2010•Advances in Water ScienceRequires access

Two-dimensional modelling of dam-break floods over actual terrain with complex geometries using a finite volume method

Guangming Tan

Open publisher page 2 citations

Abstract

Based the total variation diminishing(TVD) finite volume method,a two-dimensional hydrodynamic model using unstructured triangular meshes is developed for modelling dam-break flooding under actual terrain with complex geometries.Details include uses of the Roe's approximate Riemann solver with the TVD-MUSCL(Monotone Upstream-centered Schemes for Conservation Laws) scheme as well as the procedure of predictor-corrector in time stepping,which can result in a second-order accurate solution for dam-break flows in both time and space.The moving boundary problem is resolved through the introduction of a minimum water depth concept that can efficiently treat the wetting and drying fronts during the model integration.The effect of using different values of the minimum water depth on the simulation of dam-break flows in the dry river bed is examined.We find that the minimum water depth can significantly alter the propagation of flood waves.Model results are also compared to the analytical solution under the idealized conditions,as well as two sets of dam-break data collected from flume experiments.Lastly,the model is validated using a real dam-break case with complex geometric conditions.The model simulation compares well with the observations and the other studies.

About this research paper

What this paper is about

Based the total variation diminishing(TVD) finite volume method,a two-dimensional hydrodynamic model using unstructured triangular meshes is developed for modelling dam-break flooding under actual terrain with complex geometries.Details include uses of the Roe's approximate Riemann solver with the TVD-MUSCL(Monotone Upstream-centered Schemes for Conservation Laws) scheme as well as the procedure of predictor-corrector in time stepping,which can result in a second-order accurate solution for dam-break flows in both time and space.The moving boundary problem is resolved through the introduction of a minimum water depth concept that can efficiently treat the wetting and drying fronts during the model integration.The effect of using different values of the minimum water depth on the simulation of dam-break flows in the dry river bed is examined.We find that the minimum water depth can significantly alter the propagation of flood waves.Model results are also compared to the analytical solution under the idealized conditions,as well as two sets of dam-break data collected from flume experiments.Lastly,the model is validated using a real dam-break case with complex geometric conditions.The model simulation compares well with the observations and the other studies.

Why it matters

OpenAlex reports 2 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Based the total variation diminishing(TVD) finite volume method,a two-dimensional hydrodynamic model using unstructured triangular meshes is developed for modelling dam-break flooding under actual terrain with complex geometries.Details include uses of the Roe's approximate Riemann solver with the TVD-MUSCL(Monotone Upstream-centered Schemes for Conservation Laws) scheme as well as the procedure of predictor-corrector in time stepping,which can result in a second-order accurate solution for dam-break flows in both time and space.The moving boundary problem is resolved through the introduction of a minimum water depth concept that can efficiently treat the wetting and drying fronts during the model integration.The effect of using different values of the minimum water depth on the simulation of dam-break flows in the dry river bed is examined.We find that the minimum water depth can significantly alter the propagation of flood waves.Model results are also compared to the analytical solution under the idealized conditions,as well as two sets of dam-break data collected from flume experiments.Lastly,the model is validated using a real dam-break case with complex geometric conditions.The model simulation compares well with the observations and the other studies.

Key concepts: Total variation diminishing, Dam break, Finite volume method, Riemann solver, Terrain, Shallow water equations, Monotone polygon, Geology

Related papers

Back to paper searchBrowse research topicsOriginal source
Two-dimensional modelling of dam-break floods over actual terrain with complex geometries using a finite volume method — Research Paper | ScholarLens