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Estimation of surface runoff for Tarbela reservoir

机译:Tarbela水库表面径流的估算

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This project has done for the estimation of surface runoff for the Tarbela reservoir. The Rational Formula Method was used to determine the surface runoff. The different weighted maps were generated to estimate the overall runoff in a watershed. The weighted soil map, Landcover map and slope maps were generated. Then these maps were overlaid based on the relative weights to the different map types. The weights were assigned proportional to the surface runoff capability of the specific group in each map. Surface Runoff a weights The drainage area was calculated from the flow accumulation. The flow accumulation was gained through the Arc Hydro utility, by terrain processing. The outlet of the flow accumulation provided the high accumulated cell for the whole drainage area. The precipitation data for the year of 2002 in the drainage area was interpolated by the IDW (Inverse distance weighted) to generate the rainfall surface. The rainfall surface was used in the resultant ‘C map’ (weighted overlaid map of (LC+Soil+Slope) and drainage area to calculate the total surface runoff (Q). There are different models to calculate the surface run off, as a literature review during this study. The CN (curve number) and SCS models can also perform the same estimations.
机译:该项目已经为Tarbela水库估算了表面径流。 Rational Filitue方法用于确定表面径流。生成不同加权图以估计流域中的整体径流。生成加权土壤图,Landcover地图和斜率图。然后基于不同地图类型的相对权重覆盖这些地图。重量与每个地图中特定组的表面径流能力成比例。表面径流加权排水区域从流量累积计算。通过地形加工通过电弧水电实用性来获得流量。流动累积的出口为整个排水区域提供了高累积的电池。通过IDW(逆距离加权)插入引流区域中2002年的降水数据以产生降雨面。降雨表面用于所得的'C MAP'((LC +土壤+斜坡)和排水区域的加权覆盖图,以计算总表面径流(Q)。有不同的型号来计算表面耗尽,如a本研究期间的文献综述。CN(曲线数)和SCS模型也可以执行相同的估计。

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