A Tsunami Ball Approach to Storm Surge and Inundation: Application to Hurricane Katrina, 2005

Most analyses of storm surge and inundation solve equations of continuity and momentum on fixed finite-difference/finite-element meshes. I develop a completely new approach that uses a momentum equation to accelerate bits or balls of water over variable depth topography. The thickness of the water c...

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Bibliographic Details
Main Author: Steven N. Ward
Format: Article
Language:English
Published: Hindawi Limited 2009-01-01
Series:International Journal of Geophysics
Online Access:http://dx.doi.org/10.1155/2009/324707
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spelling doaj-1d94614bbcb14c89b064417edd9d86632020-11-24T21:23:48ZengHindawi LimitedInternational Journal of Geophysics1687-885X1687-88682009-01-01200910.1155/2009/324707324707A Tsunami Ball Approach to Storm Surge and Inundation: Application to Hurricane Katrina, 2005Steven N. Ward0Institute of Geophysics and Planetary Physics, University of California, Santa Cruz, CA 95064, USAMost analyses of storm surge and inundation solve equations of continuity and momentum on fixed finite-difference/finite-element meshes. I develop a completely new approach that uses a momentum equation to accelerate bits or balls of water over variable depth topography. The thickness of the water column at any point equals the volume density of balls there. In addition to being more intuitive than traditional methods, the tsunami ball approach has several advantages. (a) By tracking water balls of fixed volume, the continuity equation is satisfied automatically and the advection term in the momentum equation becomes unnecessary. (b) The procedure is meshless in the finite-difference/finite-element sense. (c) Tsunami balls care little if they find themselves in the ocean or inundating land. (d) Tsunami ball calculations of storm surge can be done on a laptop computer. I demonstrate and calibrate the method by simulating storm surge and inundation around New Orleans, Louisiana caused by Hurricane Katrina in 2005 and by comparing model predictions with field observations. To illustrate the flexibility of the tsunami ball technique, I run two “What If” hurricane scenarios—Katrina over Savannah, Georgia and Katrina over Cape Cod, Massachusetts.http://dx.doi.org/10.1155/2009/324707
collection DOAJ
language English
format Article
sources DOAJ
author Steven N. Ward
spellingShingle Steven N. Ward
A Tsunami Ball Approach to Storm Surge and Inundation: Application to Hurricane Katrina, 2005
International Journal of Geophysics
author_facet Steven N. Ward
author_sort Steven N. Ward
title A Tsunami Ball Approach to Storm Surge and Inundation: Application to Hurricane Katrina, 2005
title_short A Tsunami Ball Approach to Storm Surge and Inundation: Application to Hurricane Katrina, 2005
title_full A Tsunami Ball Approach to Storm Surge and Inundation: Application to Hurricane Katrina, 2005
title_fullStr A Tsunami Ball Approach to Storm Surge and Inundation: Application to Hurricane Katrina, 2005
title_full_unstemmed A Tsunami Ball Approach to Storm Surge and Inundation: Application to Hurricane Katrina, 2005
title_sort tsunami ball approach to storm surge and inundation: application to hurricane katrina, 2005
publisher Hindawi Limited
series International Journal of Geophysics
issn 1687-885X
1687-8868
publishDate 2009-01-01
description Most analyses of storm surge and inundation solve equations of continuity and momentum on fixed finite-difference/finite-element meshes. I develop a completely new approach that uses a momentum equation to accelerate bits or balls of water over variable depth topography. The thickness of the water column at any point equals the volume density of balls there. In addition to being more intuitive than traditional methods, the tsunami ball approach has several advantages. (a) By tracking water balls of fixed volume, the continuity equation is satisfied automatically and the advection term in the momentum equation becomes unnecessary. (b) The procedure is meshless in the finite-difference/finite-element sense. (c) Tsunami balls care little if they find themselves in the ocean or inundating land. (d) Tsunami ball calculations of storm surge can be done on a laptop computer. I demonstrate and calibrate the method by simulating storm surge and inundation around New Orleans, Louisiana caused by Hurricane Katrina in 2005 and by comparing model predictions with field observations. To illustrate the flexibility of the tsunami ball technique, I run two “What If” hurricane scenarios—Katrina over Savannah, Georgia and Katrina over Cape Cod, Massachusetts.
url http://dx.doi.org/10.1155/2009/324707
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