This paper provides an overall review of tsunami research, mainly in the detection and measurement of tsunami waves in the deep ocean. New tsunami magnitude scales will be discussed; it will be shown that the travel-time charts presently in use operationally by Tsunami Warning Centers in Honolulu and Palmer contain substantial errors.
Tsunami in in Thailand 2004 The tsunami in Thailand that occurred on December 26, 2004, was by far the largest tsunami catastrophe in human history. It was triggered by a magnitude 9.1-9.3 earthquake along the Indian-Australian seduction zone off the northern coast of Sumatra.
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Thailand was one of the countries that was hit by the 2004 Indian Ocean earthquake and tsunami.Due to proximity of the Andaman coasts of Thailand situated just about 500 km east of the earthquake epicentre, the tsunami took just 2 hours to reach and strike the western coastline of the country.
The tsunami that struck New Guinea on July 17, 1998 was the most devastating tsunami since the 1976 Moro Gulf, Philippines, tsunami and may surpass that event (Lockridge and Smith, 1984; Satake and Imamura, 1995). The high reported runups and the tremendous loss of life are of great concern to all, including the international scientific community.
But after appreciating the losses that occur, the researcher posits that there are ways of making returns and gains from the tsunamis. In the light of this, the research was prepared with the aim of finding ways in which residents of Ban Talae Nok in Thailand which was severely hit by the 2004 Indian Ocean earthquake and tsunami can turn the disaster into a profitable tourist attraction.
The 2004 Banda Aceh earthquake and ensuing Andaman mega tsunami that killed a quarter million people worldwide is a wake-up call to many. Active research was initiated in Universiti Sains Malaysia (USM) immediately after the infamous event with the aims to help develop human capacity and resources, and to mitigate any future earthquake and tsunami.
Research Proposal on Tsunami in Indian Ocean in 2004 Assignment While a tsunami is a natural event and hard to predict, many reports and studies of the events of December, 2004 suggest that much more could have been done to reduce the loss of life and damage to property through there use of a more adequate early warning systems.
Tsunami victims suffer psychology problems in the days and weeks after the destruction. This could even continue for years - often their entire lifetime. A study by the World Health Organisation on survivors of the tsunami in Sri Lanka on December 24 2004 found that three to four weeks after the tsunami between 14 and 39 per cent of the children had post traumatic stress disorder (PTSD).
This paper presents a methodology for tsunami risk assessment, which was applied to a case study in Kamakura, Japan. This methodology was developed in order to evaluate the effectiveness of a risk-reducing system against such hazards, also aiming to demonstrate that a risk assessment is possible for these episodic events. The tsunami risk assessment follows these general steps: (1.
Media Coverage and Charitable Giving After the 2004 Tsunami Philip H. Brown, Jessica H. Minty Goldfarb Center Working Paper No. 2006-002 June 2006 ABSTRACT Media coverage of humanitarian crises is widely believed to influence charitable giving, yet this assertion has received little empirical scrutiny. Using Internet donations after the 2004.
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An earthquake can trigger many sudden changes in the environment which can be classified as primary (e.g. subsidence, surface faulting) and secondary effects (displaced rocks, tsunami, ground.
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This paper reports on an attempt to test the latter approach. It discusses the out-come of a pilot study of adaptive capacity among Thai residents affected by the 2004 tsunami. The impact of the 2004 tsunami in Thailand The economy in the tsunami-affected provinces studied here (Figure 1) is driven by tourism, small-scale fisheries, shrimp.
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The tsunami wave, generated by the earthquake in Japan on March 11, 2011, hit the west coast of the United States many hours later. The Santa Cruz Yacht Harbor in Santa Cruz, California (pictured above, at the Murray Street bridge) experienced seiching, in which the tsunami wave oscillates in the constricted channel of the harbor from a few minutes to a few hours.
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At least 350 people are dead and hundreds missing after a tsunami caused by a huge 8.9-magnitude quake devastated north-east Japan.