GNSS Observation of Volcanic Activities in Sakurajima
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Correlating the Electrification of Volcanic Plumes With
Earth and Planetary Science Letters 492 (2018) 47–58 Contents lists available at ScienceDirect Earth and Planetary Science Letters www.elsevier.com/locate/epsl Correlating the electrification of volcanic plumes with ashfall textures at Sakurajima Volcano, Japan ∗ Cassandra M. Smith a, , Alexa R. Van Eaton b, Sylvain Charbonnier a, Stephen R. McNutt a, Sonja A. Behnke c, Ronald J. Thomas d, Harald E. Edens d, Glenn Thompson a a University of South Florida, School of Geosciences, Tampa, FL, United States of America b U.S. Geological Survey, Cascades Volcano Observatory, Vancouver, WA, United States of America c Los Alamos National Laboratory, Los Alamos, NM, United States of America d New Mexico Institute of Mining and Technology, Department of Physics, Socorro, NM, United States of America a r t i c l e i n f o a b s t r a c t Article history: Volcanic lightning detection has become a useful resource for monitoring remote, under-instrumented Received 7 September 2017 volcanoes. Previous studies have shown that the behavior of volcanic plume electrification responds to Received in revised form 26 March 2018 changes in the eruptive processes and products. However, there has not yet been a study to quantify the Accepted 27 March 2018 links between ash textures and plume electrification during an actively monitored eruption. In this study, Available online 11 April 2018 we examine a sequence of vulcanian eruptions from Sakurajima Volcano in Japan to compare ash textural Editor: T.A. Mather properties (grain size, shape, componentry, and groundmass crystallinity) to plume electrification using Keywords: a lightning mapping array and other monitoring data. -
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. -
Systems Analysis of Social Resilience Against Volcanic Risks: Case Studies of Mt
Systems Analysis of Social Resilience against Volcanic Risks: Case Studies of Mt. Merapi, Indonesia and Mt. Sakurajima, Japan by Saut Aritua Hasiholan Sagala A thesis submitted in fulfilment of the requirements of the degree of Doctor of Engineering Supervised by Prof. Norio Okada DEPARTMENT OF URBAN MANAGEMENT GRADUATE SCHOOL OF ENGINEERING Kyoto University August, 2009 Acknowledgements This thesis has benefitted from collaboration with and contribution by many people. Therefore, I want to thank a number of people for their assistance while I was preparing for this thesis and completing my doctoral study in Kyoto University (KU). First of all, I would like to express my gratitude to Prof Norio Okada, my PhD advisor, who has provided a lot of important ideas for the completion of my PhD research. His excellent experiences in research fields and ways of building networks have become my source of inspiration. Finally, Prof Okada has also kindly recommended me to the scholarship provided by Monbukagakusho under Kyoto University - International Doctoral Program which funded my study in Kyoto. The next person I would like to thank is Dr. Muneta Yokomatsu, who are very kind and friendly, but at the same time has been the role model of how a real researcher should be. I have gain many insight during our discussion time. In particular I would like to thank Dr. Yokomatsu for helping me during the field visit to Mt. Sakurajima. Prof Douglas Paton of University of Tasmania has provided an enormous help for my research and has been a great discussion partner in which we have written some research articles which are parts of this thesis. -
Case Study Notes
Hazardous Earth: Sakurajima and Nyiragongo Volcano in a Developed Country: Sakurajima, Japan Sakurajima is a composite volcano (also called a stratovolcano) located in southern Japan. The volcano has been extremely active since the 1950s; some years, up to 200 eruptions have taken place! Sakurajima is on a convergent plate boundary, where the Pacific plate subducts beneath the Eurasian plate. (Source:www.flickr.com/photos/kimon/4506849144/) This type of plate boundary causes Sakurajima eruptions to be explosive, producing lots of ash, pyroclastic flows, volcanic bombs and poisonous gases. The lava is andesitic, which has a high gas content and is very viscous (thick). Japan is a developed country, with a GDP of 4.97 trillion USD (2018). Location of Sakurajima (orange icon). h Volcano in a Developing Country: Mount Nyiragongo, DRC Mount Nyiragongo is a composite volcano located in the east of the Democratic Republic of the Congo (DRC). The volcano consists of a huge (2km wide) crater usually filled with a lava lake, and is only 20km away from the city of Goma. Nyiragongo is currently classed as active (2020). (Source: wiki) Nyiragongo is on a divergent plate boundary: the African plate is being pulled apart into the Nubian plate (east) and Somali plate (west), causing lava to rise between. This results in non-explosive eruptions with basaltic lava which has a low viscosity (runny & fast-flowing - up to 37 mph). Location of Nyiragongo (orange icon). This work by PMThttps://bit.ly/pmt-edu-cc Education is licensed under https://bit.ly/pmt-ccCC BY-NC-ND 4.0 https://bit.ly/pmt-cc https://bit.ly/pmt-edu https://bit.ly/pmt-cc Impacts of Volcanoes in Contrasting Areas Impacts in Japan Developed country Primary impacts ● Around 30km3 of ash erupts from the volcano each year, damaging crops and electricity lines. -
Seasonal Variations of Volcanic Ash and Aerosol Emissions Around Sakurajima Detected by Two Lidars
atmosphere Article Seasonal Variations of Volcanic Ash and Aerosol Emissions around Sakurajima Detected by Two Lidars Atsushi Shimizu 1,* , Masato Iguchi 2 and Haruhisa Nakamichi 2 1 National Institute for Environmental Studies, Tsukuba 305-8506, Japan 2 Sakurajima Volcano Research Center, Disaster Prevention Research Institute, Kyoto University, Kagoshima 891-1419, Japan; [email protected] (M.I.); [email protected] (H.N.) * Correspondence: [email protected]; Tel.: +81-29-850-2489 Abstract: Two polarization-sensitive lidars were operated continuously to monitor the three-dimensional distribution of small volcanic ash particles around Sakurajima volcano, Kagoshima, Japan. Here, we estimated monthly averaged extinction coefficients of particles between the lidar equipment and the vent and compared our results with monthly records of volcanic activity reported by the Japan Meteorological Agency, namely the numbers of eruptions and explosions, the density of ash fall, and the number of days on which ash fall was observed at the Kagoshima observatory. Elevated extinction coefficients were observed when the surface wind direction was toward the lidar. Peaks in extinction coefficient did not always coincide with peaks in ash fall density, and these differences likely indicate differences in particle size. Keywords: volcanic ash; aerosol; lidar; extinction coefficient; horizontal wind Citation: Shimizu, A.; Iguchi, M.; 1. Introduction Nakamichi, H. Seasonal Variations of Volcanic eruptions are a natural source of atmospheric aerosols [1]. In the troposphere Volcanic Ash and Aerosol Emissions and stratosphere, gaseous SO2 is converted to sulfate or sulfuric acid within several around Sakurajima Detected by Two days, which can remain in the atmosphere for more than a week. -
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. -
Living with the Volcano – Darrell A. Norris
LIVING WITH THE VOLCANO LIVING WITH THE VOLCANO Danell A. Norris Professorof Geography SLINY at Geneseo Geneseo.NY 14454 ABSTRACT: The volcanic peninsulaSakurajima dominates Kagoshima Bay in southem Kyushu, Japan. A major eruption in l9l4 devastatedthe city of Kagoshima. For decades,eruptions have been minor but frequent,occurring with daily frequencyin recentyears. In 1991 Sakurajimaerupted 440 times. Sakurajima'slandscape affords abundantevidence of its cataclysmicpast and of ongoing efforts to minimize the impactsof future eruptions. In one sensethe precautionarymeasures are very much what one would expect of an affluent society's responseto a major hazard. Japancan afford to protect its 5245 Sakurajimanresidents. Yet closer scrutiny revealsa pattern of adaptationand responsewhich is centeredon core valuesand their expressionin Japaneseculture. In some respects these values have been relinquishedor modified to accommodatethe harsh environment. In other respects they show almost cavalier disregard for Sakurajima's destructive potential, and astute recognition of its economic benefits. And in a wider senseSakurajima is Japan itself in uneasy microcosm, an emblematic and endlesssaga of environmentalchallenge and human response. One glancesa lot in Kagoshima. The city lies low and vulnerable,four kilometers and an exhalation away from Sakurajima,a volcano slowly reclaiming its old patrimony in the caldera expanseand ancientcrater walls of KagoshimaBay. Sakurajimais a busy volcano. Two years ago it erupted440 times. Like so much else in Japan,Sakurajima's numbers shroud its reality. precise integers pepper the Visitors' Center and the downtown Natural ScienceMuseum's volcano room. Like lava, the numbers are overpowering,inexorable, and numbing. Numbers and volcanoesfind an uneasytruce. The small eruptions,440 one year, 290 another,seem seamless and uncountable. -
Insights Into Global Explosive Volcanic Eruptive Activity Through Analysis of Volcanic Ash Advisories
Bulletin of Volcanology (2021) 83: 9 https://doi.org/10.1007/s00445-020-01419-y RESEARCH ARTICLE Near-real-time volcanic cloud monitoring: insights into global explosive volcanic eruptive activity through analysis of Volcanic Ash Advisories S. Engwell1 & L. Mastin2 & A. Tupper3,4 & J. Kibler5 & P. Acethorp6 & G. Lord7,8 & R. Filgueira1,9 Received: 29 April 2020 /Accepted: 29 October 2020 / Published online: 21 January 2021 # The Author(s) 2020 Abstract Understanding the location, intensity, and likely duration of volcanic hazards is key to reducing risk from volcanic eruptions. Here, we use a novel near-real-time dataset comprising Volcanic Ash Advisories (VAAs) issued over 10 years to investigate global rates and durations of explosive volcanic activity. The VAAs were collected from the nine Volcanic Ash Advisory Centres (VAACs) worldwide. Information extracted allowed analysis of the frequency and type of explosive behaviour, including analysis of key eruption source parameters (ESPs) such as volcanic cloud height and duration. The results reflect changes in the VAA reporting process, data sources, and volcanic activity through time. The data show an increase in the number of VAAs issued since 2015 that cannot be directly correlated to an increase in volcanic activity. Instead, many represent increased observations, including improved capability to detect low- to mid-level volcanic clouds (FL101–FL200, 3–6 km asl), by higher temporal, spatial, and spectral resolution satellite sensors. Comparison of ESP data extracted from the VAAs with the Mastin et al. (J Volcanol Geotherm Res 186:10–21, 2009a) database shows that traditional assumptions used in the classification of volcanoes could be much simplified for operational use. -
Volcanic Hazards As Components of Complex Systems: the Case of Japan
Volume 13 | Issue 33 | Number 6 | Article ID 4359 | Aug 17, 2015 The Asia-Pacific Journal | Japan Focus Volcanic Hazards as Components of Complex Systems: The Case of Japan Gregory Smits The past year or so has been a time of the earth’s crust suggested Mt. Fuji is more particularly vigorous volcanic activity in Japan, likely to erupt owing to effects from the 2011 or at least activity that has intruded into public Tōhoku earthquake.3 Well publicized by a press awareness. Perhaps most dramatic was the release on the eve of its publication, mass deadly eruption of Mt. Ontake on September media around the world have reported this 27, 2014, whose 57 fatalities were the first finding, along with speculation regarding volcano-related deaths in Japan since 1991. On possible connections between earthquakes and May 29, 2015, Mt. Shindake, off the southern volcanic eruptions. tip of Kyushu, erupted violently, forcing the evacuation of the island of Kuchinoerabu. That As of June 30, 2015, the Japan Meteorological same day, Sakurajima, located just north in Agency (JMA) designated ten volcanoes in or Kagoshima Bay, erupted more forcefully than near the main Japanese islands as warranting usual. Sakurajima has been erupting in some levels of warning ranging from Mt. Shindake’s fashion almost continuously since 1955, but Level 5 (“Evacuate”), to Level 2 (“Do not since 2006, its activity has become relatively approach the crater”) in seven cases. more vigorous. Indeed, a May 30 Asahi shinbun Sakurajima is at Level 3 (“Do not approach the article characterized these eruptions as “the volcano”), as is Hakoneyama, located near Mt. -
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. -
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.