首页> 外文期刊>Journal of Hydrology >Determination of flood-inducing rainfall and runoff for highly urbanized area based on high-resolution radar-gauge composite rainfall data and flooded area GIS data
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Determination of flood-inducing rainfall and runoff for highly urbanized area based on high-resolution radar-gauge composite rainfall data and flooded area GIS data

机译:基于高分辨率雷达仪综合降雨数据和洪水区GIS数据,确定高层城市化面积洪水诱导降雨与径流

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This study derived the Flood-Inducing-Rainfall (FIR) and Flood-Inducing-Runoff (FIRO) for urban flood warning. For this, we derived a relationship between the watershed time of concentration and accumulated rainfall depth for 261 flood events at 239 watersheds of Seoul with areas between 0.5 and 6.8 km(2) during the years 2010 and 2011, based on 10-minute 1 beta x 1 km radar-gauge composite rainfall field. This relationship was further categorized by discrete ranges of the proportion of the flooded area in the watershed (FP) and coefficient of variation (CV) of the rainfall time series. Then, minimum possible rainfall intensity calculated for each of the classified depth-duration relationship was determined as FIR for the specified range of FP and CV. A similar methodology was applied to derive FIRO, which used runoff depths that were estimated using the NRCS Curve Number method. We found that the FIR and FIRO varied between 37-62 and 10-41 mm/h, respectively. FIR and FIRO increase with an increase in FP, suggesting that greater rainfall causes larger flooded area. As rainfall CV increases, FIR and FIRO decrease, suggesting that the temporally concentrated rainfall requires less rainfall to cause the flood. A flood warning system that checks the accumulated rainfall at each of the 239 Seoul watersheds every 10 min was developed to verify the FIR and FIRO against the 21 flood events that occurred between 2012 and 2015. When flooding was tolerated on 5 percent of the watershed area, the ratios of hit, miss, and false alarm of the warning system based on the accumulated rainfall was 44.2, 9.5, and 55.8%, respectively. The ratios of hit, miss, and false alarm of the warning system based on the runoff was 66.7, 4.7, and 33.3% respectively. The flood warning system based on gauge-only or radar-only data gives approximately 3 times as much false warnings compared with the system based on radar-gauge composite data. Also, the warning system that does not consider rainfall temporal variability gave approximately twice as much false warnings as the system that considered temporal variability.
机译:本研究衍生出洪水诱导降雨(FIR)和洪水诱导径流(FIRO)用于城市洪水警告。为此,我们在2010年和2011年的239家中,在2010年和2011年的第219次的地区(6.8 km(2)之间的261次流域的分水岭间流域的分水岭时间和累计降雨量深度之间的关系。基于10分钟的1β x 1 km雷达仪综合降雨场。这种关系通过离散范围的离散范围进行了分类,流域(FP)中的洪水面积和降雨时间序列的变异系数(CV)。然后,为每个分类的深度关系计算的最低可能的降雨强度被确定为FIR,用于指定的FP和CV。应用类似的方法来导出FiRO,使用使用NRCS曲线数字方法估计的径流深度。我们发现FIR和FIRO分别在37-62和10-41 mm / h之间变化。 FIR和FIRO随着FP的增加而增加,表明降雨量更大导致较大的洪水区域。随着降雨量的CV增加,冷杉和FIRO减少,表明时间集中的降雨需要减少降雨量来引起洪水。一项洪水预警系统,每10分钟检查每10分钟的239名首尔流域中的累积降雨,以验证2012年和2015年之间发生的21场发生的洪水事件。在5%的流域地区容忍洪水时,基于累积降雨的警告系统的击球,未命中和误报的比率分别为44.2,9.5和55.8%。基于径流的警告系统的命中,未命中和误报的比率分别为66.7,4.7和33.3%。与基于雷达仪表复合数据的系统相比,基于仪表或仅雷达数据的洪水预警系统提供了大约3倍的错误警告。此外,不考虑降雨时间变异性的警告系统大约是考虑时间变异性的系统的两个错误警告。

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