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Streamflow forecasts from WRF precipitation for flood early warning in mountain tropical areas

机译:来自WRF降水的流出预测山热带地区洪水预警

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摘要

Numerical weather prediction (NWP) models are fundamental to extend forecast lead times beyond the concentration time of a watershed. Particularly for flash flood forecasting in tropical mountainous watersheds, forecast precipitation is required to provide timely warnings. This paper aims to assess the potential of NWP for flood early warning purposes, and the possible improvement that bias correction can provide, in a tropical mountainous area. The paper focuses on the comparison of streamflows obtained from the post-processed precipitation forecasts, particularly the comparison of ensemble forecasts and their potential in providing skilful flood forecasts. The Weather Research and Forecasting (WRF) model is used to produce precipitation forecasts that are post-processed and used to drive a hydrologic model. Discharge forecasts obtained from the hydrological model are used to assess the skill of the WRF model. The results show that post-processed WRF precipitation adds value to the flood early warning system when compared to zero-precipitation forecasts, although the precipitation forecast used in this analysis showed little added value when compared to climatology. However, the reduction of biases obtained from the post-processed ensembles show the potential of this method and model to provide usable precipitation forecasts in tropical mountainous watersheds. The need for more detailed evaluation of the WRF model in the study area is highlighted, particularly the identification of the most suitable parameterisation, due to the inability of the model to adequately represent the convective precipitation found in the study area.
机译:数值天气预报(NWP)模型是扩展预测超出流域的浓度时间的基础。特别是对于热带山地流域的闪蒸预测,需要预测降水来提供及时的警告。本文旨在评估洪水预警目的的NWP的潜力,以及偏压校正可以在热带山区提供的可能改进。本文重点介绍了从后处理后的降水预测获得的流出的比较,特别是集合预测的比较及其在提供熟练的洪水预测方面的潜力。天气研究和预测(WRF)模型用于产生后处理和用于驱动水文模型的降水预测。从水文模型获得的放电预测用于评估WRF模型的技能。结果表明,与零降水预测相比,处理后的WRF降水量增加了洪水预警系统的价值,尽管与气候学相比,该分析中使用的降水预测表现出很少的附加值。然而,从后处理的集合获得的偏差减少显示了这种方法和模型的潜力,以提供热带山地流域的可用降水预测。突出显示了对研究区域中的WRF模型的更详细评估的需要,特别是鉴定最合适的参数化,因为模型无法充分代表研究区域中发现的对流降水。

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