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Modeling the effect of uncertainties in rainfall characteristics on flash flood warning based on rainfall thresholds

机译:基于降雨阈值的降雨特征不确定性对山洪预警的影响建模

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摘要

This study proposes a risk assessment framework for quantifying the reliability of the rainfall threshold used in flash flood warning, which should be influenced by the uncertainties in the rainfall characteristics, including rainfall duration, depth, and storm pattern. This risk assessment framework incorporates the correlated multivariate Monte Carlo simulation method, the Sobek 1D-2D hydrodynamic model, and a logistic regression equation to establish a quantile relationship of the rainfall threshold for quantifying reliability of the rainfall threshold. The Shuhu Creek catchment locates in East Taiwan, and its historical hourly rainfall records on eight typhoon events are used as the study area and data. The results from the proposed framework indicate that the variation in the rainfall threshold declines with the duration; 12-h duration associated with a stable coefficient of variance of the rainfall threshold appears to be appropriate for the flash flood warning in the Shuhu Creek catchment. Moreover, the issued rainfall thresholds in the Shuhu Creek catchment by Water Resources Agency in Taiwan have a low exceedance probability. This infers that inundation might occur as the observed rainfall depth approaches the threshold, so that it is necessary to lower the rainfall threshold in accordance with higher exceedance probability in order to achieve the goal of early flood warning.
机译:这项研究提出了一个风险评估框架,用于量化在山洪预警中使用的降雨阈值的可靠性,该可靠性阈值应受到降雨特征的不确定性(包括降雨持续时间,深度和暴风模式)的影响。该风险评估框架结合了相关的多元蒙特卡罗模拟方法,Sobek 1D-2D流体动力学模型和逻辑回归方程,以建立降雨阈值的分位数关系,以量化降雨阈值的可靠性。蜀湖溪流域位于台湾东部,以八次台风事件的历史小时降雨量记录作为研究区域和数据。拟议框架的结果表明,降雨阈值的变化随着持续时间的延长而下降。舒湖溪流域的山洪预警似乎适合与降雨阈值的稳定变异系数相关的12小时持续时间。而且,台湾水资源管理局发布的蜀湖溪流域的降雨阈值超标概率很小。这表明,当观测到的降雨深度接近阈值时可能会发生淹没,因此有必要根据更高的超出概率降低降雨阈值,以实现早期洪水预警的目标。

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