首页> 外文期刊>Ecological engineering: The Journal of Ecotechnology >On comparison of peak flow reductions, flood inundation maps, and velocity maps in evaluating effects of restored wetlands on channel flooding
【24h】

On comparison of peak flow reductions, flood inundation maps, and velocity maps in evaluating effects of restored wetlands on channel flooding

机译:比较峰值流量减少,洪水淹没图和速度图在评估恢复湿地对河道洪水的影响方面

获取原文
获取原文并翻译 | 示例
           

摘要

With growing interest in using restored and/or new constructed wetlands as additional flood mitigation systems, it has become essential to investigate the effectiveness of wetlands in reducing the risk of flood hazards. This study examines and compares evaluation techniques based on peak flow estimation, flood inundation area estimation, and velocity maps to assess the performance of wetlands in reducing flood hazards in a Midwestern watershed affected by changing precipitation patterns. School Branch, one of the main branches of Eagle Creek watershed, located in central Indiana, was selected as a study area. A coupled hydrologic-hydraulic model approach was proposed to simulate the outflow generated by various design storms. Then the water profile and water velocity in the river were calculated and finally the inundation and velocity maps were generated. Also, the effect timing of storm on runoff modulated by wetlands was investigated by applying design storms to different months of year. The results of this study show that wetlands can reduce the peak flow up to 42%, flood areas up to 55% and maximum velocity up to 15%. Additionally, a sub-basin that had maximum peak flow reduction for a specific design storm did not necessarily have a simultaneous maximum reduction in flood inundation area, indicating the variability in how wetlands mitigate flooding in different sub-basins of a watershed. Also, deeper wetlands are more effective in reducing the impacts of storms with higher return periods. For example, at the study site, deeper wetlands (D = 1.8 m) were able to reduce peak flows up to 20% for a 500 year storm whereas shallow wetlands (D = 0.5 m) reduced the peak flow by 11% for the same storm. (C) 2014 Elsevier B.V. All rights reserved.
机译:随着人们对使用恢复的和/或新建的湿地作为附加的减灾系统的兴趣日益浓厚,研究湿地在减少洪灾风险中的有效性变得至关重要。这项研究检查和比较了基于峰值流量估算,洪水淹没面积估算和速度图的评估技术,以评估湿地在减少受降雨模式影响的中西部流域减少洪灾危害方面的性能。位于印第安纳州中部的Eagle Creek流域的主要分支之一School Branch被选为研究区域。提出了一种水文-水力耦合模型方法来模拟各种设计风暴产生的流出。然后计算河流中的水剖面和水流速度,最后生成淹没和速度图。此外,通过将设计风暴应用于一年中的不同月份,研究了风暴对湿地调节的径流的影响时间。这项研究的结果表明,湿地可减少峰值流量达42%,洪水区域可降低55%,最大速度可降低15%。此外,对于特定的设计风暴,具有最大峰值流量减少量的次流域不一定有洪水淹没面积的同时最大减少量,这表明湿地减轻流域不同次流域洪水的方式存在差异。而且,更深的湿地在减少高返还期的风暴影响方面更有效。例如,在研究地点,对于500年的暴风雨,较深的湿地(D = 1.8 m)能够将峰值流量减少多达20%,而对于同一湿地,较浅的湿地(D = 0.5 m)可以将峰值流量减少11%风暴。 (C)2014 Elsevier B.V.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号