HR: 0800h
AN: U11A-0814    [Abstracts]
TI: The 2004 Indian Ocean Tsunami in Maldives: waves and disaster affected by shape of coral reefs and islands
AU: * Kan, H
EM: kan@cc.okayama-u.ac.jp
AF: Okayama University, 3-1-1 Tsushima Naka, Okayama, 700-8530 Japan
AU: Ali, M
EM: admin@erc.gov.mv
AF: Environment Research Centre, Jamaluddin Complex, Nikagasmagu, Male, 20167 Maldives
AU: Riyaz, M
EM: maheyriyaz@yahoo.co.uk
AF: Environment Research Centre, Jamaluddin Complex, Nikagasmagu, Male, 20167 Maldives
AB: In Maldives, 39 islands are significantly damaged among 200 inhabited islands and nearly a third of the Maldivian people are severely affected by the Indian Ocean Tsunami in 26 December 2004. We surveyed tsunami impact in 43 islands by measuring island topography and run-up height, interview to local people and mapping of the flooded and destructed areas. The differences in tsunami height and disaster corresponding to the atoll shape and island topography are observed. In the northern atolls, atoll rims consist of many ring-shaped reefs, i.e. miniature atolls called `faro', and interrupted many channels between them. The interrupted atoll rim may play an important role to reducing tsunami run-up height. Severe damage was not observed in the eastern coast of the islands. Beach ridge also contribute to the protection against tsunami. However, in some islands, houses beside the lagoon are damaged by backwashing floodwater from the lagoon. Water marks show the run-up height of ­-1.8m above MSL. The lagoon water-level seems to set-up by tsunami which permeates into the lagoon through the interrupted atoll rim. The disaster was severe at the southern atolls of Meemu, Thaa and Laamu. The higher run-up heights of up to 3.2m above MSL and enormous building damages were observed at the islands on the eastern atoll rims. The continuous atoll rim of these atolls may reinforce tsunami impact at the eastern islands. In addition, tsunami surge washed the islands totally because of low island topography without beach ridge. Significant floodwater from lagoon was not observed in these atolls. It seems the lagoon water-level was not set-up largely. The continuous atoll rim reduces the tsunami influence to the lagoon and the western side of the atolls. The continuity of atoll rim is probably the major factor to cause the difference in water movement, i.e. tsunami run-up and lagoon set-up, which affects the disaster in the islands. Beach ridge contribute to reduce the tsunami impact to the settlement and agricultural land. Our results may elucidate secure atoll and island type to mitigate the risk of future tsunamis on atoll nations/districts in the Pacific and the Indian Ocean.
DE: 4217 Coastal processes
DE: 4220 Coral reef systems (4916)
DE: 4564 Tsunamis and storm surges
SC: Union [U]
MN: Fall Meeting 2005