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Evaluation of Fast Flood Diffusion through a Drainage Channel: A Flood Disaster Case Study of Japan's Kinugawa River, September 10, 2015

机译:通过排水渠道的洪水快速扩散评估:日本鬼怒川河流域的洪水灾害案例研究,2015年9月10日

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摘要

On September 10, 2015, unprecedented flood was occurred in Kinugawa River basin located on eastern Japan. It inundated 40 km2 of flood plain in Joso city, Ibaraki Prefecture, and more than 4000 people there called for help despite supposedly having sufficient time to evacuate. Some said that small initial flood before main severe flood arrived made them make a mistake in deciding whether to evacuate or stay there, despite having to actually evacuate in reality. This study focused on flood behaviour in this area, in particular, the effect of a small drainage channel lying on the flood plain which caused fast flood diffusion in case of occurring huge overflowing. Field investigations starting on time of the disaster with high-resolution positioning system were conducted to obtain spatial maps of flood depth and height. For appropriate modelling of the effect of small channel, we applied simulation model coupling 1-dimensional (1D) and 2-dimensional (2D) hydraulic scheme on the field and compared results from the 1D/2D coupled model and model without 1D scheme. The models provided information that the flood could reach 4 hours earlier to the city central of Joso city comparing in case of model without 1D scheme. The water depth rose irregularly and it was more confusing and difficult for the victims to make appropriate evacuation act.
机译:2015年9月10日,日本东部的鬼怒川流域发生了前所未有的洪水。它淹没了茨城县城总市40平方公里的洪水平原,尽管据说有足够的疏散时间,但仍有4000多人寻求帮助。一些人说,尽管主要实际上是在实际撤离,但在主要的大洪水到达之前发生的少量初始洪水使他们在决定是撤离还是停留在那里时犯了一个错误。这项研究的重点是该地区的洪水行为,特别是洪水泛滥区上的一条小排水渠的影响,在发生大面积溢洪的情况下,洪水迅速扩散。利用高分辨率定位系统从灾难发生的时间开始实地调查,以获取洪水深度和高度的空间图。为了对小通道的影响进行适当的建模,我们在现场应用了耦合一维(1D)和二维(2D)水力方案的仿真模型,并比较了1D / 2D耦合模型和无一维方案的模型的结果。这些模型提供的信息表明,与没有1D方案的模型相比,洪水可能会提前约4个小时到达Joso市中心。水深不规则地上升,受害人更难以做出适当的疏散行动。

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