Tuesday, 29 April 2014

Indonesian Tsunami



On 26 December 2004 a tsunami occurred in the Indian Ocean, causing terrible damage to the countries surrounding the Ocean and the islands around it. A tsunami is a series of huge waves which are caused by a volcano or earthquake occurring under the ocean. The effects of the earthquake on the ocean cause water to move on a huge amount which, when it reach the shore, has a huge effect on everything in its way. 

This tsunami caused by abduction occurring between two tectonic plates on the ocean floor. The Indio-Australian Plate below the Eurasian Plate sinks into the face of the earth. This caused the sea-floor to goes up and down, causing the earthquake with above 9 grades on earthquake scale and setting off a series of tsunamis along the coasts of all surrounding countries. The epicentre of the earthquake was between the island of Simulate and mainland Indonesia. The Indonesian tsunami is thought to be the 3rd biggest earthquake of all time, killing 280,000 people in 14 countries. The earthquake itself also had the longest duration time ever recorded, of between 8.3 and 10 minutes and it caused the entire planet to vibrate by around 1cm.

Of the fourteen countries affected Indonesia was the worst one with over 160,000 dead; followed by Sri Lanka with 35,000; India with 18,000 and Thailand over 8,000, moreover 1.6 million people were moved from their homes due to the huge damages happened. As well as local residents and tourists from abroad were also killed as many of the areas affected were very popular with tourists. Over 1,000 tourists from Germany and Sweden lost lives along with another 1100 plus from across the rest of the world.   
Many people have asked why there was little time to evacuate areas that were under threat, and why so few people in these areas knew what was happening until it was too late, even though there was a period of several hours following the earthquake, before the impact on land of the tsunami, almost all of the victims were totally unaware of what was coming. there were no tsunami warning systems in the Indian Ocean to detect any problems and therefore warn citizens that they needed to evacuate. While detecting tsunamis is not an easy science, it is possible, but it is expensive to set up the communication systems needed to warn people, especially in such a poor part of the world. Fortunately, following the disaster, the United Nations initiated the set up of an Indian Ocean Tsunami Warning System; and there is now a large network of graphic centers, national warning centers, agencies and deep-ocean stations in place across the Indian Ocean to detect any potential tsunamis and send out warnings to communities.
In the case of the Indonesian disaster, while the tsunami was in the open ocean the waves were less than one meter high which would not cause any alarm at all. However, by the time they had reached the coast, the waves had reached up to 30 meters in height and were travelling at speeds of up to 800 km per hour. It is easy to see why the waves caused such total mess, wiping over 140,000 homes and spreading 3km inland, carrying salt water with them. One of the most weirdest features of the tsunami is the fact that in the few minutes before the tsunami hits the coast and moves ashore (so some time after the earthquake), the sea often goes far out – like a receding tide – and leaves a large area of exposed beach. This happened in the Indonesian case, exposing around 2.5km of beach that would normally have been covered by the sea. Obviously this caused people, especially children, to go onto the beach and collect coral and fish. Sadly this was the most dangerous thing to do as the tsunami causes the sea to swell and rush back onto the coast without warning, almost always sweeping away anyone in its path. Very fortunately, on the island of Simulate which was very close to the epicenter, most of the islanders knew what was happening. This is because the ancestors of the citizens of the island had passed on their knowledge and told stories of a similar incident that had occurred in 1907. This meant that the local people recognized what the receding ocean meant; and moved to the safety of the inland areas. This factor shows that if people in all of the areas that were affected had been better educated in what can happen before a tsunami; and therefore knew the warning signs, perhaps more lives could have been saved.

However, not all tsunamis cause the sea to recede and different parts of the coast affected by the same tsunami may show different behaviors, so this is of course not the whole story. In some incidences there are no coastal warning signs at all and the sea will just swell and produce enormous waves with no retreat, meaning people have little time to flee to safety. Therefore my take on the issue is that the only factor that would have given people a chance to flee would have been a comprehensive early warning system. A full warning system under the ocean would have been able to detect the earthquake under the water and a proper communication system would have allowed the surrounding countries and communities to receive warnings to evacuate. The fact that there was a delay of several hours between the earthquake and the tsunami first striking the coast, means that most if not all of the people who were killed could have evacuated to safer areas. As it was known to be an area that could suffer from earthquakes or tsunamis, the fact that these systems were not in place can only be put down to economic reasons. Fortunately the early warning systems are now in place and hopefully this level of tragedy will not happen again.     


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