Volcanic Hazards As Components of Complex Systems: the Case of Japan
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Inflation of the Aira Caldera (Japan) Detected Over
eEarth, 2, 17–25, 2007 www.electronic-earth.net/2/17/2007/ eEarth © Author(s) 2007. This work is licensed under a Creative Commons License. Inflation of the Aira Caldera (Japan) detected over Kokubu urban area using SAR interferometry ERS data D. Remy1,2,*, S. Bonvalot1,2, M. Murakami3, P. Briole2, and S. Okuyama4 1Institut de Recherche pour le Developpement´ (IRD), UR154, France 2Institut de Physique du Globe de Paris, 4 Place Jussieu, 75005 Paris, France 3Geographical Survey Institute, Mizusawa Geodetic Observatory, Japan 4Kyoto University, Dept. of Geophysics, Kyoto, 606-8502, Japan *presently at: Dept. of Geophysics, University of Chile, Santiago, Chile Received: 20 July 2006 – Published in eEarth Discuss.: 8 August 2006 Revised: 26 October 2006 – Accepted: 30 January 2007 – Published: 2 February 2007 Abstract. Nine ERS-1 and ERS-2 descending orbit data ac- 1 Introduction quired over Aira Caldera between June 1995 and November 1998 were used to create 36 differential interferograms. Al- Numerous papers have shown the potential of SAR (Syn- though the interferograms exhibit a relatively low level of thetic Aperture Radar) interferometry data for ground defor- coherence, even for couples sampling short time intervals (6 mation studies on volcanoes (Massonnet and Sigmundsson, months), Synthetique Aperture Radar (SAR) observations re- 2000; Zebker et al., 2000; Pritchard and Simons, 2002). Un- veal a distinct range change pattern over Kokubu urban area der optimal conditions a differential interferogram derived whose amplitude increases with the time separation between from two SAR images may monitor topographic changes in- SAR images. The analysis of the ground deformation time duced by internal volcanic processes with an accuracy of a series relative to the earliest ERS images showed a maxi- few cm over periods of time up to several months or years. -
Natural Hazards Predictions Name: ______Teacher: ______PD:___ 2
1 Unit 7: Earth’s Natural Hazards Lesson 1: Natural Hazards Lesson 2: Natural Hazards Predictions Name: ___________________ Teacher: ____________PD:___ 2 Unit 7: Lesson 1 Vocabulary 3 1 Natural Hazard: 2 Natural Disaster: 3 Volcano: 4 Volcanic Eruption: 5 Active Volcano: 6 Dormant Volcano: 7 Tsunami: 8 Tornado: 4 WHY IT MATTERS! Here are some questions to consider as you work through the unit. Can you answer any of the questions now? Revisit these questions at the end of the unit to apply what you discover. Questions: Notes: What types of natural hazards are likely where you live? How could the natural hazards you listed above cause damage or injury? What is a natural disaster? What types of monitoring and communication networks alert you to possible natural hazards? How could your home and school be affected by a natural hazard? How can the effects of a natural disaster be reduced? Unit Starter: Analyzing the Frequency of Wildfires 5 Analyzing the Frequency of Wildfires Choose the correct phrases to complete the statements below: Between 1970 and 1990, on average fewer than / more than 5 million acres burned in wildfires each year. Between 2000 and 2015, more than 5 million / 10 million acres burned in more than half of the years. Overall, the number of acres burned each year has been increasing / decreasing since 1970. 6 Lesson 1: Natural Hazards In 2015, this wildfire near Clear Lake, California, destroyed property and devastated the environment. Can You Explain it? In the 1700s, scientists in Italy discovered a city that had been buried for over 1,900 years. -
HAZARD MITIGATION for NATURAL DISASTERS a Starter Guide for Water and Wastewater Utilities
HAZARD MITIGATION FOR NATURAL DISASTERS A Starter Guide for Water and Wastewater Utilities Select a menu option below. New users should start with Overview Hazard Mitigation. Overview Join Local Mitigation Develop Mitigation Implement and Mitigation Case Study Hazard Mitigation Efforts Projects Fund Project Overview Overview - Hazard Mitigation Hazard Mitigation Join Local Hazards Posed by Natural Disasters Mitigation Efforts Water and wastewater utilities are vulnerable to a variety of hazards including natural disasters such as earthquakes, flooding, tornados, and Develop wildfires. For utilities, the impacts from these hazard events include Mitigation Projects damaged equipment, loss of power, disruptions to service, and revenue losses. Why Mitigate the Hazards? Implement and Fund Project It is more cost-effective to mitigate the risks from natural disasters than it is to repair damage after the disaster. Hazard mitigation refers to any action or project that reduces the effects of future disasters. Utilities can Mitigation implement mitigation projects to better withstand and rapidly recover Case Study from hazard events (e.g., flooding, earthquake), thereby increasing their overall resilience. Mitigation projects could include: • Elevation of electrical panels at a lift station to prevent flooding damage. • Replacement of piping with flexible joints to prevent earthquake damage. • Reinforcement of water towers to prevent tornado damage. Mitigation measures require financial investment by the utility; however, mitigation could prevent more costly future damage and improve the reliability of service during a disaster. Disclaimer: This Guide provides practical solutions to help water and wastewater utilities mitigate the effects of natural disasters. This Guide is not intended to serve as regulatory guidance. Mention of trade names, products or services does not convey official U.S. -
An Overview of Analogue Models Compared to Natural Calderas ⁎ Valerio Acocella
Available online at www.sciencedirect.com Earth-Science Reviews 85 (2007) 125–160 www.elsevier.com/locate/earscirev Understanding caldera structure and development: An overview of analogue models compared to natural calderas ⁎ Valerio Acocella Dipartimento Scienze Geologiche Roma Tre, Roma, Italy Received 1 August 2006; accepted 15 August 2007 Available online 28 August 2007 Abstract Understanding the structure and development of calderas is crucial for predicting their behaviour during periods of unrest and to plan geothermal and ore exploitation. Geological data, including that from analysis of deeply eroded examples, allow the overall surface setting of calderas to be defined, whereas deep drillings and geophysical investigations provide insights on their subsurface structure. Collation of this information from calderas worldwide has resulted in the recent literature in five main caldera types (downsag, piston, funnel, piecemeal, trapdoor), being viewed as end-members. Despite its importance, such a classification does not adequately examine: (a) the structure of calderas (particularly the nature of the caldera's bounding faults); and (b) how this is achieved (including the genetic relationships among the five caldera types). Various sets of analogue models, specifically devoted to study caldera architecture and development, have been recently performed, under different conditions (apparatus, materials, scaling parameters, stress conditions). The first part of this study reviews these experiments, which induce collapse as a result of underpressure or overpressure within the chamber analogue. The experiments simulating overpressure display consistent results, but the experimental depressions require an exceptional amount of doming, seldom observed in nature, to form; therefore, these experiments are not appropriate to understand the structure and formation of most natural calderas. -
Tomographic Image of the Crust Beneath the Aira Caldera in Southern Kyushu
IAVCEI 2013 Scientific Assembly - July 20 - 24, Kagoshima, Japan Forecasting Volcanic Activity - Reading and translating the messages of nature for society 4W_1B-P5 Date/Time: July 24 Poster Tomographic image of the crust beneath the Aira caldera in southern Kyushu Hiroki Miyamachi1, Paul Karson Alanis2, Hiroshi Yakiwara1, Takeshi Tameguri3, Masato Iguchi3 1Kagoshima University, Japan, 2Philippine Institute of Volcanology and Seismology, Philippines, 3Kyoto University, Japan E-mail: [email protected] Associated with the Philippine Sea plate subduction, a nearly straight chain of active Quaternary volcanism runs almost parallel to Nankai Trough in the central part of southern Kyushu. In this region, there are four large calderas: the Kakuto, the Aira, the Ata and the Kikai calderas. We applied the tomography method with a fine grid configuration to the P- and S-wave arrival times of 829 local earthquakes well observed at 101 stations in central and southern Kyushu, and revealed the detailed three-dimensional seismic velocity structure of the crust, especially the region beneath the Aira caldera. In a shallow range from 0 to 10 km depth, low velocity zones (LVZs) are found in the eastern part of Kyushu, where basement rocks are made up of uplifted sedimentary marine terraces (Nakada et al., 2002). The LVZs are also distributed along the volcanic front between Kirishima volcano to Kaimon volcano. Meanwhile, the hypocenters occurred in the inland area are obviously concentrated in regions with a relatively higher velocity and a low Poisson’s ratio at a depth of 10 km. At 20 km depth, the most interesting feature is that a distinctly high Poisson’s ratio zone is located exactly beneath the Aira caldera. -
Natural Hazards Mitigation Planning: a Community Guide
Natural A step-by-step guide Hazards to help Massachusetts communities deal with Mitigation multiple natural Planning: hazards and A Community to minimize Guide future losses Prepared by With assistance from Massachusetts Department of Environmental Management Federal Emergency Management Agency Massachusetts Emergency Management Agency Natural Resources Conservation Service Massachusetts Hazard Mitigation Team January 2003 Mitt Romney, Governor · Peter C. Webber, DEM Commissioner · Stephen J. McGrail, MEMA Director P r e f a c e The original version of this workbook was disaster mitigation program, the Flood Mitigation published in 1997 and entitled, Flood Hazard Assistance (FMA) program, as well as other federal, Mitigation Planning: A Community Guide. Its state and private funding sources. purpose was to serve as a guide for the preparation Although the Commonwealth of of a streamlined, cost-efficient flood mitigation plan Massachusetts has had a statewide Hazard by local governments and citizen groups. Although Mitigation Plan in place since 1986, there has been the main purpose of this revised workbook has not little opportunity for community participation and changed from its original mission, this version has input in the planning process to minimize future been updated to encompass all natural hazards and disaster damages. A secondary goal of the to assist Massachusetts’ communities in complying workbook is to encourage the development of with the all hazards mitigation planning community-based plans and obtain local input into requirements under the federal Disaster Mitigation Massachusetts’ state mitigation planning efforts in Act of 2000 (DMA 2000). The parts of this order to improve the state’s capability to plan for workbook that correspond with the requirements of disasters and recover from damages. -
Issue Brief: Disaster Risk Governance Crisis Prevention and Recovery
ISSUE BRIEF: DISASTER RISK GOVERNANCE CRISIS PREVENTION AND RECOVERY United Nations Development Programme “The earthquake in Haiti in January 2010 was about the same magnitude as the February 2011 earthquake in Christchurch, but the human toll was significantly higher. The loss of 185 lives in Christchurch was 185 too many. However, compared with the estimated 220,000 plus killed in Haiti in 2010, it becomes evident that it is not the magnitude of the natural hazard alone that determines its impact.” – Helen Clark, UNDP Administrator Poorly managed economic growth, combined with climate variability and change, is driving an overall rise in global disaster Around the world, it is the poor who face the greatest risk from risk for all countries. disasters. Those affected by poverty are more likely to live in drought and flood prone regions, and natural hazards are far Human development and disaster risk are interlinked. Rapid more likely to hurt poor communities than rich ones. economic and urban development can lead to growing Ninety-five percent of the 1.3 million people killed and the 4.4 concentrations of people in areas that are prone to natural billion affected by disasters in the last two decades lived in developing countries, and fewer than two per cent of global hazards. The risk increases if the exposure of people and assets deaths from cyclones occur in countries with high levels of to natural hazards grows faster than the ability of countries to development. improve their risk reduction capacity. DISASTER RISK REDUCTION AND GOVERNANCE In the context of risk management, this requires that the general public are sufficiently informed of the natural hazard risks they are exposed to and able to take necessary The catastrophic impact of disasters is not ‘natural.’ Disasters are precautions. -
Giant Rhyolite Lava Dome Formation
Kobe University Repository : Kernel タイトル Giant rhyolite lava dome formation after 7.3 ka supereruption at Kikai Title caldera, SW Japan Tatsumi, Yoshiyuki / Suzuki-Kamata, Keiko / Matsuno, Tetsuo / Ichihara, Hiroshi / Seama, Nobukazu / Kiyosugi, Koji / Nakaoka, Reina / 著者 Nakahigashi, Kazuo / Takizawa, Hideaki / Hayashi, Kazuki / Chiba, Author(s) Tatsuro / Shimizu, Satoshi / Sano, Mamoru / Iwamaru, Hikaru / Morozumi, Haruhisa / Sugioka, Hiroko / Yamamoto, Yojiro 掲載誌・巻号・ページ Scientific Reports,8:2753 Citation 刊行日 2018-02-09 Issue date 資源タイプ Journal Article / 学術雑誌論文 Resource Type 版区分 publisher Resource Version © The Author(s) 2018 This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party 権利 material in this article are included in the article’s Creative Commons Rights license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. DOI 10.1038/s41598-018-21066-w JaLCDOI URL http://www.lib.kobe-u.ac.jp/handle_kernel/90004609 -
Calderas in Japan
Calderas in Japan ref Main Post-Caldera Volcano Most Recent Caldera Type of Ejecta ref About Period No. About Formation Caldera Name Document No. Name Eruption Period (Symbol) 番号 14 Kishimoto, T., et al. (2009) Tephrostratigraphy and Eruption Mashu f Yamamoto, T., et al. (2010) C ages for the ejecta from Style of Mashu Volcano, During the Last 14,000 years, Eastern Mashu Kamuinupuri, Kamuisshuto 7.6 ka* 1, 5 1 Kutcharo and Mashu calderas, eastern Hokkaido, Japan. Bull. Geol. 5 (Ma-f) Hokkaido, Japan. Bull.Volcanol.Soc.Japan Surv. Japan, 61, 161-170. , 54, 15-37. 14 Hasegawa, T., et al. (2010) The history of caldera-forming Kutcharo 1 Yamamoto, T., et al. (2010) C ages for the ejecta from Kutcharo Atosanupuri, Nakajima 40 ka* 1, 2 1 Kutcharo and Mashu calderas, eastern Hokkaido, Japan. Bull. Geol. 2 eruptions in eastern Hokkaido, Japan. CHIKYU MONTHLY, 33, (Kp I) Surv. Japan, 61, 161-170. 726-734. Hasegawa, T., et al. (2010) The history of caldera-forming Hasegawa, T., et al. (2010) The history of caldera-forming Akan 1 Akan Meakandake, Oakandake 120←→210 ka 2 2 eruptions in eastern Hokkaido, Japan. CHIKYU MONTHLY, 33, 726- 2 eruptions in eastern Hokkaido, Japan. CHIKYU MONTHLY, 33, (Ak1) 734. 726-734. Yamagata, K (1994) Tephrochronological Study on the Shikotsu No. 1 Hiroshi Machida and Fusao Arai (2003) Atlas of tephra in and 3 6 Shikotsu and Kuttara Volcanoes in Southwestern Hokkaido, Shikotsu Eniwadake, Tarumaesan 40←→45 ka* 3, 6 around Japan. Univ. of Tokyo Press, 336p. (Spfl, Spfa-1) Japan. Jour. Geol. Soc. -
Earthquakes That Trigger Other Natural Hazards
Chain Reaction: Earthquakes that Trigger Other Natural Hazards Compiled by Diane Noserale and Tania Larson volcanic eruptions. concave structure called a “caldera.” These structures are Scientists have known that movement of magma often found around the world. Yellowstone and Crater Lake fi re destroys much of a major city. The side triggers earthquakes, but they are discovering that this are two examples in the United States. Research shows of a mountain collapses and then explodes. relationship may also work in reverse. Scientists are look- that activity at calderas often occurred within months or A train of waves sweeps away coastal vil- ing at earthquakes that meet very specifi c criteria: a mag- even hours of large regional earthquakes, sometimes as lages over thousands of miles. All of these nitude of 6 or higher; a location on major fault zones a precursor to the earthquakes and sometimes as a result events are disasters that have started with near a volcano; and a later eruption of a nearby volcano. of them. Aor been triggered by an earthquake. Some of the triggers They are fi nding evidence that these earthquakes might were among the largest earthquakes ever recorded. But have triggered the eruptions. Landslides the disasters that followed were often so large that the In the early morning of Nov. 29, 1975, a magnitude- Heavy rain, wildfi res, volcanic eruptions and human earthquakes were overshadowed, and so, we hear about 7.2 earthquake struck the Big Island of Hawaii. Less than activity often work together to cause landslides. In hilly the eruption of Mount St. -
Breaking Volcano News
Volcano News & Questions from Students VOLCANIC ERUPTIONS Physical Phenomena Causes – movement at plate boundaries Geography – spatial distribution Forms and eruption styles Magnitude Prediction – looking back & monitoring Hazards – quakes, blasts; release of ash, gas & lava Impacts Fatalities Economic Mitigation & Preparedness Begins with understanding vulnerability Recently, eruption of Icelandic volcano halted air travel Breaking Volcano News http://www.volcanolive.com/news.html …and news of breaking volcanoes History shows that when Eyjafjallajökull erupts, it’s larger neighbour Katla is generally not far behind. Katla is overdue. Katla’s eruption may be 10 or more x the size of the Eyjafjallajökull eruption –significant floods of fresh glacial-melt water into the sea (flow equal to Amazon + Mississippi + Nile + Yangtze occurred following 1755 eruption), a column of ash rising Chaiten, Chile 20km, or more, into the jet stream and spread over N Hemisphere. The Laki eruption in Iceland in 1783 resulted in famine across W Met Office, summer 2010 Europe, and as far S as Egypt, one of the longest and coldest ..as ash entrained in the atmosphere moved from winters on record in N America, and the death of 10,000s of Iceland across the Atlantic. people from gas poisoning and famine. 1 Merapi is at a subduction zone, where the Indo-Australian Plate is sliding NEWS beneath the Eurasian Plate and part of the Pacific Ring of Fire Stratigraphic analysis reveals that eruptions in the Merapi area began about Merapi Eruption 400,000 years ago, and from then until about 10,000 years ago, eruptions were effusive, and outflowing lava emitted was basaltic. -
Inflation of the Aira Caldera (Japan) Detected Over Kokubu
eEarth, 2, 17–25, 2007 www.electronic-earth.net/2/17/2007/ eEarth © Author(s) 2007. This work is licensed under a Creative Commons License. Inflation of the Aira Caldera (Japan) detected over Kokubu urban area using SAR interferometry ERS data D. Remy1,2,*, S. Bonvalot1,2, M. Murakami3, P. Briole2, and S. Okuyama4 1Institut de Recherche pour le Developpement´ (IRD), UR154, France 2Institut de Physique du Globe de Paris, 4 Place Jussieu, 75005 Paris, France 3Geographical Survey Institute, Mizusawa Geodetic Observatory, Japan 4Kyoto University, Dept. of Geophysics, Kyoto, 606-8502, Japan *presently at: Dept. of Geophysics, University of Chile, Santiago, Chile Received: 20 July 2006 – Published in eEarth Discuss.: 8 August 2006 Revised: 26 October 2006 – Accepted: 30 January 2007 – Published: 2 February 2007 Abstract. Nine ERS-1 and ERS-2 descending orbit data ac- 1 Introduction quired over Aira Caldera between June 1995 and November 1998 were used to create 36 differential interferograms. Al- Numerous papers have shown the potential of SAR (Syn- though the interferograms exhibit a relatively low level of thetic Aperture Radar) interferometry data for ground defor- coherence, even for couples sampling short time intervals (6 mation studies on volcanoes (Massonnet and Sigmundsson, months), Synthetique Aperture Radar (SAR) observations re- 2000; Zebker et al., 2000; Pritchard and Simons, 2002). Un- veal a distinct range change pattern over Kokubu urban area der optimal conditions a differential interferogram derived whose amplitude increases with the time separation between from two SAR images may monitor topographic changes in- SAR images. The analysis of the ground deformation time duced by internal volcanic processes with an accuracy of a series relative to the earliest ERS images showed a maxi- few cm over periods of time up to several months or years.