Evaluation of the Evacuation Route Availability Based on an Inundation Flow Simulation

Daichi Nakayama, D. Morinaga, H. Matsuyama
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引用次数: 3

Abstract

This study analyzes runoff and inundation flow to reproduce the condition of the August 1993 flood that occurred in the upper reaches of Sendai River in the northern part of Kagoshima prefecture, and determines model parameters. Besides, the case of situation more serious than the past floods were assumed, and it is estimated whether the inhabitants could take refuge by traveling on foot on flooded roads to evacuation centers. In the runoff analysis, the distributed runoff model based on the kinematic wave model was used. A Gridded Digital Elevation Model ( DEM ) , 50 m resolution was used to provide terrain data and flood runoff was calculated with the Drainage Direction Matrix ( DDM ) extracted from DEM. Past discharge hydrographs were fairly well reproduced by the runoff analysis. In the inundation flow analysis, a 2-dimensional unsteady flow model based on the dynamic wave model was used to calculate the expansion of the inundation flow. In the inundation flow analysis, the order of water depth was reproduced well in comparison to actual inundation, however, the estimated inundation area was smaller than the actual one. Next, runoff and inundation flow analyses were carried out with the modeled rainfall, which was more serious than that of past floods, using the model parameters determined above. The simulated flooded areas were almost the same as those caused by torrential rain in August 1993, however, the water was deeper. The current velocity was high just after the area flooded, but it slowed after 1 to 2 hours to about 0.05 m/sec in most of the flooded areas. traveling so inhabitants could not take refuge there on foot unless they took refuge at early stage of the flood. Whether or not inhabitants could take refuge safely on foot largely depended on their height, and the areas where they could walk safely was limited by their height.
基于洪水流量模拟的疏散路线可用性评估
本研究通过分析径流和淹没流量,重现了1993年8月发生在鹿儿岛县北部仙台河上游的洪水情况,并确定了模型参数。此外,假设情况比以往的洪水更严重,并估计居民是否可以步行到被淹的道路到疏散中心避难。径流分析采用基于运动波模型的分布式径流模型。采用50 m分辨率的网格化数字高程模型(DEM)提供地形数据,利用DEM提取的排水方向矩阵(DDM)计算洪水径流。径流分析相当好地再现了过去的流量曲线。在淹没流分析中,采用基于动力波模型的二维非定常流模型来计算淹没流的扩展。在淹没流量分析中,水深的顺序与实际淹没相比得到了很好的再现,但估算的淹没面积小于实际淹没面积。然后,利用上述模型参数,利用比以往洪水更严重的模型降雨进行径流和淹没流量分析。模拟的洪泛区与1993年8月暴雨造成的洪泛区几乎相同,但水深更深。在被淹后,流速较高,但在大部分被淹区域,流速在1 ~ 2小时后减慢至0.05 m/s左右。所以居民不能步行到那里避难,除非他们在洪水早期避难。居民能否安全地步行避难很大程度上取决于他们的身高,而他们可以安全行走的区域受到身高的限制。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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