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Apr 26, 2012
Tsunami Inundation and Sediment Transport in Vicinity of Coastal Mangrove Forest
Authors: Guy Gelfenbaum [email protected], Deepak Vatvani [email protected], Bruce Jaffe [email protected], and Frank Dekker [email protected]Author Affiliations
Publication: Coastal Sediments '07
Abstract
Field measurements from Sumatra of tsunami wave height, erosion and deposition form a comprehensive data set that is tested against the Delft3D tsunami inundation and sediment transport model. Relative agreement between measured and modeled maximum water levels and sediment erosion and accumulation provides confidence that the model is reasonably characterizing the important processes of tsunami inundation. Adding a component to account for vegetation, the model is used to explore the effects of fringing mangrove forests on tsunami inundation and sedimentation. In model experiments, mangrove forests modify the water levels and flow speeds reached during tsunami inundation. Simulations with a mangrove forest result in sedimentation in the forest and not erosion, as occurs in the base case with no forest. This difference in sedimentation is important because the change in profile shape increases wave energy reflection off the beach and decreases wave energy penetration onto land.
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© 2007 American Society of Civil Engineers.
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Published online: Apr 26, 2012
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U.S. Geological Survey, 345 Middlefield Rd., MS999, Menlo Park, CA 94025. E-mail: [email protected]
Delft Hydraulics, P.O.Box 177, Delft, The Netherlands. E-mail: [email protected]
U.S. Geological Survey, 400 Natural Bridges Drive, Santa Cruz, CA 95060. E-mail: [email protected]
Delft Hydraulics, P.O.Box 177, Delft, The Netherlands. E-mail: [email protected]
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