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Sensitivity and first-order/Monte Carlo uncertainty analysis of the WEPP hillslope erosion model.

机译:WEPP山坡侵蚀模型的敏感性和一阶/蒙特卡洛不确定性分析。

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Performing a comprehensive sensitivity/uncertainty analysis is a valuable step in understanding and using a predictive hydrologic/water quality (H/WQ) model. This article applies one-factor-at-a-time (OAT) sensitivity analysis (SA) and first-order error analysis (FOEA)/Monte Carlo simulation with Latin hypercube sampling (LHS) uncertainty analysis techniques for evaluation of a complex, process-based water erosion prediction tool, the USDA Water Erosion Prediction Project (WEPP) model (version 2010.1). Assessment of the WEPP hillslope profile model on a Midwestern U.S. Miami silt loam soil for three cropping/management scenarios and three erosion process cases (as defined by topography) is described. WEPP model runoff, soil loss, and corn (Zea mays L.) yield output responses in the form of expected values and error variances were determined to illustrate model prediction uncertainty. The OAT SA showed that WEPP runoff and soil loss output responses were most sensitive to changes in the baseline effective hydraulic conductivity (Kb) and sand content. WEPP model corn yield output response was most sensitive to crop input parameters affecting the simulation of biomass development. The FOEA showed that the largest contributions to runoff, soil loss, and corn yield total error variance came from Kb and sand/clay content, Kb and baseline soil erodibility factors, and the biomass energy ratio of a crop and harvest index, respectively. The FOEA total variances presented in this study for runoff and soil loss were considerably larger than the corresponding Monte Carlo LHS simulation total variances. The Monte Carlo LHS total variance results were reasonable, making Monte Carlo LHS appear to be a better alternative for quantifying WEPP output response error variance. The Monte Carlo LHS soil loss output responses were also compared to Universal Soil Loss Equation (USLE) soil loss predictions. The USLE soil loss estimates were within the Monte Carlo LHS 90% prediction intervals for six of the nine cropping/management and erosion process cases. Results of this study illustrate the usefulness of combining SA and Monte Carlo LHS for providing detailed uncertainty analysis information for complex, physically based models such as WEPP.
机译:进行全面的敏感性/不确定性分析是理解和使用预测性水文/水质(H / WQ)模型的重要一步。本文应用一次单因素(OAT)敏感性分析(SA)和一阶误差分析(FOEA)/蒙特卡罗模拟以及拉丁文超立方体采样(LHS)不确定性分析技术来评估复杂过程基于USDA的水蚀预测工具,USDA水蚀预测项目(WEPP)模型(版本2010.1)。描述了在美国中西部粉砂壤土上的WEPP山坡剖面模型对三种种植/管理方案和三种侵蚀过程案例(由地形定义)的评估。确定了WEPP模型径流,土壤流失和玉米(Zea mays L.)产量输出响应,其形式为期望值和误差方差,以说明模型预测的不确定性。 OAT SA显示,WEPP径流和土壤流失输出响应对基线有效水导率(K b )和含砂量的变化最敏感。 WEPP模型玉米产量输出响应对影响生物量发育模拟的作物输入参数最敏感。 FOEA显示对径流,土壤流失和玉米产量总误差方差的最大贡献来自K b 和沙/粘土含量,K b 和基线土壤侵蚀性因子,以及作物的生物质能比和收获指数。在这项研究中,关于径流和土壤流失的FOEA总方差远大于相应的Monte Carlo LHS模拟总方差。蒙特卡洛LHS总方差结果是合理的,使得蒙特卡洛LHS似乎是量化WEPP输出响应误差方差的更好选择。还将蒙特卡洛LHS土壤流失输出响应与通用土壤流失方程(USLE)土壤流失预测进行了比较。在9个种植/管理和侵蚀过程案例中,有6个案例的USLE土壤流失估计在90%的蒙特卡洛预测范围内。这项研究的结果表明,结合SA和Monte Carlo LHS可以为复杂的基于物理的模型(例如WEPP)提供详细的不确定性分析信息。

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