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- W1531717413 abstract "Risk zonation maps are mostly derived from single design floods which represent a hazard based on a specified return period. The respective delineation of inundated areas and the estimation of flow depths and flow velocities are fundamental inputs for flood risk estimation of exposed objects. For this purpose in most cases 2D hydrodynamic unsteady models are applied (BMFLUW, 2006 a). In the frame of state of the art approaches it is implicitly assumed that the morphology will not change; neither during flood events nor by long term erosion or deposition. However, alluvial river beds are subjected to severe morphological changes during floods which have significant implications for the water level (Nachtnebel & Debene, 2004). It is therefore obvious that the river bed elevation can change quickly and drastically (Neuhold et al., 2009). Observed morphological developments during and after flood events (Fig.1) indicate, to some extent, tremendous changes in river bed elevation due to sediment transport, log jam, rock jam, land slide, etc." @default.
- W1531717413 created "2016-06-24" @default.
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- W1531717413 date "2011-09-30" @default.
- W1531717413 modified "2023-10-18" @default.
- W1531717413 title "Integrating River Bed Dynamics to Flood Risk Assessment" @default.
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- W1531717413 doi "https://doi.org/10.5772/20307" @default.
- W1531717413 hasPublicationYear "2011" @default.
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