首页> 外文会议>30th Asian conference on remote sensing 2009 >SURFACE RUNOFF ESTIMATION USING GRID-BASED CURVE NUMBER METHOD IN THE UPPER LAM PHRA PHLOENG WATERSHED, THAILAND
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SURFACE RUNOFF ESTIMATION USING GRID-BASED CURVE NUMBER METHOD IN THE UPPER LAM PHRA PHLOENG WATERSHED, THAILAND

机译:使用基于网格的曲线数法估算泰国上林发PH河上游流域的地表径流

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Upper Lam Phra Phloeng watershed in the lower northeastern part of Thailand, covering rolling and hilly area about 786 km2, is classified to be one of the most active agricultural areas in the country. Severe erosion of the area thus becomes the big problem. The more accurate surface runoff information of the area is required. This study employed grid-based Curve Number (CN) method through the GIS drainage analysis operating on DEM to estimate surface runoff depth for each grid cell in the watershed. The total depths of runoff in grid cells were accumulated from upstream to downstream along the flow path. Eighteen storm events in rainy season of the year 2008 were observed. Ten events were used for the model calibration with surface runoff data measured at two observation stations (M.171 and M.145). Other eight were for the model validation. The calibration results show that the coefficient of efficiency (E) is 0.94 and the coefficient of determination (R~2) is 0.95 at the M.171 station. While E is 0.87 and R~2 is 0.91 at the M.145 station. The validation results show that E is 0.87 and 0.68 and R~2 is 0.89 and 0.75 at the M.171 and M.145 stations, respectively. This indicates that the calibrated grid-based CN method working under GIS can be applied with satisfactory accuracy to the surface runoff estimation.
机译:泰国东北部下部的上林帕府流域,面积约786平方公里,起伏不平,丘陵地带,被列为泰国最活跃的农业地区之一。因此,该地区的严重侵蚀成为一个大问题。需要该区域更准确的地表径流信息。这项研究通过在DEM上进行的GIS排水分析,采用了基于网格的曲线数(CN)方法,以估算流域中每个网格单元的地表径流深度。网格单元中径流的总深度沿流动路径从上游到下游积累。在2008年的雨季中观测到18次风暴事件。在两个观测站(M.171和M.145)测得的地表径流数据使用了10个事件进行模型校准。其他八个用于模型验证。校准结果表明,在M.171站上,效率系数(E)为0.94,确定系数(R〜2)为0.95。在M.145站,E为0.87,R〜2为0.91。验证结果表明,在M.171和M.145站上,E分别为0.87和0.68,R〜2为0.89和0.75。这表明在GIS下工作的基于网格的经校准的CN方法可以令人满意的精度应用于地表径流估算。

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