Response and Recovery in India after the December 2004 Great Sumatra Earthquake and Indian Ocean Tsunami

2006 ◽  
Vol 22 (3_suppl) ◽  
pp. 731-758 ◽  
Author(s):  
C. V. R. Murty ◽  
Sudhir K. Jain ◽  
Alpa R. Sheth ◽  
Arvind Jaiswal ◽  
Suresh R. Dash
Keyword(s):  
Indian Ocean ◽  
Indian Ocean Tsunami ◽  
Sumatra Earthquake ◽  
Andaman And Nicobar Islands ◽  
2004 Indian Ocean Tsunami ◽  
Relief Work ◽  
Response And Recovery ◽  
Nicobar Islands ◽  
The Government ◽  
Rescue And Relief

The rescue and relief work undertaken in the Andaman and Nicobar islands and in mainland India after the 26 December 2004 Indian Ocean tsunami was massive. A number of new initiatives undertaken by the government and nongovernmental agencies were innovative and successful. Also, since the tsunami was not a typical disaster for India, it raised a number of new concerns related to reconstruction along the coast.

Landscape Changes in the Andaman and Nicobar Islands (India) after the December 2004 Great Sumatra Earthquake and Indian Ocean Tsunami

2006 ◽  
Vol 22 (3_suppl) ◽  
pp. 43-66 ◽  
Author(s):  
Javed N. Malik ◽  
C. V. R. Murty ◽  
Durgesh C. Rai
Keyword(s):  
Indian Ocean ◽  
Built Environment ◽  
Plate Tectonics ◽  
Tsunami Wave ◽  
Indian Ocean Tsunami ◽  
Sumatra Earthquake ◽  
Landscape Changes ◽  
Andaman And Nicobar Islands ◽  
Nicobar Islands ◽  
Reconnaissance Surveys

Plate tectonics after the 26 December 2004 Great Sumatra earthquake resulted in major topological changes in the Andaman and Nicobar islands. Aerial and land reconnaissance surveys of those islands after the earthquake provide evidence of spectacular plate tectonics that took place during the earthquake. Initial submergence of the built environment and the subsequent inundation upon arrival of the tsunami wave, as well as emergence of the new beaches along the islands—particularly on the western rims of the islands and in the northern islands—are the major signatures of this Mw=9.3 event.

The Effect of the December 2004 Great Sumatra Earthquake and Indian Ocean Tsunami on Transportation Systems in India's Andaman and Nicobar Islands

2006 ◽  
Vol 22 (3_suppl) ◽  
pp. 561-579 ◽  
Author(s):  
Durgesh C. Rai ◽  
C. V.R. Murty ◽  
Sudhir K. Jain ◽  
Hemant B. Kaushik ◽  
Goutam Mondal ◽  
...  
Keyword(s):  
Working Condition ◽  
Transportation Systems ◽  
Indian Ocean Tsunami ◽  
Andaman Islands ◽  
Sumatra Earthquake ◽  
Andaman And Nicobar Islands ◽  
Ground Shaking ◽  
Major Disaster ◽  
Trunk Road ◽  
Nicobar Islands

Boats and ships are the major modes of transportation among the Andaman and Nicobar group of islands. The Andaman Trunk Road also forms an important part of the transportation system in the Andaman Islands north of Port Blair. The harbor structures in the islands were the most affected during the ground shaking; the result heavily disrupted the lives of the island residents. These transportation systems are expected to be in working condition after a major disaster, to facilitate the search and rescue operations and the relief work in the affected areas. A reconnaissance team surveyed the damage that the 2004 earthquake and tsunami caused to the transportation structures in the islands. Damage was observed in all transportation systems, including harbors, highways, airports, and hangars.

Lifeline Systems in the Andaman and Nicobar Islands (India) after the December 2004 Great Sumatra Earthquake and Indian Ocean Tsunami

2006 ◽  
Vol 22 (3_suppl) ◽  
pp. 581-606 ◽  
Author(s):  
Alex Tang ◽  
Durgesh C. Rai ◽  
David Ames ◽  
C. V. R. Murty ◽  
Sudhir K. Jain ◽  
...  
Keyword(s):  
Transmission Lines ◽  
Indian Ocean Tsunami ◽  
Sumatra Earthquake ◽  
Andaman And Nicobar Islands ◽  
Ground Shaking ◽  
Tsunami Waves ◽  
Electric Power Supply ◽  
Power Stations ◽  
Nicobar Islands ◽  
Lifeline Systems

Lifeline systems in the Andaman and Nicobar islands performed poorly during the December 2004 Great Sumatra earthquake and tsunami. Several power stations and transmission lines were damaged by the ground shaking, affecting the electric power supply to parts of the islands. Telecommunication services were severely affected because of destruction of several telephone exchanges. These services were restored quickly by government agencies. The dams and reservoirs, which supply potable water, sustained minor damage from ground shaking. However, segmented pipelines connecting the dams and reservoirs to various storage sites broke at several places, which significantly affected the water supply for a few days. Ground shaking damaged several elevated as well as ground-supported storage tanks. Damage related to tsunami waves was substantial in the 500–1,000- m strip immediately next to the coastline.

scholarly journals RECOVERY CURVES FOR HOUSING RECONSTRUCTION IN SRI LANKA AFTER THE 2004 INDIAN OCEAN TSUNAMI

2010 ◽  
Vol 04 (02) ◽  
pp. 51-60 ◽  
Author(s):  
OSAMU MURAO ◽  
HIDEAKI NAKAZATO
Keyword(s):  
Sri Lanka ◽  
Indian Ocean ◽  
Disaster Recovery ◽  
Recovery Process ◽  
Indian Ocean Tsunami ◽  
Quantitative Methodology ◽  
2004 Indian Ocean Tsunami ◽  
Recovery Curves ◽  
The Government ◽  
Post Disaster

On the 26th of December 2004, the Tsunami damaged to five provinces in Sri Lanka and more than 40,000 people were displaced, lost, or killed within a short time. After the tsunami, the Government provided three types of houses for the victims (temporary shelters, transitional houses, and permanent houses). The authors conducted several field surveys and interviews in the damaged area to investigate the recovery conditions, and obtained dataset, which had been collected for 13 months since December 2004 by Rebuilding and Development Agency. It shows the construction status of transitional house and permanent house in the damaged areas. This paper demonstrates recovery curves for the transitional houses and the permanent houses. With the aim of constructing post-earthquake recovery curves for Sri Lanka, the factors of time (months) and completion ratio of building construction are used. The obtained curves quantitatively clarify the regional differences in the completion dates and processes of construction. The proposed quantitative methodology will be used for other damaged countries due to the 2004 Indian Ocean Tsunami. It means that this kind of analysis is essential for investigating post-disaster recovery process because it enables comparative studies of urban/rural planning among different types of post-disaster recovery processes throughout the world.

The Impact of the December 2004 Indian Ocean Tsunami on Tourism in Thailand

2006 ◽  
Vol 22 (3_suppl) ◽  
pp. 889-900 ◽  
Author(s):  
Thomas A. Birkland ◽  
Pannapa Herabat ◽  
Richard G. Little ◽  
William A. Wallace
Keyword(s):  
Indian Ocean ◽  
Perceived Risk ◽  
Tourism Industry ◽  
Indian Ocean Tsunami ◽  
2004 Indian Ocean Tsunami ◽  
Southern Thailand ◽  
Physical Infrastructure ◽  
Vertical Evacuation ◽  
Response And Recovery ◽  
The Impact

The 26 December 2004 Indian Ocean tsunami appears to have reduced tourist visits to southern Thailand and particularly to the provinces of Phuket and Phang Nga. In Thailand, a much higher proportion of the tsunami victims were tourists than in other affected nations. Also, the tourism industry, which is a major source of foreign exchange, is very sensitive to the perception of risk created by disasters like this tsunami. Although revenues may remain depressed for some time, it is likely that tourism will rebound in this region because of the attractiveness of the physical amenity and the value it offers for European tourists. Damage to the physical infrastructure did not serve as a substantial impediment to response and recovery. Information and warning systems, together with buildings that afford vertical evacuation, will protect lives and reduce perceived risk.

Observed Reconstruction of Houses in Aceh Seven Months after the Great Sumatra Earthquake and Indian Ocean Tsunami of December 2004

2006 ◽  
Vol 22 (3_suppl) ◽  
pp. 803-818 ◽  
Author(s):  
Teddy Boen
Keyword(s):  
Indian Ocean ◽  
Natural Disasters ◽  
Local Culture ◽  
Indian Ocean Tsunami ◽  
Sumatra Earthquake ◽  
Modern History ◽  
Earthquake Resistant ◽  
The World ◽  
Rescue And Relief ◽  
Relief Efforts

The 26 December 2004 earthquake ( Mw=9.2) that shook Aceh and the subsequent tsunami catastrophe was one of the worst natural disasters in modern history. The world—governments and people—responded with unprecedented generosity in solidarity with the rescue and relief efforts of the affected communities and local and national authorities. This response has been very useful in reducing or mitigating the consequences of the disaster, and particularly in speeding the current recovery and reconstruction efforts. In the wake of the recovery and reconstruction of houses in Aceh, many NGOs and donors tried to introduce house types that defy the local culture with respect to earthquake-resistant houses and that also neglect social problems.

Medieval forewarning of the 2004 Indian Ocean tsunami in Thailand

Nature ◽  
2008 ◽  
Vol 455 (7217) ◽  
pp. 1228-1231 ◽  
Author(s):  
Kruawun Jankaew ◽  
Brian F. Atwater ◽  
Yuki Sawai ◽  
Montri Choowong ◽  
Thasinee Charoentitirat ◽  
...  
Keyword(s):  
Indian Ocean ◽  
Indian Ocean Tsunami ◽  
2004 Indian Ocean Tsunami

A snapshot of the 2004 Indian Ocean tsunami: societal impacts and consequences

2006 ◽  
Vol 15 (1) ◽  
pp. 163-177 ◽  
Author(s):  
Havidan Rodriguez ◽  
Tricia Wachtendorf ◽  
James Kendra ◽  
Joseph Trainor
Keyword(s):  
Indian Ocean ◽  
Indian Ocean Tsunami ◽  
2004 Indian Ocean Tsunami ◽  
Societal Impacts

Myanmar Coastal Area Field Survey after the December 2004 Indian Ocean Tsunami

2006 ◽  
Vol 22 (3_suppl) ◽  
pp. 285-294 ◽  
Author(s):  
Tint Lwin Swe ◽  
Kenji Satake ◽  
Than Tin Aung ◽  
Yuki Sawai ◽  
Yukinobu Okamura ◽  
...  
Keyword(s):  
Indian Ocean ◽  
Real Time ◽  
West Coast ◽  
Coastal Area ◽  
Field Survey ◽  
Indian Ocean Tsunami ◽  
Sumatra Earthquake ◽  
The West ◽  
Tide Level ◽  
The Indian Ocean

A post-tsunami survey was conducted along the Myanmar coast two months after the 2004 Great Sumatra earthquake ( Mw=9.0) that occurred off the west coast of Sumatra and generated a devastating tsunami around the Indian Ocean. Visual observations, measurements, and a survey of local people's experiences with the tsunami indicated some reasons why less damage and fewer casualties occurred in Myanmar than in other countries around the Indian Ocean. The tide level at the measured sites was calibrated with reference to a real-time tsunami datum, and the tsunami tide level range was 2–3 m for 22 localities in Myanmar. The tsunami arrived three to four hours after the earthquake.

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