Shallow Water Equations (SWE) provide a fundamental component for the quantification and mapping of hydraulic hazard. In steep mountain valleys, the use of one-dimensional SWE (also known as St. Venant Equations, SVE) is often legitimate and computationally competitive against two-dimensional solvers. However, in the same environment, the solution of SVE is hindered by the need of an accurate bathymetric reconstruction, which implies a number of cross sections which cannot be readily acquired by conventional field surveys. On the other hand, Digital Elevation Models (DEM) with resolution adequate for studies of flood propagation are available in many areas of the world. In this paper, I propose to compute cross sections automatically by ope...
Two-dimensional (2D) depth-averaged shallow water equations (SWE) are widely used to model unsteady ...
International audienceThe consequences of rapid and extreme flooding events, such as tsunamis, river...
Abstract: The availability of new technologies far the measurement of surface elevation has addresse...
Coping with the problem of hydraulic risk evaluation in mountain regions requires the development of...
Coping with the problem of hydraulic risk evaluation in mountain regions requires the development of...
Dam-break analysis is of great importance in mountain environment, especially where reservoirs are l...
In hydrological and hydraulic modelling, river geometry is a crucial input data. Recent investigatio...
Most of the recent developments concerning efficient numerical schemes to solve the shallow-water eq...
Most of the recent developments concerning efficient numerical schemes to solve the shallow-water eq...
International audienceRiverbed geometry is crucial information of water flow models. Despite precise...
An important element in hydraulic modelling is the topography data of the riverbed and the floodplai...
It is well known that choosing a suitable set of cross-sections for the representation of the natura...
Dam-break floods on steep slopes occur in diverse settings. They may result from failure of either n...
Hydrological and hydrodynamic models are the practical tool for flood modelling. Watershed delineati...
Extraction of hydrological information from digital elevation models (DEMs) is a required Step When ...
Two-dimensional (2D) depth-averaged shallow water equations (SWE) are widely used to model unsteady ...
International audienceThe consequences of rapid and extreme flooding events, such as tsunamis, river...
Abstract: The availability of new technologies far the measurement of surface elevation has addresse...
Coping with the problem of hydraulic risk evaluation in mountain regions requires the development of...
Coping with the problem of hydraulic risk evaluation in mountain regions requires the development of...
Dam-break analysis is of great importance in mountain environment, especially where reservoirs are l...
In hydrological and hydraulic modelling, river geometry is a crucial input data. Recent investigatio...
Most of the recent developments concerning efficient numerical schemes to solve the shallow-water eq...
Most of the recent developments concerning efficient numerical schemes to solve the shallow-water eq...
International audienceRiverbed geometry is crucial information of water flow models. Despite precise...
An important element in hydraulic modelling is the topography data of the riverbed and the floodplai...
It is well known that choosing a suitable set of cross-sections for the representation of the natura...
Dam-break floods on steep slopes occur in diverse settings. They may result from failure of either n...
Hydrological and hydrodynamic models are the practical tool for flood modelling. Watershed delineati...
Extraction of hydrological information from digital elevation models (DEMs) is a required Step When ...
Two-dimensional (2D) depth-averaged shallow water equations (SWE) are widely used to model unsteady ...
International audienceThe consequences of rapid and extreme flooding events, such as tsunamis, river...
Abstract: The availability of new technologies far the measurement of surface elevation has addresse...