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Correlation Between Coastal Geomorphology and Tsunami Inundation Along the Coast of Kanyakumari,India

Correlation Between Coastal Geomorphology and Tsunami Inundation Along the Coast of Kanyakumari,India
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摘要 An investigation has been carried out in the vicinity of the coastal villages of Kanyakumari District,India to decode the influence of coastal geomorphology on inundation degree and run-up level.Even though the tsunami waves approach the study area in different patterns,the consequences are found to be mainly dependent upon the coastal configuration and local geographic setting,the study area are considered to be of three types based upon the geomorphic arrangement,namely shallow coast,elevated coast and estuarine coast.The inundation and run-up level vary from coast to coast even though there is no remarkable variation in the intensity of the approaching tsunami surge.The inundation extent ranges from to 54 m to 413 m with maximum along estuarine coast and minimum along elevated coast.Estuarine coast recorded the maximum run-up level of about 6 m and the minimum of about 1 m along the elevated coast.The percentage of inundated area in the total coastal area varies between 19% to 10% along estuarine coast and elevated coast respectively.Inundation and run-up level cannot be appreciable in the inland along the elevated coast.The beaches of elevated coast are less affected whereas those of estuarine coast are highly affected.Inundation is limited in the elevated beaches along the study area. An investigation has been carried out in the vicinity of the coastal villages of Kanyakumari District,India to decode the influence of coastal geomorphology on inundation degree and run-up level.Even though the tsunami waves approach the study area in different patterns,the consequences are found to be mainly dependent upon the coastal configuration and local geographic setting,the study area are considered to be of three types based upon the geomorphic arrangement,namely shallow coast,elevated coast and estuarine coast.The inundation and run-up level vary from coast to coast even though there is no remarkable variation in the intensity of the approaching tsunami surge.The inundation extent ranges from to 54 m to 413 m with maximum along estuarine coast and minimum along elevated coast.Estuarine coast recorded the maximum run-up level of about 6 m and the minimum of about 1 m along the elevated coast.The percentage of inundated area in the total coastal area varies between 19% to 10% along estuarine coast and elevated coast respectively.Inundation and run-up level cannot be appreciable in the inland along the elevated coast.The beaches of elevated coast are less affected whereas those of estuarine coast are highly affected.Inundation is limited in the elevated beaches along the study area.
出处 《Journal of Ocean University of China》 SCIE CAS 2012年第1期1-6,共6页 中国海洋大学学报(英文版)
基金 the National Resource Data Management System (NRDMS) Division of the Department of Science and Technology (DST) Government of India for supplying the necessary equipment and financial assistance
关键词 tsunami India coast geomorphology inundation 河口海岸 沿海地区 淹没 海啸 地貌 马里 印度 淹水程度
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  • 1Chandrasekar,N.,and Immanuel,J.L.,2005.GIS supported categorisation of tsunami experienced beaches along the southern east coast of India:usage in mitigation activities.Proceeding of the National Seminar on GIS Application in Rural Development.Hyderabad,India,349-362.
  • 2Chandrasekar,N.,Immanuel,J.J.,Rajarnanickam,M.,Singh,D.S.H.,Sahayam,J.D.,and Rajamanickam,G.V.,2005.Geospatial Assessment of Tsunami (2004) Damages along the rocky coast of Kanyakumari,India.In:Geomatics in Tsunami.Ramasamy,Sm,et al.,eds.,New India Publishing Company,New Delhi,135-146.
  • 3Chandrasekar,N.,Saravanan,S.,Immanuel,J.L.,Rajamanickam,M.,and Rajamanickam,G.V.,2006.Classification of tsunami hazard along the southern coast of India:An initiative to safeguard the coastal environment from similar debacle.Science of Tsunami Hazards,24 (1):3-24.
  • 4Clague,J.J.,Hutchinson,1.,and Lesemarm,J.L.,2005.Tsunami Hazard at the Fraser River delta,British Columbia,Canada.Report for the Corporation of Delta and the City of Richmond,27pp.
  • 5Dawson,A.G.,1994.Geomorphological effects of tsunami run-up and backwash.Geomorphology,10 (1-4):83-94.
  • 6Goff,J.,Dudley,W.C.,Maintenon,M.J.,Cain,G.,and Coney.J.P.,2006.The largest local tsunami in 20th century Hawaii.Marine Geology,226:65-79.
  • 7Grauert,M.,Bjorck,S.,and Bondevik,S.,2001.Storegga tsunami deposits in a coastal lake on Suouroy,the Faroe Islands.Boreas,30 (4):263-271.
  • 8Kench,S.P.,Nichol,S.L.,Mclean,R.F.,Smithers,S.G.,and Brander,R.W.,2007.Impact of the Sumatran Tsunami on the geomorphology and sediments of reef islands:South Maalhosmadulu Atoll,Maldives.Atoll Research Bulletin,544:105-134.
  • 9Kumanan,C.J.,2005.Global scenario of tsunamis.In:Tsunami:The Indian Context.Ramasamy,Sm,and Kumanan,C.J.,eds.,Allied Publishers,New Delhi,15-26.
  • 10Kurian,N.P.,Pillai,A.P.,Rajith,K.,Krishnan,B.T.M.,and Kalaiarasan,P.,2006.Inundation characteristics and geomorphological impacts of December 2004 tsunami on Kerala Coast.Current Science,90 (2):240-249.

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