REFRACTION OF TSUNAMI WAVES OF 26 DECEMBER 2004, ALONG SOUTHWEST COAST OF INDIA

In this paper the refraction of the tsunami of 26 December 2004, which caused severe damage along the south west coast of India has been studied. Wave refraction diagrams for the possible wave directions indicate convergence around the places like Kolachel, around Kollam and Alappuzha, where greater...

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Main Authors: K.K.Varma, A. Sakkeer Hussain
Format: Article
Language:English
Published: Tsunami Society International 2007-01-01
Series:Science of Tsunami Hazards
Subjects:
Online Access:http://tsunamisociety.org/261Varma.pdf
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author K.K.Varma
A. Sakkeer Hussain
author_facet K.K.Varma
A. Sakkeer Hussain
author_sort K.K.Varma
collection DOAJ
description In this paper the refraction of the tsunami of 26 December 2004, which caused severe damage along the south west coast of India has been studied. Wave refraction diagrams for the possible wave directions indicate convergence around the places like Kolachel, around Kollam and Alappuzha, where greater destructions occurred due to this tsunami and divergence at the places spared by the tsunami. Broad areas vulnerable to tsunamis have been identified. Possible causes for increased destruction in Kolachel at the southern tip of Indian peninsula are discussed. Bottom topography is one of the factors that determine the intensity of the tsunami waves. Bottom steering is caused by the wave refraction. Comparatively gentler sloping topography in a zone north of Kollam at depths beyond 200m and the topographic dome off Kollam appear to have influence on determining the impact of tsunamis.
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spelling doaj.art-a9a9bbc4a8b9436b828cb4ab1af1712b2022-12-21T19:46:12ZengTsunami Society InternationalScience of Tsunami Hazards8755-68392007-01-012614258REFRACTION OF TSUNAMI WAVES OF 26 DECEMBER 2004, ALONG SOUTHWEST COAST OF INDIAK.K.VarmaA. Sakkeer HussainIn this paper the refraction of the tsunami of 26 December 2004, which caused severe damage along the south west coast of India has been studied. Wave refraction diagrams for the possible wave directions indicate convergence around the places like Kolachel, around Kollam and Alappuzha, where greater destructions occurred due to this tsunami and divergence at the places spared by the tsunami. Broad areas vulnerable to tsunamis have been identified. Possible causes for increased destruction in Kolachel at the southern tip of Indian peninsula are discussed. Bottom topography is one of the factors that determine the intensity of the tsunami waves. Bottom steering is caused by the wave refraction. Comparatively gentler sloping topography in a zone north of Kollam at depths beyond 200m and the topographic dome off Kollam appear to have influence on determining the impact of tsunamis.http://tsunamisociety.org/261Varma.pdftsunamitsunami wavestsunami 2004Indiaearthquake
spellingShingle K.K.Varma
A. Sakkeer Hussain
REFRACTION OF TSUNAMI WAVES OF 26 DECEMBER 2004, ALONG SOUTHWEST COAST OF INDIA
Science of Tsunami Hazards
tsunami
tsunami waves
tsunami 2004
India
earthquake
title REFRACTION OF TSUNAMI WAVES OF 26 DECEMBER 2004, ALONG SOUTHWEST COAST OF INDIA
title_full REFRACTION OF TSUNAMI WAVES OF 26 DECEMBER 2004, ALONG SOUTHWEST COAST OF INDIA
title_fullStr REFRACTION OF TSUNAMI WAVES OF 26 DECEMBER 2004, ALONG SOUTHWEST COAST OF INDIA
title_full_unstemmed REFRACTION OF TSUNAMI WAVES OF 26 DECEMBER 2004, ALONG SOUTHWEST COAST OF INDIA
title_short REFRACTION OF TSUNAMI WAVES OF 26 DECEMBER 2004, ALONG SOUTHWEST COAST OF INDIA
title_sort refraction of tsunami waves of 26 december 2004 along southwest coast of india
topic tsunami
tsunami waves
tsunami 2004
India
earthquake
url http://tsunamisociety.org/261Varma.pdf
work_keys_str_mv AT kkvarma refractionoftsunamiwavesof26december2004alongsouthwestcoastofindia
AT asakkeerhussain refractionoftsunamiwavesof26december2004alongsouthwestcoastofindia