![]() On the other hand, Digital Elevation Models ( DEM) with resolution adequate for studies of flood propagation are available in many areas of the world. 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. Venant Equations, SVE) is often legitimate and computationally competitive against two-dimensional solvers. In steep mountain valleys, the use of one-dimensional SWE (also known as St. Shallow Water Equations (SWE) provide a fundamental component for the quantification and mapping of hydraulic hazard.
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