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Fully-Coupled Simulations of Megathrust Earthquakes and Tsunamis in the Japan Trench, Nankai Trough, and Cascadia Subduction Zone
Noname manuscript No. (will be inserted by the editor) Fully-coupled simulations of megathrust earthquakes and tsunamis in the Japan Trench, Nankai Trough, and Cascadia Subduction Zone Gabriel C. Lotto · Tamara N. Jeppson · Eric M. Dunham Abstract Subduction zone earthquakes can pro- strate that horizontal seafloor displacement is a duce significant seafloor deformation and devas- major contributor to tsunami generation in all sub- tating tsunamis. Real subduction zones display re- duction zones studied. We document how the non- markable diversity in fault geometry and struc- hydrostatic response of the ocean at short wave- ture, and accordingly exhibit a variety of styles lengths smooths the initial tsunami source relative of earthquake rupture and tsunamigenic behavior. to commonly used approach for setting tsunami We perform fully-coupled earthquake and tsunami initial conditions. Finally, we determine self-consistent simulations for three subduction zones: the Japan tsunami initial conditions by isolating tsunami waves Trench, the Nankai Trough, and the Cascadia Sub- from seismic and acoustic waves at a final sim- duction Zone. We use data from seismic surveys, ulation time and backpropagating them to their drilling expeditions, and laboratory experiments initial state using an adjoint method. We find no to construct detailed 2D models of the subduc- evidence to support claims that horizontal momen- tion zones with realistic geometry, structure, fric- tum transfer from the solid Earth to the ocean is tion, and prestress. Greater prestress and rate-and- important in tsunami generation. state friction parameters that are more velocity- weakening generally lead to enhanced slip, seafloor Keywords tsunami; megathrust earthquake; deformation, and tsunami amplitude. -
Groundwater and Borehole Strain Monitoring for the Prediction
P06 Groundwater and borehole strain monitoring for the prediction research of the Tonankai and Nankai earthquakes Norio Matsumoto ([email protected]) , Naoji Koizumi, Makoto Takahashi, Yuichi Kitagawa, Satoshi Itaba, Ryu Ohtani and Tsutomu Sato Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (GSJ, AIST) 1. Nankai and Tonankai earthquakes Great earthquakes about magnitude 8 or more along the Nankai trough, off central to southwest Japan have been recognized nine times since 684 by ancient writings. Recent events were the 1944 Tonankai (M 7.9) and the 1946 Nankai (M 8.0) earthquakes along the Nankai trough after 90 - 92 years from the 1854 Ansei Tokai (M 8.4) and the 1854 Ansei Nankai (M 8.4) earthquakes. 2. Groundwater anomalies before and after the Nankai and Tonankai earthquakes Hydrological anomalies related to the past Nankai-Tonankai Preseismic hydrological anomalies at fifteen wells several days before the 1946 earthquakes were repeatedly reported in and around Shikoku Nankai earthquake were reported by Hydrographic Bureau (1948). Reported and Kii Peninsula by ancient writings. In particular, discharges anomalies were turbid groundwater and/or decreases of groundwater level or hot of hot spring stopped or decreased at the Dogo and Yunomine spring discharge. The manuscript also reported that there were legends in which hot springs after four and five of the nine Nankai-Tonankai decreases of groundwater level might happen before the occurrence of the Nankai- earthquakes, respectively. The 1946 Nankai earthquake caused Tonankai earthquakes around the wells where the preseismic anomalies were 11.2 m drop of well water level at the Dogo hot spring. -
HFA Irides Review Report Focusing on the 2011
Hyogo Framework for Action 2005-2015: Building the Resilience of Nations and Communities to Disasters HFA IRIDeS Review Report Focusing on 2011 Great East Japan Earthquake May 2014 International Research Institute of Disaster Science Tohoku University Japan Hyogo Framework for Action 2005-2015: Building the Resilience of Nations and Communities to Disasters HFA IRIDeS Review Report Focusing on 2011 Great East Japan Earthquake May 2014 International Research Institute of Disaster Science Tohoku University Japan Preface Having experienced the catastrophic disaster in 2011, Tohoku University has founded the International Research Institute of Disaster Science (IRIDeS). Together with collaborating organizations from many countries and staff with a broad array of specializations, the IRIDeS conducts world-leading research on natural disaster science and disaster mitigation. Based on the lessons from the 2011 Great East Japan (Tohoku) Earthquake and Tsunami disaster, the IRIDeS aims to become a world center for the research/ study of disasters and disaster mitigation, learning from and building upon past lessons in disaster management from Japan and others around the world. Throughout, the IRIDeS should contribute to on- going recovery/reconstruction efforts in areas affected by the 2011 tsunami, conducting action-oriented research and pursuing effective disaster management to build a sustainable and resilient society. The 3rd United Nations World Conference on Disaster Risk Reduction 2015 will be held on 14-18 March 2015 in Sendai City, one of the areas seriously damaged due to the 2011 Earthquake and Tsunami. The IRIDeS shall play an important role at the conference as an academic organization located in the hosting city. Drafting of this report, focusing on the 2011 Earthquake and Tsunami in terms of the core indicators of the Hyogo Framework for Action 2005-2015, is one of the contributory activities to the forthcoming event. -
Japan Is One of the Most Earthquake-Prone Countries
Research on Urban Earthquake Engineering at Tokyo Tech. - Earthquake Disaster Mitigation - The 2011 Tohoku Earthquake (M9) Anticipated Tokyo Earthquake Technologies for Earthquake Disaster Mitigation Hiroaki Yamanaka, Center for Urban Earthquake Engineering Tokyo Institute of Technology 1 Japan is one of the most earthquake-prone countries. Epicenters of Large Earthquakes 2 Damage Earthquakes with more than 1,000 Fatalities in Japan since Meiji era 1894 Nobi Earthquake M8.0 7,300 1896 Sanriku Tsunami M8.3 22,000 1923 Kanto Earthquake M7.9 105,000 1927 Kita-Tango Earthquake M7.3 2,900 1933 Sanriku Tsunami M8.1 3,100 1943 Tottori Earthquake M7.2 1,100 1944 Tonankai Earthquake M7.9 1,000 1945 Mikawa Earthquake M6.8 2,000 1946 Nankai Earthquake M8.0 1,400 1948 Fukui Earthquake M7.1 3,800 1995 Kobe Earthquake M7.3 6,300 2011 Tohoku Earthquake M9.0 19,000 3 Strong Shaking during the 1995 Kobe Earthquake 4 Damage of the 1995 Kobe (Inland) Earthquake The 2011 off the Pacific coast of Tohoku Earthquake Origin Time: 14:46, March/11/2011 Magnitude: Mw9.0 Number of dead and missing: 19,000 Number of displaced people: 300,000 Number of damaged houses: 1,000,000 Direct monetary loss: 200 billion US$ 6 Tectonic Plates in the Japanese archipelago and surrounding areas Fault Plane of the Tohoku Earthquake 500km Length Pacific plate subducts Japan Islands, and Japan Islands spring up after HERP generating tsunami and shaking. 7 Video of Tsunami in Sendai From You Tube8 Onagawa 9 Seismic Intensity Map MM Intensity Ⅵ Ⅶ Ⅷ Ⅸ Ⅹ XI JMA Intensity 4 5L 5U 6L 6U 7 after JMA The area of intensity 5 upper (MMI 8) or greater is approx. -
Source Rupture Process of the 2016 Central Tottori, Japan, Earthquake
Kubo et al. Earth, Planets and Space (2017) 69:127 DOI 10.1186/s40623-017-0714-3 EXPRESS LETTER Open Access Source rupture process of the 2016 central Tottori, Japan, earthquake (MJMA 6.6) inferred from strong motion waveforms Hisahiko Kubo1* , Wataru Suzuki1, Shin Aoi1 and Haruko Sekiguchi2 Abstract The source rupture process of the 2016 central Tottori, Japan, earthquake (MJMA 6.6) was estimated from strong motion waveforms using a multiple-time-window kinematic waveform inversion. A large slip region with a maximum slip of 0.6 m extends from the hypocenter to the shallower part, caused by the frst rupture propagating upward 0–3 s after rupture initiation. The contribution of this large slip region to the seismic waves in the frequency band of the waveform inversion is signifcant at all stations. Another large slip region with smaller slips was found in north- northwest of the hypocenter, caused by the second rupture propagating in the north-northwest direction at 3–5 s. Although the contribution of this slip region is not large, seismic waveforms radiating from it are necessary to explain the later part of the observed waveforms at several stations with diferent azimuths. The estimated seismic moment of 18 the derived source model is 2.1 10 Nm (Mw 6.1). The high-seismicity area of aftershocks did not overlap with large- slip areas of the mainshock. Two× wave packets in the high frequency band observed at near-fault stations are likely to correspond to the two signifcant ruptures in the estimated source model. Keywords: The 2016 central Tottori earthquake, Source rupture process, Strong motion waveforms Background the JMA scale and a maximum peak ground acceleration Te 2016 central Tottori earthquake occurred in the cen- (PGA) of over 1000 cm/s/s (Fig. -
International Comparative Study on Mega-Earthquake Disasters: an Introduction
INTERNATIONAL COMPARATIVE STUDY ON MEGAEARTHQUAKE DISASTERS: COLLECTION OF PAPERS Vol.1 巨大地震災害の国際比較研究報告書 - 1 2016 年 9 月 名古屋大学大学院環境学研究科 September 2016 Graduate School of Environmental Studies Nagoya University PDF VERSION INTERNATIONAL COMPARATIVE STUDY ON MEGAEARTHQUAKE DISASTERS: COLLECTION OF PAPERS Vol.1 巨大地震災害の国際比較研究報告書 - 1 2016 年 9 月 名古屋大学大学院環境学研究科 September 2016 Graduate School of Environmental Studies Nagoya University PDF VERSION International Comparative Study on Megaearthquake Disasters: Collection of Papers Vol.1 PDF Version Includes 120 + x pages Supported by the Grand‐in‐Aid, Japan Society for the Promotion of Sciences: www.jsps.go.jp Copyright © 2016 Graduate School of Environmental Studies, Nagoya University, Japan. All rights reserved ISBN 978‐4‐904316‐13‐9 Edited by Makoto Takahashi, Kenji Muroi and Shigeyoshi Tanaka, Graduate School of Environmental Studies, Nagoya University Published on September 30, 2016 Published by Graduate School of Environmental Studies, Nagoya University, Nagoya, Japan http://www.env.nagoya‐u.ac.jp/ Printed by Nagoya University Cooperative, Nagoya, Japan http://www.nucoop.jp/ i 緒 言 本報告書は、日本学術振興会科学研究費補助金(基盤研究 A)「多層的復興モデルに基づく巨 大地震災害の国際比較研究」の報告書(第 1 報)であり、巨大地震やその他の地球物理的災害、 防災制度やその変化などを扱った 8 編のワーキングパーパーを収録した。また、研究プロジェク ト開始以降の 1 年半におけるワークショップや研究会等の活動記録も掲載した。 米国地質調査所のデータベースによれば、21 世紀の 15 年間で死者 1 万人以上を数えるような 地震災害は世界全体で 7 つあり、そのうちの 6 つがアジアで起こっている。被害の大きさや影響 の社会的・空間的な広がり、その後の国の防災政策の転換に及ぼした意味において、とりわけ、 2004 年スマトラ地震、2008 年四川大地震、2011 年東日本大震災(東北地方太平洋沖地震)の 3 つが重要である。一方、地域的スケールで起こる規模の地震災害は、それよりも頻度が高いも のの、他の自然災害に比べて低頻度であることには違いはない。また、国際的には注目されるこ -
Detailed Coseismic Slip Distribution of the 1944 Tonankai Earthquake Estimated from Tsunami Waveforms
Detailed coseismic slip distribution of the 1944 Tonankai earthquake estimated from tsunami waveforms by Yuichiro TANIOKA1) ABSTRACT Various instrumental data have been used to study the 1944 Tonankai earthquake. Coseismic slip distribution on the fault plane Kanamori [1972] used seismological data to of the 1944 Tonankai earthquake is estimated estimate the focal mechanism, and inferred from inversion of tsunami waveforms. The that the source area agreed with the one-day inversion result shows that a maximum slip aftershock distribution off the Kii Peninsula. of about 3 m occurred on the plate interface Recently, Kikuchi et al. [1999] estimated the off Shima peninsula. The total seismic seismic moment distribution using strong moment is estimated to be 2.0 X 1021 Nm (Mw motion waveforms recorded by the Japan 8.2). The result confirms that the 1944 Meteorological Agency. Ando [1975], Inouchi Tonankai earthquake did not rupture the and Sato [1975], and Ishibashi [1981] plate interface beneath the Tokai region and estimated the fault parameters using geodetic supports the existence of the seismic gap in data. A more detailed study based on geodetic the Tokai region. The slip of about 1.5 m on data [Sagiya and Thatcher, 1999] estimated the plate interface beneath Atsumi peninsula, the heterogeneous slip distribution on the northeast of the large slip area, is necessary down-dip side of the fault plane. However, the to explain the observed tsunami waveforms, geodetic data do not have resolution to although no seismic moment release was estimate the slips on the up-dip (offshore) estimated from strong motion data by side of the fault plane. -
A Revised Tsunami Source Model for the 1707 Hoei Earthquake and Simulation of Tsunami Inundation of Ryujin Lake, Kyushu, Japan
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 116, B02308, doi:10.1029/2010JB007918, 2011 A revised tsunami source model for the 1707 Hoei earthquake and simulation of tsunami inundation of Ryujin Lake, Kyushu, Japan Takashi Furumura,1,2 Kentaro Imai,1,2,3 and Takuto Maeda1,2 Received 9 August 2010; revised 5 November 2010; accepted 1 December 2010; published 16 February 2011. [1] Based on many recent findings such as those for geodetic data from Japan’s GEONET nationwide GPS network and geological investigations of a tsunami‐inundated Ryujin Lake in Kyushu, we present a revised source rupture model for the great 1707 Hoei earthquake that occurred in the Nankai Trough off southwestern Japan. The source rupture area of the new Hoei earthquake source model extends further, to the Hyuga‐nada, more than 70 km beyond the currently accepted location at the westernmost end of Shikoku. Numerical simulation of the tsunami using a new source rupture model for the Hoei earthquake explains the distribution of the very high tsunami observed along the Pacific coast from western Shikoku to Kyushu more consistently. A simulation of the tsunami runup into Ryujin Lake using the onshore tsunami estimated by the new model demonstrates a tsunami inundation process; inflow and outflow speeds affect transport and deposition of sand in the lake and around the channel connecting it to the sea. Tsunamis from the 684 Tenmu, 1361 Shokei, and 1707 Hoei earthquakes deposited sand in Ryujin Lake and around the channel connecting it to the sea, but lesser tsunamis from other earthquakes were unable to reach Ryujin Lake. -
HFA Irides Review Preliminary Report Focusing on 2011 Great East Japan Earthquake
October, 2013 Having experienced the catastrophic disaster in 2011, Tohoku University has founded the International Research Institute of Disaster Science (IRIDeS). Together with collaborating organizations from many countries and staff with a broad array of specializations, IRIDeS conducts world-leading research on natural disaster science and disaster mitigation. Based on the lessons from the 2011 Great East Japan (Tohoku) Earthquake and Tsunami disaster, IRIDeS aims to become a world center for the study of disasters and disaster mitigation, learning from and building upon past lessons in disaster management from Japan and around the world. Throughout, IRIDeS will contribute to on-going recovery/reconstruction efforts in areas affected by the 2011 tsunami, conducting action-oriented research and pursuing effective disaster management to build a sustainable and resilient society. The 3rd United Nations World Conference on Disaster Risk Reduction 2015 will be held in Sendai City, one of the areas seriously damaged due to the 2011 Great East Japan Earthquake and Tsunami. IRIDeS will play an important role for the conference as an academic organization located in the hosting city. Drafting of this report, focusing on the 2011 Great East Japan Earthquake and Tsunami in terms of the core indicators of the Hyogo Framework for Action 2005-2015, is one of the contributory activities to the forthcoming event. This publication is the preliminary report toward the final issue, which will be released in March 2014. We hope that the Japanese experience of past disasters including the Great East Japan Earthquake and Tsunami will be shared among national/local governments, the private sector, and citizens all over the world. -
Source Modeling for Long-Period Ground Motion Simulation of the 1946 Nankai Earthquake, Japan
Source Modeling for Long-Period Ground Motion Simulation of the 1946 Nankai Earthquake, Japan T. Kagawa Graduate School of Engineering, Tottori University, Japan A. Petukhin Geo-Research Institute, Japan K. Koketsu, H. Miyake, and S. Murotani Earthquake Research Institute, University of Tokyo, Japan SUMMARY Long-period ground motions over 2 seconds due to the 1946 Nankai earthquake are simulated. Minute 3-D crustal and sedimentary structure model developed for the purpose is employed for the simulation. Source model of the earthquake is reconsidered through source inversions with Green’s functions calculated from the 3-D structure model. Keywords: The 1946 Nankai earthquake, Japan, Source Inversion, 3-D Green’s function 1. INTRODUCTION Among earthquakes, repeatedly rupturing along the Nankai trough, source of the M8 class Nankai earthquake covers segments from cape Shiono-misaki to cape Ashizuri-misaki, southwest Japan. The last event was the 1946 Nankai earthquake (the Showa Nankai earthquake). Considering that average interval is 110 years, probability of occurrence of the next Nankai earthquake within next 30 years is estimated about 60% (HERP, 2011). Figure 0. Target area for long-period ground motion modeling. Dashed lines: Nankai Trough and source area of Nankai and Tonankai earthquakes. Circled numbers are major sedimentary basins and structures: 1:Mikawa, 2:Nobi, 3:Ise, 4:Ohmi, 5:Kyoto, 6:Nara, 7:Osaka, 8:Wakayama, 9:Tokushima, 10:Kochi, 11:Yonago, 12:Oita, 13:Miyazaki, 14:Aso-Kushu volcanic area, 15:Unzen volcano. In this study, long-period ground motions due to the earthquake are simulated assuming that the next Nankai earthquake will be similar to the 1946 Nankai earthquake relatively well recorded and studied in details. -
Appendix (PDF:4.3MB)
APPENDIX TABLE OF CONTENTS: APPENDIX 1. Overview of Japan’s National Land Fig. A-1 Worldwide Hypocenter Distribution (for Magnitude 6 and Higher Earthquakes) and Plate Boundaries ..................................................................................................... 1 Fig. A-2 Distribution of Volcanoes Worldwide ............................................................................ 1 Fig. A-3 Subduction Zone Earthquake Areas and Major Active Faults in Japan .......................... 2 Fig. A-4 Distribution of Active Volcanoes in Japan ...................................................................... 4 2. Disasters in Japan Fig. A-5 Major Earthquake Damage in Japan (Since the Meiji Period) ....................................... 5 Fig. A-6 Major Natural Disasters in Japan Since 1945 ................................................................. 6 Fig. A-7 Number of Fatalities and Missing Persons Due to Natural Disasters ............................. 8 Fig. A-8 Breakdown of the Number of Fatalities and Missing Persons Due to Natural Disasters ......................................................................................................................... 9 Fig. A-9 Recent Major Natural Disasters (Since the Great Hanshin-Awaji Earthquake) ............ 10 Fig. A-10 Establishment of Extreme Disaster Management Headquarters and Major Disaster Management Headquarters ........................................................................... 21 Fig. A-11 Dispatchment of Government Investigation Teams (Since -
Preseismic Slip Associated with Large Earthquakes Along the Nankai
Groundwater and Coastal Phenomena Preceding the 1944 Tsunami (Tonankai Earthquake) Masataka Ando Institute of Earth Sciences, Academia Sinica [email protected] Study Area Osaka Nagoya Mt. Fuji 600 km Tokyo West East 2 cm/y 5 cm/y 4 cm/y Philippine Sea Plate Characteristics of large earthquakes along the Nankai trough 1. Strong ground motions in a large region 2. Tsunami damages in a large region 3. Groundwater level changes at hot springs *4. Crustal deformation (not always documented) Hot spring Uplift Subsi- dence Well Expansion Documented Oldest Nankai Trough Earthquake, 684 A.D. • Documented only with about 100 characters in an official document (“Nihon Shoki”), • But this information is sufficient to identify the event as a large subduction earthquake along Nankai trough since it describes three following key words: 1) Regional strong shaking 2) Regional large tsunami 3) Groundwater level changes Large Earthquakes along the Nankai Trough 1944 and 1946 Events ( Tonankai and Nankai) Tide gage records at San Diego 1944 1946 (Tanioka and Satake, 1993) Data from Kenji Satake 1854 Two Earthquakes (Ansei) 32 hours time difference Two tsunamis recorded at San Diego West East 1944 and 1946 events, 1/2 –1/3 of 1854 events Recorded at San Diego, Filtered West East East West (Tanioka and Satake,(Kenji 1993) Satake) 1707 Earthquake (Hoei) 1703 7 170 Casualties 5,049 + (10,000 in Osaka?) Injured 1,430 Lost houses by tsunamis 18,025 Collapsed houses 59,272 Wrecked ships 3,915 1605 earthquake (Keicho) • Only slight damage by strong ground motions • Extensive tsunami damage over West Japan • No Groundwater level change at hot springs ・What is the mechanism of 1605 earthquake? ・Is this really a Nankai trough earthquake? In 1603 Tokugawa Shogunate was established but the center of culture was still Kyoto.