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首页> 外文期刊>Transactions of the ASABE >Modeling Streamflow in a Snow-Dominated Forest Watershed Using the Water Erosion Prediction Project (WEPP) Model
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Modeling Streamflow in a Snow-Dominated Forest Watershed Using the Water Erosion Prediction Project (WEPP) Model

机译:使用水腐蚀预测项目(WEPP)模型在雪撬森林流域中建模流流。

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The Water Erosion Prediction Project (WEPP) model was originally developed for hillslope and small watershed applications. Recent improvements to WEPP have led to enhanced computations for deep percolation, subsurface lateral flow, and frozen soil. Inaddition, the incorporation of channel routing has made the WEPP model well suited for large watersheds with perennial flows. However, WEPP is still limited in modeling forested watersheds where groundwater baseflow is substantial. The objectives of this study were to (1) incorporate nonlinear algorithms into WEPP (v2012.8) for estimating groundwater baseflow, (2) auto-calibrate the current and modified WEPP model using a model-independent parameter estimation tool, and (3) evaluate and compare the performance of the current version of WEPP without baseflow (WEPP-Cur) and the modified WEPP model with baseflow (WEPP-Mod) in simulating the hydrology of a snow-dominated watershed in the U.S. Pacific Northwest. A subwatershed of the Upper Cedar River Watershed in western Washington State was chosen for WEPP application and assessment. Simulations were conductedfor two periods: 1997-2003 to calibrate the model and 2004-2011 to assess the model performance. The WEPP-Cur simulations resulted in Nash-Sutcliffe efficiency (NSE) and deviation of runoff volume (Dv) values of 0.55 and 24%, respectively, for the calibration period, and 0.60 and 21%, respectively, for the assessment period. The WEPP-Mod simulated streamflow showed improved agreement with observedstreamflow, with NSE and Dv values of 0.76 and 6%, respectively, for the calibration period, and 0.74 and 2% , respectively, for the assessment period. The WEPP-Mod model reproduced hydrograph recessions during the low-flow periods and the general trendof the hydrographs, demonstrating its applicability to a watershed where groundwater baseflow was significant. The incorporation of a baseflow component into WEPP will help forest managers to assess the alterations in hydrological processes and water yield for their forest management practices.
机译:水腐蚀预测项目(WEPP)模型最初是为山坡和小流域应用开发的。 WEPP最近的改进导致了增强的渗透,地下横向流动和冻土的计算。 Inddition,渠道路由的纳入使WEPP模型适合具有多年生流动的大型流域。然而,WEPP仍然有限于建模森林流域,地下水基础流量很大。本研究的目标是(1)将非线性算法与Wepp(V2012.8)合并,用于估计地下水基础流,(2)使用型号无关的参数估计工具自动校准电流和修改的WEPP模型,(3)在没有Baseflow(WEPP-CUR)的情况下,评估和比较当前版本的WEPP的性能和基础流(WEPP-MOD)的修改后的WEPP模型在模拟美国太平洋西北部的雪撬流域水文中。选择了华盛顿州西部雪松河流域的一艘河底,为WEPP申请和评估。为两个时期进行模拟:1997-2003校准模型和2004-2011以评估模型性能。 WEPP-CUS模拟导致NASH-SUTCLIFFE效率(NSE)和频率(DV)值分别为0.55和24%,分别为评估期间分别为0.60和21%。 WEPP-MOD模拟流流量显示出与观察到流程流程的改进的协议,NSE和DV值分别为校准期,分别为0.76和6%,分别为评估期间和0.74和2%。 WEPP-MOD模型在低流量期间再现水文衰退,以及水文编程的一般趋势,证明了其对地下水基流显着的流域的适用性。将基流组件纳入WEPP将有助于森林经理评估其森林管理实践的水文过程和水收益率的改变。

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