interpretable water temperature prediction model was constructed. The model demonstrated credible accuracy. Based on the inversion results, the study revealed the spatiotemporal evolution characteristics of water temperature in the main stem of the Yangtze River before and after cascaded dam construction in the lower Jinsha River region and the Three Gorges Reservoir area. The results found that after the construction of the Three Gorges Dam, the annual average water temperature increased significantly by 0.813 °C. The “cold water stagnation effect” induced by cascaded development caused the water temperature amplitude to increase from 8.96 °C to 10.6 °C. Furthermore, the regulating effect of tributary confluence exhibited significant differences. For instance, colder tributaries like the Yalong River reduced the main stem water temperature, while warmer tributaries like the Jialing River, conversely, increased the main stem temperature. The construction of cascaded dams led to distinct variation characteristics in the areas downstream of the dams within the reservoir regions, where tributary inflows caused corresponding changes in the main stem water temperature. This study elucidates the long-term spatiotemporal variation characteristics of water temperature in the main stem of the Yangtze River. The model prediction results can assist in constructing an early warning indicator system for water temperature changes, providing reliable data support for promoting water environment sustainability and ecological civilization construction in the river basin.
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References listed on IDEAS
- Tong Liu & Xudong Cui & Li Mo, 2025.
"A Daily Runoff Prediction Model for the Yangtze River Basin Based on an Improved Generative Adversarial Network,"
Sustainability, MDPI, vol. 17(7), pages 1-28, March.
- Tianfu He & Yun Deng & Youcai Tuo & Yanjing Yang & Naisheng Liang, 2020.
"Impact of the Dam Construction on the Downstream Thermal Conditions of the Yangtze River,"
IJERPH, MDPI, vol. 17(8), pages 1-14, April.
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