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    黑河上游年径流模拟模型优选与归因分析

    Optimization and attribution analysis of annual runoff simulation models in the upper reaches of the Heihe River, northwestern China

    • 摘要:
      目的 本研究旨在深入探究人类活动与气候变化对黑河上游年径流量的影响,为区域水资源保护与规划利用提供科学支持。
      方法 研究综合Mann-Kendall非参数统计检验、Pettitt检验和滑动t检验方法,对1954—2020年黑河上游年径流序列进行趋势检验,识别年径流序列趋势变化的突变点并划分基准期与分析期。在此基础上,采用BP神经网络模型、灰色时间序列模型和多元线性回归模型,模拟基准期年径流变化,优选模拟效果最佳模型,进而借助优选模型与径流变化归因方法,定量解析人类活动与气候变化要素对年径流变化的驱动规律。
      结果 趋势检验发现,年径流序列在1982年和2006年前后发生了突变,黑河上游年径流序列可划分为1954—1982年(基准期)、1982—2006年(分析期1)和2006—2020年(分析期2)3个阶段。在基准期年径流序列的模拟中,BP神经网络模型在验证期的相对误差(0.79%)、纳什效率系数(0.84)与拟合优度(0.84)3个参数上相较其他模型优势明显。借助神经网络模型进行年径流变化归因分析,发现人类活动导致年径流在1982—2020年间减少的平均值为7.56 × 108 m3。但2006—2020年间黑河上游人类活动对径流的负面贡献率较1982—2006年间减少约18.00%。详细解析气候变化对年径流量的影响,发现在2006—2020年间,降水量与蒸散发对年径流的贡献率较1954—1982年分别增加约11.00%和8.00%。
      结论 BP神经网络模型对于黑河上游年径流序列模拟有较好效果,模拟合格率达94.23%,最大误差仅为1.36%;黑河流域上游年径流量序列在1982年和2006年发生了趋势突变,1982年后人类活动强度增大导致上游年径流量减小,2006年后黑河流域综合治理效果显现,人类活动对年径流量的负面效应减弱;1982—2020年期间的气候变化影响中,蒸散发与降水对径流的贡献分别占46.57%与53.43%。

       

      Abstract:
      Objective The primary objective of this study is to conduct an in-depth investigation into the impact of human activities and climate change on the annual runoff in the upper reaches of the Heihe River of northwestern China, with the aim of providing scientific support for regional water resource conservation and planning.
      Method This study employed a comprehensive approach involving the Mann-Kendall non-parametric statistical test, Pettitt test, and sliding t-test methods to assess the trends in the annual runoff series in the upper reaches of the Heihe River from 1954 to 2020. The objective was to identify abrupt change points in the annual runoff series and delineate the reference period and analysis period. Building upon this foundation, we employed the BP neural network model, the grey time series model, and the multivariate linear regression model to simulate the annual runoff variations during the reference period. We then selected the model with the best simulation performance. Subsequently, utilizing the selected model and runoff attribution methods, we quantitatively analyzed the driving mechanisms of human activities and climate change factors on the annual runoff variations.
      Result Trend analysis revealed that the annual runoff series experienced abrupt changes around 1982 and 2006. Consequently, the annual runoff series in the upper reaches of the Heihe River can be divided into three phases: 1954–1982 (reference period), 1982–2006 (analysis period 1), and 2006–2020 (analysis period 2). In the simulation of the annual runoff series during the reference period, the BP neural network model exhibited a clear advantage over the other two models in three parameters during the validation period: relative error (0.79%), Nash-Sutcliffe efficiency coefficient (0.84), and goodness of fit (0.84). Utilizing the neural network model for annual runoff attribution analysis, it was determined that human activities led to an average decrease of 7.56 × 108 m3 in annual runoff between 1982 and 2020. However, during the period of 2006 to 2020, the adverse contribution of human activities in the upper reaches of the Heihe River to runoff decreased by approximately 18.00% compared with the period from 1982 to 2006. A detailed analysis of the impact of climate change on annual runoff revealed that between 2006 and 2020, precipitation and evapotranspiration contributed approximately 11.00% and 8.00% more, respectively, to annual runoff compared with the period from 1954 to 1982.
      Conclusion The BP neural network model demonstrates a strong performance in simulating the annual runoff series of the upper reaches of the Heihe River, achieving a simulation accuracy of 94.23% with a maximum error of only 1.36%. The annual runoff series in the upper Heihe River Basin exhibited trend transitions in 1982 and 2006. Increased human activities after 1982 lead to a reduction in annual runoff, while the comprehensive river basin management measures implemented after 2006 result in a mitigation of the negative impacts of human activities on annual runoff. Regarding the influence of climate change during the period from 1982 to 2020, evapotranspiration and precipitation contribute 46.57% and 53.43%, respectively to runoff.

       

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