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Drinking Water Engineering and Science An interactive open-access journal
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CiteScore value: 2.2
SNIP value: 0.828
SJR value: 0.391
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Volume 6, issue 2
Drink. Water Eng. Sci., 6, 81–87, 2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Young scientists workshop of the International Water Week...

Drink. Water Eng. Sci., 6, 81–87, 2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

  12 Jul 2013

12 Jul 2013

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

T. L. A. Driessen1 and M. van Ledden2 T. L. A. Driessen and M. van Ledden
  • 1Royal HaskoningDHV, Rivers, Deltas & Coasts, Nijmegen, the Netherlands
  • 2Royal HaskoningDHV, Rivers, Deltas & Coasts, Rotterdam, the Netherlands

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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