Literatura académica sobre el tema "India Ocean Tsunami"

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Artículos de revistas sobre el tema "India Ocean Tsunami"

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MATSUMOTO, HIROYUKI, YUICHIRO TANIOKA, YUICHI NISHIMURA, YOSHINOBU TSUJI, YUICHI NAMEGAYA, TADASHI NAKASU y SIN-ITI IWASAKI. "REVIEW OF TIDE GAUGE RECORDS IN THE INDIAN OCEAN". Journal of Earthquake and Tsunami 03, n.º 01 (marzo de 2009): 1–15. http://dx.doi.org/10.1142/s1793431109000378.

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According to the NOAA earthquake database, at least 31 events have been found in the Indian Ocean in terms of tsunami event since 1900, most of which occurred along the Sunda Trench. In this study, we review the history of tide level measurements and their datasets archives in Thailand, Indonesia, India, and Australia. We collected tide gauge paper charts recording historical tsunamis including the 2004 Indian Ocean tsunami in those countries. As a result, systematic collection of historical tsunami records by tide gauges in the Indian Ocean has been difficult, because few tsunamigenic earthquakes occurred in the Indian Ocean during the instrumentally observed period.
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Heidarzadeh, Mohammad, Alexander Rabinovich, Satoshi Kusumoto y C. P. Rajendran. "Field surveys and numerical modelling of the 2004 December 26 Indian Ocean tsunami in the area of Mumbai, west coast of India". Geophysical Journal International 222, n.º 3 (4 de junio de 2020): 1952–64. http://dx.doi.org/10.1093/gji/ggaa277.

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ABSTRACT In the aftermath of the 2004 Indian Ocean (Sumatra-Andaman) tsunami, numerous survey teams investigated its effects on various locations across the Indian Ocean. However, these efforts were focused only on sites that experienced major destruction and a high death toll. As a consequence, some Indian Ocean coastal megacities were not examined. Among the cities not surveyed was Mumbai, the principal west coast port and economical capital of India with a population of more than 12 million. Mumbai is at risk of tsunamis from two major subduction zones in the Indian Ocean: the Sumatra–Andaman subduction zone (SASZ) and the Makran subduction zone (MSZ). As a part of the present study, we conducted a field survey of the 2004 Indian Ocean tsunami effects in Mumbai, analysed the available tide gauge records and performed tsunami simulations. Our field survey in 2018 January found run-up heights of 1.6−3.3 m in the Mumbai area. According to our analysis of tide gauge data, tsunami trough-to-crest heights in Okha (550 km to the north of Mumbai) and in Mormugao (410 km to the south of Mumbai) were 46 cm and 108 cm, respectively. Simulations of a hypothetical MSZ Mw 9.0 earthquake and tsunami, together with the Mw 9.1 Sumatra–Andaman earthquake and tsunami, show that the tsunami heights generated in Mumbai by an MSZ tsunami would be significantly larger than those generated by the 2004 Sumatra–Andaman tsunami. This result indicates that future tsunami hazard mitigation for Mumbai needs to be based on a potential large MSZ earthquake rather than an SASZ earthquake.
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Yongjia, Liang. "Between Science and Religion: An Astrological Interpretation of the Asian Tsunami in India". Asian Journal of Social Science 36, n.º 2 (2008): 234–49. http://dx.doi.org/10.1163/156853108x298716.

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AbstractAstrology plays an important role in Indian social life. Indian astrologers' claim to have accurately predicted the 2004 Indian Ocean Tsunami, or the Asian Tsunami, was an effort to legitimize astrology as a full science. This effort demonstrates a difficulty in knowledge categorization, for in India, astrology is neither classified as a science nor as a religion. This is a result of the idea of an Indian nation-state, which rests upon both science and religion as foundations, but at the expense of expelling astrology from religion for not being scientific. However, as astrology continues to be important in India, the astrological interpretation of the Indian Ocean Tsunami drew substantial public attention. Astrology's significant presence in Indian society shows the role of a mature civil society in India as well.
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Murty, C. V. R., Sudhir K. Jain, Alpa R. Sheth, Arvind Jaiswal y Suresh R. Dash. "Response and Recovery in India after the December 2004 Great Sumatra Earthquake and Indian Ocean Tsunami". Earthquake Spectra 22, n.º 3_suppl (junio de 2006): 731–58. http://dx.doi.org/10.1193/1.2206137.

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The rescue and relief work undertaken in the Andaman and Nicobar islands and in mainland India after the 26 December 2004 Indian Ocean tsunami was massive. A number of new initiatives undertaken by the government and nongovernmental agencies were innovative and successful. Also, since the tsunami was not a typical disaster for India, it raised a number of new concerns related to reconstruction along the coast.
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Yeh, Harry, R. K. Chadha, Mathew Francis, Toshitaka Katada, G. Latha, Curt Peterson, G. Raghuraman y J. P. Singh. "Tsunami Runup Survey along the Southeast Indian Coast". Earthquake Spectra 22, n.º 3_suppl (junio de 2006): 173–86. http://dx.doi.org/10.1193/1.2202651.

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The 26 December Indian Ocean tsunami was an extraordinary event in the history of natural hazards. It severely affected many countries surrounding the Indian Ocean: Indonesia, Thailand, Malaysia, Myanmar, Bangladesh, India, Sri Lanka, the Maldives, and African countries. Unlike the previous tsunami events in the last 40 years, the seriously affected areas are so vast that a traditional ground-level tsunami survey covering all the necessary areas by a single survey team was impractical. This destructive event will undoubtedly provide many opportunities to explore both basic and applied research in tsunami science and engineering fields and will lead to better preparedness for future disasters. A tsunami runup survey was conducted that spans Vedaranniyam (10° 23.5′ N) to Vodarevu (15° 47.6′ N)—more than 600 km of the southeast Indian coast—which suffered from the distant tsunami, whose source was more than 1,500 km away.
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Sheth, Alpa, Snigdha Sanyal, Arvind Jaiswal y Prathibha Gandhi. "Effects of the December 2004 Indian Ocean Tsunami on the Indian Mainland". Earthquake Spectra 22, n.º 3_suppl (junio de 2006): 435–73. http://dx.doi.org/10.1193/1.2208562.

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The 26 December 2004 tsunami significantly affected the coastal regions of southern peninsular India. About 8,835 human lives were lost in the tsunami in mainland India, with 86 persons reported missing. Two reconnaissance teams traveled by road to survey the damage across mainland India. Geographic and topological features affecting tsunami behavior on the mainland were observed. The housing stock along the coast, as well as bridges and roads, suffered extensive damage. Structures were damaged by direct pressure from tsunami waves, and scouring damage was induced by the receding waves. Many of the affected structures consisted of nonengineered, poorly constructed houses belonging to the fishing community.
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Ramadass, Gidugu Ananada, Narayanaswamy Vedachalam, Tata Sudhakar, Raju Ramesh, Vandavasi Bala Naga Jyothi, Naranamangalam Balaji Prashanth y Malayath Aravindakshan Atmanand. "A Study of the Algorithms for the Detection of Tsunami Using an Ocean Bottom Pressure Recorder". Marine Technology Society Journal 48, n.º 1 (1 de enero de 2014): 76–83. http://dx.doi.org/10.4031/mtsj.48.1.6.

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AbstractThe National Institute of Ocean Technology (NIOT), an autonomous organization under the Ministry of Earth Sciences, government of India, is engaged in developing and installing systems for tsunami detection and reporting. This involves high-precision bottom pressure recorders (BPRs) installed on the ocean floor, which can detect water level changes in the order of a few centimeters. Data are logged and recorded subsea by instruments located close to the BPRs. The detection of abnormal changes in the water level is required for detecting a tsunami event. This paper describes algorithms incorporated in most BPRs for detecting a tsunami by predictive methods such as Newton’s Extrapolation and Kalman predictor techniques. The most widely used tsunami detection algorithm is based on Newton’s extrapolation. The tsunami detection technique based on the Kalman prediction algorithm developed by NIOT can be an alternative for the existing technique. This paper describes both the algorithms and analyzes their effectiveness during tsunami event detection using MATLAB software. It is found that the Kalman algorithm has a better detection performance over the Newton extrapolation technique for tsunami wave amplitudes up to 300 mm. The Newton extrapolation technique has a better detection performance for tsunami wave duration of less than 10 min. For tsunami wave durations greater than 10 min, the Kalman algorithm has a better detection performance. As the wave durations of most of the recorded tsunamis are greater than 10 min, the Kalman algorithm could be a viable substitute for tsunami detection.
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Saini, Ajay. "Disciplining the other". Contributions to Indian Sociology 52, n.º 3 (12 de agosto de 2018): 308–35. http://dx.doi.org/10.1177/0069966718785961.

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The Indian Ocean tsunami (2004) devastated the Nicobar archipelago, a remote tribal reserve in the Indian Ocean, which the Nicobarese indigenes have traditionally inhabited. The catastrophe attracted a massive humanitarian response from the Government of India (GoI), leading to a sociocultural crisis among the Nicobarese that is inextricably linked to the post-tsunami humanitarian government in the Nicobar, which undermined what was once a self-sustaining community. Using Michel Foucault’s analytic of governmentality, this article elucidates how the humanitarian government in the southern Nicobar, motivated by a raison d’état of national security, attempted to discipline the traditional Nicobarese by developing new forms of subjectivities among them.
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GUPTA, HARSH. "INDIA'S INITIATIVE IN MITIGATING TSUNAMI AND STORM SURGE HAZARD". Journal of Earthquake and Tsunami 02, n.º 04 (diciembre de 2008): 287–95. http://dx.doi.org/10.1142/s1793431108000360.

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Soon after the occurrence of the most devastating tsunami caused by the 26th December, 2004 Sumatra earthquake, India took the initiative to set up an end-to-end system to mitigate tsunami and storm surge hazard. The system includes all the necessary elements: networking of seismic stations; deployment of ocean bottom pressure recorders; real time sea level monitoring stations; establishment of radar based monitoring stations for real time measurement of surface currents and waves; modeling for tsunamis and storm surges; generation of coastal inundation and vulnerability maps; operation of a tsunami and storm surges warning centre on 24 × 7 basis; capacity building and training of all the stakeholders and communication with the global community. This initiative was estimated to have a direct cost of US $30 million and was to be operative by August 2007. This has been achieved. The Indian National Centre for Ocean Information and Services (INCOIS), belonging to the Ministry of Earth Sciences (MoES), located at Hyderabad, is the nodal agency for this program. The system fared well during the occurrence of September 12/13, 2007 tsunamigenic earthquakes. One of the problems is delay in estimating the size of large earthquakes. Empirical approaches are being developed to quickly estimate the size of the earthquakes occurring in Sumatra–Andaman zone of tsunamigenic earthquakes.
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Maheshwari, B. K., M. L. Sharma y J. P. Narayan. "Geotechnical and Structural Damage in Tamil Nadu, India, from the December 2004 Indian Ocean Tsunami". Earthquake Spectra 22, n.º 3_suppl (junio de 2006): 475–93. http://dx.doi.org/10.1193/1.2206148.

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A reconnaissance team surveyed the geotechnical and structural engineering aspects of tsunami damage on the coast of Tamil Nadu in India. The area surveyed was from Chennai on the east coast to Thiruvananthapuram on the west coast. There was practically no major evidence of damage from direct ground shaking, although damage from the tsunami was extensive. The geotechnical engineering damage observed was mostly due to erosion of soil, settlement of soil, damage to port and harbor facilities, and damage to lifelines. The structural engineering damage involved damage to compound walls, collapse of rural houses, failure of columns, and toppling of roofs; some of the damage occurred because reinforcement details were lacking. Analyses of damage and its causes were performed, and the level of damage correlated well with the tsunami runup for the localities visited.
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Tesis sobre el tema "India Ocean Tsunami"

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Alevras, Dimitrios. "Simulating tsunamis in the Indian Ocean with real bathymetry by using a high-order triangular discontinuous Galerkin oceanic shallow water model". Thesis, Monterey, Calif. : Naval Postgraduate School, 2009. http://edocs.nps.edu/npspubs/scholarly/theses/2009/March/09Mar%5FAlevras.pdf.

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Thesis (M.S. in Meteorology and Physical Oceanography and M.S. in Applied Mathematics)--Naval Postgraduate School, March 2009.
Thesis Advisor(s): Giraldo, Francis X. ; Radko, Timour. "March 2009." Description based on title screen as viewed on April 24, 2009. Author(s) subject terms: Tsunami Simulation, Indian Ocean Tsunami 2004, Triangular Discontinuous Galerkin Method, Propagation stage, Oceanic Shallow Water Model. Includes bibliographical references (p. 91-93). Also available in print.
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Banford, Alyssa J. Wickrama Thulitha. "The association between marital functioning, family closeness, and tsunami related health moderation by religiosity /". Auburn, Ala, 2009. http://hdl.handle.net/10415/1777.

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Letukas, Lynn Ann. "Is aid a social problem? cross-national media constructions of relief efforts following the Indian Ocean tsunami /". Access to citation, abstract and download form provided by ProQuest Information and Learning Company; downloadable PDF file, 79 p, 2009. http://proquest.umi.com/pqdweb?did=1674100731&sid=5&Fmt=2&clientId=8331&RQT=309&VName=PQD.

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Courtney, Claire. "Reporting Death and Disaster: The Paradox beyond the Numbers". The University of Waikato, 2007. http://hdl.handle.net/10289/2306.

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The 2004 Indian Ocean tsunami killed over two hundred thousand people in the fifteen countries the tsunami struck. Amidst extensive media coverage, the New Zealand Herald published in excess of two hundred online articles focusing on the event and aftermath. Representations of death and the dead within these articles are often stereotypical and formulaic. Discourse analysis revealed that death and the dead are represented through both metaphorical images and abject descriptions on two distinct scales. Both the bodies and the characters of the dead are handled explicitly according to socially acceptable trends. The dead are also situated spatially with specific identities constructed and reported on. Utilising discourses from throughout the social sciences, analysis of online publications reveals the way perceptions of media consumers to death both inform and are informed by media producers.
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Nafesa, Binti Ismail. "Livelihood Changes After the 2004 Indian Ocean Tsunami Disaster: Case Study in Banda Aceh, Indonesia". Kyoto University, 2018. http://hdl.handle.net/2433/232441.

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Heger, Martin. "The causal effects of the Indian Ocean tsunami and armed conflict on Aceh's economic development". Thesis, London School of Economics and Political Science (University of London), 2016. http://etheses.lse.ac.uk/3402/.

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This PhD thesis investigates the causal long-term economic effects of the Indian Ocean Tsunami and the armed conflict in Aceh, Indonesia (chapters 2, 3 and 4). It also contains an analysis of land use change and the consequences for soil-organic carbon (SOC) in Eastern Panama that is unrelated to previous chapters. Chapter 2 stands at the core of my PhD thesis; it is the equivalent of a job market paper. In chapter 1, I provide an introduction to and summary of my PhD thesis. In particular, I describe why I believe that I make original contributions to knowledge that are significant and rigorous. In chapter 2, I carry out a quasi-experimental analysis investigating the causal effects of Tsunami flooding on long-term per capita economic output. The existing literature suggests that natural disasters are growth depressing in the short-term, and in the longterm, natural disasters either cause a continued shortfall of economic output, or an eventual convergence to the pre-disaster counterfactual trend. I picked the Indian Ocean Tsunami in Aceh as a case study for this PhD thesis, because I posit that if there is one case for which there is evidence that goes against the conventional wisdom, namely in the form of increased economic output in the long run, it probably is Aceh. The reason why I expect to see creative destruction is that Aceh received a windfall of aid and was the stage of the largest reconstruction effort the developing world has ever seen. I conclude that natural disasters are not necessarily the cause of output reductions and that they can be windows of opportunity for the economy. In chapter 3, I investigate the reasons behind the creative destruction, and take a closer look at different sectors and subcomponents of the economy. I examine three channels through which the Tsunami may have affected per capita economic output. First, I find that the Tsunami causally accelerated the structural transformation process, a process through which people and the economy move out of agriculture, and into more productive sectors such as services. Second, I show that the Tsunami brought with it a windfall of aid and other funds, which allowed for a building back better of physical capital and increased capital formation. Third, I show that aggregate private consumption not only was smoothed in a reaction to the Tsunami, but even boosted to sustainably higher levels, compared to the no-Tsunami counterfactual. In chapter 4, I investigate whether the 30 years long armed conflict in Aceh left any negative economic legacy effects, once the fighting stopped and the peace agreement was signed. The separatist war took a toll on the Acehnese economy. Even though the conflict has ended, did the negative economic effects also end? Aceh’s economy has higher per capita growth rates in times of peace than in times of war, which can be either a sign of a peace dividend or creative destruction from the Tsunami. But does the armed conflict leave a negative legacy for future growth rates, even after peace has officially been declared? I find that that peacetime growth rates are negatively affected by the wartime conflict intensity. Using violence data on the incidence of killings, injuries, and other ‘measurable human suffering’, I assess whether districts that were heavily affected by armed conflict grew systematically differently from those that were spared from the brunt of the violence. I find that there are severe negative economic legacy effects of violence, and the more violence occurred in a district during the separatist war, the slower it was growing during times of peace. Chapter 5, topically unrelated to the previous chapters, is looking at land use change in Eastern Panama and the consequences for soil organic carbon (SOC). In this chapter, I compare SOC concentrations of primary forests to two competing land use alternatives: Forest-to-pasture conversion for cattle grazing versus indigenous forest-to-crop conversion. I find that both land use changes reduce SOC concentrations significantly, yet the pasture land use has lower levels of SOC than indigenous crop cultivation. The soil carbon levels of secondary forests are not statistically different from primary forests, implying that the forest conversions are reversible, in terms of their impact on SOC, which suggests that allowing secondary forests to re-grow in former cultivated areas in the Eastern part of Panama holds promise for climate change mitigation. In the concluding chapter 6, I present a summary of the main findings and an outline for future research.
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Aswalap, Supaluk Joy O'Connor Brian C. "Tsunami disaster response a case analysis of the information society in Thailand /". [Denton, Tex.] : University of North Texas, 2009. http://digital.library.unt.edu/ark:/67531/metadc12075.

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Matsumoto, Dan. "Characteristics of the 2004 Indian Ocean tsunami deposits formed upon a lagoon floor and coastal lowland". 京都大学 (Kyoto University), 2008. http://hdl.handle.net/2433/136900.

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Monsinee, Attavanich. "A Study of Living Conditions in Post-Tsunami Houses: The Case of the Moklen Ethnic Minority in Phang Nga Province, Southern Thailand". 京都大学 (Kyoto University), 2016. http://hdl.handle.net/2433/217215.

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Widianti, Ezki. "The ulama in Aceh in time of conflict, tsunami and peace process an ethnographic approach /". Ohio : Ohio University, 2006. http://www.ohiolink.edu/etd/view.cgi?ohiou1150410650.

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Libros sobre el tema "India Ocean Tsunami"

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K, Das P. VCRC response to Tsunami. Pondicherry: Vector Control Research Centre, Indian Council of Medicinal Research, 2005.

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India United Nations Country Team. Recovery framework in support of government of India for a Post-Tsunami Rehabilitation and Reconstruction Programme. New Delhi: United Nations Country Team, India, 2005.

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Aceh Nias Settlements Support Programme. Post tsunami Aceh-Nias settlement and housing recovery review: Comprehensive review of the response, UN-HABITAT's monitoring methodology and scorecards, directory of implementation organisations. Jakarta, Indonesia: UN-HABITAT Aceh Nias Settlements Support Programme in collaboration with the Government of Indonesia, BRR NAD-Nias, the Provincial Government of Aceh, and UNDP, 2009.

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Regional Workshop on Post-tsunami Rehabilitation of Fishing Communities and Fisheries-based Livelihoods (2006 Madras, India). Regional Workshop on Post-tsunami Rehabilitation of Fishing Communities and Fisheries-based Livelihoods: Proceedings : 18 and 19 January 2006, Chennai, India. Chennai: International Collective in Support of Fishworkers, 2007.

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Lüsted, Marcia Amidon. The 2004 Indian Ocean Tsunami. Edina, Minn: ABDO Pub., 2008.

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R, Cummins Phil, Kong Laura S. L, Satake Kenji 1958- y SpringerLink (Online service), eds. Tsunami science four years after the 2004 Indian Ocean Tsunami. Basel: Birkhäuser, 2009.

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Pasaribu, Bien. Tsunami: Petaka terbesar abad 21. Jakarta: Pustaka Mina, 2005.

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M, M. Dzikron A. Tragedi tsunami di Aceh: Bencana alam atau rekayasa. Solo: Muhammad Taufiq & Partners, 2006.

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Diposaptono, Subandono. Hidup akrab dengan gempa dan tsunami. Bogor: Buku Ilmiah Populer, 2008.

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Rekonstruksi, Indonesia Badan Rehabilitasi &. Aceh dan Nias setahun setelah tsunami: Upaya pemulihan dan langkah ke depan : laporan bersama BRR dan rekanan-rekanan internasional, Desember 2005. Banda Aceh, Indonesia: Badan Rehabilitasi dan Rekonstruksi NAD-Nias, 2005.

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Capítulos de libros sobre el tema "India Ocean Tsunami"

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Srivastava, Ajay. "Role of GI Services in Emergency Response Management in India". En Recovery from the Indian Ocean Tsunami, 299–314. Tokyo: Springer Japan, 2014. http://dx.doi.org/10.1007/978-4-431-55117-1_20.

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Abe, Miwa y Rajib Shaw. "Critical Factors for Sustainable Post-tsunami Resettlement: Cases from India and Sri Lanka". En Recovery from the Indian Ocean Tsunami, 89–102. Tokyo: Springer Japan, 2014. http://dx.doi.org/10.1007/978-4-431-55117-1_7.

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Ravindran, Irene Stephen. "Healthy Ecosystems for Long Term Security and Sustainability of Natural Resource Management: Case of India". En Recovery from the Indian Ocean Tsunami, 315–30. Tokyo: Springer Japan, 2014. http://dx.doi.org/10.1007/978-4-431-55117-1_21.

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Krishnamurthy, R. R. y K. Kamala. "Impact of Higher Education in Enhancing the Resilience of Disaster Prone Coastal Communities: A Case Study in Nemmeli Panchayat, Tamil Nadu, India". En Recovery from the Indian Ocean Tsunami, 361–80. Tokyo: Springer Japan, 2014. http://dx.doi.org/10.1007/978-4-431-55117-1_24.

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Lavigne, Franck, Raphaël Paris, Frédéric Leone, J. C. Gaillard y Julie Morin. "Indian Ocean Tsunami, 2004". En Encyclopedia of Natural Hazards, 529–35. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-1-4020-4399-4_192.

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Madigan, Michael L. "Indian Ocean Tsunami 2004 Case Study". En Handbook of Emergency Management Concepts, 307–12. Boca Raton, FL : CRC Press, 2018.: CRC Press, 2017. http://dx.doi.org/10.1201/b22489-18.

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Fakhruddin, S. H. M. "Indian Ocean Tsunami Warning System (IOTWS)". En Recovery from the Indian Ocean Tsunami, 59–72. Tokyo: Springer Japan, 2014. http://dx.doi.org/10.1007/978-4-431-55117-1_5.

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Heidarzadeh, Mohammad, Moharram D. Pirooz, Nasser H. Zaker y Costas E. Synolakis. "Evaluating Tsunami Hazard in the Northwestern Indian Ocean". En Tsunami Science Four Years after the 2004 Indian Ocean Tsunami, 2045–58. Basel: Birkhäuser Basel, 2008. http://dx.doi.org/10.1007/978-3-0346-0057-6_5.

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Menon, N. Vinod Chandra. "Rhetoric and Ground Reality of Institutionalizing Disaster Risk Reduction". En Recovery from the Indian Ocean Tsunami, 281–97. Tokyo: Springer Japan, 2014. http://dx.doi.org/10.1007/978-4-431-55117-1_19.

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Shaw, Rajib. "Ten Years of Recovery Lessons from Indian Ocean Tsunami". En Recovery from the Indian Ocean Tsunami, 3–15. Tokyo: Springer Japan, 2014. http://dx.doi.org/10.1007/978-4-431-55117-1_1.

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Actas de conferencias sobre el tema "India Ocean Tsunami"

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Heidarzadeh, Mohammad, Moharram D. Pirooz, Nasser H. Zaker y Mohammad Mokhtari. "Modeling of Tsunami Propagation in the Vicinity of the Southern Coasts of Iran". En ASME 2007 26th International Conference on Offshore Mechanics and Arctic Engineering. ASMEDC, 2007. http://dx.doi.org/10.1115/omae2007-29082.

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The extensive death toll and sever economical damages brought by the 2004 Indian Ocean tsunami has emphasized the urgent need for assessing the hazard of tsunami in this ocean, and determining the most vulnerable coastlines to the impact of possible tsunami. In this paper the hazard of tsunami for southern coasts of Iran bordering the Indian Ocean is discussed. At first, historical data of tsunami occurrences on the Iranian southern coasts are collected, described and analyzed. Then, numerical simulation of potential tsunamis in the Makran subduction zone is performed and the tsunami wave height distribution along the Iranian coast is calculated. The Makran subduction zone is among two main tsunamigenic zones in the Indian Ocean. In this zone the Oman oceanic plate subducts beneath the Iranian Micro-plate at an estimated rate of about 19 mm/yr. Historically, there is the potential for tsunami generation in this region and several tsunamis attacked the Makran coastlines in the past. The most recent tsunami in this region has occurred on 28 November 1945 which took the lives of more than 4000 people in the coasts of Iran, Pakistan, India, and Oman. Here we examine the seafloor uplift of the Makran zone and its potential for generating destructive tsunamis in the southern coastlines of Iran. Several earthquake scenarios with moment magnitudes ranging between 6.5 and 8.5 are used as initial conditions for analysis. For scenario of an earthquake with magnitude of 8.0, propagation of tsunami waves on coastlines and wave time histories in selected reference locations are calculated.
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Heidarzadeh, Mohammad. "Far-Field Effects of Large Tsunamis Produced by the Makran Subduction Zone". En ASME 2009 28th International Conference on Ocean, Offshore and Arctic Engineering. ASMEDC, 2009. http://dx.doi.org/10.1115/omae2009-79362.

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The 2004 Indian Ocean tsunami which exported death and destruction to far distant shores, once more emphasized the tsunami hazards associated with transoceanic tsunamis. Historical records of tsunamis in the Makran subduction zone (MSZ) reveal that Makran tsunamis are capable of producing large waves in the far-field. The Makran tsunami of 1945 produced by an Mw8.1 earthquake was reported to cause far-field effects in the Indian Ocean and reached a height of about 30 cm in the Seychelles, at the distance of about 3500 km from the MSZ. Here, we assess historical observations of this event and perform numerical modeling of this tsunami with emphasis on its far-field effects. Our numerical modeling successfully reproduces most feathers of the historical observations including its far-field effects. Southward propagation of Makran large tsunamis is investigated and their possible effects on Maldives and Seychelles islands are discussed. This study will help to better understand tsunami hazard associated with the MSZ, especially its far-field hazard.
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Heidarzadeh, Mohammad, Moharram D. Pirooz y Nasser H. Zaker. "Tsunami Hazards in the Northwestern Indian Ocean". En ASME 2008 27th International Conference on Offshore Mechanics and Arctic Engineering. ASMEDC, 2008. http://dx.doi.org/10.1115/omae2008-57837.

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Although northwestern Indian Ocean has experienced some deadly tsunamis in the past, this region remains one of the least studied regions in the world and little research work has been devoted to its tsunami hazard assessment. In this study, we compile and analyze historical tsunami in the northwestern Indian Ocean and present a tsunami list for this region. Then, a deterministic method has been employed to give a preliminary estimation of the tsunami hazard faced by different coastlines in this region. Different source scenarios are considered and for each scenario, numerical modeling of tsunami is performed. For each case, the maximum positive tsunami wave heights along the coasts are calculated which provide a preliminary estimation of tsunami hazard and show which locations face the greatest threat from a large tsunami.
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Behera, Manasa Ranjan, K. Murali y V. Sundar. "Modeling of the Indian Ocean Tsunami". En ASME 2007 26th International Conference on Offshore Mechanics and Arctic Engineering. ASMEDC, 2007. http://dx.doi.org/10.1115/omae2007-29691.

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Shallow Water Equations are solved using an Unstructured Explicit Finite Element Method (UEFEM) to simulate long waves in the ocean. The formulation of the UEFEM has been described and found to be computationally efficient for large problems such as basin level modeling of tsunamis. Different domains have been considered to simulate the propagation of the waves due to an artificially imposed initial disturbance. The domain of Bay of Bengal has been considered for simulation with an initial disturbance which resembles the type and location of the 2004 Indian Ocean Tsunami. The Wave elevation and deformations as well as time of travel of tsunami are reproduced. The method hence has high potential of being attractive for application of simulation of global tsunamis.
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Yamamoto, Yoshimichi, Hiroaki Takanashi y Takashi Tomita. "MECHANISM OF COASTAL STRUCTURE DAMAGE DUE TO TSUNAMIS, AND CASE STUDIES OF COASTAL DAMAGE FROM INDIAN OCEAN TSUNAMI". En Proceedings of the 30th International Conference. World Scientific Publishing Company, 2007. http://dx.doi.org/10.1142/9789812709554_0429.

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Kawata, Y. "Recent development of tsunami disaster reduction management in Japan after the 2004 Indian Ocean Tsunami". En RISK ANALYSIS 2008. Southampton, UK: WIT Press, 2008. http://dx.doi.org/10.2495/risk080171.

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Lauterjung, Jörn. "Installation of a tsunami early warning system in the Indian Ocean". En the 2005 international workshop. New York, New York, USA: ACM Press, 2005. http://dx.doi.org/10.1145/1097064.1097065.

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Chen, R., J. Coles, J. Lee y H. R. Rao. "Emergency communication and system design: The case of Indian Ocean Tsunami". En 2009 International Conference on Information and Communication Technologies and Development (ICTD). IEEE, 2009. http://dx.doi.org/10.1109/ictd.2009.5426699.

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SCHWARZER, KLAUS, PETER FELDENS, DAROONWAN SAKUNA-SCHWARTZ, SIWATT PONGPIACHAN, YVONNE MILKER y DANAI TIPMANEE. "THE INDIAN OCEAN TSUNAMI 2004: IDENTIFICATION OF TSUNAMI DEPOSITS OFFSHORE IN THE ANDAMAN SEA BY DIFFERENT PROXIES". En Coastal Sediments 2015. WORLD SCIENTIFIC, 2015. http://dx.doi.org/10.1142/9789814689977_0184.

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Tanathong, Supannee, Kurt T. Rudahl y Sally E. Goldin. "Object oriented change detection of buildings after the Indian ocean tsunami disaster". En 2008 5th International Conference on Electrical Engineering/Electronics, Computer, Telecommunications and Information Technology (ECTI-CON). IEEE, 2008. http://dx.doi.org/10.1109/ecticon.2008.4600373.

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Informes sobre el tema "India Ocean Tsunami"

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Singh, Chandni, Mark Tebboth, Jasmitha Arvind y Yashodara Udupa. Representing Disasters and Long-term Recovery – Insights from Tamil Nadu. Indian Institute for Human Settlements, 2021. http://dx.doi.org/10.24943/rdlrtn06.2021.

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This study focuses on disaster impacts and recovery in Tamil Nadu, drawing on insights from Chennai city and Nagapattinam district. The research is part of a larger three-year project called “Recovery with Dignity”, which examines the experiences of recovery in post-disaster situations across three states in India – Odisha, Tamil Nadu, and Kerala – and explores how recovery processes represent vulnerable populations. In this report, we focus on three key disasters in Tamil Nadu: the 2004 Indian Ocean Tsunami, the 2015 South India flood, and the 2018 Cyclone Gaja. Through these events, we examine how the ways disasters and their losses are represented shape recovery outcomes. The study uses a range of data, from a review of state policies in Tamil Nadu (2005-2019), an analysis of media articles published in English and Tamil (2004-2019), to interviews with disaster-affected people and secondary stakeholders. The findings indicate that disaster responses and outcomes are highly differentiated based on how disaster-affected people and their needs and losses are represented. To enable inclusive recovery, it is necessary to recognising the heterogenous nature of disaster impacts and acknowledge different ideas of what recovery means.
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Jackson, L. E., J. V. Barrie, D. L. Forbes, J. Shaw, G K Manson y M. Schmidt. Effects of the 26 December 2004 Indian Ocean tsunami in the Republic of Seychelles: Report of the Canada-UNESCO Indian Ocean Tsunami Expedition, 19 January - 5 February 2005. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2005. http://dx.doi.org/10.4095/220622.

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Ho, Jessica, Elizabeth Frankenberg, Cecep Sumantri y Duncan Thomas. Adult Mortality Five Years after a Natural Disaster: Evidence from the Indian Ocean Tsunami. Cambridge, MA: National Bureau of Economic Research, junio de 2016. http://dx.doi.org/10.3386/w22317.

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Cas, Ava, Elizabeth Frankenberg, Wayan Suriastini y Duncan Thomas. The Impact of Parental Death on Child Well-being: Evidence from the Indian Ocean Tsunami. Cambridge, MA: National Bureau of Economic Research, agosto de 2013. http://dx.doi.org/10.3386/w19357.

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