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首页> 外文期刊>Journal of South American earth sciences >Geostatistical modeling and traditional approaches for streamflow regionalization in a Brazilian Southeast watershed
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Geostatistical modeling and traditional approaches for streamflow regionalization in a Brazilian Southeast watershed

机译:巴西东南部流行区流统计建模与传统方法

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Focused on supporting the planning and management of water resources in a watershed domain, this study aimed to assess and compare the performance of multiple approaches for streamflow regionalization. The applied methods were based on linear interpolation, regional regressions (RR), and kriging. The dependent variables used were low-flows of reference (Q7.10, Q95, and Q90) and the long-term mean streamflow (Qmld). The independent variables used by the RR method were drainage area, mean annual precipitation, mean precipitation in the dry and rainy seasons, besides the flow equivalent to the precipitated volume minus the 750 mm abstraction (Peq750). The RR's equations were best fitted using the potential model, and three hydrologically homogeneous regions (RHH) were identified. Meanwhile, the exponential model provided the best fit to the experimental semivariograms in the geostatistical analysis. The methodologies' performance was estimated by the following metrics: mean relative error, percent bias, root mean square error, Nash-Sutcliffe coefficient, and coefficient of determination. The evaluated methodologies had similar performance for the low-flows and long-term mean streamflow, despite the lower accuracy by using the kriging methods for the Q7.10 at the RHH III. All approaches performed better for Qmld, since it is not an extreme variable. Although all methods have shown good results, the adoption of kriging and linear interpolation must always be linked with a careful analysis of factors such as the density and spatial distribution of stream gauge stations in the watershed.
机译:专注于支持流域域中水资源的规划和管理,本研究旨在评估和比较流流程区域化的多种方法的性能。应用方法基于线性插值,区域回归(RR)和Kriging。所使用的依赖变量是低流程(Q7.10,Q95和Q90),并且长期平均流流(QMLD)。 RR方法使用的独立变量是排水区,平均降水,干燥和雨季中的平均沉淀,除了相当于沉淀体积减去750 mm抽象(PEQ750)的流量。使用潜在模型最适合RR等式,并确定三个水文均匀区域(RHH)。同时,指数模型为地质统计分析中的实验半造型函数提供了最佳拟合。方法估计了以下度量:均值相对误差,偏差百分比,均匀平方误差,纳什 - Sutcliffe系数和确定系数。尽管通过在RHH III下使用Q7.10的Q7.10的克里明方法,所评估的方法具有类似的低流量和长期平均流流的性能。所有方法对于QMLD来说更好,因为它不是一个极端变量。虽然所有方法都显示出良好的结果,但必须始终将Kriging和线性插值的采用仔细分析流域中流量表电台的密度和空间分布等因素的仔细分析。

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