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Probabilistic flood forecasting on the Rhone River: evaluation with ensemble and analogue-based precipitation forecasts

机译:罗讷河的概率洪水预测:与集合和基于模拟的降水预测的评价

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摘要

Hydrological ensemble forecasting performances are analysed over 5 basins up to 2000 km2 in the French Upper Rhone region. Streamflow forecasts are issued at an hourly time step from lumped ARX rainfall-runoff models forced by different precipitation forecasts. Ensemble meteorological forecasts from ECMWF and NCEP are considered, as well as analogue-based forecasts fed by their corresponding control forecast. Analogue forecasts are rearranged using an adaptation of the Schaake-Shuffle method in order to ensure the temporal coherence. A new evaluation approach is proposed, separating forecasting performances on peak amplitudes and peak timings for high flow events. Evaluation is conducted against both simulated and observed streamflow (so that relative meteorological and hydrological uncertainties can be assessed), by means of CRPS and rank histograms, over the 2007-2014 period. Results show a general agreement of the forecasting performances when averaged over the 5 basins. However, ensemble-based and analogue-based streamflow forecasts produce a different signature on peak events in terms of bias, spread and reliability. Strengths and weaknesses of both approaches are discussed as well as potential improvements, notably towards their merging.
机译:水文集合预测性能在法国上部罗纳地区的5至2000平方公里分析了5次盆地。通过不同降水预测的集成ARX Rainfall-Runoff模型的一小时时间步单发出Streamflow预测。考虑了来自ECMWF和NCEP的集合气象预测,以及通过其相应的对照预测馈送的基于模拟的预测。使用Schaake-Shuffle方法的调整重新排列模拟预测,以确保时间相干。提出了一种新的评估方法,将预测性能分离在高流动事件的峰值幅度和峰值时序上。在2007 - 2014年期间,通过CRP和等级直方图进行模拟和观察到的流出和观察到的流流程(可以评估相对气象和水文不确定性)进行评估。结果显示预测性能的一般协议,当平均在5个盆地上。然而,基于组合的和基于模拟的Stream流量预测在偏差,传播和可靠性方面产生了不同的峰值事件签名。讨论了两种方法的优势和弱点以及潜在的改进,特别是符合其合并。

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