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ON THE CHOICE OF SPATIAL INTERPOLATION METHOD FOR THE ESTIMATION OF 1-TO 5- DAY BASIN AVERAGE DESIGN PRECIPITATION

机译:关于估计1至5天盆地平均设计降水的空间插值方法的选择

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The aim of the study was to derive frequency curves of annual maximum basin average of 1-to 5- day precipitation depths for the upper Hron River basin. Three spatial interpolation schemes were selected for the analysis. The Thiessen polygon method and the inverse distance method gave systematically lower values for shorter durations of precipitation then the altitudinal zones method; most probably due to the fact, that convective precipitation can play a significant role in annual maximum daily precipitation values. For longer durations all methods gave comparable results. The inverse distance method has a better potential to reflect and project the actual spatial distribution of daily measured data into the spatially interpolated rainfall surface than the Thiessen polygon method, since the measurements reflect altitudinal zonality as well. Co-kriging, which can included the effect of topography, could probably also provide accurate and realistic estimates, but its application is tedious when compared with the inverse distance method. This method can be therefore recommended as an appropriate interpolation scheme for engineering applications.
机译:该研究的目的是导出上校长河流盆地1至5天降水深度的年度最大盆地的频率曲线。选择三个空间插值方案进行分析。 Thiessen Polygon方法和逆距离方法系统地较低的沉淀持续时间较短的值,然后是高度的区域方法;最重要的是由于事实,对流降水可以在年度最大日降水值中发挥重要作用。对于更长的持续时间,所有方法所有方法都具有可比的结果。逆距离方法具有更好的潜力,可以将每日测量数据的实际空间分布的潜力更好地,该逆距离是泰森多边形方法,因为测量也反映了高度的区域性。可以包括地形效果的共同克里格可能还可以提供准确和现实的估计,但与逆距离方法相比,其应用是乏味的。因此,可以建议使用该方法作为工程应用的适当插值方案。

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