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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Evaluation of the WEPP model and digital elevation grid size, for simulation of streamflow and sediment yield in a heterogeneous catchment
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Evaluation of the WEPP model and digital elevation grid size, for simulation of streamflow and sediment yield in a heterogeneous catchment

机译:评估WEPP模型和数字高程网格大小,以模拟非均质流域的水流和沉积物产量

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The paper presents the result of an application of the GeoWEPP model in a heterogeneous semi-agricultural catchment located in the northern Italian Apennines mountain range. The objectives were: (a) to evaluate the GeoWEPP model in a heterogeneous catchment in a Mediterranean climate and (b) to examine the effect of digital elevation model grid size on hydrological and sediment yield simulations. The catchment is characterized by large heterogeneity in geology, soil type, vegetation cover and topography. In addition, 10% of its area is occupied by calanchi (badlands), characterized by steep, bare soil and accentuated erosion. Experimental streamflow data were compared with those simulated by GeoWEPP for a period of eight years and the results were evaluated by means of statistical indices, with the analysis of the flow duration curve. Simulated sediment yields were compared with experimental data for one year. The streamflow cumulative annual results were satisfactory with NSE oscillating between 0.40 and 0.83 and RMSE between 1.1 and 2.9 mm. Also, the performance of the model with daily streamflow data was positive (NSE = 0.68 and RMSE = 1.9 mm). The flow duration curve indicated that GeoWEPP could represent the experimental streamflow for fluxes over 1mm d~(-1). The model performance for simulation of sediment yield was satisfactory with both digital elevation models of different grid sizes (NSE = 0.84 and 0.87). Indeed, the sensitivity analysis tests of the model showed that there was no statistically significant improvement in the accuracy of the digital elevation model between 10 and 2m resolution. These results were confirmed for both streamflow as well as sediment yield. Additional sensitivity analysis of other model parameters performed on the entire catchment and badlands hillslopes showed that bedrock hydraulic conductivity primarily affected the model in both settings.
机译:本文介绍了在意大利北部亚平宁山脉的异质半农业流域应用GeoWEPP模型的结果。目的是:(a)在地中海气候的非均质流域中评估GeoWEPP模型,以及(b)检查数字高程模型网格大小对水文和沉积物产量模拟的影响。流域的特点是地质,土壤类型,植被覆盖和地形的异质性很大。另外,其面积的10%被荒地(荒地)占据,其特征是陡峭,裸露的土壤和加剧的侵蚀。将实验流量数据与GeoWEPP模拟的数据进行了为期八年的比较,并通过统计指标评估了结果,并分析了流量持续时间曲线。将模拟的沉积物产量与一年的实验数据进行了比较。 NSE在0.40至0.83之间波动,RMSE在1.1至2.9 mm之间波动,流量累计年度结果令人满意。此外,该模型的每日流量数据的性能为正(NSE = 0.68,RMSE = 1.9 mm)。流量持续时间曲线表明,GeoWEPP可以代表流量大于1mm d〜(-1)的实验流量。在不同网格大小的两个数字高程模型(NSE = 0.84和0.87)下,模拟沉积物产量的模型性能令人满意。实际上,该模型的灵敏度分析测试表明,在10m至2m分辨率之间,数字高程模型的准确性没有统计学上的显着提高。流量和泥沙产量均得到了这些结果的证实。在整个集水区和荒地山坡上对其他模型参数进行的其他敏感性分析表明,在两种环境下,基岩的水力传导率都主要影响模型。

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