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Modelling floods in the Ammer catchment: limitations and challenges with a coupled meteo-hydrological model approach

机译:对Ammer流域的洪水进行建模:采用耦合水文水文模型方法的局限性和挑战

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Numerous applications of hydrological models have shown their capability to simulate hydrological processes with a reasonable degree of certainty. For flood modelling, the quality of precipitation data — the key input parameter — is very important but often remains questionable. This paper presents a critical review of experience in the EU-funded RAPHAEL project. Different meteorological data sources were evaluated to assess their applicability for flood modelling and forecasting in the Bavarian pre-alpine catchment of the Ammer river (709 km2), for which the hydrological aspects of runoff production are described as well as the complex nature of floods. Apart from conventional rain gauge data, forecasts from several Numerical Weather Prediction Models (NWP) as well as rain radar data are examined, scaled and applied within the framework of a GIS-structured and physically based hydrological model. Multi-scenario results are compared and analysed. The synergetic approach leads to promising results under certain meteorological conditions but emphasises various drawbacks. At present, NWPs are the only source of rainfall forecasts (up to 96 hours) with large spatial coverage and high temporal resolution. On the other hand, the coarse spatial resolution of NWP grids cannot yet address, adequately, the heterogeneous structures of orographic rainfields in complex convective situations; hence, a major downscaling problem for mountain catchment applications is introduced. As shown for two selected Ammer flood events, a high variability in prediction accuracy has still to be accepted at present. Sensitivity analysis of both meteo-data input and hydrological model performance in terms of process description are discussed and positive conclusions have been drawn for future applications of an advanced meteo-hydro model synergy. style="line-height: 20px;">Keywords: RAPHAEL, modelling, forecasting, model coupling, PROMET-D, TOPMODEL
机译:水文模型的许多应用已显示出它们具有合理程度的确定性来模拟水文过程的能力。对于洪水模型而言,降水数据的质量(关键的输入参数)非常重要,但常常令人怀疑。本文对欧盟资助的RAPHAEL项目的经验进行了严格的评论。对不同的气象数据源进行了评估,以评估其在Ammer河(709 km 2 )的巴伐利亚阿尔卑斯山前流域的洪水建模和预报中的适用性,其径流产生的水文方面被描述为:以及洪水的复杂性。除了常规的雨量计数据以外,还可以在基于GIS的基于物理的水文模型框架内检查,缩放和应用来自多个数值天气预报模型(NWP)的预报以及降雨雷达数据。多情景结果进行了比较和分析。协同方法在某些气象条件下会产生可喜的结果,但会强调各种缺点。当前,NWP是唯一具有大空间覆盖和高时间分辨率的降雨预报(长达96小时)的来源。另一方面,NWP网格的粗略空间分辨率尚不能充分解决复杂对流情况下地形雨场的非均质结构。因此,引入了山区集水应用的主要降尺度问题。如针对两个选定的Ammer洪水事件所示,目前仍必须接受预测准确性的高变异性。讨论了从过程描述角度对气象数据输入和水文模型性能的敏感性分析,并为先进的气象水文模型协同作用的未来应用得出了积极的结论。 style =“ line-height: 20px;“> 关键字: RAPHAEL,建模,预测,模型耦合,PROMET-D,TOPMODEL

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