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Development of a precipitation-area curve for warning criteria of short-duration flash flood

机译:开发沉淀区曲线,用于警告短期闪电洪水的标准

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摘要

This paper presents quantitative criteria for flash flood warning that can be used to rapidly assess flash flood occurrence based on only rainfall estimates. This study was conducted for 200 small mountainous sub-catchments of the Han River basin in South Korea because South Korea has recently suffered many flash flood events. The quantitative criteria are calculated based on flash flood guidance (FFG), which is defined as the depth of rainfall of a given duration required to cause frequent flooding (1-2-year return period) at the outlet of a small stream basin and is estimated using threshold runoff (TR) and antecedent soil moisture conditions in all sub-basins. The soil moisture conditions were estimated during the flooding season, i.e., July, August and September, over 7 years (2002-2009) using the Sejong University Rainfall Runoff (SURR) model. A ROC (receiver operating characteristic) analysis was used to obtain optimum rainfall values and a generalized precipitation-area (P-A) curve was developed for flash flood warning thresholds. The threshold function was derived as a P-A curve because the precipitation threshold with a short duration is more closely related to basin area than any other variables. For a brief description of the P-A curve, generalized thresholds for flash flood warnings can be suggested for rainfall rates of 42, 32 and 20mmh(-1) in sub-basins with areas of 22-40, 40-100 and 100 km(2), respectively. The proposed P-A curve was validated based on observed flash flood events in different sub-basins. Flash flood occurrences were captured for 9 out of 12 events. This result can be used instead of FFG to identify brief flash flood (less than 1 h), and it can provide warning information to decision-makers or citizens that is relatively simple, clear and immediate.
机译:本文介绍了闪光洪水警告的定量标准,可用于快速评估仅基于降雨估算的闪现洪水发生。这项研究是在韩国在韩国汉河流域的200个小型山地集水区进行,因为韩国最近遭受了许多闪现洪水事件。定量标准是基于闪光泛洪指导(FFG)计算的,其定义为在小型溪流盆地出口频繁洪水(1-2岁返回期)所需的给定持续时间的降雨深度,并且是在所有子盆地中使用阈值径流(TR)和前一种土壤水分条件估计。在洪水季节,即7月,8月和9月期间,估计土壤水分条件超过7年(2002-2009),使用Sejong大学降雨径流(SURR)模型。 ROC(接收器操作特性)分析用于获得最佳的降雨量值,并且开发了广义降水区(P-A)曲线,用于闪蒸泛滥警告阈值。阈值函数作为P-A曲线导出,因为具有短持续时间的降水阈值与盆地区域比任何其他变量更密切。对于P-A曲线的简要说明,可以在22-40,40-100和GT的区域中的42,32和20mmH(-1)中的降雨率来提出闪光警告的广义阈值。 100公里(2)分别。基于不同子盆地中观察到的闪蒸事件,验证了所提出的P-A曲线。闪存洪水发生捕获为12个活动中的9个。该结果可以使用而不是FFG来识别短暂的闪光洪水(小于1小时),可以向决策者或公民提供警告信息,相对简单,清晰,即时。

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