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dc.contributor.authorHiripong Thepsiriamnuayen_US
dc.contributor.authorNathsuda Pumijumnongen_US
dc.date.accessioned2019-12-03T06:32:25Z-
dc.date.available2019-12-03T06:32:25Z-
dc.date.issued2019en_US
dc.identifier.citationChiang Mai Journal of Science 46, 5 (Sep 2019), 960 - 974en_US
dc.identifier.issn0125-2526en_US
dc.identifier.urihttp://it.science.cmu.ac.th/ejournal/dl.php?journal_id=10248en_US
dc.identifier.urihttp://cmuir.cmu.ac.th/jspui/handle/6653943832/66925-
dc.description.abstractThis paper focuses on the spatial and temporal aspects of rising sea levels on sandy beach erosion in Thailand. The SimCLIM/CoastCLIM model with RCP 2.6 and RCP 8.5 was utilised to forecast changes in sea level and shoreline over the 1940 to 2100 period in Rayong, Nakhon Si Thammarat and Trang. Input parameters underlying the modified Brunn Rule were applied. Sand loss and forced people migration were estimated using fundamental equations. In the 1940 to 1995 period, estimated sea-level rise was 0.14 cm yr-1 and shoreline retreat was 5.33 m yr-1. Sea level is predicted to rise by 124.38 cm by 2100, compared to the 1995 level. Trang is the most vulnerable area with 507.90 m of eroded beaches and 2.15 km2 of sand loss. Rayong’s population is the most susceptible, with 873 people being forced to migrate. These results could be beneficial to national-scale data and adaptation planning processes in Thailand.en_US
dc.language.isoEngen_US
dc.publisherScience Faculty of Chiang Mai Universityen_US
dc.subjectsea-level riseen_US
dc.subjectsandy beach erosionen_US
dc.subjectthe SimCLIM/CoastCLIM modelen_US
dc.subjectsand lossen_US
dc.subjectforced people migrationen_US
dc.titleClimate Change Impact on Sandy Beach Erosion in Thailanden_US
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