| Project/Area Number |
22241042
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| Research Category |
Grant-in-Aid for Scientific Research (A)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
Natural disaster science
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| Research Institution | Tohoku University |
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Principal Investigator |
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| Co-Investigator(Kenkyū-buntansha) |
GOTO Kazuhisa 東北大学, 災害科学国際研究所, 准教授 (10376543)
MATSUMOTO Hideaki 東北学院大学, 教養学部, 教授 (30173909)
KOSHIMURA Shunichi 東北大学, 災害科学国際研究所, 教授 (50360847)
都司 喜宣 東京大学, 地震研究所, 准教授 (30183479)
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| Co-Investigator(Renkei-kenkyūsha) |
MAKI Norio 京都大学, 防災研究所, 准教授 (40283642)
TAKAHASI Tomoyuki 関西大学, 社会安全学部, 教授 (40261599)
KOIWA Naohito 弘前大学, 教育学部, 准教授 (70296002)
SUGAWARA Daisuke 東北大学, 災害科学国際研究所, 助教 (50436078)
TSUJI Yoshinobu (財)深田地質研究所, 研究部, 客員研究員 (30183479)
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| Project Period (FY) |
2010-04-01 – 2014-03-31
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| Project Status |
Completed (Fiscal Year 2013)
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| Budget Amount *help |
¥47,060,000 (Direct Cost: ¥36,200,000、Indirect Cost: ¥10,860,000)
Fiscal Year 2013: ¥11,960,000 (Direct Cost: ¥9,200,000、Indirect Cost: ¥2,760,000)
Fiscal Year 2012: ¥12,090,000 (Direct Cost: ¥9,300,000、Indirect Cost: ¥2,790,000)
Fiscal Year 2011: ¥10,790,000 (Direct Cost: ¥8,300,000、Indirect Cost: ¥2,490,000)
Fiscal Year 2010: ¥12,220,000 (Direct Cost: ¥9,400,000、Indirect Cost: ¥2,820,000)
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| Keywords | ミレニアム災害 / 被害関数 / 津波堆積物 / 被害推定 / 回復 / 地震津波 / 低頻度災害 / 歴史災害 / 津波防災 / ミレニアム歴史津波 / 貞観地震津波 / 明和地震津波 / 東日本大震災 / 津波石 / 慶長地震津波 |
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| Research Abstract |
The purpose of the research is to evaluate the millennium tsunami hazard ,which is a low frequency giant tsunami disaster which occurs once in about 1000 years, by complementing based on scientific techniques, such as geology, sedimentology, topography, and seismology, in addition to the historical fact and documents in literatures. Millennium tsunami hazard evaluation was carried out in Okinawa and the Tohoku district. First, a possibility that 850yrBP and two terms of 1100 yrBP would be suggested by the investigation and analysis of a coral fossil (tsunami stone) which were launched from tsunami in Yaeyama Islands in addition to the 1771 Meiwa tsunami was shown. Furthermore, interdisciplinary investigation is conducted in Sendai plane that 1260yrBP and 2050 yrBP would is added to the 869 Jogan earthquake. Examination of the tsunami damage function etc. which were obtained by the 2011 Great East Japan Earthquake was also carried out.
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