Tsunami Simulations after the Mw7.5 78km N of Palu, Indonesia September 28, 2018
|
|
- Willis Fisher
- 5 years ago
- Views:
Transcription
1 Tsunami Simulations after the Mw7.5 78km N of Palu, Indonesia September 28, 2018 Luisa Urra, Erick Mas, Luis Moya, Shunichi Koshimura LABORATORY OF REMOTE SENSING AND GEOINFORMATICS FOR DISASTER MANAGEMENT
2 Summary of Cases Modeled Uniform Slip Model (USM) Case 0 (LxW:120x20km, H:5km, Sk:349, Dp:86, Sp:-17, Slip:3.1, Lat:-0.89, Lon:119.75) Case 1 (LxW:100x20km, H:5km, Sk:347, Dp:86, Sp:-17, Slip:3.7, Lat:-0.89, Lon:119.85) Case 2 (LxW:100x20km, H:1km, Sk:347, Dp:86, Sp:-17, Slip:3.7, Lat:-0.89, Lon:119.75) Finite Fault Models (USGS) USGS1-Case0 (Basic Inversion - Link) USGS2-Case0 (Complete Inversion - Link) USGS2-Case1 (Complete Inversion adjusted to the trench) USGS2-Case2 (Shifted south towards Palu Bay) USGS2-Case3 (Shifted southern inside Palu) TOHOKU UNIVERSITY Geoinformatics for Disaster Management 2
3 Summary of Max Tsunami Heights Case Height (m) USM-C0 1.3 USM-C1 2.7 USM-C2 2.7 Case Height (m) USGS1-C USGS2-C0 Under Simulation USGS2-C USGS2-C USGS2-C 'N Okada's deformation [m] 0 0' TOHOKU UNIVERSITY 0 30'S 'E 'E 'E USGS FFM file2-case 'E 120 0'E 'E 'E Source: Esri, DigitalGlobe, GeoEye, Earthstar Geographics, CNES/Airbus DS, USDA, USGS, AeroGRID, IGN, and the GIS User Community Geoinformatics for Disaster Management Note: Maximum value was extracted from smallest region in Palu Bay. For best comparison confirm with max plots. 3
4 Uniform Slip Model Case 0 USGS Moment Tensor (NP2) Parameters (modified) Parameters (Mw7.5) (LxW, Depth, strike, dip, slip, dislocation) 120kmx20km, 5km, 349deg, 86deg, -17deg, 3.1m Max Tsunami Height: 1.3m (1 Region GEBCO) TOHOKU UNIVERSITY Geoinformatics for Disaster Management 4
5 Uniform Slip Model Case 1 USGS Moment Tensor (NP2) Parameters (modified) Parameters (Mw7.5) (LxW, Depth, strike, dip, slip, dislocation) 100kmx20km, 5km, 347deg, 86deg, -17deg, 3.7m Max Tsunami Height: 2.7 m (5 Regions GEBCO) TOHOKU UNIVERSITY Geoinformatics for Disaster Management 5
6 Uniform Slip Model Case 1 USGS Moment Tensor (NP2) Parameters (modified) Parameters (Mw7.5) (LxW, Depth, strike, dip, slip, dislocation) 100kmx20km, 5km, 347deg, 86deg, -17deg, 3.7m Max Tsunami Height: 2.7 m (5 Regions GEBCO) '0"E '30"E '0"E '30"E '0"E '30"E '0"E 0 52'30"S 0 52'0"S 0 53'0"S 0 53'30"S Tsunami height [ m] ,000 m TOHOKU UNIVERSITY Geoinformatics for Disaster Management 6
7 Uniform Slip Model Case 1 TOHOKU UNIVERSITY Geoinformatics for Disaster Management 7
8 8
9 Uniform Slip Model Case 2 USGS Moment Tensor (NP2) Parameters (modified) Parameters (Mw7.5) (LxW, Depth, strike, dip, slip, dislocation) 100kmx20km, 1km, 347deg, 86deg, -17deg, 3.7m Max Tsunami Height: 2.7 m TOHOKU UNIVERSITY Geoinformatics for Disaster Management 9
10 Uniform Slip Model Case 2 USGS Moment Tensor (NP2) Parameters (modified) Parameters (Mw7.5) (LxW, Depth, strike, dip, slip, dislocation) 100kmx20km, 1km, 347deg, 86deg, -17deg, 3.7m Max Tsunami Height: 2.7 m (5 Regions GEBCO) '0"E '30"E '0"E '30"E '0"E '30"E '0"E 0 52'30"S 0 52'0"S 0 53'0"S 0 53'30"S Tsunami height [ m] ,000 m TOHOKU UNIVERSITY Geoinformatics for Disaster Management 10
11 Uniform Slip Model Case 2 TOHOKU UNIVERSITY Geoinformatics for Disaster Management 11
12 12
13 Finite Fault Model USGS1-Case0 S l i p [ m ] 0 40'S 0 20'S 0 0' 0 20'N 0 40'N 'E 'E 120 0'E USGS/FFM1/case0 Dip angle: 86 Strike angle: 358 xll: yll: 'E Esri, HERE, Garmin, OpenStreetMap contributors, and the GIS user community 13
14 Finite Fault Model USGS1-Case0 14
15 Finite Fault Model USGS1-Case0 Max Tsunami Height: 3.19 m '0"E '30"E '0"E '30"E '0"E '30"E '0"E 0 52'30"S 0 52'0"S 0 53'0"S 0 53'30"S Tsunami height [ m] ,000 m 15
16 Finite Fault Model USGS2-Case0 S l i p [ m ] 0 40'S 0 20'S 0 0' 0 20'N 0 40'N 'E 'E 120 0'E USGS/FFM2/original Dip angle: 86 Strike angle: 358 xll: yll: 'E Esri, HERE, Garmin, OpenStreetMap contributors, and the GIS user community Under Simulation 17
17 Finite Fault Model USGS2-Case1 S l i p [ m ] 0 40'S 0 20'S 0 0' 0 20'N 0 40'N USGS/FFM2/case1 Dip angle: 86 Strike angle: 347 (-11) xll: (-15km) yll: (+10km) 'E 'E *( ) Delta from original data 120 0'E 'E Esri, HERE, Garmin, OpenStreetMap contributors, and the GIS user community 20
18 Finite Fault Model USGS2-Case1 21
19 Finite Fault Model USGS2-Case1 Max Tsunami Height: 1.17 m '0"E '30"E '0"E '30"E '0"E '30"E '0"E 0 52'30"S 0 52'0"S 0 53'0"S 0 53'30"S Tsunami height [ m] ,000 m 22
20 23
21 Finite Fault Model USGS2-Case1 0 30'N USGS/FFM2/case1 Dip angle: 86 Strike angle: 347 (-11) xll: (-15km) yll: (+10km) *( ) Delta from original data Horizontal deformation [m] F F F F F F F F F 'S 0 0' 'E 'E 'E 'E 'E USGS FFM file 'E 'E Source: Esri, DigitalGlobe, GeoEye, Earthstar Geographics, CNES/Airbus DS, USDA, USGS, AeroGRID, IGN, and the GIS User Community Source: Esri, DigitalGlobe, GeoEye, Earthstar Geographics, CNES/Airbus DS, USDA, USGS, AeroGRID, IGN, and the GIS User Community 'E
22 Finite Fault Model USGS2-Case2 S l i p [ m ] 0 40'S 0 20'S 0 0' 0 20'N 0 40'N 'E 'E USGS/FFM2/case Dip angle: 86 Strike angle: 346 (-12) xll: (-11km) yll: (-2 k) 120 0'E *( ) Delta from original data 'E Esri, HERE, Garmin, OpenStreetMap contributors, and the GIS user community 25
23 Finite Fault Model USGS2-Case2 26
24 Finite Fault Model USGS2-Case2 Max Tsunami Height: 3.17 m '0"E '30"E '0"E '30"E '0"E '30"E '0"E 0 52'30"S 0 52'0"S 0 53'0"S 0 53'30"S Tsunami height [ m] ,000 m 27
25 28
26 Finite Fault Model USGS2-Case3 S l i p [ m ] 0 40'S 0 20'S 0 0' 0 20'N 0 40'N 'E 'E USGS/FFM2/case Dip angle: 86 Strike angle: 346 (-12) xll: (-11km) yll: (-6 k) 120 0'E *( ) Delta from original data 'E Esri, HERE, Garmin, OpenStreetMap contributors, and the GIS user community 29
27 Finite Fault Model USGS2-Case3 30
28 Finite Fault Model USGS2-Case3 Max Tsunami Height: 2.80 m '0"E '30"E '0"E '30"E '0"E '30"E '0"E 0 52'30"S 0 52'0"S 0 53'0"S 0 53'30"S Tsunami height [ m] ,000 m 31
29 32
SOURCE INVERSION AND INUNDATION MODELING TECHNOLOGIES FOR TSUNAMI HAZARD ASSESSMENT, CASE STUDY: 2001 PERU TSUNAMI
Paper No. TS-4-1 SOURCE INVERSION AND INUNDATION MODELING TECHNOLOGIES FOR TSUNAMI HAZARD ASSESSMENT, CASE STUDY: 2001 PERU TSUNAMI Bruno Adriano 1, Shunichi Koshimura 2 and Yushiro Fujii 3 ABSTRACT The
More informationMark H. Horwitz Ping Wang PhD Coastal Research Laboratory, School of Geosciences University of South Florida
Mark H. Horwitz Ping Wang PhD Coastal Research Laboratory, School of Geosciences University of South Florida American Shore & Beach Preservation Association 2015 National Coastal Conference, New Orleans,
More informationLidar-derived Hydrography as a Source for the National Hydrography Dataset
Lidar-derived Hydrography as a Source for the National Hydrography Dataset Lidar-Derived Hydrography, Bathymetry, and Topobathymetry in the National Hydrography Dataset and 3-Dimensional Elevation Program
More informationSURVEY OF SUBMERGED NOXIOUS WEED SPECIES IN LAKE CHELAN WASHINGTON
SURVEY OF SUBMERGED NOXOUS WEED SPECES N LAKE CHELAN WASHNGTON 1/26/215 Produced by AquaTechnex Lake Chelan was surveyed by air and by boat in the fall of 214 to locate noxious weeds and assess their overall
More informationMethodology for Estimating Floodwater Depths from Remote Sensing Flood Inundation Maps and Topography
Methodology for Estimating Floodwater Depths from Remote Sensing Flood Inundation Maps and Topography Sagy Cohen - Surface Dynamics Modeling Lab, University of Alabama Robert Brakenridge, Albert Kettner
More informationCase Study 2: 2014 Iquique Sequence
Case Study 2: 2014 Iquique Sequence Overview Mw 8.2 earthquake on 1 April 2014 at 11:08:43 UTC Pictures of damage Seismicity maps Foreshock seismicity -> Main shock -> Aftershock 1 April 2014 11:08:43
More informationThe determinants of transport modal choice in Bodensee-Alpenrhein region
The determinants of transport modal choice in Bodensee-Alpenrhein region Seyedeh Ashrafi University of Vienna Energie Innovation, February 2018 Modal choice is a decision process to choose between different
More informationopulation genetics undamentals for SNP datasets
opulation genetics undamentals for SNP datasets with crocodiles) Sam Banks Charles Darwin University sam.banks@cdu.edu.au I ve got a SNP genotype dataset, now what? Do my data meet the requirements of
More informationCase Study 1: 2014 Chiang Rai Sequence
Case Study 1: 2014 Chiang Rai Sequence Overview Mw 6.1 earthquake on 5 May 2014 at 11:08:43 UTC Largest recorded earthquake in Thailand Fault Orientation How does the orientation of the fault affect the
More informationTSUNAMI PROPAGATION AND INUNDATION MODELINGS ALONG SOUTH-EAST COAST OF PAPUA NEW GUINEA
TSUNAMI PROPAGATION AND INUNDATION MODELINGS ALONG SOUTH-EAST COAST OF PAPUA NEW GUINEA Martin WAREK Supervisor: Yushiro FUJII MEE12620 Bunichiro SHIBAZAKI ABSTRACT This study covers tsunami generation,
More informationCITY OF MORRO BAY WRFCAC Presentation May 3, 2016
CITY OF MORRO BAY WRFCAC Presentation May 3, 2016 Presenta>on Overview Community Goals Review of March 8, 2016 City Council Direc>on Ac>ons Since March 8 Community Outreach Outreach to Key Agencies, including
More informationNUMERICAL SIMULATION OF TSUNAMI PROPAGATION AND INUNDATION ALONG THE RAKHINE COAST AREAS IN MYANMAR
NUMERICAL SIMULATION OF TSUNAMI PROPAGATION AND INUNDATION ALONG THE RAKHINE COAST AREAS IN MYANMAR Su Hninn Htwe Supervisor: Bunichiro SHIBAZAKI MEE12619 Yushiro FUJII ABSTRACT This study aimed to assess
More informationAPPROVED JURISDICTIONAL DETERMINATION FORM U.S. Army Corps of Engineers
APPROVED JURISDICTIONAL DETERMINATION FORM U.S. Army Corps of Engineers This form should be completed by following the instructions provided in Section IV of the JD Form Instructional Guidebook. SECTION
More informationPreliminary Geotechnical Evaluation
I Preliminary Geotechnical Evaluation Dry Creek/Mount Veeder Winery P17-00343 & P17-00345 Planning Commission Hearing April 18, 2018 Condor Project No. 7464 September 8, 2017 Thomas F. Carey c/o Law Office
More informationRupture process of the 2010 M w 7.8 Mentawai tsunami earthquake from joint inversion of near-field hr-gps and
Rupture process of the 2010 M w 7.8 Mentawai tsunami earthquake from joint inversion of near-field hr-gps and teleseismic body wave recordings constrained by tsunami observations Han Yue 1, Thorne Lay
More informationIntegrated Approach to Assess the Impact of Tsunami Disaster
Integrated Approach to Assess the Impact of Tsunami Disaster Shunichi Koshimura & Shintaro Kayaba Disaster Control Research Center, Graduate School of Engineering, Tohoku University, Japan Masashi Matsuoka
More informationUS Highway 14 Streetscape Workgroup Meeting Notice and Agenda. Thursday, January 22, :00 pm
US Highway 14 Streetscape Workgroup Meeting Notice and Agenda Village of Cross Plains 2417 Brewery Road, PO Box 97 Cross Plains, WI 53528 (608) 798-3241 Thursday, January 22, 2015 7:00 pm I. Call to Order
More informationLand cover modeling in the Travis County
Land cover modeling in the Travis County Contents Introduction.1 Data collection 3 Data pre-processing 6 Land cover modeling 12 Final considerations 13 Prepared for: GIS and Water Resources By Julie C
More informationIntroduction to Displacement Modeling
Introduction to Displacement Modeling Introduction Deformation on the Earth surface informs us about processes and material properties below surface Observation tools: GPS (static-dynamic) InSAR (static)
More informationTSUNAMI HAZARD ASSESSMENT IN NORTHERN EGYPT USING NUMERICAL SIMULATION
TSUNAMI HAZARD ASSESSMENT IN NORTHERN EGYPT USING NUMERICAL SIMULATION Abutaleb Ali Supervisor: Bunichiro SHIBAZAKI MEE16717 Yushiro FUJII ABSTRACT To investigate the tsunami hazard along the northern
More information95 59'30"W '30"W
5 5' : 2 2 4'N Mile 2 4'N 122 2 2 33 34 2 1 1 1 12 252 21 1 1 - - - 1. HORZONTAL COORDNATES ARE REFERENCED TO TEAS STATE PLANE COORDNATE SYSTEM, SOUTH CENTRAL ZONE NAD3 US SURVEY FEET. - Depth in (MLL
More informationMaterials and Methods The deformation within the process zone of a propagating fault can be modeled using an elastic approximation.
Materials and Methods The deformation within the process zone of a propagating fault can be modeled using an elastic approximation. In the process zone, stress amplitudes are poorly determined and much
More information«540. North. Bend. Coos Bay. Coos Bay. Coos Bay. Study Area Coquille Indian Tribe Comprehensive Plan. North. Bend Parcels. Empire Lakes.
Date: 6/19/18 Path: U:\Port\Projects\lients\46-KittelsonAndAssociates\273-46-005 oquillendtribemp\99svcs\gs\mapdocs\figure1_oquille_studyarea.mxd Empire Empire Miles 0 0.5 1 First hickses oos Bay Empire
More informationNUMERICAL SIMULATIONS FOR TSUNAMI FORECASTING AT PADANG CITY USING OFFSHORE TSUNAMI SENSORS
NUMERICAL SIMULATIONS FOR TSUNAMI FORECASTING AT PADANG CITY USING OFFSHORE TSUNAMI SENSORS Setyoajie Prayoedhie Supervisor: Yushiro FUJII MEE10518 Bunichiro SHIBAZAKI ABSTRACT We conducted numerical simulations
More informationMURDOCK PASS. Corpus Christi-Baffin Bay Buoy 37. Corpus Christi-Baffin Bay Buoy '30"W
South Bird sland to Light 1 2' 2' 1 + 2 'N MURDOCK PASS 1 + 1 + Mil e: 1 + 2 Corpus Christi-Baffin Bay Buoy 2 of Mapped by: MAOPAC Scale: 1:, 1 + 2 'N Survey Date(s: May 21 magery Date: October 2, 2 DigitalGlobe
More informationSurry-Skiffes Creek 500 kv Transmission Line James River Crossing
Service Layer Credits: Source: Esri, DigitalGlobe, GeoEye, i-cubed, Earthstar Geographics, CNES/Airbus DS, USDA, USGS, AEX, Getmapping, Aerogrid, IGN, IGP, Viewpoint 09 Colonial Parkway Viewpoint 11 Kingsmill
More informationTHE IMPACT OF A VIOLENT TORNADO IN NORMAN, OKLAHOMA. Norman, Oklahoma
THE IMPACT OF A VIOLENT TORNADO IN NORMAN, OKLAHOMA Karen M. Montes Berríos 1,2, Ashton Robinson Cook 3, Amber Cannon Davis 4, Mark Shafer 5 and Somer Erickson 6 1 University of Puerto Rico Río Piedras
More informationTsunami Simulation of 2009 Dusky Sound Earthquake in New Zealand
Tsunami Simulation of 2009 Dusky Sound Earthquake in New Zealand Polina Berezina 1 Institute of Geology, Taras Shevchenko National University of Kyiv, Kyiv, Ukraine Supervisor: Prof. Kenji Satake Earthquake
More informationSCIENCE OF TSUNAMI HAZARDS
SCIENCE OF TSUNAMI HAZARDS ISSN 8755-6839 Journal of Tsunami Society International Volume 31 Number 4 2012 RESPONSE OF THE GDACS SYSTEM TO THE TOHOKU EARTHQUAKE AND TSUNAMI OF 11 MARCH 2011 Annunziato,
More informationAVERAGE AND VARIATION OF FOCAL MECHANISM AROUND TOHOKU SUBDUCTION ZONE
13 th World Conference on Earthquake Engineering Vancouver, B.C., Canada August 1-6, 24 Paper No. 414 AVERAGE AND VARIATION OF FOCAL MECHANISM AROUND TOHOKU SUBDUCTION ZONE Shunroku YAMAMOTO 1 Naohito
More informationCopies: Deborah Chismar Stu Brown
MEMO To: Danielle Taber John Patricki Copies: Deborah Chismar Stu Brown ARCADIS U.S., Inc. 410 N. 44th Street Suite 1000 Phoenix Arizona 85008 Tel 602 438 0883 Fax 602 438 0102 From: Jeff Gillow Shawn
More informationPreliminary slip model of M9 Tohoku earthquake from strongmotion stations in Japan - an extreme application of ISOLA code.
Preliminary slip model of M9 Tohoku earthquake from strongmotion stations in Japan - an extreme application of ISOLA code. J. Zahradnik 1), F. Gallovic 1), E. Sokos 2) G-A. Tselentis 2) 1) Charles University
More informationSeismogeodesy for rapid earthquake and tsunami characterization
Seismogeodesy for rapid earthquake and tsunami characterization Yehuda Bock Scripps Orbit and Permanent Array Center Scripps Institution of Oceanography READI & NOAA-NASA Tsunami Early Warning Projects
More informationYavapai County Flood Control District. Prescott Valley Mapping Activity Statement Activities (Zone A Floodplain Delineation and Base Map Updates)
Yavapai County Flood Control District Prescott Valley Mapping Activity Statement Activities (Zone A Floodplain Delineation and Base Map Updates) Scope of ork Prepar by: October 2014 Scope of ork TABLE
More informationReport on Site Selection SR-0879 SR SR-0050i SR-0049 SR-0399 SR SR-0050ii SR Drawing No. EFDC-S Rev1.
SR-879 SR-48 SR-5i SR-49 SR-399 SR-131 SR-5ii SR-128 Report on Site Selection. EFDC-S2-5-Rev1 Date: September 216 Scale: 1:15, @A3 Content Source: Esri, Legend DigitalGlobe, GeoEye, Earthstar Geographics,
More informationNUMERICAL SIMULATION AS GUIDANCE IN MAKING TSUNAMI HAZARD MAP FOR LABUAN ISLAND
NUMERICAL SIMULATION AS GUIDANCE IN MAKING TSUNAMI HAZARD MAP FOR LABUAN ISLAND MOHD RIDZUAN bin Adam Supervisor: Fumihiko IMAMURA MEE09199 ABSTRACT At the northeast end of the South China Sea, tsunamis
More informationSTUDY ON APPROPRIATE MODELING OF TSUNAMIS IN MALAYSIA FOR RISK EVALUATION
STUDY ON APPROPRIATE MODELING OF TSUNAMIS IN MALAYSIA FOR RISK EVALUATION Zaty Aktar binti Mokhtar* Supervisor: Fumihiko Imamura** MEE06025 Shunichi Koshimura** ABSTRACT In order to design a tsunami warning
More informationMagnitude 7.5 PALU, INDONESIA
A magnitude 7.5 earthquake occurred 80.8 km (50.2 mi) north of Palu, Indonesia at a depth of 10 km (6.2 miles). This earthquake triggered a tsunami with wave heights up to 2 m (6.6 ft) that an official
More informationRupture Characteristics of Major and Great (M w 7.0) Megathrust Earthquakes from : 1. Source Parameter Scaling Relationships
Journal of Geophysical Research Solid Earth Supporting Information for Rupture Characteristics of Major and Great (M w 7.0) Megathrust Earthquakes from 1990-2015: 1. Source Parameter Scaling Relationships
More information2016HighwaySafetyImprovementProgram (HSIP)Cycle8 GrantApplication. ApplicationID:07-Compton-1
CITYOFCOMPTON 2016HighwaySafetyImprovementProgram (HSIP)Cycle8 GrantApplication ApplicationID:07-Compton-1 Application Prepared By: EvanBrooksAssociates 1030 South Arroyo Parkway, Suite 106 Pasadena, CA
More informationP l a t e F t. S h e r i d a n P r o j e c t A r e a
P l a t e 0 1 - F t. S h e r i d a n P r o j e c t A r e a McCormick Ravine Janes Ravine The Ft. Sheridan Section 506 study area consists of eight (8) mature ravines, (1) immature ravine (MacArthur) and
More informationTsunami and earthquake in Chile Part 2
EUROPEAN COMMISSION DIRECTORATE GENERAL JRC JOINT RESEARCH CENTRE Institute for the Protection and Security of the Citizen Global Security and Crisis Management Unit CriTech Sunday, 28 February 2010 Executive
More informationInversion of tsunami data. A. Sladen CNRS, Géoazur 1/35
Inversion of tsunami data A. Sladen CNRS, Géoazur 1/35 DEFINITION Tsunami waves are gravity wave with a long period need a BIG source! 2/35 DEFINITION Krakatoa, 1883 Summer 2015, E.T. pers. comm. Lituya
More informationDerivation of Table 2 in Okada (1992)
Derivation of Table 2 in Okada (1992) [ I ] Derivation of Eqs.(4) through (6) Eq.(1) of Okada (1992) can be rewritten, where is the displacement at due to a j-th direction single force of unit magnitude
More informationFALL. El Dorado County Baseline Load Update
FALL El Dorado County Baseline Load Update 2016 FINAL REVISED BASELINE LOAD REPORT 16 Prepared for: Prepared by: Funded by: 2 0 1 6 F I N A L R E V I S E D B A S E L I N E L O A D R E P O R T TABLE OF
More informationDEVELOPING TIME HISTORIES WITH ACCEPTABLE RECORD PARAMETERS FOR DILLON DAM. Dina Bourliea Hunt, P.E. 1 Justin Beutel, P.E. 2 Christine Weber, P.E.
DEVELOPING TIME HISTORIES WITH ACCEPTABLE RECORD PARAMETERS FOR DILLON DAM Dina Bourliea Hunt, P.E. 1 Justin Beutel, P.E. 2 Christine Weber, P.E. 3 ABSTRACT Dillon Dam project is located in Summit County,
More informationSpecial feature: Are its lessons being adequately applied? Follow-up on the ten-year anniversary of the Hanshin-Awaji Earthquake
Special feature: Are its lessons being adequately applied? Follow-up on the ten-year anniversary of the Hanshin-Awaji Earthquake - Are we prepared for future massive earthquakes? - Hisakazu SAKAI Member
More informationTSUNAMI HAZARD ASSESSMENT FOR THE CENTRAL COAST OF PERU USING NUMERICAL SIMULATIONS FOR THE 1974, 1966 AND 1746 EARTHQUAKES
TSUNAMI HAZARD ASSESSMENT FOR THE CENTRAL COAST OF PERU USING NUMERICAL SIMULATIONS FOR THE 1974, 1966 AND 1746 EARTHQUAKES Sheila Yauri Supervisor: Yushiro FUJII MEE10521 Bunichiro SHIBAZAKI ABSTRACT
More informationTsunami potential and modeling
Tsunami potential and modeling GEORGE PRIEST OREGON DEPT. OF GEOLOGY AND MINERAL INDUSTRIES NEWPORT COASTAL FIELD OFFICE April 7, 2012 GeoPRISMS Cascadia Workshop, Portland, Oregon What creates most uncertainty
More informationRELATION BETWEEN RAYLEIGH WAVES AND UPLIFT OF THE SEABED DUE TO SEISMIC FAULTING
13 th World Conference on Earthquake Engineering Vancouver, B.C., Canada August 1-6, 24 Paper No. 1359 RELATION BETWEEN RAYLEIGH WAVES AND UPLIFT OF THE SEABED DUE TO SEISMIC FAULTING Shusaku INOUE 1,
More informationDETERMINATION OF SLIP DISTRIBUTION OF THE 28 MARCH 2005 NIAS EARTHQUAKE USING JOINT INVERSION OF TSUNAMI WAVEFORM AND GPS DATA
Synopses of Master Papers Bulletin of IISEE, 47, 115-10, 013 DETERMINATION OF SLIP DISTRIBUTION OF THE 8 MARCH 005 NIAS EARTHQUAKE USING JOINT INVERSION OF TSUNAMI WAVEFORM AND GPS DATA Tatok Yatimantoro
More informationSource of the July 2006 West Java tsunami estimated from tide gauge records
GEOPHYSICAL RESEARCH LETTERS, VOL. 33, L24317, doi:10.1029/2006gl028049, 2006 Source of the July 2006 West Java tsunami estimated from tide gauge records Yushiro Fujii 1 and Kenji Satake 2 Received 13
More informationSeismic Activity and Crustal Deformation after the 2011 Off the Pacific Coast of Tohoku Earthquake
J-RAPID Symposium March 6-7, 2013 Seismic Activity and Crustal Deformation after the 2011 Off the Pacific Coast of Tohoku Earthquake Y. Honkura Tokyo Institute of Technology Japan Science and Technology
More information2. Tsunami Source Details
2. Tsunami Source Details The Northland area faces a range of potential tsunamigenic sources that include several local and distant fault systems and underwater landslides. A NIWA study (Goff et al. 2006)
More informationEarthquake Focal Mechanisms and Waveform Modeling
Earthquake Focal Mechanisms and Waveform Modeling Rengin Gök Lawrence Livermore National Laboratory USA RELEMR Workshop İstanbul 2008 Gudmundar E. Sigvaldason The Dynamic Earth, USGS The size of the event
More informationEarthquake and Volcano Deformation
Earthquake and Volcano Deformation Paul Segall Stanford University Draft Copy September, 2005 Last Updated Sept, 2008 COPYRIGHT NOTICE: To be published by Princeton University Press and copyrighted, c
More informationTsunami waveform inversion of the 2007 Bengkulu, southern Sumatra, earthquake
LETTER Earth Planets Space, 60, 993 998, 2008 Tsunami waveform inversion of the 2007 Bengkulu, southern Sumatra, earthquake Yushiro Fujii 1 and Kenji Satake 2 1 International Institute of Seismology and
More informationTSUNAMI CHARACTERISTICS OF OUTER-RISE EARTHQUAKES ALONG THE PACIFIC COAST OF NICARAGUA - A CASE STUDY FOR THE 2016 NICARAGUA EVENT-
TSUNAMI CHARACTERISTICS OF OUTER-RISE EARTHQUAKES ALONG THE PACIFIC COAST OF NICARAGUA - A CASE STUDY FOR THE 2016 NICARAGUA EVENT- Amilcar Cabrera Supervisor: Yuichiro TANIOKA MEE16718 ABSTRACT Nicaragua
More informationEARTHQUAKE SOURCE PARAMETERS FOR SUBDUCTION ZONE EVENTS CAUSING TSUNAMIS IN AND AROUND THE PHILIPPINES
EARTHQUAKE SOURCE PARAMETERS FOR SUBDUCTION ZONE EVENTS CAUSING TSUNAMIS IN AND AROUND THE PHILIPPINES Joan Cruz SALCEDO Supervisor: Tatsuhiko HARA MEE09186 ABSTRACT We have made a set of earthquake source
More informationProbabilistic Tsunami Hazard Assessment addressing the uncertainty of tsunami source
Probabilistic Tsunami Hazard Assessment addressing the uncertainty of tsunami source Pacific Rim Forum 2017 January 23, 2017 Yuta Abe, ITOCHU Techno-Solutions Corporation, Japan Copyright (c)2017 ITOCHU
More informationBuilding up Seismsic Models for Ground Motion Prediction of Taiwan: Problems and Challenges
Building up Seismsic Models for Ground Motion Prediction of Taiwan: Problems and Challenges Kuo-Fong Ma 馬國鳳 Institute of Geophysics National Central University What approaches we can make toward a reliable
More informationHazard and Vulnerability of Moderate Seismicity Regions
Hazard and Vulnerability of Moderate Seismicity Regions presented by Professor Tso-Chien PAN Dean, College of Engineering Director, 25 October 2010 DRM GDLN Session on Earthquake Vulnerability Reduction
More informationREAL-TIME TSUNAMI INUNDATION FORECAST STUDY IN CHIMBOTE CITY, PERU
REAL-TIME TSUNAMI INUNDATION FORECAST STUDY IN CHIMBOTE CITY, PERU Nabilt Moggiano Supervisor: Kenji SATAKE MEE16720 ABSTRACT For rapid forecast of tsunami inundation during a tsunamigenic event, we constructed
More informationJCR (2 ), JGR- (1 ) (4 ) 11, EPSL GRL BSSA
Dun Wang ( ) In collaboration with: Hitoshi Kawakatsu, Jim Mori, Kazuki Koketsu, Takuto Maeda, Hiroshi Tsuroka, Jiancang Zhunag, Lihua Fang, and Qiang Yao School of Geosciences, China University of Geosciences
More informationPreliminary Study of Possible Tsunami Hazards in Taiwan Region
Preliminary Study of Possible Tsunami Hazards in Taiwan Region Xiaoming Wang and Philip L.-F. Liu Cornell University (First Draft on May 25 2006) (Second Draft on June 1 2006) (Final Update on June 8 2006)
More informationLab 9: Satellite Geodesy (35 points)
Lab 9: Satellite Geodesy (35 points) Here you will work with GPS Time Series data to explore plate motion and deformation in California. This lab modifies an exercise found here: http://www.unavco.org:8080/cws/pbonucleus/draftresources/sanandreas/
More informationROLE OF RIVER BATHYMETRY IN HYDRAULIC MODELING OF RIVER CHANNELS. A Thesis. Submitted to the Faculty. Purdue University. Sayan Dey
i ROLE OF RIVER BATHYMETRY IN HYDRAULIC MODELING OF RIVER CHANNELS A Thesis Submitted to the Faculty of Purdue University by Sayan Dey In Partial Fulfillment of the Requirements for the Degree of Master
More informationThe Mw 6.2 Leonidio, southern Greece earthquake of January 6, 2008: Preliminary identification of the fault plane.
The Mw 6.2 Leonidio, southern Greece earthquake of January 6, 28: Preliminary identification of the fault plane. J. Zahradnik 1, E. Sokos 2, A.Serpetsidaki 2, and G A.Tselentis 2 1 Charles University in
More informationENVIRONMENTAL ENGINEERING LAND SURVEYING
ENVIRONMENTL ENGINEERING LND SURVEYING Location Restrictions Otter Tail Power Company Coyote Station Introduction This report presents documentation and certification for the location standards for the
More informationRapid source characterization of the 2011 M w 9.0 off the Pacific coast of Tohoku Earthquake
LETTER Earth Planets Space, 63, 529 534, 2011 Rapid source characterization of the 2011 M w 9.0 off the Pacific coast of Tohoku Earthquake Gavin P. Hayes 1,2 1 U.S. Geological Survey, National Earthquake
More informationUpstream Information Management & Business Projects
Remote Sensing & Lithological Mapping: The Milh Kharwah Salt Diapir Lisboa, December 2017 Upstream Information Management & Business Projects OMV Upstream Agenda Background & Geological Setting Methodology
More informationTHE 2011 OFF THE PACIFIC COAST OF TOHOKU-OKI EARTHQUAKE AND TSUNAMI: INFLUENCE OF THE SOURCE CHARACTERISTICS ON THE MAXIMUM TSUNAMI HEIGHTS
Proceedings of the International Symposium on Engineering Lessons Learned from the 2011 Great East Japan Earthquake, March 1-4, 2012, Tokyo, Japan THE 2011 OFF THE PACIFIC COAST OF TOHOKU-OKI EARTHQUAKE
More informationSATELLITE IMAGERY STUDY REPORT
JULY 2017 SATELLITE IMAGERY REPORT FOR SATELLITE IMAGERY STUDY REPORT [Covering 5 km Radius Around The Project Site] [FOR USING SATELLITE IMAGERY & GEOGRAPHIC INFORMATION SYSTEM (GIS)] Prepared for M/s.IMC
More informationDeveloping fragility functions for tsunami damage estimation using the numerical model and satellite imagery
Developing fragility functions for tsunami damage estimation using the numerical model and satellite imagery Shunichi KOSHIMURA 1 and Hideaki YANAGISAWA 2 1 Associate Professor, Disaster Control Research
More informationEstimation of hazard assessment by FINSIM for west coast and son narmada faults
Estimation of hazard assessment by FINSIM for west coast and son narmada faults Shivamanth Angadi 1, Mayank Desai 2 1 Research Scholar, Dept. of Applied Mechanics, SVNIT, SURAT-39007, India 2 Assistant
More informationMagnitude 7.1 NEAR THE EAST COAST OF HONSHU, JAPAN
Japan was rattled by a strong aftershock and tsunami warning Thursday night nearly a month after a devastating earthquake and tsunami flattened the northeastern coast. This earthquake can be considered
More informationEarthquakes of and successive. A. Caporali and L. Ostini Department of Geosciences University of Padova 2012 EUREF Symposium, Paris France
Earthquakes of 2.5.22 and successive A. Caporali and L. Ostini Department of Geosciences University of Padova 22 EUREF Symposium, Paris France Historical Seismicity: 234 M 5.8 +/-.2 near Ferrara 57 M 5.5
More informationAbdul Muhari 1, Fumihiko Imamura 2, Taro Arikawa 3, and Bagus Afriyanto 1. Date; 15 October 2018
Finding of the unexpected tsunami due to the strike-slip fault at central Sulawesi, Indonesia on 28 September 2018, from the preliminary field survey at Palu Abdul Muhari 1, Fumihiko Imamura 2, Taro Arikawa
More informationFIGURE 2. Alborn Township Ness Township. Alborn Township. Ness Township. USGS Topographic Map
Barr Footer: ArcIS 1.4, 216-1-24 1:1 File: I:\Client\Minntac\Work_Orders\Pit_Extension\Maps\Reports\Spider_Creek\Maps\EAW\Final Figures\Figure 1 Map.mxd User: MAK3 RainyRiver ^_ Spider Creek Restoration
More informationMethod to Determine Appropriate Source Models of Large Earthquakes Including Tsunami Earthquakes for Tsunami Early Warning in Central America
Pure Appl. Geophys. 174 (2017), 3237 3248 Ó 2017 The Author(s) This article is published with open access at Springerlink.com DOI 10.1007/s00024-017-1630-y Pure and Applied Geophysics Method to Determine
More informationStreams in the Ranching Country of South Texas
Streams in the Ranching Country of South Texas Watershed Analysis of HUC 12110207 Sandranell Moerbe CE GIS in Water Resources Fall 2015 INTRODUCTION This project investigates the portion of South Texas
More informationFinding Fault Geologic History from a Road Cut
Finding Fault Geologic History from a Road Cut Elisabeth M. Price, DD LaPointe, and Jonathan G. Price 4 July 2005 Introduction Earth science is an important science to present to students because it directly
More informationChapter 2. Earthquake and Damage
EDM Report on the Chi-Chi, Taiwan Earthquake of September 21, 1999 2.1 Earthquake Fault 2.1.1 Tectonic Background The island of Taiwan is located in the complex junction where the Eurasian and Philippine
More informationNumerical Tsunami Propagation of 1703 Kanto Earthquake
Numerical Tsunami Propagation of 1703 Kanto Earthquake Wu Yifei Supervisor: Kenji Satake Introduction Near Tokyo Bay, the 1703 Genroku Kanto Earthquake is known to generate a tsunami which hit the nearby
More informationA PROTOTYPE OF WEB-APPLICATION FOR TSUNAMI DATABASE ALONG SOUTHERN JAVA ISLAND COASTLINE
A PROTOTYPE OF WEB-APPLICATION FOR TSUNAMI DATABASE ALONG SOUTHERN JAVA ISLAND COASTLINE Ariska Rudyanto MEE07170 Supervisor: Yohei HASEGAWA Yosuke IGARASHI Yushiro FUJII ABSTRACT Development of tsunami
More informationS. Toda, S. Okada, D. Ishimura, and Y. Niwa International Research Institute of Disaster Science, Tohoku University, Japan
The first surface-rupturing earthquake in 20 years on a HERP major active fault: Mw=6.2 2014 Nagano, Japan, event along the Itoigawa-Shizuoka Tectonic Line is not characteristic S. Toda, S. Okada, D. Ishimura,
More informationEffect of the Emperor seamounts on trans-oceanic propagation of the 2006 Kuril Island earthquake tsunami
GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L02611, doi:10.1029/2007gl032129, 2008 Effect of the Emperor seamounts on trans-oceanic propagation of the 2006 Kuril Island earthquake tsunami S. Koshimura, 1 Y.
More informationThe potential tsunami threats from the South China Sea and hazard mitigation
The potential tsunami threats from the South China Sea and hazard mitigation Dr. Tso-Ren Wu ( 吳祚任 ) Graduate Institute of Hydrological and Oceanic Sciences National Central University 國立中央大學水文與海洋科學研究所
More informationMagnitude 7.2 OAXACA, MEXICO
A magnitude 7.2 earthquake has occurred in Oaxaca, Mexico at a depth of 24.6 km (15 miles). It was felt as far away as Guatemala. There have been no reported deaths directly linked to the earthquake. Emergency
More informationHYDROGRAPHIC SURVEY. Mile 20 to Mile Station: to Channel to Harlingen ^ # * " Aids to Navigation
Mile 2 to Mile 2. ' 2 1'N ' 1 1+ ' 2 + + + 1 1 + 2 1'N 1 2 1'N 1 1 + Authorized Depth: -ft. 1 1 + 2 1 1 1 1 Mapped by: modnmfp ' 1+ Scale: 1:, 1 1 of 1 1 Survey Date(s: 1 December 21 magery Date: October
More informationResolving Stress Components and Earthquake Triggering
Resolving Stress Components and Earthquake Triggering Earthquake Triggering Do certain events make an earthquake more likely to occur? Earthquakes Slow Slip Wastewater Fluids Dams The focus of this presentation
More informationMagnitude 7.0 PAPUA, INDONESIA
A 7.0 magnitude earthquake struck eastern Indonesia's mountainous West Papua province on Saturday but there were no immediate reports of casualties or damage. The region is sparsely populated. According
More informationA GLOBAL SURGE OF GREAT EARTHQUAKES FROM AND IMPLICATIONS FOR CASCADIA. Thorne Lay, University of California Santa Cruz
A GLOBAL SURGE OF GREAT EARTHQUAKES FROM 2004-2014 AND IMPLICATIONS FOR CASCADIA Thorne Lay, University of California Santa Cruz Last 10 yrs - 18 great earthquakes: rate 1.8/yr; rate over preceding century
More informationA Method for Estimating Casualties due to the Tsunami Inundation Flow
A Method for Estimating Casualties due to the Tsunami Inundation Flow Shunichi Koshimura Disaster Reduction and Human Renovation Institution Toshitaka Katada Depertment of Civil Engineering, Gunma University
More informationHow GNSS CORS in Japan works for geodetic control and disaster mitigations
ICG Working Group D Reference Frames, Timing and Applications How GNSS CORS in Japan works for geodetic control and disaster mitigations ICG11, Nov. 7-11, 2016, Sochi, Russia Hiromichi TSUJI Geodetic Observation
More informationBasics of the modelling of the ground deformations produced by an earthquake. EO Summer School 2014 Frascati August 13 Pierre Briole
Basics of the modelling of the ground deformations produced by an earthquake EO Summer School 2014 Frascati August 13 Pierre Briole Content Earthquakes and faults Examples of SAR interferograms of earthquakes
More informationApplication of a GIS for Earthquake Hazard Assessment and Risk Mitigation in Vietnam
Application of a GIS for Earthquake Hazard Assessment and Risk Mitigation in Vietnam Nguyen Hong Phuong Earthquake Information and Tsunami Warning Centre, VAST OUTLINE Introduction Fault Source Model and
More information2011/3/11 14:46, Depth 24km, M9.0 (JMA)
Off the Pacific Coast of Tohoku earthquake, Strong Ground Motion /3/ 4:46, Depth 4km, M9. (JMA) Peak Ground Acceleration (surface) Peak Ground Velocity (surface) 45 45 4 4 PGA [gal].. 5... 5... 5....5.
More informationDEFORMATION PATTERN IN ELASTIC CRUST
DEFORMATION PATTERN IN ELASTIC CRUST Stress and force in 2D Strain : normal and shear Elastic medium equations Vertical fault in elastic medium => arctangent General elastic dislocation (Okada s formulas)
More informationFeatures of Tsunami height according to type of coastal landforms 2011 Tohoku oki tsunami case
Features of Tsunami height according to type of coastal landforms 2011 Tohoku oki tsunami case (70 Nobuhisa Matta (Disaster Mitigation Research Center Nagoya Univ.) July 3 rd, 2013, at Taipei Outline +
More information