Estimating peak flow of Farahzad River in Tehran under climate change and debris flow scenarios: A novel approach and its implications for urban flood hazard mapping

Maryam Masoumi, Amin Sarang, M. Ardestani, Mohammad Hossein Niksokhan
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Abstract

Urban river flooding is a serious threat to cities that have altered their river buffer zones due to urbanization and climate change. This study aims to estimate the peak flow of urban rivers by considering the effects of climate change and debris flow on flood hazard. A novel approach is proposed that integrates hydrological, sedimentological, and hydraulic method and models to account for the influence of sediment volume, woody debris, and culvert blockage on peak flow estimation and flow parameters. The approach is applied to the Farahzad River basin in Tehran, Iran, using future data downscaled from a global climate model under the RCP8.5 scenario for 50- and 100-year return periods. The results show a significant increase in the peak flood discharge by nearly 3.2 times, the flood zone by 10–20%, the flood velocity by 15–30%, and the inundation depth by 10–40% due to climate change and debris flow scenarios. The study demonstrates the importance of considering multiple factors in estimating the peak flow of urban rivers and provides a useful tool for urban flood risk management.
估算气候变化和泥石流情景下德黑兰 Farahzad 河的峰值流量:新方法及其对城市洪水灾害绘图的影响
由于城市化和气候变化,城市河流缓冲区发生了变化,城市河流洪水对城市构成了严重威胁。本研究旨在通过考虑气候变化和泥石流对洪水危害的影响来估算城市河流的洪峰流量。研究提出了一种新方法,该方法综合了水文、沉积学和水力方法和模型,以考虑沉积物量、木质碎屑和暗渠堵塞对洪峰流量估算和流量参数的影响。该方法应用于伊朗德黑兰的 Farahzad 河流域,使用的是 RCP8.5 情景下全球气候模型缩减的 50 年和 100 年重现期未来数据。结果表明,在气候变化和泥石流情景下,洪峰流量将大幅增加近 3.2 倍,洪泛区增加 10-20%,洪流速度增加 15-30%,淹没深度增加 10-40%。这项研究表明,在估算城市河流的洪峰流量时必须考虑多种因素,并为城市洪水风险管理提供了有用的工具。
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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