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Areal rainfall estimation using spatial interpolation techniques

机译:使用空间插值技术的地区降雨估算

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Accuracy in runoff and flood estimation is important for mitigating water related problems. The accuracydepends on the methods used for areal rainfall approximation. The thin plate spline (TPS) technique was introduced in thisstudy for daily areal rainfall approximation in the Upper Ping river basin and was compared with the areal rainfall estimatedfrom two conventional techniques, the isohyetal and Thiessen polygon techniques. Two data sets of maximum rainfallregistered in August 2001 and September 2003 at 68 non-automatic rainfall stations located in the basin and nearby areaswere used in the analysis. The TPS technique was carried out in conjunction with two separate sources of digital elevationmodel (DEM), namely, GLOBE-DEM and SRTM-DEM, which were downloaded from the NOAA and NASA websites andhave horizontal resolutions of 1 km and 90 m, respectively. The TPS technique proved to provide more accurate results ofrainfall estimation than the other two techniques. The coarser DEM resolution (GLOBE-DEM) performed marginally betterin rainfall estimation than the finer DEM resolution (SRTM-DEM).
机译:径流和洪水估算的准确性对于缓解与水有关的问题很重要。精度取决于用于区域降雨近似的方法。本文将薄板样条(TPS)技术引入到坪河上游地区的每日面雨量估算中,并将其与根据等时线和蒂森多边形技术这两种常规技术估算的面雨量进行了比较。分析中使用了2001年8月和2003年9月在流域及附近地区的68个非自动降雨站登记的两个最大降雨量数据集。 TPS技术是与两个单独的数字高程模型(DEM)源,即GLOBE-DEM和SRTM-DEM结合使用的,它们是从NOAA和NASA网站下载的,其水平分辨率分别为1 km和90 m。与其他两种技术相比,TPS技术被证明可以提供更准确的降雨估算结果。在降雨估计中,较粗的DEM分辨率(GLOBE-DEM)比较细的DEM分辨率(SRTM-DEM)稍好。

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