2003
DOI: 10.1002/hyp.1201
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Two‐dimensional hydraulic flood modelling using a finite‐element mesh decomposed according to vegetation and topographic features derived from airborne scanning laser altimetry

Abstract: Abstract:Airborne scanning laser altimetry (LiDAR) is an important new data source that can provide two-dimensional river flood models with spatially distributed floodplain topography for model bathymetry, together with vegetation heights for parameterization of model friction. Methods are described for improving such models by decomposing the model's finite-element mesh to reflect floodplain vegetation features such as hedges and trees having different frictional properties to their surroundings, and signific… Show more

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Cited by 143 publications
(115 citation statements)
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“…Although for LiDAR data, automated algorithms to remove Earth surface features are routinely and successfully applied (e.g., Cobby et al, 2001Cobby et al, , 2003, SAR height data prove far more challenging given the inherent errors in the data and only limited progress has been achieved over recent years, often using ancillary data sets or models (e.g., Baugh et al, 2013).…”
Section: Sar Dem Generationmentioning
confidence: 99%
“…Although for LiDAR data, automated algorithms to remove Earth surface features are routinely and successfully applied (e.g., Cobby et al, 2001Cobby et al, , 2003, SAR height data prove far more challenging given the inherent errors in the data and only limited progress has been achieved over recent years, often using ancillary data sets or models (e.g., Baugh et al, 2013).…”
Section: Sar Dem Generationmentioning
confidence: 99%
“…For example, Cobby et al (2003) refine the mesh in areas of significant variations of roughness. Bates et al (2003) build an optimized mesh that incorporates "topographically significant points" and use, as CaviedesVoullième et al (2012), vertical curvature as an indicator of areas to refine.…”
Section: Refining the Meshmentioning
confidence: 99%
“…Elevation data for the calculation grid were configured using aerial lidar (light detection and ranging) for the riverside region, and a 50 m grid DEM (digital elevation model) was utilized for the intermountain area. A comparatively small grid size (3 m for the length of a side of a triangle) was used around the river and the railway to represent the details of the topography Cobby et al, 2003;Rath and Bajat, 2004). In the mountain area, a larger grid size (40 m in length) was used to reduce computational load.…”
Section: (A) Asa River Modelmentioning
confidence: 99%