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首页> 外文期刊>Hydrology and Earth System Sciences >Comparative assessment of predictions in ungauged basins - Part 3: Runoff signatures in Austria
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Comparative assessment of predictions in ungauged basins - Part 3: Runoff signatures in Austria

机译:非流域盆地预报的比较评估-第3部分:奥地利的径流特征

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摘要

This is the third of a three-part paper series through which we assess the performance of runoff predictions in ungauged basins in a comparative way. Whereas the two previous papers by Parajka et al. (2013) and Salinas et al. (2013) assess the regionalisation performance of hydrographs and hydrological extremes on the basis of a comprehensive literature review of thousands of case studies around the world, in this paper we jointly assess prediction performance of a range of runoff signatures for a consistent and rich dataset. Daily runoff time series are predicted for 213 catchments in Austria by a regionalised rainfall-runoff model and by Top-kriging, a geostatistical estimation method that accounts for the river network hierarchy. From the runoff time-series, six runoff signatures are extracted: annual runoff, seasonal runoff, flow duration curves, low flows, high flows and runoff hydrographs. The predictive performance is assessed in terms of the bias, error spread and proportion of unexplained spatial variance of statistical measures of these signatures in cross-validation (blind testing) mode. Results of the comparative assessment show that, in Austria, the predictive performance increases with catchment area for both methods and for most signatures, it tends to increase with elevation for the regionalised rainfall-runoff model, while the dependence on climate characteristics is weaker. Annual and seasonal runoff can be predicted more accurately than all other signatures. The spatial variability of high flows in ungauged basins is the most difficult to estimate followed by the low flows. It also turns out that in this data-rich study in Austria, the geostatistical approach (Top-kriging) generally outperforms the regionalised rainfall-runoff model.
机译:这是一个由三部分组成的论文系列的第三部分,通过该系列文章,我们以比较的方式评估了未灌流盆地的径流预报性能。而Parajka等人的前两篇论文。 (2013)和Salinas等人。 (2013年)在对全球成千上万个案例研究进行全面文献综述的基础上,评估了水文图和极端水文的区域化表现,在本文中,我们联合评估了一系列径流特征的预测表现,从而获得了一个一致且丰富的数据集。通过区域降雨径流模型和Top-kriging(一种考虑河网层次结构的地统计学估计方法),可以预测奥地利213个集水区的每日径流时间序列。从径流时间序列中,提取了六个径流特征:年度径流,季节性径流,水流持续时间曲线,低流量,高流量和径流水位图。在交叉验证(盲测)模式下,根据这些签名的统计量的偏差,误差分布和无法解释的空间方差的比例来评估预测性能。比较评估的结果表明,在奥地利,两种方法和大多数特征的预测性能都随着集水区的增加而增加,区域降雨径流模型的预测性能往往随海拔的升高而增加,而对气候特征的依赖性则较弱。与所有其他特征相比,可以更准确地预测年径流量和季节径流量。无流量盆地的高流量的空间变异性是最难估计的,其次是低流量。事实证明,在奥地利的这项数据丰富的研究中,地统计学方法(Top-kriging)通常优于区域化降雨径流模型。

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