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Flood and Inundation Forecasting in the Sparsely Gauged Transboundary Chenab River Basin Using Satellite Rain and Coupling Meteorological and Hydrological Models

机译:使用卫星雨和耦合气象和水文模型稀疏跨界川河流域洪水和洪水预测

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摘要

Flood forecasting in a transboundary river basin is challenging due to insufficient data sharing between countries in the upper and lower reaches of a basin. A solution is the use of satellite-observed rainfall and numerical weather prediction (NWP) for hydrological forecasting. We applied this method to the transboundary sparsely gauged Chenab River basin in Pakistan and India to reproduce the exceptionally high flood in 2014. We employed global NWPs by three weather centers to consider forecast uncertainty and downscaled them using the Weather Research and Forecasting (WRF) Model to prepare precipitation inputs. For hydrological simulations, we used a kinematic wave model, the Integrated Flood Analysis System (IFAS), for the upper-reach basin with high mountains and steep slopes, and we used a diffusive-wave rainfall-runoff-inundation (RRI) model for low altitudes and mild slopes. In our forecasting experiment, the precipitation by the global NWP was not able to predict flood peaks consistently. However, the downscaled rainfall by regional NWP showed good performance in predicting flood waves quantitatively, and a multimodel approach provided added value in issuing reliable warning as early as 6 days in advance. A confident streamflow forecasting near the border of the countries also led to reliable inundation forecasting by the RRI model in the lower-reach basin.
机译:由于盆地的上游和下游国家之间的数据共享不足,跨界河流域的洪水预测挑战。解决方案是使用卫星观察的降雨和数值天气预报(NWP)进行水文预报。我们将这种方法应用于巴基斯坦和印度的跨界稀少喀布河流域,并在2014年重现了极高的洪水。我们在三个天气中心雇用了全球NWP,以考虑使用天气研究和预测(WRF)模型的不确定性和缩小。准备降水输入。对于水文模拟,我们使用了高山脉和陡坡的上到达盆地的运动波模型,集成洪水分析系统(IFAS),我们使用了扩散波降雨 - 径流淹没(RRI)模型低海拔和轻度斜坡。在我们的预测实验中,全球NWP的降水无法持续预测洪水峰。然而,区域NWP的较低的降雨显示出良好的性能,在定量上预测洪水波,而多模型方法在提前6天提前发出可靠的警告。在各国边境附近的自信流出预测也导致了较低到达盆地的RRI模型可靠的泛滥预测。

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