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    Flood‐plain Delineation in Ice Jam Prone Regions

    Source: Journal of Water Resources Planning and Management:;1984:;Volume ( 110 ):;issue: 002
    Author:
    Richard M. Vogel
    ,
    Jery R. Stedinger
    DOI: 10.1061/(ASCE)0733-9496(1984)110:2(206)
    Publisher: American Society of Civil Engineers
    Abstract: Flood‐plain delineation in ice jam prone regions is in its infancy. A methodology is introduced for incorporating the risk of ice jams into flood‐plain delineations in northern regions of the U.S. The distribution of flood elevations is derived from the marginal probability distributions for ice cover and storm induced (non‐ice) flood elevations. An application indicates that incorporation of the hydraulics of an ice cover into flood‐plain delineations can result in substantial increases in the inundation levels which generally implies a significant increase in the lateral extent of flood‐plain boundaries. These results document the need to consider the probability of ice jam flood events in the computation of annual maximum flood elevation distributions and flood risk in ice jam prone regions.
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      Flood‐plain Delineation in Ice Jam Prone Regions

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    http://yetl.yabesh.ir/yetl1/handle/yetl/38688
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    contributor authorRichard M. Vogel
    contributor authorJery R. Stedinger
    date accessioned2017-05-08T21:06:04Z
    date available2017-05-08T21:06:04Z
    date copyrightApril 1984
    date issued1984
    identifier other%28asce%290733-9496%281984%29110%3A2%28206%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/38688
    description abstractFlood‐plain delineation in ice jam prone regions is in its infancy. A methodology is introduced for incorporating the risk of ice jams into flood‐plain delineations in northern regions of the U.S. The distribution of flood elevations is derived from the marginal probability distributions for ice cover and storm induced (non‐ice) flood elevations. An application indicates that incorporation of the hydraulics of an ice cover into flood‐plain delineations can result in substantial increases in the inundation levels which generally implies a significant increase in the lateral extent of flood‐plain boundaries. These results document the need to consider the probability of ice jam flood events in the computation of annual maximum flood elevation distributions and flood risk in ice jam prone regions.
    publisherAmerican Society of Civil Engineers
    titleFlood‐plain Delineation in Ice Jam Prone Regions
    typeJournal Paper
    journal volume110
    journal issue2
    journal titleJournal of Water Resources Planning and Management
    identifier doi10.1061/(ASCE)0733-9496(1984)110:2(206)
    treeJournal of Water Resources Planning and Management:;1984:;Volume ( 110 ):;issue: 002
    contenttypeFulltext
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