Japan’s earthquake monitoring and tsunami warning system is one of the most sophisticated -- and costliest -- in the world, befitting an economically … Aftershocks continued, many exceeding magnitude-7.0. For that reason, Japan had already introduced a number of defences prior to 2011. contributes on conception, structure and drafting of the article. Nevertheless, ports were pounded by the tsunami and the airport in Sendai was inundated. The great plates are rough and stick together, building up energy that is released as earthquakes. The economic losses reached about 10% of the national budget of the time [4]. Remarkable paradigm shifts in designing coastal protection and disaster mitigation measures were introduced, leading with a new concept of potential tsunami levels: Prevention (Level 1) and Mitigation (Level 2) levels according to the level of ‘protection’. In a subduction zone, one plate slides beneath another into the mantle, the hotter layer beneath the crust. A field survey, Mapping of building damage of the 2011 Tohoku earthquake tsunami in Miyagi prefecture, Developing fragility functions for tsunami damage estimation using numerical model and post-tsunami data from Banda Aceh, Indonesia, Tsunami fragility, a new measure to assess tsunami damage, Lessons from the 2011 Tohoku Earthquake Tsunami disaster, 2003 Near field survey of the 1946 Aleutian tsunami on Unimak and Senak islands, Time and space distribution of Coseismic slip of the 2011 Tohoku earthquake as inferred from Tsunami waveform data, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, Tsunamis: bridging science, engineering and society, www.pari.go.jp/en/files/3653/460607839.pdf, https://www.jstage.jst.go.jp/article/zisin1948/55/4/55_4_389/_article, www2.jpgu.org/meeting/2011/yokou/MIS036-P120.pdf, www.bousai.go.jp/kaigirep/chousakai/tohokukyokun/pdf/sankou.pdf, http://www.bousai.go.jp/kaigirep/chousakai/tohokukyokun/pdf/Report.pdf, www.tsunami.civil.tohoku.ac.jp/hokusai3/J/events/tohoku_2011/model/dcrc_ver1.2.pdf, www.city.sendai.jp/shinsai/shinsaihukkokentou/pdf/keikakushiryou/plan%20English.pdf, www.city.sendai.jp/kurashi/bosai/jishin/_icsFiles/afieldfile/2015/03/24/tebiki-English.pdf, Evolution of tsunami warning systems and products, the 2011 Great East Japan Earthquake and Tsunami disaster, post-disaster recovery and reconstruction. The map was delivered to every household before the 2011 event to announce the tsunami inundation zone in past events, list of evacuation facilities, and brief instructions for earthquake and tsunami preparedness. Tsunami waves smashed the coast, causing massive damage and flooding. Receiving the tsunami warning from JMA, some residents claimed that they thought they were safe based on the 3 m estimation: they did not feel that they had to evacuate, as they felt safe behind a 10 m seawall. [Click here to read an independent report] 1. Revisiting the modern histories of Tohoku tsunami disasters and pre-2011 tsunami countermeasures, we clarified how Japan's coastal communities have prepared for tsunamis. On 6 October 2011, the Ministry of Education, Culture, Sports, Science & Technology published a report of student fatalities and injuries: in total, 635 children, students and teachers were killed by the tsunami, and 221 were injured. There were many earthquake and tsunami-related solutions put into place in Japan both as precautions and direct consequences of the natural disasters. Consequently, the devastated trees headed inland producing large amounts of waste, and may have caused more destruction. How Japan’s Earthquake and Tsunami Warning Systems Work. (b) The extent of the tsunami inundation zone with the measurement of the run-up heights at tsunami inundation limit in Sendai Coast [23].Download figureOpen in new tabDownload powerPoint. In one sense, the belief was right. (b) The map of tsunami inundation extent in the 2011 event (www.gsi.go.jp). East of Japan, the Pacific plate dives beneath the overriding Eurasian plate. 97 0 obj
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1. March 11, 2011 | Infant, Reader's Picks, School Age, Teens, … It lasted 6 minutes. How can we educate children to be prepared? After this tsunami, several villages were relocated to high ground at the personal expenses of individuals or village leaders [5]. by . Figure 5a indicates the plan view for the multiple protection of Sendai city with a 7.2 m seawall and river dyke and 6 m elevated prefectural road. Even now, numerical simulations cannot predict everything that will happen in a disaster. Third, the post-disaster paradigm shifts in reconstruction are discussed through a case study in Sendai city, Miyagi prefecture. The March 11 Tohoku earthquake was caused by thrust faulting at the plate boundary between the Pacific and North American plates as expected. The discussion mainly focuses on structural measures such as seawalls and breakwaters and non-structural measures of … H�l�I��6��>�/���i�E�#. Cause And Effects Of Tsunami In Japan 1294 Words | 6 Pages. %PDF-1.6
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Figure 3. In the 2011 tsunami/earthquake, some damage could have been avoided if Japan were as prepared for the tsunami as they were for the earthquake. Japan is located on the Ring of Fire, an extremely seismically active plate boundary that surrounds the Pacific Ocean. Paleoseismological studies suggested the predecessor of the 2011 Tohoku earthquake had been the 869 Jogan earthquake [13,14]. The devastating tsunami followed by the 2011 Great East Japan Earthquake and Tsunami left many lessons to be learned that have led the paradigm shift of Japan's tsunami disaster management. Second, we revisit the responses to the 2011 event, specifically on the tsunami warning system and efforts to identify the tsunami impacts and lessons learned. … These plans consist of the combination of structural prevention/mitigation, urban planning, preparedness and provide suggestions for land-use management, relocation, housing reconstruction and tsunami disaster mitigation plans. Following the guideline, coastal cities and towns in Japan had prepared tsunami hazard maps with estimated inundation zones, the list of shelters where people could evacuate and instructions on how to survive a tsunami. Japan should use what it already knows and learn from its experiences in order to prepare more effectively in case of a future natural disaster. In those guidelines, three basic concepts of tsunami countermeasures were recommended: (i) building seawalls, breakwaters and flood gates to protect lives and properties; (ii) urban planning to create a tsunami-resilient community through effective land-use management and arrangement of redundant facilities to increase the safe area, such as vertical evacuation buildings; (iii) disaster information dissemination, evacuation planning and public education. For the largest-possible tsunami level of the more than 150 year recurrence interval, the so-called extreme event (such as the 2011 Tohoku event), the government refers to this as ‘Level 2’ or ‘Preparedness/Mitigation Level’ to protect human lives and to reduce the losses and damage with comprehensive disaster management measures including coastal protection, urban planning, evacuation and public education. Measurements of tsunami inundation flow velocities on land were quite rare, and it was thus difficult to understand what really happened in the devastated area and to identify the cause and mechanisms of structural destruction by tsunami inundation flow. The maximum run-up height was 29 m at Ryori Shirahama. G>c�A'�}�5b��
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w�D��r1���宜��lY�[��d�Տ��\�D��E��\ߎ���Iq��H��5n�U3}ξ��E9��o�Ӝ��j�衪.=]�L�RG�j���D�ڣ�ÏM��7�}0�}� Some have probably worked well, while others appear to have failed. Coastal infrastructure such as breakwaters and seawalls cannot always protect life and property. On March 11, 2011, a 9.1 magnitude earthquake occurred 231 miles northeast of Tokyo. Using this result, Sendai city determined the land-used plan and the area of housing reconstruction and relocation. It was widely believed that Japan was one of the most prepared countries in the world for tsunami events. The first tsunami breakwater was constructed at the mouth of Ofunato Bay, Iwate prefecture, where the maximum water depth was 38 m. The functionality of this breakwater for protection was investigated through numerical analysis [6]. Scattering residential areas will isolate people and weaken community connections, and consequently, undermine the community's sustainability with shrinking population in rural areas. N.S. The solid lines are obtained from the devastated municipalities of Miyagi prefecture (from the 2011 event) and the dashed one is from Banda Aceh, Indonesia (the 2004 Indian Ocean tsunami) [37].Download figureOpen in new tabDownload powerPoint. Everyone knows that Japan is an earthquake-prone country, but the events of March 2011 made it much more real for many of us living in Japan or considering a move to Japan. Governments can reduce risk, but communities must not become complacent. endstream
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This fact led to a revision of the requirement for structural design of tsunami evacuation buildings [51], specifically focusing on the tsunami loading effect. Another story from Kamaishi city will give answers to the above questions. The earthquake and subsequent tsunami that struck northeastern Japan on March 11 was perhaps the most widely recorded natural disaster in human history. Therefore, we emphasize that Tohoku was one of the areas best prepared for a tsunami. Based on the promptly estimated magnitude 7.9, 3 min after the quake (14.49 JST), JMA issued a Major tsunami warning to the coasts of Iwate, Miyagi and Fukushima prefectures with estimates of 3 m, 6 m and 3 m, respectively. International Atomic Energy Agency (IAEA). (Online version in colour. A new paradigm of coastal structural design has caused significant arguments in some Sanriku coastal communities. In 1997, the Japan central government council, which consists of seven ministries, issued a guideline for comprehensive tsunami countermeasures that should be taken as part of regional tsunami disaster prevention. The tsunami was predicted to hit Tuvalu at 1.30am. The 2011 tsunami disaster also implied that hazard maps have two functional aspects. The coastal plain along Sendai Bay experienced some of the farthest-reaching tsunami waters. Tsunami safety has been a focus of coastal city planning throughout the nation. The Japan Meteorological Agency (JMA), which is responsible for issuing tsunami warnings/ advisories and for estimating tsunami height, employed a new system in 1999 [18] and updated it using Earthquake Early Warnings (EEWs) in 2006 [19]. When verifying the proposed reconstruction plan, numerical modelling is useful. (a) Tsunami hazard map published for Kesennuma city, Miyagi prefecture. Enter your email address below and we will send you the reset instructions. Coastal residents did not feel any ground shaking and the Japan Metrological Agency did not issue a tsunami warning. Several nuclear power plant facilities were affected by the strong ground motions and great tsunamis: the Tokai, Higashi Dori, Onagawa and Fukushima Dai-ichi and Dai-ni plants. For such cases, JMA has introduced methods to quickly highlight the possibility of underestimation in magnitude estimation and issues an initial tsunami warning based on the largest seismic fault expected in the area where the earthquake was triggered [21]. It was found in the 2011 event that this lack of toe protection became a weak point, once overflowed. 4. Japan's famed bullet trains slow to an automatic halt in the event of a large earthquake. Figure 2. It was the fifth most powerful earthquake ever recorded, and within 30 minutes, a 133-foot high tsunami pummeled Japan's northeastern shoreline. Black dots on the coastline indicate the points of the 2011 tsunami height measurement. Japan's historic earthquake and tsunami serve as a great reminder to prepare our families for catastrophic events. A significant feature of Sendai city's reconstruction plan is integrating several coastal protection facilities, such as seawalls, coastal forests, park (artificial hill) and elevated roads to minimize the potential losses. “If this could happen to Japan, what about us?” In many coastal communities, people have conducted regular evacuation drills and have held workshops to learn which areas are at risk, by referring to a hazard map prepared by the local government. Northeast of Tohoku, the maximum run-up height in this event was similar to the events of both 1896 and 1933, especially of the 1896 Meiji Sanriku tsunami. Figure 1. The tsunami created over 300,000 refugees in the Tōhoku region of Japan, and resulted in shortages of food, water, shelter, medicine and fuel for survivors. For that reason, Japan had already introduced a number of defences prior to 2011. Re-cap of last week Japan was hit by a massive 9.0 magnitude earthquake that caused a tsunami. %%EOF
The Kamaishi tsunami breakwater is in the Guinness Book of World Records as the deepest tsunami breakwater at nearly 63 m deep, and was designed to protect the densely populated area in Kamaishi city located at the bottom of the bay. VANCOUVER, British Columbia — In 2011, Japan was one of the most prepared countries in the world for a massive earthquake. Issued on: 01/06/2011 - 10:37 Modified: 01/06/2011 - 14:28. Even worse, in several communities, the radio or speaker system did not work because of the blackout caused by the earthquake. The seafloor moved and a small tsunami was generated, largely because this was a much smaller earthquake than 2011, about 40 times smaller, and it released about 250 times less energy. The nation-wide post-tsunami survey results shed light on the mechanisms of structural destruction, tsunami loads and structural vulnerability to inform structural rehabilitation measures and land-use planning. The seawall is designed with reference to Level 1 tsunami scenario, while comprehensive disaster management measures should refer to Level 2 tsunami for protection of human lives and reducing potential losses and damage. The responses to the 2011 event are discussed specifically on the tsunami warning system and efforts to identify the tsunami impacts. All the municipalities in the 2011 tsunami-affected areas needed to draft their reconstruction plans following the ‘Act on the Development of Tsunami-resilient Communities’. With the participation of researchers from throughout Japan, joint research groups conducted a tsunami survey along a 2000 km stretch of the Japanese coast. One option was a hill with a steep slope behind the school, which looked difficult for small children to climb. However, the affected area of this event was much more extensive than in those historical events. This 18 m tall lighthouse built on a cliff 10 m a.s.l. For Sendai city, we performed numerical modelling of tsunami inundation in the city by setting several tsunami source scenarios [47,48]. h�bbd``b`��@�q/�`-�����_@b�A�7!$8> �6 �H�?RW�@����? 4. “If this could happen to Japan, what about us?” An earthquake that struck Japan in March 2011 unleashed a massive tsunami. Figure 2 illustrates the measured tsunami inundation and run-up heights by the survey team, with plots of historical tsunami heights of the 1611 Keicho Sanriku, 1896 Meiji Sanriku, and 1933 Showa Sanriku earthquake tsunamis [24]. Their very quick and resolute response prompted local residents and even the students and teachers in a neighbouring elementary school to follow and consequently saved lots of lives. At the same time, rapid economic growth resulted from the ‘Income-Doubling Plan’ that started in 1960, an age of rapid growth, could cover the expensive construction costs. (b) Result of tsunami numerical modelling to evaluate the effect of the proposed reconstruction plan in Sendai city (maximum flow depth).Download figureOpen in new tabDownload powerPoint, Figure 4. [4] Avoiding a similar outcome in a future tsunami … ���J�*Q"��kю��@Gq�,���������Y'������zsZ��+� ����g�9�qV���o��f$}~�܈X�f�v̘�H"t���5oo�>��O��uAE���{N����^��i ��S-���hQ��X8B�� ܷ�����4����mz��=?�P��>��x�qg���P�ὀV��]�_�2�֦ ܃e˱�|�J�����5�e����` (��
Earthquake source studies indicate that the fault ruptured with a maximum slip of 60–80 m [11] over an area approximately 450 km by 200 km [12], making the pre-2011 estimates irrelevant. The bulk of this layer cake is made up of sediment from old … These hydrodynamic parameters appear capable of devastation for the coastal forests that have been planted for the past centuries. Published online 29 March 2011 | Nature 471, 556-557 (2011) | doi:10.1038/471556a . Under the limitations and uncertain conditions of funding, prefectural and local governments have developed their own recovery and reconstruction plans, which require 10 years to be completed (National budget is allocated for the first 5 years). Opinion. Another video was taken from the roof of a building in Onagawa town by one survivor. July 6, 2011 March 11, 2011 by News Desk. Maanjäristyksen voimakkuus oli 9,0 momenttimagnitudia. 113 0 obj
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