The large-scale impact of climate change to Mississippi flood hazard in New Orleans

T. Driessen, M. Ledden
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引用次数: 7

Abstract

Abstract. The objective of this paper was to describe the impact of climate change on the Mississippi River flood hazard in the New Orleans area. This city has a unique flood risk management challenge, heavily influenced by climate change, since it faces flood hazards from multiple geographical locations (e.g. Lake Pontchartrain and Mississippi River) and multiple sources (hurricane, river, rainfall). Also the low elevation and significant subsidence rate of the Greater New Orleans area poses a high risk and challenges the water management of this urban area. Its vulnerability to flooding became dramatically apparent during Hurricane Katrina in 2005 with huge economic losses and a large number of casualties. A SOBEK Rural 1DFLOW model was set up to simulate the general hydrodynamics. This model included the two important spillways that are operated during high flow conditions. A weighted multi-criteria calibration procedure was performed to calibrate the model for high flows. Validation for floods in 2011 indicated a reasonable performance for high flows and clearly demonstrated the influence of the spillways. 32 different scenarios were defined which included the relatively large sea level rise and the changing discharge regime that is expected due to climate change. The impact of these scenarios on the water levels near New Orleans were analysed by the hydrodynamic model. Results showed that during high flows New Orleans will not be affected by varying discharge regimes, since the presence of the spillways ensures a constant discharge through the city. In contrary, sea level rise is expected to push water levels upwards. The effect of sea level rise will be noticeable even more than 470 km upstream. Climate change impacts necessitate a more frequent use of the spillways and opening strategies that are based on stages.
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气候变化对密西西比河新奥尔良洪水灾害的大规模影响
摘要本文的目的是描述气候变化对新奥尔良地区密西西比河洪水灾害的影响。由于受到气候变化的严重影响,这座城市面临着独特的洪水风险管理挑战,因为它面临着来自多个地理位置(例如庞恰特雷恩湖和密西西比河)和多个来源(飓风、河流、降雨)的洪水灾害。此外,大新奥尔良地区的低海拔和显著的下沉率对该城市地区的水管理构成了高风险和挑战。2005年的卡特里娜飓风造成了巨大的经济损失和大量的人员伤亡,在洪水面前,它的脆弱性变得非常明显。建立SOBEK Rural 1DFLOW模型模拟一般水动力学。该模型包括在大流量条件下运行的两条重要溢洪道。采用加权多准则校准方法对高流量模型进行了校准。2011年的洪水验证表明,对大流量具有合理的性能,并清楚地表明了溢洪道的影响。确定了32种不同的情景,其中包括相对较大的海平面上升和由于气候变化而预期的排放模式的变化。通过水动力模型分析了这些情景对新奥尔良附近水位的影响。结果表明,在高流量期间,新奥尔良不会受到不同排放制度的影响,因为溢洪道的存在确保了通过城市的恒定流量。相反,海平面上升预计会推动水位上升。即使在上游470公里以上,海平面上升的影响也会很明显。气候变化的影响需要更频繁地使用溢洪道和基于阶段的开放策略。
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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来源期刊
Drinking Water Engineering and Science
Drinking Water Engineering and Science Environmental Science-Water Science and Technology
CiteScore
3.90
自引率
0.00%
发文量
3
审稿时长
40 weeks
期刊最新文献
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