Case Studies
Sep 29, 2012

Surge Generation Mechanisms in the Lower Mississippi River and Discharge Dependency

Publication: Journal of Waterway, Port, Coastal, and Ocean Engineering
Volume 139, Issue 4

Abstract

The Lower Mississippi River protrudes into the Gulf of Mexico, and manmade levees line only the west bank for 55 km of the Lower Plaquemines section. Historically, sustained easterly winds from hurricanes have directed surge across Breton Sound, into the Mississippi River and against its west bank levee, allowing for surge to build and then propagate efficiently upriver and thus increase water levels past New Orleans. This case study applies a new and extensively validated basin- to channel-scale, high-resolution, unstructured-mesh ADvanced CIRCulation model to simulate a suite of historical and hypothetical storms under low to high river discharges. The results show that during hurricanes, (1) total water levels in the lower river south of Pointe à La Hache are only weakly dependent on river flow, and easterly wind-driven storm surge is generated on top of existing ambient strongly flow-dependent river stages, so the surge that propagates upriver reduces with increasing river flow; (2) natural levees and adjacent wetlands on the east and west banks in the Lower Plaquemines capture storm surge in the river, although not as effectively as the manmade levees on the west bank; and (3) the lowering of manmade levees along this Lower Plaquemines river section to their natural state, to allow storm surge to partially pass across the Mississippi River, will decrease storm surge upriver by 1 to 2 m between Pointe à La Hache and New Orleans, independent of river flow.

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Information & Authors

Information

Published In

Go to Journal of Waterway, Port, Coastal, and Ocean Engineering
Journal of Waterway, Port, Coastal, and Ocean Engineering
Volume 139Issue 4July 2013
Pages: 326 - 335

History

Received: Feb 3, 2012
Accepted: Sep 26, 2012
Published online: Sep 29, 2012
Published in print: Jul 1, 2013

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Authors

Affiliations

P. C. Kerr, M.ASCE [email protected]
P.E.
Graduate Student, Dept. of Civil and Environmental Engineering and Earth Sciences, Univ. of Notre Dame, Notre Dame, IN 46556 (corresponding author). E-mail: [email protected]
J. J. Westerink, M.ASCE
Professor, Dept. of Civil and Environmental Engineering and Earth Sciences, Univ. of Notre Dame, Notre Dame, IN 46556.
J. C. Dietrich
Research Associate, The Institute for Computational Engineering and Sciences, Univ. of Texas at Austin, Austin, TX 78712.
R. C. Martyr, M.ASCE
Graduate Student, Dept. of Civil and Environmental Engineering and Earth Sciences, Univ. of Notre Dame, Notre Dame, IN 46556.
S. Tanaka
Assistant Professor, Earthquake Research Institute, Univ. of Tokyo, Tokyo, Japan.
D. T. Resio
Professor, Dept. of Civil Engineering, Univ. of North Florida, FL 32224.
J. M. Smith, M.ASCE
Research Hydraulic Engineer, Coastal and Hydraulics Laboratory, U.S. Army Engineer Research and Development Center, Vicksburg, MS 39180.
H. J. Westerink
Research Assistant, Dept. of Civil and Environmental Engineering and Earth Sciences, Univ. of Notre Dame, Notre Dame, IN 46556.
L. G. Westerink
Research Assistant, Dept. of Civil and Environmental Engineering and Earth Sciences, Univ. of Notre Dame, Notre Dame, IN 46556.
T. Wamsley, Ph.D.
Chief, Flood and Storm Protection Division, Coastal and Hydraulics Laboratory, U.S. Army Engineer Research and Development Center, Vicksburg, MS 39180.
M. van Ledden
Director, Business Development, Business Line Water, Haskoning Nederland B.V., Postbus 8520, 3009 AM Rotterdam, George Hintzenweg 85, 3068 AX Rotterdam, Netherlands.
W. de Jong
Hydraulic and Morphologic Engineer, Advisory Group Hydraulics & Morphology, Haskoning Nederland B.V., Postbus 151, 6500 AD Nijmegen, Barbarossastraat 35, 6522 DK Nijmegen, Netherlands.

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