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首页> 外文期刊>Environmental earth sciences >The application of the Water Erosion Prediction Project (WEPP) model for the estimation of runoff and sediment on a monthly time resolution
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The application of the Water Erosion Prediction Project (WEPP) model for the estimation of runoff and sediment on a monthly time resolution

机译:水蚀预测项目(WEPP)模型在月度分辨率下用于径流和泥沙估算的应用

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The Water Erosion Prediction Project (WEPP) model is utilized to simulate the sediment and runoff processes. According to previous studies, WEPP model provides impressive results in watersheds of diverse climates and scales. It is also capable of modeling the sediment transportation processes and consequently predicting subsequent deposition sites. In this study, the geo-spatial interface for WEPP (GeoWEPP) was employed as a GIS framework to extract the data required from the ASTER Global Digital Elevation Model (ASTER-GDEM) dataset which was subsequently used as the model input. The case study was based on monthly data consisting of average sediment and runoff estimation from the Emameh sub-basin, in northern Iran. The model estimations were validated through field measurements. Two statistical measures of co-efficiency including the Nash-Sutcliffe Efficiency (NSE), and the coefficient of determination (R-2) were considered to evaluate how well the model predictions could explain the variability of observations in the field. The model performed favorably as corroborated by a reasonably high NSE of 0.99 and an R-2 value of 0.92 for sediment. In the case of runoff, the results were slightly inferior, but still acceptable with an NSE of 0.76 and R-2 value of 0.62.
机译:水蚀预测项目(WEPP)模型用于模拟沉积物和径流过程。根据以前的研究,WEPP模型在不同气候和规模的流域中提供了令人印象深刻的结果。它还能够对沉积物的输送过程进行建模,从而预测随后的沉积位置。在这项研究中,WEPP的地理空间接口(GeoWEPP)被用作GIS框架,以从ASTER全球数字高程模型(ASTER-GDEM)数据集中提取所需的数据,随后将其用作模型输入。该案例研究基于每月数据,包括伊朗北部Emameh子流域的平均沉积物和径流估算。通过现场测量验证了模型估计。考虑了两个联合效率的统计量度,包括纳什-萨克利夫效率(Nash-Sutcliffe效率)(NSE)和确定系数(R-2),以评估模型预测可以很好地解释现场观测结果的变异性。该模型表现良好,得到了较高的NSE 0.99和沉积物的R-2值为0.92的证实。在径流的情况下,结果稍差,但仍可接受,NSE为0.76,R-2值为0.62。

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