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Methodology for flood frequency estimations in small catchments

机译:小流域洪水频率估算的方法

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Estimations of flood frequencies in small catchments are difficult due to a lack of measured discharge data. This problem is usually solved in the Czech Republic by hydrologic modelling when there is a reason not to use the data provided by the Czech hydrometeorological institute, which are quite expensive and have a very low level of accuracy. Another way is to use a simple method which provides sufficient estimates of flood frequency based on the available spatial data. A new methodology is being developed considering all important factors affecting flood formation in small catchments. The relationship between catchment descriptors and flood characteristics has been analysed first to get an overview of the importance of each considered descriptor. The results for different descriptors vary from a highly correlated relationship of an expected shape to a relationship which is opposite to that expected, mainly in the case of land use. The parameterisation of the methodology is also presented, including the sensitivity tests on each involved catchment descriptor and cross-validation of achieved results. In its present form, the methodology achieves an R-adj(2) value of about 0.61 for 10- and 0.60 for 100-year return periods.
机译:由于缺乏实测的排放数据,很难估算小流域的洪水频率。在捷克共和国,当有理由不使用捷克水文气象研究所提供的数据时,通常会通过水文模型解决该问题,因为捷克水文气象研究所的数据非常昂贵且准确性很低。另一种方法是使用一种简单的方法,该方法可根据可用的空间数据提供足够的洪水频率估计。考虑到影响小流域洪水形成的所有重要因素,正在开发一种新的方法。首先分析了流域描述符与洪水特征之间的关系,以概述每个所考虑描述符的重要性。不同描述符的结果从预期形状的高度相关关系变化到与预期相反的关系,主要是在土地使用的情况下。还介绍了该方法的参数化,包括对每个涉及的流域描述符的敏感性测试以及所获得结果的交叉验证。以目前的形式,该方法在10年的回报期内实现了约0.61的R-adj(2)值,在100年的回报期内实现了约0.60的R-adj(2)值。

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