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    Effects of Levee Extension on Marsh Flooding

    Source: Journal of Water Resources Planning and Management:;1987:;Volume ( 113 ):;issue: 002
    Author:
    Flora Chu Wang
    DOI: 10.1061/(ASCE)0733-9496(1987)113:2(161)
    Publisher: American Society of Civil Engineers
    Abstract: Western Terrebonne Parish, a low‐lying coastal marsh with numerous meandering bayous and small lakes, is located in south‐central Louisiana. The area is frequently inundated by backwater, tidal, and headwater floodings. An extension of the existing Avoca Island levee is proposed for further providing flood protection to the area. This paper evaluates the potential changes in the hydrologic regime and the area's hydrodynamics caused by the proposed levee extension. The study area is modeled as a network of junctions and channels. Riverine and tidal boundary conditions are used as input to a watershed model that predicts the time history of water level, flow, and sediment of the area. The response of the marsh to flooding events is simulated with both existing and future conditions. The results in terms of surface water contours, current discharge patterns, and sediment concentration distributions are presented. The changes before and after the levee extension are discussed.
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      Effects of Levee Extension on Marsh Flooding

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    contributor authorFlora Chu Wang
    date accessioned2017-05-08T21:06:17Z
    date available2017-05-08T21:06:17Z
    date copyrightMarch 1987
    date issued1987
    identifier other%28asce%290733-9496%281987%29113%3A2%28161%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/38814
    description abstractWestern Terrebonne Parish, a low‐lying coastal marsh with numerous meandering bayous and small lakes, is located in south‐central Louisiana. The area is frequently inundated by backwater, tidal, and headwater floodings. An extension of the existing Avoca Island levee is proposed for further providing flood protection to the area. This paper evaluates the potential changes in the hydrologic regime and the area's hydrodynamics caused by the proposed levee extension. The study area is modeled as a network of junctions and channels. Riverine and tidal boundary conditions are used as input to a watershed model that predicts the time history of water level, flow, and sediment of the area. The response of the marsh to flooding events is simulated with both existing and future conditions. The results in terms of surface water contours, current discharge patterns, and sediment concentration distributions are presented. The changes before and after the levee extension are discussed.
    publisherAmerican Society of Civil Engineers
    titleEffects of Levee Extension on Marsh Flooding
    typeJournal Paper
    journal volume113
    journal issue2
    journal titleJournal of Water Resources Planning and Management
    identifier doi10.1061/(ASCE)0733-9496(1987)113:2(161)
    treeJournal of Water Resources Planning and Management:;1987:;Volume ( 113 ):;issue: 002
    contenttypeFulltext
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