Publication:
Monitoring coastal change after the tsunami in Thailand

dc.contributor.authorPantanahiran W.
dc.date.accessioned2021-04-05T03:36:51Z
dc.date.available2021-04-05T03:36:51Z
dc.date.issued2014
dc.date.issuedBE2557
dc.description.abstractThe tsunami on December 26, 2004 caused widespread devastation along the coast of Thailand, especially in Ban Nam Khem, Phang Nga province. This disaster claimed more than 941 lives, with 502 other people missing when the storm surge caught the residents of this area. The coastal geomorphology was impacted by this disaster. The objectives of the research were to study the effect of the tsunami on coastal change and the recovery of coastal areas. Six time-series datasets of aerial photographs and satellite images from 2002, 2004, 2005, 2006, 2009, and 2010 were compared using the Geographic Information System (GIS). The results showed the effect of the tsunami on the buildings in the area. Fifty-eight point sixty-three percent of the buildings in the urban area were destroyed by the tsunami and constructions was raised to 103.60% and 197.12% between 2004 and 2010, thus indicating the recovery of the local community. Geomorphological change in Ko Kho Khao (the island) was found after the tsunami disaster, including coastal erosion and coastal deposition. The balance of nature played a major role in controlling the erosion and deposition. The coastal deposits were the highest in 2005; however, deposition was not found in 2004. The erosion rate from 2002-2003 was the highest (48.10 meter per year) and higher than 2003-2004 (39.03 meters per year), 2004-2009 (15.64 meters per year) and 2009-2010 (29.49 meters per year). The coastal area was more severe eroded than the estuary area, and severe coastal erosion caused the loss of coastal area, approximately 0.28 ha. Severe coastal erosion has been repeatedly found since 2005 in the lower part of the area, and hard structures such as concrete seawalls might have been affected by coastal erosion. In addition, extrapolation of coastal erosion at the rate of 30 meters per year showed that the lower part of Ko Kho Khao should disappear in 2015.
dc.format.mimetypeapplication/pdf
dc.identifier.citationIOP Conference Series: Earth and Environmental Science. Vol 17, No.1 (2014)
dc.identifier.doi10.1088/1755-1315/17/1/012108
dc.identifier.issn17551307
dc.identifier.other2-s2.0-84902190909
dc.identifier.urihttps://hdl.handle.net/20.500.14740/7627
dc.rights.holderมหาวิทยาลัยศรีนครินทรวิโรฒ
dc.subject.otherCoastal zones
dc.subject.otherDeposition
dc.subject.otherDisasters
dc.subject.otherGeographic information systems
dc.subject.otherRemote sensing
dc.subject.otherTsunamis
dc.subject.otherAerial Photographs
dc.subject.otherCoastal erosion
dc.subject.otherErosion and deposition
dc.subject.otherGeomorphological change
dc.subject.otherHard structure
dc.subject.otherLocal community
dc.subject.otherSatellite images
dc.subject.otherTsunami disaster
dc.subject.otherErosion
dc.subject.otherAerial photography
dc.subject.otherCoastal erosion
dc.subject.otherCoastal zone management
dc.subject.otherDisaster management
dc.subject.otherEnvironmental monitoring
dc.subject.otherGeomorphology
dc.subject.otherTsunami
dc.subject.otherCentral Region [Thailand]
dc.subject.otherChonburi
dc.subject.otherKhang Khao Island
dc.subject.otherPhangnga
dc.subject.otherSouthern Region
dc.subject.otherThailand
dc.titleMonitoring coastal change after the tsunami in Thailand
dc.typeConference Paper
dspace.entity.typePublication
swu.datasource.scopushttps://www.scopus.com/inward/record.uri?eid=2-s2.0-84902190909&doi=10.1088%2f1755-1315%2f17%2f1%2f012108&partnerID=40&md5=45b4c7b427e7817f5f367152c30b5e61

Files