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Application of TOPNET in the distributed model intercomparison project

机译:TOPNET在分布式模型比对项目中的应用

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This paper describes the application of a networked version of TOPMODEL, TOPNET, as part of the Distributed Model Intercomparison Project (DMIP). The model implementation is based on a topographically derived river network with spatially distributed sub-basins draining to each network reach. The river network is mapped from the US National Elevation Dataset Digital Elevation Model (DEM) using procedures that objectively estimate drainage density from geomorphic principles. Rainfall inputs are derived from NEXRAD (radar) for each sub-basin. For each sub-basin, the wetness index distribution is derived from the DEM. The initial model parameters for each sub-basin are estimated using look up tables based on soils (STATSGO) and vegetation (1-km AVHRR). These initial model parameters provide the spatially distributed pattern of parameters at the scale of each sub-basin. Calibration uses a multiplier for each parameter to adjust the parameters while retaining the relative spatial pattern obtained from the soils and vegetation data. Parameter multipliers were calibrated using the shuffled complex evolution algorithm [J. Optim. Theory Appl. 61 (1993)] with the objective to minimize the mean square error between observed and modeled hourly streamflows. We describe the model and calibrated results submitted for all basins for the time periods involved in the DMIP study. We were encouraged by the relatively good performance of the model, especially in comparison to streamflow from smaller interior watersheds not used in calibration and simulated as ungaged basins. The limited resources used to achieve these results show some of the potential for distributed models to be useful operationally. (C) 2004 Elsevier B.V. All rights reserved.
机译:本文描述了TOPMODEL的网络版本TOPNET的应用,它是分布式模型比较项目(DMIP)的一部分。该模型的实现基于地形派生的河网,每个河网都有空间分布的子流域。该河网是根据美国国家高程数据集数字高程模型(DEM)绘制的,该程序使用根据地貌原理客观估算排水密度的程序。降雨输入来自每个子流域的NEXRAD(雷达)。对于每个子流域,湿度指数分布均从DEM得出。使用基于土壤(STATSGO)和植被(1 km AVHRR)的查找表估算每个子流域的初始模型参数。这些初始模型参数以每个子流域的规模提供参数的空间分布模式。校准使用每个参数的乘数来调整参数,同时保留从土壤和植被数据获得的相对空间格局。参数乘数使用改组的复杂演化算法进行了校准[J.最佳理论应用61(1993)]的目标是使观测和模拟的每小时流量之间的均方误差最小。我们描述了DMIP研究涉及的时间段内所有盆地提交的模型和校准结果。该模型的相对良好的性能使我们感到鼓舞,尤其是与较小的内部集水区的水流(未用于标定和模拟为非流域盆地)相比。用于获得这些结果的有限资源显示了分布式模型在操作上有用的一些潜力。 (C)2004 Elsevier B.V.保留所有权利。

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