Energy flux as a tool in locating tsunami secondary sources

The sea levels recorded in the wake of Indian Ocean Tsunami of December 2004 and of the Kuril Island Tsunami of November 2006 show strong tsunami signal enhancement of the late arriving secondary waves. Using these tsunami eventswe demonstrate thatsudden changes caused by higher energy pulses in the...

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Main Author: Zygmunt Kowalik
Format: Article
Language:English
Published: Tsunami Society International 2008-01-01
Series:Science of Tsunami Hazards
Subjects:
Online Access:http://tsunamisociety.org/273Kowalik.pdf
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spelling doaj-eacace35e4284d52af6260fcd20504012021-04-02T07:46:32ZengTsunami Society InternationalScience of Tsunami Hazards8755-68392008-01-01273129Energy flux as a tool in locating tsunami secondary sourcesZygmunt KowalikThe sea levels recorded in the wake of Indian Ocean Tsunami of December 2004 and of the Kuril Island Tsunami of November 2006 show strong tsunami signal enhancement of the late arriving secondary waves. Using these tsunami eventswe demonstrate thatsudden changes caused by higher energy pulses in the intermittent tsunami wave trains can be assessed by energy fluxes. Therefore, to delineate the regions of tsunami wave amplification and travel time we propose to use energy flux.A series of numerical experimentsdefinedinexplicitwaythe bathymetric features which scatter tsunami signal towards ports, like Crescent City. Identification of the distant bathymetric featureswas achievable sincethe energy fluxvectordelineatedthe energy pathways that coupled distant bathymetric features to portslocated thousands of kilometers apart. Calculations of the energy flux vector involves simple formulas based on two components of velocity and sea level. The maximum of the energy flux (which has no directional properties) can be evaluated from the sea level amplitude, hence both observed and computed sea level can be used for this purpose. The main task of this paper is to suggest that tsunami warning and prediction services should use numerical-hydrodynamical models with wider scope of physical processes by incorporating the energy balance equation into presently used tools.http://tsunamisociety.org/273Kowalik.pdftsunamitsunami travel timecomputational methodstsunami propagationtsunami energy flus
collection DOAJ
language English
format Article
sources DOAJ
author Zygmunt Kowalik
spellingShingle Zygmunt Kowalik
Energy flux as a tool in locating tsunami secondary sources
Science of Tsunami Hazards
tsunami
tsunami travel time
computational methods
tsunami propagation
tsunami energy flus
author_facet Zygmunt Kowalik
author_sort Zygmunt Kowalik
title Energy flux as a tool in locating tsunami secondary sources
title_short Energy flux as a tool in locating tsunami secondary sources
title_full Energy flux as a tool in locating tsunami secondary sources
title_fullStr Energy flux as a tool in locating tsunami secondary sources
title_full_unstemmed Energy flux as a tool in locating tsunami secondary sources
title_sort energy flux as a tool in locating tsunami secondary sources
publisher Tsunami Society International
series Science of Tsunami Hazards
issn 8755-6839
publishDate 2008-01-01
description The sea levels recorded in the wake of Indian Ocean Tsunami of December 2004 and of the Kuril Island Tsunami of November 2006 show strong tsunami signal enhancement of the late arriving secondary waves. Using these tsunami eventswe demonstrate thatsudden changes caused by higher energy pulses in the intermittent tsunami wave trains can be assessed by energy fluxes. Therefore, to delineate the regions of tsunami wave amplification and travel time we propose to use energy flux.A series of numerical experimentsdefinedinexplicitwaythe bathymetric features which scatter tsunami signal towards ports, like Crescent City. Identification of the distant bathymetric featureswas achievable sincethe energy fluxvectordelineatedthe energy pathways that coupled distant bathymetric features to portslocated thousands of kilometers apart. Calculations of the energy flux vector involves simple formulas based on two components of velocity and sea level. The maximum of the energy flux (which has no directional properties) can be evaluated from the sea level amplitude, hence both observed and computed sea level can be used for this purpose. The main task of this paper is to suggest that tsunami warning and prediction services should use numerical-hydrodynamical models with wider scope of physical processes by incorporating the energy balance equation into presently used tools.
topic tsunami
tsunami travel time
computational methods
tsunami propagation
tsunami energy flus
url http://tsunamisociety.org/273Kowalik.pdf
work_keys_str_mv AT zygmuntkowalik energyfluxasatoolinlocatingtsunamisecondarysources
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