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Hello. We're H1 Geography students. We're doing a case study on the Indian Ocean Tsunami that occured in 2004. We hope this blog will be of help for you to have a better understanding of the incident. Animation Members Zeenat Beevi Xue Ying Ting Chuan Nur Farhana Credits Layout16thday InspirationM.M. |
Friday, April 2, 2010
/ Hazards Impact of Tsunami on the Heavy Metal Accumulation in Water, Sediments and Fish at Poompuhar Coast, Southeast Coast of India http://www.e-journals.in/PDF/V5N1/16-22.pdf
3:19 AM ! / Mitigation Mangroves and coral reefs
The most immediate need during the destructive event is to rescue those who can be saved. During the tsunami events, some were able to reach out and provide assistance to others, pulling them to safety in a boat, in a tree, in a house left standing. In the immediate aftermath, some were saved by being pulled from the rubble, pulled from the receding water, dug out of still-flowing mud. In the first minutes, this can only be done by those who are there already; in the following hours, help from more organized responders, may be able to extract injured and partially buried people, provide first aid and emotional support for victims. As those in most desperate need have been saved, attention turns to the immediate needs of those injured, traumatized, or separated from loved ones. Medical attention, food, water, cooking, shelter, and basic sanitation arrangements are the most critical priorities. Public education
![]() Hazard mapping
Meeting people’s needs
References Tsunami Evaluation Coalition However, these relief responses were generally not based on joint needs assessments and were not well coordinated, leading to an excess of some interventions such as medical teams, alongside shortages in less accessible areas or less popular sectors such as water supply. The scale of the funding allowed an early shift to rehabilitation and the use of cash assistance programmes. It also acted as a giant lens, highlighting many of the existing problems in humanitarian response systems. The scale of funding also created coordination problems as it increased the number of agencies while removing some of the normal incentives for agencies to engage with coordination mechanisms. Despite the generous response to the tsunami, the appeals-based system for funding humanitarian emergencies is flawed, with a pattern of under-funding humanitarian response in general. This pattern of low funding for most emergencies limits the development of capacity within the international aid system, and makes it difficult for the system to scale-up to respond appropriately to a large emergency such as this. Cleanup and the beginning of recovery Identification of, religious rites for, and burial of the dead, identification and exchange of information about displaced survivors, reduction of dangerous conditions (unstable houses, infrastructure, and so on), and early attempts to restore vital services where possible now become the focus of activity and effort. 1. An operational command (carrying out activities). Unfortunately, the peculiar circumstances of the 2004 South Asian tsunamis create unusually challenging circumstances for the rapid establishment and coordination of relief efforts. In particular, it is difficult to establish effective incident command systems as a result of the following circumstances:
>The tsunamis affected a very large number of different locations along a shoreline stretching for thousands of miles, spreading across about a dozen countries. >Relief efforts will have to be mounted—and locally coordinated—in hundreds of different locations, challenging the capacity to mount teams with incident command experience in so many locations simultaneously. (2) Multiple and confusing jurisdictions. >The impact zone is characterized by many locations with multiple authorities—federal, local, international, community—of many different types—governmental, military, police, paramilitary, public health. >These are now joined by many outside organizations—international NGOs, the U.N., and so on. >Sorting out who is in charge, and of what, and who reports to whom, is challenge. >Incident management experts report that their work is greatly facilitated in locations where clear authority can be established—and delegated to them. >Where authority is multiple, or shared, and contested, it can be exceedingly difficult to coordinate, direct, and distribute aid.
>In the short run, most of the decisions that need to be made are technical and straightforward—people are doing everything they can, with the resources available, to rescue victims, support the injured, and care for traumatized survivors. >As the immediate human needs come to be met, however, and the situation stabilizes, the decisions become more controversial. >While people are generally willing to accept expert guidance and judgment for the technical matters, when it comes to setting longer-term priorities the community will expect to play a more determinative role. >At this point, the political instability of some of the affected areas caused conflict among different groups about who should be consulted and whose priorities should receive the greatest attention. 3:00 AM ! / Predictions Warning System
![]() Seismic monitoring
Animal early warning http://news.nationalgeographic.com/news/2003/11/1111_031111_earthquakeanimals.html
Recurrence interval prediction
Seismic gap
2:41 AM ! Wednesday, March 24, 2010
/ THE INDIAN OCEAN TSUNAMI ![]() INDIAN OCEAN TSUNAMI / 2004 The 2004 Indian Ocean tsunami was due to an earthquake of 9.0 moment magnitude. Singapore, India, Bangladesh, Malaysia, Myanmar, Thailand and Maldives felt the earthquake tremors. Studies have shown that previous great earthquakes and this recent one is due to megathrust motion in the subduction zones. There were many aftershocks felt at the Andaman Islands, the Nicobar Islands and near the region of the original epicentre. Some observers noticed that a tsunami as far as Struisbaai in South Africa where a high tide as high as 1.5 m surged on shore. That is 16 hours after the earthquake and South Africa is very far!! From this earthquake and tsunami, the government has started to install a proper warning system to detect any oceanic earthquake that could trigger another tsunami. 8:51 AM ! / What caused it? WHAT CAUSED IT? The oceanic crust of the Indo-Australian plate is denser and heavier than the continental crust of the Eurasian plate. Therefore, the Indo-Australian plate subducts under the Eurasian plate at the Sunda trench since a very long time ago. The plates move at an average of 60-70 mm per year. Over the years, subduction causes rocks at the subduction zone to bend and energy to be stored in the rocks. When the energy stored in the rock is very high and exceeds the breaking strength of the rock, the rock will break suddenly. This release of energy causes earthquake to occur. Earthquake that occurred during 26 December 2004 caused the Indo-Australian plate to slip 20 meters further below the Eurasian plate. As a result, the Eurasian plate was lifted 5 meters. ![]() This major shift in the plates in turn discharges colossal energy almost equal to the simultaneous explosion of 32,000 A-bombs of Hiroshima size which spread and travelled in the water of the ocean. Consequently, there was a large displacement of water above the shifting plates in the Indian Ocean that began to radiate. In the beginning, the huge waves could not be seen as the water was deep, with a depth of more than 4000 meters. However, the waves were moving at a very fast speed of 500 to 1000 km/h. As the waves neared the coastline, the shallow seafloor caused the waves to slow down but the water collects to form larger, more destructive waves. The waves reaching as high as 24 to 30 meters, travelled inland to cause massive destruction. ![]() 8:19 AM ! Monday, March 22, 2010
/ IMPACTS OF THE TSUNAMI Health Impacts http://www.unep.org/Documents.Multilingual/Default.asp?DocumentID=434&ArticleID=4817&l=en ![]() High levels of nitrates in the groundwater, which pose serious health threats such as ethemoglobinemia to infants and young children, if ingested. Cholera, typhoid and dysentery were prevalent due to contaminated water supplies. Numerous mosquito breeding which hastened the spread of malaria. Malnutrition due to shortage of food aids which cannot reach badly affected areas. Victims suffered severe trauma and anxiety of anticipating another major tsunami. Glossary Aquifers- underground layer of water-bearing permeable rock or unconsolidated materials (gravel, sand, silt, or clay) Ethemoglobinemia- The growth of certain bacteria that readily convert nitrate to nitrite since infants have relatively low acidity in their stomachs compared to adults. ENVIRONMENTAL IMPACT ![]() The spread of solid and liquid waste and industrial chemicals, water pollution and the destruction of sewage collectors and treatment plants threaten the environment Rapid clean-up of affected areas has also resulted in inappropriate disposal methods, including air burning and open dumping, leading to secondary impacts on the environment. Salinisation and contamination of water bodies such as rivers and aquifers due to leakage in sewer tanks affected soil fertility and made its sterile. This affects yield of crops. ECONOMIC IMPACT http://en.wikipedia.org/wiki/2004_Indian_Ocean_earthquake ![]() ![]() Seamen and the coastal fishing communities suffered a plunge in their income uptake due to the damage of fishing gears and boats An estimated 66% of the fishing fleet and industrial infrastructure in coastal regions were damaged by the wave surges which accounts for several millions of dollars Tourist were reluctant to visit unaffected resorts near the disaster stricken area due to psychological fears resulting a drop in tourist arrivals Both the earthquake and the tsunami may have affected shipping in the Malacca Straits by changing the depth of the seabed and by disturbing navigational buoys and old shipwrecks. Compiling new navigational charts may take months or years. 7:40 AM ! / Signs and Warnings ![]() All the victims were taken completely by surprise. There were no tsunami warning systems in the Indian Ocean to detect tsunamis or to warn the general populace living around the ocean. Tsunami detection is not easy because it requires a network of sensors to detect the and the warning system is not entirely reliable. The shortcoming of the warning systems is that it cannot detect sudden waves. Setting up the communications infrastructure to issue timely warnings is a problem particularly for the poorer countires. The first warning sign of a possible tsunami is the earthquake itself. However, tsunami can strike thousands of kilometres away where the earthquake is only felt weakly or not at all. Also, in a few minutes before a tsunami strikes, the sea may recedes temporarily from the coast. However, not all tsunami causes this 'disappearing sea' effect. In some cases, the sea will suddenly rise up without retreating, surprising many people and leave them little time to escape. It is also interesting to note that very few animals were killed by the tsunami. Apparently before the tsunami hits, elephants were seen running to higher ground and dogs refused to go outdoors. It is said that animals can sense when a disaster is coming. In the wake of the 2004 indian ocean tsunami , there is now an awareness of the need for a tsunami warning system for the Indian Ocean. The United Nations started working on an Indian Ocean Tsunami Warning System and by 2005, they had the initial steps in place. Some have even proposed creating a unified global tsunami warning system, to include the Atlantic Ocean and Caribbean. 7:37 AM ! |