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Dive into the research topics where Shinji Takarada is active.

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Featured researches published by Shinji Takarada.


Journal of Applied Volcanology | 2012

Global database on large magnitude explosive volcanic eruptions (LaMEVE)

Helen Sian Crosweller; Baneet Arora; Sarah K. Brown; Elizabeth Cottrell; Natalia Irma Deligne; Natalie Ortiz Guerrero; Laura Hobbs; Koji Kiyosugi; Susan C. Loughlin; Jonathan Lowndes; Martin Nayembil; Lee Siebert; R. S. J. Sparks; Shinji Takarada; Edward Venzke

To facilitate the assessment of hazards and risk from volcanoes, we have created a comprehensive global database of Quaternary Large Magnitude Explosive Volcanic Eruptions (LaMEVE). This forms part of the larger Volcanic Global Risk Identification and Analysis Project (VOGRIPA), and also forms part of the Global Volcano Model (GVM) initiative (http://www.globalvolcanomodel.org). A flexible search tool allows users to select data on a global, regional or local scale; the selected data can be downloaded into a spreadsheet. The database is publically available online at http://www.bgs.ac.uk/vogripa and currently contains information on nearly 3,000 volcanoes and over 1,800 Quaternary eruption records. Not all volcanoes currently have eruptions associated with them but have been included to allow for easy expansion of the database as more data are found. Data fields include: magnitude, Volcanic Explosivity Index (VEI), deposit volumes, eruption dates, and rock type. The scientific community is invited to contribute new data and also alert the database manager to potentially incorrect data. Whilst the database currently focuses only on large magnitude eruptions, it will be expanded to include data specifically relating to the principal volcanic hazards (e.g. pyroclastic flows, tephra fall, lahars, debris avalanches, ballistics), as well as vulnerability (e.g. population figures, building type) to facilitate risk assessments of future eruptions.


Journal of Applied Volcanology | 2014

Characterisation of the Quaternary eruption record: analysis of the Large Magnitude Explosive Volcanic Eruptions (LaMEVE) database

Sarah K. Brown; Helen Sian Crosweller; R. S. J. Sparks; Elizabeth Cottrell; Natalia Irma Deligne; Natalie Ortiz Guerrero; Laura Hobbs; Koji Kiyosugi; Susan C. Loughlin; Lee Siebert; Shinji Takarada

The Large Magnitude Explosive Volcanic Eruptions (LaMEVE) database contains data on 1,883 Quaternary eruption records of magnitude (M) 4 and above and is publically accessible online via the British Geological Survey. Spatial and temporal analysis of the data indicates that the record is incomplete and is thus biased. The recorded distribution of volcanoes is variable on a global scale, with three-quarters of all volcanoes with M≥4 Quaternary activity located in the northern hemisphere and a quarter within Japan alone. The distribution of recorded eruptions does not strictly follow the spatial distribution of volcanoes and has distinct intra-regional variability, with about 40% of all recorded eruptions having occurred in Japan, reflecting in part the country’s efforts devoted to comprehensive volcanic studies. The number of eruptions in LaMEVE decreases with increasing age, exemplified by the recording of 50% of all known Quaternary eruptions during the last 20,000 years. Historical dating is prevalent from 1450 AD to the present day, substantially improving record completeness. The completeness of the record also improves as magnitude increases. This is demonstrated by the calculation of the median time, T50, for eruptions within given magnitude intervals, where 50% of eruptions are older than T50: T50 ranges from 5,070 years for M4-4.9 eruptions to 935,000 years for M≥8 eruptions. T50 follows a power law fit, suggesting a quantifiable relationship between eruption size and preservation potential of eruptive products. Several geographic regions have T50 ages of <250 years for the smallest (~M4) eruptions reflecting substantial levels of under-recording. There is evidence for latitudinal variation in eruptive activity, possibly due to the effects of glaciation. A peak in recorded activity is identified at 11 to 9 ka in high-latitude glaciated regions. This is absent in non-glaciated regions, supporting the hypothesis of increased volcanism due to ice unloading around this time. Record completeness and consequent interpretation of record limitations are important in understanding volcanism on global to local scales and must be considered during rigorous volcanic hazard and risk assessments. The study also indicates that there need to be improvements in the quality of data, including assessment of uncertainties in volume estimates.


Frontiers of Earth Science in China | 2017

The Volcanic Hazards Assessment Support System for the Online Hazard Assessment and Risk Mitigation of Quaternary Volcanoes in the World

Shinji Takarada

Volcanic hazards assessment tools are essential for risk mitigation of volcanic activities. A number of offline volcanic hazard assessment tools have been provided, but in most cases, they require relatively complex installation procedure and usage. This situation causes limited usage of volcanic hazard assessment tools among volcanologists and volcanic hazards communities. In addition, volcanic eruption chronology and detailed database of each volcano in the world are essential key information for volcanic hazard assessment, but most of them are isolated and not connected to and with each other. The Volcanic Hazard Assessment Support System aims to implement a user-friendly, WebGIS-based, open-access online system for potential hazards assessment and risk-mitigation of Quaternary volcanoes in the world. The users can get up-to-date information such as eruption chronology and geophysical monitoring data of a specific volcano using the direct link system to major volcano databases on the system. Currently, the system provides 3 simple, powerful and notable deterministic modelling simulation codes of volcanic processes, such as Energy Cone, Titan2D and Tephra2. The system provides deterministic tools because probabilistic assessment tools are normally much more computationally demanding. By using the volcano hazard assessment system, the area that would be affected by volcanic eruptions in any location near the volcano can be estimated using numerical simulations. The system is being implemented using the ASTER Global DEM covering 2790 Quaternary volcanoes in the world. The system can be used to evaluate volcanic hazards and move this toward risk-potential by overlaying the estimated distribution of volcanic gravity flows or tephra falls on major roads, houses and evacuation areas using the GIS-enabled systems. The system is developed for all users in the world who need volcanic hazards assessment tools.


Journal of Applied Volcanology | 2015

How many explosive eruptions are missing from the geologic record? Analysis of the quaternary record of large magnitude explosive eruptions in Japan

Koji Kiyosugi; Charles B. Connor; R. S. J. Sparks; Helen Sian Crosweller; Sarah K. Brown; Lee Siebert; Ting Wang; Shinji Takarada


Journal of the Geological Society of Japan | 2004

Geology and volcanic history of Kita-Hakkoda volcanic group, Northeast Japan

Takashi Kudo; Shinji Takarada; Minoru Sasaki


Earth, Planets and Space | 2016

Estimation of total discharged mass from the phreatic eruption of Ontake Volcano, central Japan, on September 27, 2014

Shinji Takarada; Teruki Oikawa; Ryuta Furukawa; Hideo Hoshizumi; Jun’ichi Itoh; Nobuo Geshi; Isoji Miyagi


Island Arc | 2007

Petrological variation of large-volume felsic magmas from Hakkoda-Towada caldera cluster : Implications for the origin of high-K felsic magmas in the Northeast Japan Arc

Takashi Kudo; Minoru Sasaki; Yoshihiro Uchiyama; Akifumi Nozawa; Hisashi Sasaki; Takeshi Tokizawa; Shinji Takarada


Journal of the Geological Society of Japan | 2007

Eruptive history of Hokkaido-Komagatake volcano, northern Japan

Mituhiro Yoshimoto; Shinji Takarada; Ryo Takahashi


BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN | 2001

Ground deformation of the Usu 2000 eruption: Crack deformation measurements and theodolite monitoring at the northern and western foot of Usu Volcano, Japan@@@-北東山麓割れ目群の変位およびセオドライトによる北麓,西麓の観測結果-

Toshikazu Hasaka; Yuichi Nishimura; Shinji Takarada; Yuhei Takahashi; Mitsuru Nakagawa; Eiji Saito; Kazuaki Watanabe; Kohei Kazahaya; Yoshihisa Kawanabe; Takahiro Yamamoto; Wataru Hirose; Mitsuhiro Yoshimoto


BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN | 2001

Volcanic ash falls from the Usu 2000 eruption and situation at the source area.

Shinji Takarada; Mitsuhiro Yoshimoto; Jun-ichi Kitagawa; Naoto Hiraga; Takahiro Yamamoto; Yoshihisa Kawanabe; Akira Takada; Shun Nakano; Hideo Hoshizumi; Isoji Miyagi; Yuichi Nishimura; Daisuke Miura; Wataru Hirose; Satoshi Ishimaru; Yasuyuki Kakihara; Yuji Endo; Masahiro Yahata; Susumu Norota; Kiyoaki Niida; Yoshihiro Ishizuka; Takashi Kudo; Koji Aizawa; Hiroki Honma; Masamichi Egusa; Eiichi Ishii; Ryo Takahashi

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Joel Bandibas

National Institute of Advanced Industrial Science and Technology

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Yoshiharu Nishioka

National Institute of Advanced Industrial Science and Technology

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Akira Takada

National Institute of Advanced Industrial Science and Technology

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Yuzo Ishikawa

National Institute of Advanced Industrial Science and Technology

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Hideo Hoshizumi

National Institute of Advanced Industrial Science and Technology

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Makoto Saito

National Institute of Advanced Industrial Science and Technology

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Ryuta Furukawa

National Institute of Advanced Industrial Science and Technology

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Tadashi Maruyama

Japan Agency for Marine-Earth Science and Technology

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