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Advancing representation of hydrologic processes in the Soil and Water Assessment Tool (SWAT) through integration of the TOPographic MODEL (TOPMODEL) features

机译:通过整合TOPographic模型(TOPMODEL)功能,在水土评估工具(SWAT)中加快水文过程的表示

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This paper presents a study of the integration of the Soil and Water Assessment Tool (SWAT) model and the TOPographic MODEL (TOPMODEL) features for enhancing the physical representation of hydrologic processes. In SWAT, four hydrologic processes, which are surface runoff, baseflow, groundwater re-evaporation and deep aquifer percolation, are modeled by using a group of empirical equations. The empirical equations usually constrain the simulation capability of relevant processes. To replace these equations and to model the influences of topography and water table variation on streamflow generation, the TOPMODEL features are integrated into SWAT, and a new model, the so-called SWAT-TOP, is developed. In the new model, the process of deep aquifer percolation is removed, the concept of groundwater re-evaporation is refined, and the processes of surface runoff and baseflow are remodeled. Consequently, three parameters in SWAT are discarded, and two new parameters to reflect the TOPMODEL features are introduced. SWAT-TOP and SWAT are applied to the East River basin in South China, and the results reveal that, compared with SWAT, the new model can provide a more reasonable simulation of the hydrologic processes of surface runoff, groundwater re-evaporation, and baseflow. This study evidences that an established hydrologic model can be further improved by integrating the features of another model, which is a possible way to enhance our understanding of the workings of catchments.
机译:本文介绍了对土壤和水评估工具(SWAT)模型和TOPographic模型(TOPMODEL)功能进行集成以增强水文过程物理表示的研究。在SWAT中,使用一组经验方程对地表径流,基流,地下水再蒸发和深层含水层渗流这四个水文过程进行了建模。经验公式通常会约束相关过程的仿真能力。为了取代这些方程式并模拟地形和地下水位变化对水流产生的影响,将TOPMODEL功能集成到SWAT中,并开发了一种新模型,即所谓的SWAT-TOP。在新模型中,去除了深层含水层的渗流过程,完善了地下水再蒸发的概念,并对地表径流和基流过程进行了重塑。因此,SWAT中的三个参数被丢弃,并且引入了两个新参数以反映TOPMODEL功能。 SWAT-TOP和SWAT被应用到华南东部流域,结果表明,与SWAT相比,新模型可以为地表径流,地下水再蒸发和基流的水文过程提供更合理的模拟。 。这项研究表明,可以通过整合另一个模型的特征来进一步完善已建立的水文模型,这是增强我们对流域工作原理的理解的一种可能方法。

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