首页> 外文会议>International Conference on Hydroinformatics >REGIONAL VERSUS PHYSICALLY-BASED METHODS FOR FLOOD INUNDATION MODELLING IN DATA SCARCE AREAS: AN APPLICATION TO THE BLUE NILE
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REGIONAL VERSUS PHYSICALLY-BASED METHODS FOR FLOOD INUNDATION MODELLING IN DATA SCARCE AREAS: AN APPLICATION TO THE BLUE NILE

机译:基于区域对物理的数据稀疏区洪水淹没建模方法:在蓝尼罗河中的应用

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One of the main obstacles in mapping flood hazard in data scarce areas is the difficulty in estimating the design flood, i.e. river discharge corresponding to a given return period. This exercise can be carried out using regionalization techniques, which are based on flood data of regions with similar hydro-climatic conditions, or employing physically based model cascades. In this context, we compared the flood extents maps derived for a river reach of the Blue Nile following two alternative methods: ⅰ) regional envelope curve (REC), whereby design floods (e.g. 1-in-20 and 1-in-100 year flood peaks) are derived from African envelope curves and ⅱ) physical model cascade (PMC), whereby design floods are calculated from the physical model chain of the European Centre for Medium-Range Weather Forecasts (ECMWF,). The two design flood estimates are then used as input of a 2D hydraulic model LISFLOOD-FP and the simulated flood extents are quantitatively evaluated by comparing to a reference flood extent model, which uses design floods estimated from in situ data. The results show the complexity in assessing flood hazard in data scarce area as PMC largely overestimates the flood extent, while REC underestimates it.
机译:在数据稀缺地区绘制洪水危险图的主要障碍之一是难以估算设计洪水,即与给定返回期相对应的河流流量。可以使用区域化技术(基于具有相似水文气候条件的区域的洪水数据)或使用基于物理的模型级联来进行此练习。在这种情况下,我们通过以下两种方法比较了青尼罗河河段的洪水范围图:ⅰ)区域包络线(REC),从而设计洪水(例如20年1分和100年1分洪水峰值)来自非洲的包络线和ⅱ)物理模型级联(PMC),由此设计洪水是根据欧洲中型天气预报中心(ECMWF)的物理模型链计算得出的。然后将这两个设计洪水估算值用作2D水力模型LISFLOOD-FP的输入,并且通过与使用从现场数据估算的设计洪水量的参考洪水范围模型进行比较,对模拟洪水范围进行定量评估。结果表明,由于PMC大大高估了洪灾程度,而REC却低估了数据稀缺地区的洪灾危害,因此评估工作很复杂。

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