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Distributed hydrological modeling study with the dynamic water yielding mechanism and RS/GIS techniques

机译:具有动态水产机制和RS / GIS技术的分布水文模拟研究

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Water yielding in the hydrologic cycle is a temporally and spatially varied process. However, water yielding mechanics expressed in hydrological simulations seldom accurately characterize such dynamic processes thus weakens the simulation capabilitiesof present hydrological modeling systems. In this study a conceptual distributed hydrological model entitled ESSI (infiltration Excess and Saturation excess Soil-water Integration model for hydrology) was developed for flooding simulation and long termwater resource management studies by means of RS, GIS and data mining techniques. This distributed hydrological modeling system has three significant characteristics: 1) capable of determining temporally and spatially varied water yielding mechanics overthe most basic simulated grid by comparing with real-time computed rainfall and soil water variables; 2) excellent weather adoptability to ensure the model perform excellently for either wet and dry watershed conditions; 3) fully distributed simulatingcapabilities enable the model output about 20 distributed hydrological process components in different time scales, i.e. evapotranspiration (potential and actual), canopy storage, and soil moisture contents in different soil depth etc.Calibration and validation of the modeling system was conducted on two carefully selected climatologically typical watersheds in China, one located in the typical humid climate condition of upper stream of the Hanjiang river Basin, gauged by the Jiangkouhydrometric station (drainage area: 2413 km2), and another the Yingluoxia watershed (drainage area: 10029 km2), situated in typical cold and arid Heihe Mountainous region. With the calibrated model parameters and the appropriate combination of hydrological simulating module, ESSI successfully reproduced the flooding events and long term hydrological processes for the both experiment watershed, which implies the model an excellent hydrological simulation tool under various weather conditions.
机译:水文循环中的水是在时间上和空间上变化的过程。然而,在水文模拟中表达的水产量很少能够精确地表征这种动态过程,从而削弱了现有水文建模系统的模拟能力。在这项研究中,通过RS,GIS和数据挖掘技术开发了一个概念分布式水文模型(渗透过量和饱和过量的水文水中的水性过量土壤 - 水整合模型)。该分布式水文建模系统具有三种显着特性:1)通过与实时计算的降雨和土壤水分变量相比,能够在最基本的模拟网格中确定时间和空间变化的水屈服力学; 2)卓越的天气依赖性,以确保模型以潮湿和干燥的流域条件优良而言; 3)完全分布式的模拟电缆使模型输出大约20个分布式水文过程组分在不同的时间尺度,即蒸发蒸腾(潜力和实际),树冠储存和土壤水分含量在不同的土壤深度等中进行了建模系统的校准和验证在两人精心挑选的中国典型的气候典型流域,一个位于汉江流域上游典型潮湿的气候条件,由江口步骤衡量(排水区:2413公里),另一个横罗西亚流域(排水区:10029 KM2),坐落在典型的寒冷和干旱的黑河山区。通过校准的模型参数和水文模拟模块的适当组合,ESSI成功地再现了两种实验流域的洪水事件和长期水文过程,这意味着在各种天气条件下模型是一种优异的水文模拟工具。

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