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首页> 外文期刊>Journal of the American Water Resources Association >GIS-BASED SPATIAL PRECIPITATION ESTIMATION: A COMPARISON OF GEOSTATISTICAL APPROACHES
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GIS-BASED SPATIAL PRECIPITATION ESTIMATION: A COMPARISON OF GEOSTATISTICAL APPROACHES

机译:基于GIS的空间降水估计:地统计学方法的比较

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摘要

As one of the primary inputs that drive watershed dynamics, the estimation of spatial variability of precipitation has been shown to be crucial for accurate distributed hydrologic modeling. In this study, a Geographic Information System program, which incorporates Nearest Neighborhood (NN), Inverse Distance Weighted (IDW), Simple Kriging (SK), Ordinary Kriging (OK), Simple Kriging with Local Means (SKlm), and Kriging with External Drift (KED), was developed to facilitate automatic spatial precipitation estimation. Elevation and spatial coordinate information were used as auxiliary variables in SKlm and KED methods. The above spatial interpolation methods were applied in the Luohe watershed with an area of 5,239 km2, which is located downstream of the Yellow River basin, for estimating 10 years' (1991-2000) daily spatial precipitation using 41 rain gauges. The results obtained in this study show that the spatial precipitation maps estimated by different interpolation methods have similar areal mean precipitation depth, but significantly different values of maximum precipitation, minimum precipitation, and coefficient of variation. The accuracy of the spatial precipitation estimated by different interpolation methods was evaluated using a correlation coefficient, Nash-Sutcliffe efficiency, and relative mean absolute error. Compared with NN and IDW methods that are widely used in distributed hydrologic modeling systems, the geostatistical methods incorporated in this GIS program can provide more accurate spatial precipitation estimation. Overall, the SKlm_EL_X and KED_EL_X, which incorporate both elevation and spatial coordinate as auxiliary into SKlm and KED, respectively, obtained higher correlation coefficient and Nash-Sutcliffe efficiency, and lower relative mean absolute error than other methods tested. The GIS program developed in this study can serve as an effective and efficient tool to implement advanced geo-statistics methods that incorporate auxiliary information to improve spatial precipitation estimation for hydro-logic models.
机译:作为驱动流域动力学的主要输入之一,降水的空间变异性估计已证明对准确的分布式水文模型至关重要。在这项研究中,一个地理信息系统程序结合了最近邻域(NN),反距离加权(IDW),简单Kriging(SK),普通Kriging(OK),使用局部均值的简单Kriging(SKlm)和外部Kriging漂移(KED)是为了促进自动空间降水估算而开发的。高程和空间坐标信息在SKlm和KED方法中用作辅助变量。以上空间插值方法应用于位于黄河下游的面积为5239 km2的Lu河流域,利用41个雨量计估算了10年(1991-2000年)的日降水量。这项研究获得的结果表明,通过不同插值方法估算的空间降水图具有相似的面积平均降水深度,但最大降水,最小降水和变异系数的值却明显不同。使用相关系数,纳什-苏特克利夫效率和相对平均绝对误差评估通过不同插值方法估算的空间降水的准确性。与分布式水文建模系统中广泛使用的NN和IDW方法相比,此GIS程序中包含的地统计方法可以提供更准确的空间降水估算。总体而言,与其他测试方法相比,将高程和空间坐标作为辅助辅助分别输入到SKlm和KED中的SKlm_EL_X和KED_EL_X获得了更高的相关系数和Nash-Sutcliffe效率,以及更低的相对平均绝对误差。在这项研究中开发的GIS程序可以作为一种有效的工具来实施先进的地统计学方法,该方法结合了辅助信息来改善水文模型的空间降水估算。

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