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Mesh type tradeoffs in 2D hydrodynamic modeling of flooding with a Godunov-based flow solver

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TLDR
The results point to mesh-type tradeoffs that should be considered in flood modeling applications, and a mixed mesh model formulation with LTS is recommended as a general purpose solver because the mesh type can be adapted to maximize computational efficiency.
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This article is published in Advances in Water Resources.The article was published on 2014-06-01 and is currently open access. It has received 88 citations till now. The article focuses on the topics: Grid & Unstructured grid.

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Citations
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An intercomparison of remote sensing river discharge estimation algorithms from measurements of river height, width, and slope

TL;DR: In this article, the authors evaluated the possibility of estimating discharge in ungauged rivers using synthetic, daily "remote sensing" measurements derived from hydraulic models corrupted with minimal observational errors, and found at least one algorithm able to estimate instantaneous discharge to within 35% relative root-mean-squared error (RRMSE) on 14/16 nonbraided rivers despite out-ofbank flows, multichannel planforms, and backwater effects.
Journal ArticleDOI

A high resolution coupled hydrologic-hydraulic model (HiResFlood-UCI) for flash flood modeling

TL;DR: HiResFlood-UCI as mentioned in this paper was developed by coupling the NWS hydrologic model (HL-RDHM) with the hydraulic model (BreZo) for flash flood modeling at decameter resolutions.
Journal ArticleDOI

Urban flood modeling with porous shallow-water equations: A case study of model errors in the presence of anisotropic porosity

TL;DR: In this paper, anisotropic porosity models are examined in the presence of unevenly spaced obstacles in the cross-flow and along-flow directions, which is common in practical applications.
Journal ArticleDOI

A framework for the case-specific assessment of Green Infrastructure in mitigating urban flood hazards

TL;DR: In this paper, a case-specific assessment of green infrastructure performance in mitigating flood hazard in small urban catchments is presented, where the urban hydrologic modeling tool (MUSIC) is coupled with a fine resolution 2D hydrodynamic model (BreZo) to test to what extent retrofitting an urban watershed with GI, rainwater tanks and infiltration trenches in particular, can propagate flood management benefits downstream and support intuitive flood hazard maps useful for communicating and planning with communities.
Journal ArticleDOI

Is local flood hazard assessment in urban areas significantly influenced by the physical complexity of the hydrodynamic inundation model

TL;DR: In this article, the performance of three different approaches to two-dimensional flood modeling (fully dynamic, diffusive and porosity approaches) have been evaluated with reference not only to the hydrodynamic variables, water depths and velocities, but also focusing the attention on their product and the consequences associated to their different estimations on the vulnerability assessment.
References
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Journal ArticleDOI

Approximate Riemann Solvers, Parameter Vectors, and Difference Schemes

TL;DR: In this article, it is shown that these features can be obtained by constructing a matrix with a certain property U, i.e., property U is a property of the solution of the Riemann problem.
Book ChapterDOI

Triangle: Engineering a 2D Quality Mesh Generator and Delaunay Triangulator

TL;DR: Triangle as discussed by the authors is a robust implementation of two-dimensional constrained Delaunay triangulation and Ruppert's Delaunayer refinement algorithm for quality mesh generation, and it is shown that the problem of triangulating a planar straight line graph (PSLG) without introducing new small angles is impossible for some PSLGs.
Journal ArticleDOI

Drag, turbulence, and diffusion in flow through emergent vegetation

TL;DR: In this article, a model is developed to describe the drag, turbulence and diffusion for flow through emergent vegetation, which for the first time captures the relevant underlying physics, and covers the natural range of vegetation density and stem Reynolds' numbers.
Book

Shock-Capturing Methods for Free-Surface Shallow Flows

TL;DR: In this article, the Shallow Water Equations are expressed as linearised shallow water equations, and the Riemann solver is used to solve the problem of Dam-Break Modelling.
Journal ArticleDOI

The surface gradient method for the treatment of source terms in the shallow-water equations

TL;DR: In this paper, a novel scheme has been developed for data reconstruction within a Godunov-type method for solving the shallow-water equations with source terms, which is suitable for both steady and unsteady flow problems.
Related Papers (5)
Frequently Asked Questions (15)
Q1. What contributions have the authors mentioned in the paper "Mesh type tradeoffs in 2d hydrodynamic modeling of flooding with a godunov-based flow solver" ?

The effect of mesh type on the accuracy and computational demands of a two-dimensional Godunov-type flood inundation model is critically examined. 

Three mesh types are examined including a Cartesian grid, a constrained Delaunay mesh (triangular grid), and a mixed mesh of triangular and quadrilateral cells. 

Two other important considerations in flood modeling include model selection, which bears on structural model errors, and the demands of model set up and parameterization. 

in applications involving natural topography and irregular domain boundaries, there is a benefit to localized refinement in terms of reducing both input data errors (better sampling of topography) and reducing numerical errors, and in this context the unstructured mesh designs prove advantageous. 

Previous studies suggest topographic and hydrologic errors are generally greater than numerical errors in flood prediction models [6], and results here also indicate that numerical errors may be negligible, compared to structural model errors and input data errors, for the purpose of predicting maximum flood heights. 

Field-scale performance is the ultimate goal of flood inundation models, and here attention turns to the Malpasset dam-break flood which is one of the most-studied historical events from a 2D modeling perspective [16,34,40,46,50,51,69,77,84]. 

in rectangular channel geometries, a uniform resolution mesh works well so unstructured meshing capabilities (localized refinement) are not advantageous. 

The impact of LTS on runtimes is greater for the unstructured meshes (factor of 2–3 change) than the Cartesian grid (less than 30% change). 

Topography data used in previous modeling studies is also used here, and consists of a digitized set of 13,541 points taken from a historical 1:20,000 scale topographic map and spaced from 6 to 450 m apart [36]. 

There is no optimal mesh type for flood modeling with Godunov-type shallow-water models, because each element type (e.g., triangle and quadrilateral) is advantageous under different circumstances. 

A 5 m resolution raster DTM was created from these points using the terrain-to-raster tool in ArcGIS (ESRI, Redlands, CA, USA), which was found to be preferable to a TIN structure for representing the channel thalweg. 

To parameterize building drag using Eq. (11), a uniform drag coefficient was used coD ¼ 1Table 4 Properties of meshes, run times for Toce valley test case. 

These classic problems in computational hydraulics test whether a model is capable of resolving trans-critical flows with shocks without spurious oscillations or excessive numerical diffusion. 

This is attributed to the ability of unstructured meshes to locally focus computational resources (local refinement), and the sensitivity of unstructured mesh models to LTS. 

To summarize, this test problem shows that Cartesian meshes are best suited to modeling flows in prismatic channels, and unconstrained Delaunay meshes represent the least accurate alternative.