基于机器学习的气候变化下大型水库水温结构预测
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1.河海大学水利水电学院;2.河海大学环境学院

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国家重点研发计划(2024YFC3214600),国家自然科学基金(52379061)


Research on Predicting Water Temperature Structure in Large Reservoirs Under Climate Change Using Machine Learning
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State Key Laboratory of Water Cycle and Water Security, Hohai University

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    摘要:

    为克服纯数据驱动模型缺乏物理约束的局限性,实现传统水库水温模型在未来气候非平稳情景下的快速预测,本文提出一种融合物理机制与数据驱动的水库水温结构预测框架。基于三板溪水库2007-2016年实测资料,结合一维水动力-水温GLM模型、RF-BILSTM机器学习模型、全球气候模型GCMs,反演了三板溪水库历史水温结构,预测了未来气候情境下2023-2100年水温结构演变情势。研究结果表明:(1)基于一维水动力-水温GLM模型和实测数据,生成物理约束下的训练数据集,克服了纯数据驱动模型在缺乏物理机制时的伪关联问题, RF-BILSTM水温预测框架的模拟精度R2>0.9。(2)基于全球气候模型GCMs,表明三板溪水库未来气温呈现显著的上升趋势(p < 0.01),SSP5-8.5情景下的气温升高幅度远大于SSP2-4.5情景,而降水呈显著增加趋势。(3)至2100年,在SSP2-4.5和SSP5-8.5情境下,三板溪水库平均水温预计分别上升0.39和0.87℃,且呈现明显的垂向差异性:表层升温更显著,预计分别上升0.94和2.04℃,年均表底温差分别上升1.32和1.55℃,最大垂向温差都发生在8月。年均水体稳定度St分别增加643.41J/m2(+7.85%)和1829.47J/m2(+22.31%),水温分层加剧,可增加表层水华和营养盐层化富集的风险,提前下游鱼类产卵时间。本文提出了物理机制和数据驱动深度融合新思路,为水库水温管理提供了技术支撑。

    Abstract:

    To address the limitations of data-driven model, which lack physical constraints, and to enable rapid prediction of reservoir thermal structure under future non-stationary climate scenarios, this study proposes a hybrid framework that integrates physical mechanisms with data-driven modeling for predicting reservoir water temperature profiles. Utilizing observed data from the Sanbanxi Reservoir (2007-2016), a one-dimensional hydrodynamic-water temperature model (GLM), a Random Forest-Bidirectional Long Short-Term Memory (RF-BILSTM) machine learning model, and Global Climate Models (GCMs), we reconstructed the historical thermal structure of the reservoir and projected its evolution under future climate scenarios from 2023 to 2100. The results indicate that: (1) A physically constrained training data set generated by combining the GLM model with measured data effectively mitigates spurious correlations inherent in purely data-driven approaches. The RF-BILSTM prediction framework achieved high simulation accuracy, with R2> 0.9. (2) Projections from GCMs show a significant increasing trend in future air temperature at the Sanbanxi Reservoir (p < 0.01). The temperature increase under the SSP5-8.5 scenario is substantially greater than under SSP2-4.5, while precipitation also exhibits a significant upward trend. (3) By 2100, the average water temperature in the reservoir is projected to rise by 0.39 ℃ and 0.87 ℃ under the SSP2-4.5 and SSP5-8.5 scenarios, respectively, showing pronounced vertical differentiation. Surface warming is more significant, with projected increases of 0.94℃ and 2.04℃, respectively. The annual mean surface-bottom temperature difference is expected to increase by 1.32℃ and 1.55℃, with the maximum vertical difference occurring in August. Annual water column stability (Schmidt stability, St) is projected to increase by 643.41 J/m2(+7.85%) and 1829.47 J/m2(+22.31%), respectively, indicating intensified thermal stratification. This could elevate the risks of surface algal blooms and nutrient stratification enrichment, while also advancing the spawning timing of downstream fish. This study presents a novel approach that deeply integrates physical mechanisms with data-driven techniques, providing technical support for reservoir water temperature management.

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  • 收稿日期:2025-10-19
  • 最后修改日期:2025-12-29
  • 录用日期:2026-01-04
  • 在线发布日期: 2026-05-08
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