青藏高原湖泊表层水温的非线性协同驱动机制:基于深度学习+SHAP融合分析框架OA
Nonlinear synergistic driving mechanisms of surface water temperature in lakes on the Tibetan Plateau:A Deep Learning+SHAP integrated analytical framework
青藏高原是全球气候变化敏感区,其高海拔湖泊表层水温(LSWT)的演变对区域生态安全具有重要指示意义.在探究影响湖泊水温变化的因素时,相关研究普遍涉及气象条件、地形地貌等多种影响因子.然而,传统方法对多因子非线性交互效应的定量解析能力有限.本研究以青藏高原106个大中型湖泊为对象,构建基于长短期记忆网络(LSTM)的深度学习模型,结合SHAP(SHapley Additive exPlanation)可解释性方法,分别从整体与个体湖泊尺度上,定量分析了气温、降水、向下长波辐射、向下短波辐射、气压、比湿和风速7项因子对LSWT的影响.具体而言,研究系统解析了各驱动因子的独立作用效应、因子间的交互作用效应,以及这些效应在不同湖泊间的差异性,进而揭示了LSWT变化的驱动机制及其协同作用模式.结果表明:(1)向下长波辐射和向下短波辐射是LSWT的主导驱动因子,在整体与个体尺度的贡献度分别位列前两位(全局SHAP值占比>80%),且与LSWT呈显著正相关;气温、比湿次之,气压、降水和风速影响最小.(2)因子间交互效应普遍存在,识别出4类主导协同驱动模式:线型(如向下长波辐射—气温,67.92%湖泊)、倒U型(如比湿—气温,51.89%湖泊)、效应交叉型(如风速—比湿,70.75%湖泊)及阈值约束型(如降水—气压,100%湖泊).(3)SHAP方法有效量化了协同驱动的非线性特征,揭示了高原湖泊对辐射因子的高度敏感性,归因于稀薄大气下太阳辐射的高渗透性.本研究创新性地融合深度学习与可解释性分析,为高海拔湖泊水温的复杂驱动机制提供了定量化解析框架,对预测气候变化背景下的水温响应及制定差异化调控策略具有重要科学意义.
The Tibetan Plateau,a region highly sensitive to global climate change,exhibits significant evolution in lake surface wa-ter temperature(LSWT),which has profound implications for regional ecological security.Investigations into the drivers of LSWT changes involve multiple factors,including meteorological conditions and topographic features.However,conventional approaches possess limited capability to quantitatively resolve nonlinear interactions among these drivers.This study examined 106 large and medium-sized lakes across the Tibetan Plateau,employing a deep learning model based on long short-term memory(LSTM)net-works combined with SHapley Additive exPlanation(SHAP)interpretability analysis.This framework quantitatively disentangles the individual and interactive contributions of seven drivers-air temperature,precipitation,downward longwave radiation,down-ward shortwave radiation,air pressure,specific humidity,and wind speed-to LSWT variations at both regional and individual lake scales,thereby systematically elucidating driving mechanisms and synergistic patterns.Key findings include:(1)Longwave and shortwave radiation were identified as the dominant drivers,collectively accounting for over 80.0%of global SHAP values across scales and showing strong positive correlations with LSWT.Air temperature and specific humidity exerted secondary influ-ences,whereas precipitation and wind speed had minimal effects.(2)Widespread interactive effects revealed four primary syner-gistic modes:a linear pattern(e.g.,downward longwave radiation and air temperature,affecting 67.92%of lakes),an inverted U-shape pattern(e.g.,specific humidity and air temperature,51.89%of lakes),an effect cross-driven pattern(e.g.,wind speed and specific humidity,70.75%of lakes),and a threshold-constrained pattern(e.g.,precipitation and air pressure,100%of lakes).(3)The SHAP methodology effectively quantified nonlinear synergistic behaviors,highlighting the heightened sensitivi-ty of plateau lakes to radiative factors due to high solar radiation permeability under thin atmospheric conditions.This study innova-tively integrates deep learning with interpretability analysis to establish a quantitative framework for unraveling complex driving mechanisms behind high-altitude LSWT dynamics.The results offer critical insights for predicting thermal responses under ongoing climate change and for developing differentiated management strategies,thereby holding substantial scientific and practical rele-vance.
石海韵;祁毅;李婉宁;沈吉;倪天华
南京大学地理与海洋科学学院,南京 210023南京大学建筑与城市规划学院,南京 210023南京大学地理与海洋科学学院,南京 210023南京大学地理与海洋科学学院,南京 210023南京大学地理与海洋科学学院,南京 210023
湖泊表层水温深度学习SHAP可解释性协同驱动机制阈值效应青藏高原
Lake surface water temperaturedeep learningSHapley Additive exPlanationsynergistic driving mechanismsthreshold effectsTibetan Plateau
《湖泊科学》 2026 (2)
842-856,15
国家自然科学基金项目(42230507)资助.
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