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Simulating the Soil Moisture and Runoff in Baohe Catchment Based on TOPMODEL and DEM

机译:基于TOPMODEL和DEM的宝河流域土壤水分与径流模拟。

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TOPMODEL, a rainfall-runoff distributed physical concept frame to simulate hydrological process in watershed or slope mathematically, has been proposed for decades. This paper combines the new geo-information system (GIS) and this model to simulate the soil moisture and runoff in a Baohe River basin. Based on the 90 m-resolution grid-based digital elevation model data, the digital drainage network is generated to simulate the stream flow processes and the soil moisture distribution. The years from 1981 to 1983 are selected as the calibration period and the years from 1984 to 1985 are selected as the verification period for daily stream flow simulation. Nash-Sutcliffe efficiency is utilized to evaluate the performance of TOPMODEL. Through the above-mentioned studies, primary conclusions can be drawn that the Nash-Sutcliffe during the calibration period is 87.10% and during the verification period is 78.06%. And the soil moisture distribution simulated by TOPMODEL is agreement with the field observation, which suggest that TOPMODEL can be used as a soil moisture prediction tool and hence as an agricultural drought forecasting tool.
机译:数十年来,已经提出了TOPMODEL,这是一种降雨径流分布式物理概念框架,可以用数学方法模拟流域或斜坡中的水文过程。本文结合了新的地理信息系统(GIS)和该模型来模拟宝河流域的土壤水分和径流。基于90 m分辨率的基于网格的数字高程模型数据,生成了数字排水网络来模拟水流过程和土壤水分分布。选择1981年至1983年作为标定期,并选择1984年至1985年作为日常流量模拟的验证期。 Nash-Sutcliffe效率用于评估TOPMODEL的性能。通过上述研究,可以得出主要结论:校准期间的纳什-萨克克利夫检验为87.10%,验证期间的纳什-萨克克利夫检验为78.06%。 TOPMODEL模拟的土壤水分分布与实测结果吻合,表明TOPMODEL可以作为土壤水分预测工具,从而可以作为农业干旱预测工具。

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