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Top-kriging - geostatistics on stream networks

机译:顶级克里格-流网络上的地统计

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摘要

We present Top-kriging, or topological kriging, as a method for estimating streamflow-related variables in ungauged catchments. It takes both the area and the nested nature of catchments into account. The main appeal of the method is that it is a best linear unbiased estimator (BLUE) adapted for the case of stream networks without any additional assumptions. The concept is built on the work of Sauquet et al. (2000) and extends it in a number of ways. We test the method for the case of the specific 100-year flood for two Austrian regions. The method provides more plausible and, indeed, more accurate estimates than Ordinary Kriging. For the variable of interest, Top-kriging also provides estimates of the uncertainty. On the main stream the estimated uncertainties are smallest and they gradually increase as one moves towards the headwaters. The method as presented here is able to exploit the information contained in short records by accounting for the uncertainty of each gauge. We suggest that Top-kriging can be used for spatially interpolating a range of streamflow-related variables including mean annual discharge, flood characteristics, low flow characteristics, concentrations, turbidity and stream temperature.
机译:我们介绍Top-kriging或拓扑kriging,作为一种方法来估算未排放集水区中与流量相关的变量。它同时考虑了流域的面积和嵌套性质。该方法的主要吸引力在于,它是一种适用于流网络情况的最佳线性无偏估计器(BLUE),无需任何其他假设。这个概念是建立在Sauquet等人的工作之上的。 (2000),并以多种方式对其进行了扩展。我们针对两个奥地利地区特定的100年洪水案例测试了该方法。与普通克里金法相比,该方法提供了更合理,甚至更准确的估计。对于感兴趣的变量,Top-kriging还提供不确定性的估计。在主流上,估计的不确定性最小,随着不确定性的增加,不确定性会逐渐增加。通过考虑每个量规的不确定性,此处介绍的方法能够利用短记录中包含的信息。我们建议可以使用Top-kriging在空间上对一系列与流量有关的变量进行插值,包括年均流量,洪水特征,低流量特征,浓度,浊度和河流温度。

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