NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 WP7 Modelling of tsunami impact in SW Portugal Berlim 8-9 October 2008 NEAREST FFCUL Rachid Omira Maria Ana.

Slides:



Advertisements
Similar presentations
Treasure Island Development Project How Tsunamis Are Generated Most tsunamis are caused by earthquakes generated in a subduction zone (where oceanic plate.
Advertisements

Application of tsunami modelling for escape and refuge planning in Aceh (Indonesia) May 2008 Odelinde Nieuwenhuis, DHV BV Deepak Vatvani, Deltares (Delft.
FFCUL, PORTUGALBologna Oct 2006 NEAREST Coordinator: Maria Ana V Baptista NEAREST PARTNER FFCUL PORTUGAL.
Generation of the 2004 Sumatra-Andaman Tsunami WHIO, 30 Oct., 2006.
Structural character of the terrace zone and implications for crater formation: Chicxulub impact crater David L. Gorney Sean Gulick Gail Christeson GSA.
Coastal Hazards: Tsunami & Hurricanes Week 7. Homework Questions Would you live near a coast? If so, where? What level of risk from tsunami & hurricanes.
Coastal Hazards: Tsunamis. Homework Questions Would you live in an area at risk for tsunamis? If so, where? What level of risk from tsunamis is acceptable.
Numerical Simulation of Benchmark Problem 2
Instrumentation and Quantification of Tsunamis With an Emphasis on the Santa Barbara Channel.
Key factors determining the extent of tsunami inundation – Investigations using ANUGA Biljana Lukovic and William Power GNS Science, Lower Hutt, New Zealand.
Seismic Refraction. Some uses of seismic refraction Mapping bedrock topography Determining the depth of gravel, sand or clay deposits Delineating perched.
A nearfield Tsunami warning system in Taiwan by unit tsunami method Po-Fei Chen 1, Yun-Ru Chen 2, Bor-Yaw Lin 1,3, Wu-Ting Tsai 2 1. Institute of Geophysics,
Multi-scale Simulation of tsunami from Tohoku Earthquake and Diffracted Tsunami Waves in Hokkaido ZHU AIYU, Zhang Dongning Institute of Geophysics, China.
FE Watershed Analysis Lecture 1a - Overview Finn Krogstad UW Forest Engineering
Locating the source of earthquakes Focus - the place within Earth where earthquake waves originate Epicenter on an earthquake– location on the surface.
NEW CHALLENGES CONCERNING GEO-HAZARD EVALUATION – J M MIRANDA J Miguel Miranda CGUL / IDL.
President’s Proposed Expansion of Tsunami Warning System Eddie Bernard Director, Pacific Marine Environmental Laboratory (PMEL)/NOAA Member, National Tsunami.
Near-Field Modeling of the 1964 Alaska Tsunami: A Source Function Study Elena Suleimani, Natalia Ruppert, Dmitry Nicolsky, and Roger Hansen Alaska Earthquake.
Tsunamis Presented by: Saira Hashmi Oct. 14 th,2005 EPS 131 Introduction to Physical Oceanography.
Tsunami Warning System Elements IOC Assessment Mission to Indonesia 29 August-1 September 2005.
Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from.
THE NEXT DESTRUCTIVE TSUNAMI: ITS NOT IF, BUT WHEN.
Earthquake Hazard Session 1 Mr. James Daniell Risk Analysis
FEASIBILITY STUDY OF A REGIONAL EEW SYSTEM FOR THE EASTERN CARIBBEAN REGION ZUCCOLO Elisa, SALAZAR Walter, DI SARNO Luigi, FARRELL Anthony, GIBBS Tony,
Tsunami-prone Areas Japan, 2011 Sumatra, 2004 Mentawai, 2010
FFCUL, PORTUGALBologna Oct 2006 NEAREST Coordinator: Maria Ana V Baptista NEAREST PARTNER - FFCUL PORTUGAL.
Tsunami Hazard Assessment along the Coast of Lingayen Gulf, Pangasinan, Philippines Julius M. GALDIANO PHIVOLCS Julius M. GALDIANO PHIVOLCS 4 th International.
Design and Implementation of an Operational Tsunami Forecast Tool Donald W. Denbo, John R. Osborne, Clinton K. Pells and Mike A. Traum Joint Institute.
NEAREST WP5.- Data Integration/ Integrated Tsunami Detection Network: LEADER: UGR PARTNERS INVOLVED: FCCUL, IM, CNRST, UGR Marrakech Meeting 25 and 26.
NEAREST PROJECT PARTICIPANT N° 10 Institut National de Géophysique Centre National pour la Recherche Scientifique et Technique (CNRST) (CNRST) in collaboration.
FFCUL, PORTUGALBologna Oct 2006 NEAREST Coordinator: Maria Ana V Baptista NEAREST PARTNER FFCUL PORTUGAL.
WP1 WP1 - Tsunami sources Identification WP1 - Tsunami sources Identification FFCUL group Marrakesh, Oct
Tsunamis Learning Objectives: -To develop your understanding of the term Tsunami. -To be able to identify the reason a tsunami occurs and its affects.
Zadonina E.O. (1), Caldeira B. (1,2), Bezzeghoud M. (1,2), Borges J.F. (1,2) (1) Centro de Geofísica de Évora (2) Departamento de Física, Universidade.
COMPARISON OF ANALYTICAL AND NUMERICAL APPROACHES FOR LONG WAVE RUNUP by ERTAN DEMİRBAŞ MAY, 2002.
About 8000 years ago and the flooding of DoggerLand.
Using HAZUS-MH to Assess Tsunami Risk Bill Bohn, Tetra Tech June 19, 2007.
Paleo-tsunami record and tsunami hazard in Wallis and Futuna
Large Earthquake Rapid Finite Rupture Model Products Thorne Lay (UCSC) USGS/IRIS/NSF International Workshop on the Utilization of Seismographic Networks.
Effect of the 1755 Lisbon tsunami in the French West India Andrey Zaitsev, Anton Chernov, Tatiana Talipova Efim Pelinovsky Narcisse Zahibo Ahmet Yalciner.
WORKSHOP ON LONG-WAVE RUNUP MODELS Khairil Irfan Sitanggang and Patrick Lynett Dept of Civil & Ocean Engineering, Texas A&M University.
Comparison of the different proposed sources for the 1755 Lisbon tsunami: modeling in the West Antilles. Jean ROGER, M.A. BAPTISTA, H. HEBERT ITS 2009,
ISMAR-BO, ITALY SIXTH FRAMEWORK PROGRAMME PRIORITY Contract n (GOCE) NEAREST Integrated Observations from NEAR shore sourcES of Tsunamis:
Sources and scenarios for tsunami hazard assessment in the Mediterranean A very preliminary view.
CISN: Draft Plans for Funding Sources: OES/FEMA/ANSS/Others CISN-PMG Sacramento 10/19/2004.
MARsite kickoff meeting December 19-20, 2012, Istanbul INGV contribution to WP5 Tasks 2 & 4 Alessio Piatanesi.
Lecture 6: Tsunamis Our Hazardous Environment GEOG 1110 Dr. Thieme.
Xiaoming Wang and Philip L.-F. Liu Cornell University
1 Storms activity: wave modelling and atmospheric circulation Part 1. Wave modelling. V. Arkhipkin 1, S. Myslenkov 1 Part 2. Atmospheric circulation. A.
IOC Expert Missions May-August, 2005 UNESCO IOC TSUNAMI PROGRAMME.
Following the suggestion of the NEAREST Project leader, to invite several partners to a Workshop in Rabat in order to integrate Moroccan input into the.
Caribbean Training Course in Seismology and Tsunami Warnings June 25-30, 2007, St. Augustine, Trinidad Tsunami Warning Center Operations: Caribbean Simulations.
WP8 - From hazard to risk assessment LIST OF PARTICIPANTS.
International Workshop on Long-Wave Runup Models 2-Dimensional Model with Boundary-Fitting Cell System Benchmark #2:Tsunami Runup onto a Complex 3Dimensional.
State of Tsunami Science and Early Warnings Dr. François Schindelé, CEA-DASE Chairman of the International Coordination Group for the Tsunami Warning System.
Barcelona 8th-9th May 2008 NEAREST 2nd mid-year meeting Introduction.
May 9, 2016 Learning Target: I will be able to describe the processes that cause earthquakes. Success Criteria: I can explain what will cause “the big.
Tsunami Jens Havskov and Mathilde B. Sørensen. What is a tsunami A tsunami is an abnormal large wave hitting the coast.
Cabled systems for near-field tsunami early warning: An observation system simulation experiment (OSSE) offshore Portugal A. Babeyko1, M. Nosov2 and.
FLOOTSI Development of GIS-GPU-based flood-simulation model and its application to flood-risk assessment Examples of applications Augusto Maidana,
F. Løvholt1, C. Harbitz1, J. Griffin2, G. Davies2, S. Lorito3, R
Tsunami heights off southeast Indian coast from run-up measurements
NEAREST FFCUL WP7 Modelling of tsunami impact in SW Portugal
F. Løvholt1, C. Harbitz1, J. Griffin2, G. Davies2, S. Lorito3, R
NEAREST FFCUL WP7 Modelling of tsunami impact in SW Portugal
Tsunami Early Warning System: SOPs and Communication Strategies Initiatives by Pakistan Meteorological Department presenter Zahid Rafi Dated: 08 Oct,
Tsunamis.
Hazards Planning and Risk Management Tsunami Inundation Mapping
MONITORING, DETECTING AND WARNING OF TSUNAMIS
COASTAL RISKS By: NACER JABOUR CEPRIS – RABAT - MOROCCO
Presentation transcript:

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 WP7 Modelling of tsunami impact in SW Portugal Berlim 8-9 October 2008 NEAREST FFCUL Rachid Omira Maria Ana Baptista Miguel Miranda

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 WP7 Modelling of tsunami impact in SW Portugal WP7.1 Collation of the new Bathymetric Data (merge data not complete) WP7.2 Implementation of a Numerical Tsunami Model for SW Portugal WP7.3 Simulation of the 1755 tsunami in the “Boca do Rio” area WP7.4 Production of Inundation Maps for Lagos-Sagres WP7.5 Model Parametrization and Validation

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 COMCOT _ LX Adopted from COMCOT (Cornell University, Liu et al., 1994) COMCOT code (Cornell University) COMCOT code (Cornell University) Tsunami Simulation Code Based on Shallow Water Equations Tsunami Simulation Code Based on Shallow Water Equations Leap-frog scheme Leap-frog scheme Nested grid system Nested grid system Moving boundary scheme Moving boundary scheme WP7.5 Model Parametrization and Validation CGUL changes: COMCOT – Lx Surfer format input / output Output Inundation / Flow depths

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 TRANSFER AREAS Nested grid system NEAREST AREAS WP7.5 Model Parametrization and Validation

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 Benchmark testing (collab.with TRANFER project) #1 – RUNUP ONTO A PLANE BEACH #1 – RUNUP ONTO A PLANE BEACH WP7.5 Model Parametrization and Validation

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 The model earthquake - Lisbon event WP7.3 Simulation of the 1755 tsunami in the “Boca do Rio” area Fault Plane Strike / Dip / Rake: 340 / 45 / 90 Fault centre Lat / Lon: 37.0N / 9.75W (SW Lisbon) L = 210 km, W = 75 km, D = 13.6 m

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 WP7.3 Simulation of the 1755 tsunami in the “Boca do Rio” area

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 Does Inundation correlate well to sedimentological evidence? WP7.3 Simulation of the 1755 tsunami along Algarve

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 CASABLANCA TEST SITE CASABLANCA TEST SITE

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 WP7 Modelling of tsunami impact in Casablanca (Johnston,1996)(Zitellini, 2001, 2003) (Gutscher, 2002,2006) (Baptista, 1998) (Omira et al, 2007) to be sub. To Natural Hazards Modelled Run up correlates well slip (Okal & Synolakis, GJInt., 2004 et al)

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 WP7 Modelling of tsunami impact in Casablanca Vunerability study

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 Casablanca Harbour area building stock Casablanca Harbour area building stock Building Survey by Rachid April 2007

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 WP7 Modelling of tsunami impact in Casablanca Tsunami Vulnerability Assessment

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 On going… Modelling tsunami impact in the study Areas using WP1 +TRANSFER & ERSTA Zones WP7 Modelling of tsunami impact in test areas

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 On going… Modelling tsunami impact in the study Areas using WP1 +TRANSFER & ERSTA Zones WP7 Modelling of tsunami impact in test areas Miranda JM, Baptista MA, Terrinha P, Matias, L. 31st ESC Crete Sept 2008

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 ts Initial displacements using heterogeneous slip (SCC (Geist & Domovska,1999)) INVESTIGATION OF THE EFFECT IN INNUNDATION MAPS ON GOING

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 CONTRIBUTION TO IOC-NEAMTWS

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 Maximum wave elevation + Energy radiation + Travel time For each scenario

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 Computed maximum wave height, energy direction and tsunami travel time for the tsunami scenarios in the Golf of Cadiz WP7 Modelling of tsunami impact in test areas Red line First arrival to the coast Less 30 minutes

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 WP7 Modelling of tsunami impact in test areas Priority tsunameter location Tsunami travel time + Radiation pattern + bottom topography Warning time 15 min =Arrival Time – Detection time

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 NEXT STEPS Tune Model for Flow Depth Velocity WP7 Modelling of tsunami impact in test areas Produce FDVelocity maps Ouput of TRANSFER: standards for Inundation maps (next week Messina ) DoW 27 – Month 29

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 Next steps GEOSUB August 08 survey Improvement of inundation results with new data

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 Tsunami Vulnerability Assessment of Casablanca-Morocco using Numerical Modelling and GIS tools R. Omira, M. A. Baptista, J. M. Miranda,C. Catita, E. Toto Subm to Natural Hazards (may 2008, under revision) REVISION OF THE PORTUGUESE CATALOGUE OF TSUNAMIS M. A. Baptista, J. M. Miranda (subm NHESS, accept with minor revision) REVISION OF THE MOROCCO TSUNAMI CATALOGUE F. Kaabouben, M. A. Baptista, A. Iben Brahim, A. Toto, A. Elmouraouah Ready for submission to NHESS ? publications

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 WP1.1 - INGV - Database for paleotsunamis Euro-Mediterranean area (boulders or sediments) TRANSFER web site The DB can be visited and updated through the web interface ( and data can be downloaded in a format ready to be included in the TRANSFER GIS DB. TRANSFER WP1 DATABASE

NEAREST 2nd year Meet ing – Berlim 8 -9oct 08 WP7 Modelling of tsunami impact in SW Portugal Del. n. Deliverable name Workpackag e Workpac kage n. Due Date (project month) Actual/ Forecas t delivery date Estimated indicative person months (all partners involved) Used indicative person months (all partners involved) Lead contractor D24a D24b new bathymetric map cruise report WP FFCUL D25 implementation of a numerical tsunami model for SW Portugal WP FFCUL D26 simulation of the 1755 tsunami in the Boca de Rio area WP FFCUL D27 inundation maps for Lagos-Sagres WP FFCUL D28 validation of the model WP FFCUL