Core Concepts
GeoFlood is a powerful computational model for accurately predicting flood wave propagation on complex terrain, validated through benchmark tests and historical dam break simulations.
Abstract
The content discusses the development and validation of GeoFlood, a computational model for overland flooding. It covers the background, methodology, benchmark tests, numerical methods, adaptive mesh refinement, and simulation results for various scenarios including dam breaks. The model's efficiency and accuracy in predicting flood extents are highlighted through comparisons with other models like HEC-RAS and GeoClaw.
1. Introduction to GeoFlood:
Presents a new open-source software package for solving shallow water equations on mapped grids.
Validates the GeoFlood model against standard benchmark tests and historical dam break events.
2. Software for Modeling Overland Flooding:
Discusses fundamental building libraries like Clawpack, p4est, and ForestClaw used in GeoFlood.
3. Numerical Methods for Overland Flooding:
Explains the governing equations of shallow water wave equations and finite volume discretization techniques.
4. Adaptive Mesh Refinement Using Quadtree Meshing:
Describes the multi-resolution grid hierarchy in ForestClaw using non-overlapping fixed-sized grids stored as leaves in a quadtree forest.
5. Benchmark Test Cases:
Evaluates GeoFlood's performance in filling floodplain depressions, speed of flood propagation, and dam break simulations.
Compares simulation results with HEC-RAS and GeoClaw to validate accuracy.
6. Malpasset Dam Break Simulations:
Details the historical background of the Malpasset Dam failure event.
Discusses topography data, initial conditions, simulation results, validation against field observations, Google Earth visualization, parallel efficiency analysis.
Stats
The potential Mosul dam failure could cause catastrophic floods affecting millions of people (Filkins, 2016).
The Malpasset dam failure resulted in 433 fatalities and significant infrastructure damages (Boudou et al., 2017).