Tsunami Detection Systems for International Requirements

R. Lawson
{"title":"Tsunami Detection Systems for International Requirements","authors":"R. Lawson","doi":"10.1109/OCEANS.2007.4449208","DOIUrl":null,"url":null,"abstract":"Results are presented regarding the first commercially available, fully operational, tsunami detection system to have passed stringent U.S. government testing requirements and to have successfully demonstrated its ability to detect an actual tsunami at sea. Spurred by the devastation of the December 26, 2004, Indian Ocean tsunami that killed more than 230,000 people, the private sector actively supported the Intergovernmental Oceanographic Commission's (IOC's) efforts to develop a tsunami warning system and mitigation plan for the Indian Ocean region. As each country in the region developed its requirements, SAIC recognized that many of these underdeveloped countries would need significant technical assistance to fully execute their plans. With the original focus on data fusion, consequence assessment tools, and warning center architecture, it was quickly realized that the cornerstone of any tsunami warning system would be reliable tsunami detection buoys that could meet very stringent operational standards. Our goal was to leverage extensive experience in underwater surveillance and oceanographic sensing to produce an enhanced and reliable deep water sensor that could meet emerging international requirements. Like the NOAA Deep-ocean Assessment and Recording of Tsunamis (DARTtrade) buoy, the SAIC Tsunami Buoy (STB) system consists of three subsystems: a surface communications buoy subsystem, a bottom pressure recorder subsystem, and a buoy mooring subsystem. With the operational success that DART has demonstrated, SAIC decided to build and test to the same high standards. The tsunami detection buoy system measures small changes in the depth of the deep ocean caused by tsunami waves as they propagate past the sensor. This is accomplished by using an extremely sensitive bottom pressure sensor/recorder to measure very small changes in pressure as the waves move past the buoy system. The bottom pressure recorder component includes a processor with algorithms that recognize these characteristics, and then immediately alerts a tsunami warning center through the communications buoy when the processor senses one of these waves. In addition to the tsunami detection buoy system, an end-to-end tsunami warning system was developed that builds upon the country's existing disaster warning infrastructure. This warning system includes 1) components that receive, process, and analyze buoy, seismic and tide gauge data; 2) predictive tools and a consequence assessment tool set to provide decision support; 3) operation center design and implementation; and 4) tsunami buoy operations and maintenance support. The first buoy was deployed Oct. 25, 2006, approximately 200 nautical miles west of San Diego in 3,800 meters of water. Just three weeks later, it was put to the test during an actual tsunami event. On Nov. 15, 2006, an 8.3 magnitude earthquake rocked the Kuril Islands, located between Japan and the Kamchatka Peninsula of Russia. That quake generated a small tsunami. Waves from the tsunami propagated approximately 4,000 nautical miles across the Pacific Ocean in about nine hours- a speed of about 445 nautical miles per hour when this commercial buoy first detected them. Throughout that event, the tsunami buoy system showed excellent correlation with data collected by a NOAA DART buoy located 28 nautical miles north of it. Subsequent analysis revealed that the STB matched DART operational capabilities and performed flawlessly. The buoy proved its capabilities again on Jan. 13, 2007, when an 8.1 magnitude earthquake occurred in the same region, and the STB detected the seismic event. As a result of the successes of this entire project, SAIC recently applied for and received a license from NOAA to build DART systems.","PeriodicalId":214543,"journal":{"name":"OCEANS 2007","volume":"85 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2007-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"7","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"OCEANS 2007","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/OCEANS.2007.4449208","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 7

Abstract

Results are presented regarding the first commercially available, fully operational, tsunami detection system to have passed stringent U.S. government testing requirements and to have successfully demonstrated its ability to detect an actual tsunami at sea. Spurred by the devastation of the December 26, 2004, Indian Ocean tsunami that killed more than 230,000 people, the private sector actively supported the Intergovernmental Oceanographic Commission's (IOC's) efforts to develop a tsunami warning system and mitigation plan for the Indian Ocean region. As each country in the region developed its requirements, SAIC recognized that many of these underdeveloped countries would need significant technical assistance to fully execute their plans. With the original focus on data fusion, consequence assessment tools, and warning center architecture, it was quickly realized that the cornerstone of any tsunami warning system would be reliable tsunami detection buoys that could meet very stringent operational standards. Our goal was to leverage extensive experience in underwater surveillance and oceanographic sensing to produce an enhanced and reliable deep water sensor that could meet emerging international requirements. Like the NOAA Deep-ocean Assessment and Recording of Tsunamis (DARTtrade) buoy, the SAIC Tsunami Buoy (STB) system consists of three subsystems: a surface communications buoy subsystem, a bottom pressure recorder subsystem, and a buoy mooring subsystem. With the operational success that DART has demonstrated, SAIC decided to build and test to the same high standards. The tsunami detection buoy system measures small changes in the depth of the deep ocean caused by tsunami waves as they propagate past the sensor. This is accomplished by using an extremely sensitive bottom pressure sensor/recorder to measure very small changes in pressure as the waves move past the buoy system. The bottom pressure recorder component includes a processor with algorithms that recognize these characteristics, and then immediately alerts a tsunami warning center through the communications buoy when the processor senses one of these waves. In addition to the tsunami detection buoy system, an end-to-end tsunami warning system was developed that builds upon the country's existing disaster warning infrastructure. This warning system includes 1) components that receive, process, and analyze buoy, seismic and tide gauge data; 2) predictive tools and a consequence assessment tool set to provide decision support; 3) operation center design and implementation; and 4) tsunami buoy operations and maintenance support. The first buoy was deployed Oct. 25, 2006, approximately 200 nautical miles west of San Diego in 3,800 meters of water. Just three weeks later, it was put to the test during an actual tsunami event. On Nov. 15, 2006, an 8.3 magnitude earthquake rocked the Kuril Islands, located between Japan and the Kamchatka Peninsula of Russia. That quake generated a small tsunami. Waves from the tsunami propagated approximately 4,000 nautical miles across the Pacific Ocean in about nine hours- a speed of about 445 nautical miles per hour when this commercial buoy first detected them. Throughout that event, the tsunami buoy system showed excellent correlation with data collected by a NOAA DART buoy located 28 nautical miles north of it. Subsequent analysis revealed that the STB matched DART operational capabilities and performed flawlessly. The buoy proved its capabilities again on Jan. 13, 2007, when an 8.1 magnitude earthquake occurred in the same region, and the STB detected the seismic event. As a result of the successes of this entire project, SAIC recently applied for and received a license from NOAA to build DART systems.
符合国际要求的海啸探测系统
介绍了首个商用、全面运行的海啸探测系统的结果,该系统通过了美国政府严格的测试要求,并成功证明了其探测海上实际海啸的能力。2004年12月26日,印度洋海啸造成23万多人死亡。在海啸造成巨大破坏的刺激下,私营部门积极支持政府间海洋学委员会(IOC)为印度洋地区制定海啸预警系统和减灾计划的努力。随着该地区每个国家都制定了自己的需求,工商总局认识到,许多不发达国家需要大量技术援助才能充分执行其计划。最初的重点是数据融合、后果评估工具和预警中心架构,但人们很快意识到,任何海啸预警系统的基石都是能够满足非常严格的操作标准的可靠海啸探测浮标。我们的目标是利用在水下监测和海洋传感方面的丰富经验,生产一种增强的、可靠的深水传感器,以满足新兴的国际要求。与NOAA深海海啸评估和记录(DARTtrade)浮标一样,SAIC海啸浮标(STB)系统由三个子系统组成:水面通信浮标子系统、海底压力记录仪子系统和浮标系泊子系统。随着DART的成功运行,SAIC决定按照同样的高标准进行建造和测试。海啸探测浮标系统测量海啸波经过传感器时引起的深海深度的微小变化。这是通过使用一个非常灵敏的底部压力传感器/记录仪来测量波浪经过浮标系统时压力的微小变化来实现的。海底压力记录仪组件包括一个处理器,该处理器具有识别这些特征的算法,当处理器感知到这些波浪之一时,它会立即通过通信浮标向海啸预警中心发出警报。除了海啸探测浮标系统外,还在该国现有灾害预警基础设施的基础上开发了端到端的海啸预警系统。该预警系统包括1)接收、处理和分析浮标、地震和潮汐计数据的组件;2)提供决策支持的预测工具和后果评估工具集;3)运营中心设计与实施;4)海啸浮标操作和维护支持。第一个浮标于2006年10月25日部署在圣地亚哥以西约200海里的3800米水域。仅仅三周后,它就在一次真正的海啸事件中受到了考验。2006年11月15日,位于日本和俄罗斯堪察加半岛之间的千岛群岛发生了8.3级地震。那次地震引发了一场小型海啸。海啸产生的波浪在大约9个小时内在太平洋上传播了大约4000海里——当这个商业浮标第一次探测到它们时,速度约为每小时445海里。在整个事件过程中,海啸浮标系统与位于海啸以北28海里的NOAA DART浮标收集的数据显示出良好的相关性。随后的分析表明,STB符合DART的操作能力,并且性能完美。2007年1月13日,该浮标再次证明了它的能力,当时同一地区发生了8.1级地震,STB探测到了地震事件。由于整个项目的成功,SAIC最近向NOAA申请并获得了建造DART系统的许可证。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信