百年尺度黄河流域水沙演变特征与气候-人类驱动机制解析

Centennial-scale evolution of the runoff—sediment system and its climatic and anthropogenic drivers in the Yellow River Basin

  • 摘要: 针对黄河流域百年尺度水沙演变特征认识不足及不同时间尺度驱动机理辨识不清的问题,以花园口站以上控制流域为对象,基于1919—2022年逐月径流、输沙和气候资料,构建融合Budyko水热平衡与分形弹性理论的多尺度归因框架。结果表明:百年尺度黄河流域降水呈显著增加趋势(0.31 mm/a,p<0.01),而径流和输沙均显著减少(− 2.35亿m3/a和 − 0.16亿t/a,p<0.01),水沙系统表现出明显非稳态特征;水沙演变具有显著多尺度非同步性,年代尺度上变化时序、幅度和方向存在差异,年内尺度上2000年后水沙分配由“汛期集中”向“全年均化”转变;人类活动是百年尺度水沙变化的主导因素,对径流和输沙减少的贡献率分别为73.2%和81.4%,减沙效应强于减流效应;水沙归因具有显著时间尺度依赖性,汛期及强干扰阶段以人类活动主导,而非汛期及部分年代转换阶段气候变化作用相对占优。黄河流域百年尺度水沙系统已由以气候波动驱动为主转向以人为调控主导的非稳态演化阶段。

     

    Abstract: To address the insufficient understanding of centennial-scale water—sediment evolutionary characteristics in the Yellow River Basin and the ambiguous identification of driving mechanisms across different temporal scales, the drainage area upstream of the Huayuankou Station is taken as the research object in this study. Based on monthly runoff, sediment transport and climatic datasets from 1919 to 2022, a multi-scale attribution framework coupling the Budyko hydrothermal balance principle and fractal elasticity theory is constructed. The analysis results show that over the centennial timescale, the annual precipitation in the Yellow River Basin exhibits a statistically significant increasing trend (0.31mm/a, p<0.01), while both runoff and sediment transport decrease markedly (−2.35×108m3/a and −0.16×108t/a, p<0.01), with the water—sediment coupled system exhibiting prominent non-stationary properties. Water and sediment evolution feature notable multi-scale asynchronous variations: decadal changes differ greatly in timing, amplitude, and trajectory; at the intra-annual scale, the seasonal allocation of water and sediment has transformed from a flood-season-concentrated pattern toward a more uniformized annual distribution since 2000. Human activities act as the predominant driver of water—sediment variations at the centennial scale, contributing 73.2% to runoff reduction and 81.4% to sediment transport reduction, and the magnitude of sediment reduction outweighs the runoff reduction. Attribution results display clear temporal scale dependence: human interference dominates water—sediment changes during flood seasons and periods with intensive human activities, while climate change exerts a relatively predominant effect in non-flood seasons and certain decadal transition stages. In general, the centennial water—sediment system of the Yellow River Basin has completed a regime shift, transitioning from an evolutionary stage mainly driven by natural climate fluctuations to a non-stationary evolutionary stage governed by human regulation.

     

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