Leveraging a novel hybrid ensemble and optimal interpolation approach for enhanced streamflow and flood prediction

Mohamad El Gharamti, A. Rafieeinasab, James L. McCreight
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Abstract

Abstract. In the face of escalating instances of inland and flash flooding spurred by intense rainfall and hurricanes, the accurate prediction of rapid streamflow variations has become imperative. Traditional data assimilation methods face challenges during extreme rainfall events due to numerous sources of error, including structural and parametric model uncertainties, forcing biases, and noisy observations. This study introduces a cutting-edge hybrid ensemble and optimal interpolation data assimilation scheme tailored to precisely and efficiently estimate streamflow during such critical events. Our hybrid scheme uses an ensemble-based framework, integrating the flow-dependent background streamflow covariance with a climatological error covariance derived from historical model simulations. The dynamic interplay (weight) between the static background covariance and the evolving ensemble is adaptively computed both spatially and temporally. By coupling the National Water Model (NWM) configuration of the WRF-Hydro modeling system with the Data Assimilation Research Testbed (DART), we evaluate the performance of our hybrid prediction system using two impactful case studies: (1) West Virginia's flash flooding event in June 2016 and (2) Florida's inland flooding during Hurricane Ian in September 2022. Our findings reveal that the hybrid scheme substantially outperforms its ensemble counterpart, delivering enhanced streamflow estimates for both low and high flow scenarios, with an improvement of up to 50 %. This heightened accuracy is attributed to the climatological background covariance, mitigating bias and augmenting ensemble variability. The adaptive nature of the hybrid algorithm ensures reliability, even with a very small time-varying ensemble. Moreover, this innovative hybrid data assimilation system propels streamflow forecasts up to 18 h in advance of flood peaks, marking a substantial advancement in flood prediction capabilities.
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利用新颖的混合集合和优化插值方法加强河水流量和洪水预测
摘要面对强降雨和飓风引发的不断升级的内陆洪水和山洪暴发,准确预测快速的流量变化已成为当务之急。由于结构和参数模型的不确定性、强迫偏差和噪声观测等众多误差来源,传统的数据同化方法在极端降雨事件中面临挑战。本研究介绍了一种前沿的混合集合和最优插值数据同化方案,专门用于在此类关键事件中精确、高效地估算河水流量。我们的混合方案采用基于集合的框架,将与流量相关的背景流量协方差与从历史模式模拟中得出的气候误差协方差整合在一起。静态背景协方差与不断变化的集合之间的动态相互作用(权重)在空间和时间上都是自适应计算的。通过将 WRF-Hydro 建模系统的国家水模型(NWM)配置与数据同化研究试验台(DART)耦合,我们利用两个具有影响力的案例研究评估了混合预测系统的性能:(1)2016 年 6 月西弗吉尼亚州的山洪暴发事件;(2)2022 年 9 月 "伊恩 "飓风期间佛罗里达州的内陆洪水。我们的研究结果表明,混合方案的性能大大优于其对应的集合方案,在低流量和高流量情况下都能提供更高的流量估计值,最高可提高 50%。这种准确性的提高归功于气候背景协方差,它减轻了偏差并增加了集合变异性。混合算法的自适应特性确保了可靠性,即使是很小的时变集合也是如此。此外,这种创新的混合数据同化系统可在洪峰到来之前提前 18 个小时预报河水流量,标志着洪水预报能力的巨大进步。
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