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Natural disaster of tsunami have occurred in Indonesia, Thailand, India, the Maldives and Sri Lanka after an earthquake measuring 9.0 on the Richter scale erupted, on Dec 26, 2004 of Sunday morning centered near the Indonesian island of Sumatra. The tsunamis washed away fishing villages and resorts throughout the region. The biggest tsunami on history has hit Aceh on Dec 26, 2004. In Banda Aceh as well as several coastal cities in Aceh, many people are not aware and care about the sign of nature before wave came. On the contrary, in a small island Simelue, the local people were aware of the sign of nature, and they know how to avoid the incoming wave and where to evacuate. The tsunami warning can be circulated via established communication systems to issue timely alarms to permit evacuation of coastal areas. Such high-technology warning system is surely needed high funding. Moreover, the sign of nature from animal behavior can be used potentially as a low-technology warning system t...
Tsunami, 2016
The establishment of the tsunami warning system is based on the fact, that the seismic waves propagate faster then tsunami wave. The tsunami wave arrive in the shore line after the earthquake parameters can be determined, so that there is time left to evaluate the earthquake, whether the earthquake is tsunamigenic or not, disseminated the information or warning to the target area, and finally to do evacuation if necessary. For the tele-tsunami, in which the tsunami will arrive in the beach more then one hour after the origin time of earthquake, generally there is enough time to do all of those processes, so that the warning can be disseminate in 100 % confidence level. For local tsunami, in which the tsunami will arrive in the beach less then one hour, the warning is disseminated in the lower the confidence level. For example, Indonesia Tsunami Warning System (InaTEWS) is designed for local tsunami warning for Indonesian region. Any tsunami-genic earthquake occurs in the Indian Ocean plate boundary, the tsunami wave will sweep the closest shore line within 20-40 minutes after the origin time of the earthquake. The warning is determined just only based on the evaluation of the earthquake parameters and tsunami modeling. It is difficult to add sea level data to increase the confidence level of he warning. Although the confidence level is lower, the tsunami warning could be disseminated. In some cases, especially for the eastern of Indonesia, the tsunami can be generated within inner sea, such as Flores sea, Banda sea, Ceram sea, Maluku sea, and any others. In that cases, tsunami wave will reach the closest shore line within 10 minutes or less. This tsunami may be called as very local tsunami. By evaluating the time line for issuing the tsunami warning, it is clear that very critical to disseminate tsunami warning based on the available technology recently. The effectiveness of the warning is very small, therefore another possibility warning for very local tsunami should be designed. In this presentation, we propose to use natural signs as the warning. As we might know that in general tsunami can be generated by large earthquake. This kind earthquake could be felt strongly by most peoples. This natural sign could be applied as a tsunami warning. The other possibility is to use rather simple technology, as compliment to the natural
Science of Tsunami Hazards, 2019
Effective early warning at local to regional distances is maximum 10 minutes after the OT. The shorter the tsunami early warning time that is announced, of course, the more time the community will have to prepare for mitigating the disaster. The purpose of this study is to develop a tsunami application and show the current real-time data available in most tsunami hazard areas in Indonesia - in particular, earthquake location, magnitude and tsunami discriminant Td, T50Ex, T0, Td x T50, and Td x T0 can be determined about four minutes after the earthquake occurs. This process will be implemented and continues in real-time in earthquake monitoring and tsunami early warning installed by the Meteorology Climatology and Geophysics Council. The availability of this rapid tsunami application (about 4 minutes after the OT) can help in tsunami early warning that is faster and more reliable for short distances to areas that have the potential of having the a tsunami impact. The purpose of this...
Natural Hazards and Earth System Science, 2010
The great Sumatra earthquake (Mw 9.3) of 26th December, 2004, was rated as the world’s second largest recorded earthquake. The tsunami was considered as one of the deadliest natural hazards in the history, killing over 225,000 people in fourteen countries. In response to this disaster, the government of India took up the task of establishing an Early Warning System for Tsunamis. The Makran coast is extremely vulnerable to tsunamis and earthquakes due to the presence of three very active tectonic plates namely, the Arabian, Eurasian and Indian plates. On 28 November 1945 at 21:56 UTC, a massive Makran earthquake generated a destructive tsunami in the Northern Arabian Sea and the Indian Ocean. The tsunami was responsible for loss of life and great destruction along the coasts of Pakistan, Iran, India and Oman. In this paper NAMI-DANCE numerical model has been used to simulate 1945 Makran tsunamigenic source. In this study tsunami early warning system is try to develop by modeling of various tsunami scenarios and the worst case detect for location along coastal area of Gujarat, India. At the time of event, the closest scenario is picked from the database for emergency management of disaster and early warns to coastal community.
Please note that this briefing is based on the limited and incomplete information available to the secretariat at this date.
Procedia Economics and Finance, 2014
It is necessary to conduct a timely and sustainable Early Warning System (EWS) evaluation. The purpose of this study was to evaluate the effectiveness of Tsunami EWS in Aceh, specifically for dissemination and communication element, as well as to provide recommendations for enhancing efforts and strengthen the effectiveness of Tsunami EWS in Aceh. This study was carried out using qualitative and quantitative approaches. A qualitative approach was performed through Focus Group Discussion (FGD) and in-depth interview in order to capture deep information on dissemination and communication effectiveness of Tsunami EWS in Aceh. A quantitative approach was used to quantify the qualitative information from evaluation results. According to the evaluation, the final score obtained was 1,16 with the results of the evaluation were at Level 2, which means Tsunami EWS in Aceh has a progress, but systematic policy and/ or institutional commitment was not existed yet. This study has recommended several efforts need to be done by the Government of Aceh to strengthen and to improve the effectiveness of existing Tsunami EWS in Aceh, especially for dissemination and communication element.
Environmental Hazards, 2019
Aceh province is vulnerable to multiple hazards. Despite improvements in disaster preparedness efforts including the early warning system (EWS) following the catastrophic 2004 earthquaketsunami, ineffective disaster responses still occur here. An EWS is essential to provide early disaster information to people in order to respond appropriately. An integrated EWS consists of risk knowledge; monitoring; dissemination and communication; and response capability elements. This study investigates how Aceh's disaster management and preparedness have evolved since 2004 focusing on its EWS and in particular how the contemporary integrated EWS approach has been incorporated into its development and operation. In-depth interviews, along with review of relevant policy and procedures were conducted to understand current practices and existing governance and structure of EWS design and operation. Findings suggest that a multi-hazard EWS is not well developed and a linear EWS model is prominent. Dissemination and response elements dominate the EWS design and operation with a lack of ongoing risk assessment that incorporates vulnerability concepts and some important governance issues that impact on response and capability. Key recommendations are made for review of policy and practice for Aceh governments at provincial and district levels and other relevant stakeholders to improve the current EWS.
iisee.kenken.go.jp
This study is on how to make the database for tsunami forecast using the tsunami simulation, retrieve and apply it to the Tsunami Early Warning System messages. Firstly, we searched the seismicity around Malaysia and found out the tsunamigenic earthquakes by comparing the earthquake event with the tsunami record. The earthquake events shallower than 100 km and trench area were considered the potential tsunami source. The most appropriate forecast points were determined by setting up and examining candidates along the coast of Malaysia, each of which has 4-minutes, 10-minutes, 20-minutes distance from the coast and they were with the 10-minutes intervals along the coast. Later, magnitude and depth interval are set up by considering the historical events. The magnitude intervals are 6.6, 7.2, 7.8, and 8.4, and depth intervals are 30 km, 50 km, 70 km and 90 km. The tsunami simulation is run for all the set up tsunami source and the result of tsunami height and travel time for all the forecast points are input into the database. The location of tsunami source is calculated using interpolation or extrapolation.
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