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Impacts of Urbanization and Climate Variability on Floods in Northeastern Illinois

机译:城市化和气候变化对伊利诺伊州东北部洪水的影响

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Trend analysis of annual flood peaks on 12 small urbanizing watersheds in northeastern Illinois indicated that annual peaks, and thus frequency and impact of flooding, increased over the past several decades. An increase in flood peaks could be attributed to intensive urbanization and increasing incidences of heavy rainfall. Average urbanization of the 12 watersheds increased significantly from 10.6% in 1954 to 61.8% in 1996. In addition, numerous studies have reported increasing frequency and intensity of heavy rainfall in the region. This outcome is consistent with lower design rainfall estimates produced by older studies, such as U.S. Weather Bureau Technical Paper No. 40 (TP-40), compared to more recent sources, such as National Oceanic and Atmospheric Administration Atlas-14. This study used a design storm approach and the Hydrologic Engineering Center for Hydrologic Modeling System (HEC-HMS) model to calculate design flood peaks. Hydrologic model parameters were calibrated using hourly rainfall-runoff data of two large regional floods, observed in 1954 and 1996 at 12 small urbanizing watersheds in the metropolitan Chicago area. A sensitivity analysis was performed to evaluate the effects of urbanization and climate variability on increasing flood peaks. Results indicated that, on average, urbanization caused a 34% greater increase in peak flows than climate variability. In addition, this study indicated that present discharges are, on average, at least 19% larger than regulatory discharges. Ongoing urbanization may cause flood peaks to become even higher. The proposed framework can be used to provide input for flood study prioritization by comparing published regulatory discharges and flood discharges computed for current conditions, and investigating potential impacts of future land use changes and precipitation on flood peaks.
机译:对伊利诺伊州东北部12个小型城市化集水区的年洪峰趋势分析表明,在过去的几十年中,年洪峰以及洪水的频率和影响都在增加。洪峰的增加可能归因于集约化的城市化和暴雨发生率的增加。 12个流域的平均城市化水平从1954年的10.6%显着提高到1996年的61.8%。此外,许多研究报告称该地区强降雨的频率和强度增加。此结果与较早的研究(例如美国气象局第40号技术文件(TP-40))相比,较之最新的资料(例如美国国家海洋与大气管理局Atlas-14)所得出的设计降雨估算值更低。这项研究使用设计风暴方法和水文工程中心水文建模系统(HEC-HMS)模型来计算设计洪峰。水文模型参数是使用两个大区域性洪水的每小时降雨-径流数据校准的,该数据是在1954年和1996年在大都会芝加哥地区的12个小型城市化集水区观测到的。进行了敏感性分析,以评估城市化和气候变化对洪水高峰的影响。结果表明,平均而言,城市化导致的高峰流量增长比气候多变性大34%。此外,这项研究表明,目前的排放量平均比管制排放量至少大19%。持续的城市化可能导致洪峰达到更高。通过比较已发布的管制排放量和针对当前条件计算的洪水排放量,并调查未来土地利用变化和降雨对洪水高峰的潜在影响,所提出的框架可用于为洪水研究优先级提供输入。

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