THE PERUVIAN TSUNAMI WARNING CENTER
|
|
|
- Ilene Parks
- 10 years ago
- Views:
Transcription
1 THE PERUVIAN TSUNAMI WARNING CENTER César Jiménez TSUNAMI The Tsunamis are a set of several marine waves of long period generated by a perturbation, generally an earthquake with epicenter on the sea. Tsunami: word of japanese origin used in many languages as english and spanish. TSU = PORT, NAMI = WAVE Literally, it means «waves in y, the port», no damage at offshore, but can be destructive in coasts.
2 HISTORYCAL PERUVIAN TSUNAMIS Seismicity of the world: Peru is located in the Pacific Ring of Fire. Therefore, there is a great seismic, tsunami and volcanic activity. Earthquakes generators of tsunami in Peru ( ). The last great earthquake in Peru was in Pisco CALLAO TSUNAMI, 1746 (CENTRAL PERU) EPICENTER 11.9 S; 77.1 W MAGNITUDE > 9.0 Mw DATE October 30, 1746 TIME 22:30 Local Time ARRIVAL TIME 30 minutes MAXIMUM WAVE HEIGHT 10 m (Callao) 24 m (Miraflores cliffs) EFFECTS CASUALTIES: 5000 in Callao 200 survivors EXTENSIVE DAMAGES
3 CAMANA TSUNAMI, (SOUTHERN PERU) 2001 EPICENTER S; 74.4 W MAGNITUDE 8.4 Mw IGP USGS El Chorro La Punta 10 Kms La Punta Nueva DATE Saturday June 23, 2001 TIME 20:33:13 GMT ARRIVAL TIME 15 minutes MAXIMUM WAVE HEIGHT 7 to 8 m EFFECTS CASUALTIES: 23 EXTENSIVE DAMAGES 1, m. ESCALA 1:20000 El Chorro m. PISCO TSUNAMI, 2007 SOUTHERN PERU EPICENTER S; W MAGNITUDE 8.0 Mw DATE August 15, 2007 TIME 23:40 GMT ARRIVAL TIME 20 minutes MAXIMUM WAVE HEIGHT 10 m (Lagunillas) EFFECTS CASUALTIES: 500 (earthquake) 03 (tsunami) EXTENSIVE DAMAGES
4 CHILEAN TSUNAMI FEB 2010 EPICENTER: Lat: 36.1 S Lon: 72.6 W PAITA HORA PTWC HORA DHN HORA MAREÓGRAFO LECTURA MAREÓGRAFO (cm.) AMPLITUD PTWC (cm.) MAGNITUDE: 8.8 Mw DATE: Feb 27, 2010 TIME: 06:33 GMT 115 km NNE of Concepción Subduction zone Nazca-Pacific plates. CALLAO HORA PTWC HORA DHN HORA MAREÓGRAFO LECTURA MAREÓGRAFO (cm.) AMPLITUD PTWC (cm.) MATARANI / ILO HORA PTWC HORA DHN LECTURA HORA MAREÓGRAFO MAREÓGRAFO (cm.) AMPLITUD PTWC (cm.) Variacion del nivel del mar en la punta valor en metros Perú time: 0134 hrs. Lat.: 36.85º S Lon.: 72.72º W Magnitude: 8.8 Mw Depth: 35 km 0 18:00:58 20:08:58 22:16:58 00:24:58 02:32:58 04:40:58 06:48:58 08:56:58 11:04:58 13:12:58 15:20:58 17:28:58 19:36:58 21:44:58 23:52:58 02:00:58 04:08:58 06:16:58 08:24:58 10:32:58 12:40:58 14:48:58 16:56:58 19:04:58 21:12:58 23:20:58 01:28:58 03:36:58 05:44:58 07:52:58 10:00:58 12:08:58 Valores medidos del 26 feb al 01 marzo hora UTC MIRAFLORES BAY Observation time: 1020 Tidal phase: Descendent Amplitude: 15 cm Moon phase: Full MIRAFLORES BAY Hora de observación: 1020 Fase de Marea: Descendente Amplitud: 15 cm Fase Luna: Llena
5 PARACAS BAY Observation time: 0830 Tidal phase: Descendent Amplitude: 100 cm Moon phase: Full CALETA LAGUNILLAS (ICA) Hora de observación: 1740 Fase de Marea: Ascendente Amplitud: 106 cm Fase Luna: Llena COMPONENTS OF A TSUNAMI WARNING SYSTEM This system allows to provide early warning in case of an imminent tsunami. Consists of the following elements: 1) Seismographic network.- In order to detect the focal parameters and calculate the focal mechanism of great earthquakes generators of tsunami. The seismic network of Peru is managed by IGP (Geophysical Institute of Peru). 2) Tide gauge network.- This consists of strategically stations located along the Peruvian coast. Verifies that the tsunami has originated and is traveling through the sea. This tidal network is managed by DHN (Directorate of Hydrography and Navigation). 3) Geodesic Network.- Composed of several permanent GPS stations. Allows real-time detection of coseismic deformation of the crust, this will decide if it will generate a tsunami (before seismic calculations). But should be managed by IGP and IGN (National Geographical Institute). 4) Database of tsunamis simulated.- A set of seismic source events (Green functions) for all the peruvian coasts simulated by numerical modeling. Will allow a fast calculation of arrival times and maximum wave height for warning purposes. This system is not implemented yet. 5) A system of alerting the public.- Formed by a group of sirens, radio and television messages to issue an evacuation notice to people living in potential flood areas. This system will be managed by Civil Defense and regional and local governments. All elements of the seismic, tide gauge and geodetic networks must be interconnected to a central operation through redundant radio, fax-telephone and satellite communications, and the signals arriving i in real time, so that t operators can process data and make the right decision i and to give timely warning to evacuate.
6 PERUVIAN TSUNAMI WARNING CENTER The National Tsunami Warning System is managed by DHN of peruvian navy and integrated t by several institutions: IGP: through seismic service INDECI: civil defense APN: port authority DICAPI: navy authority CORPAC, etc. FLOWCHART OF COMMUNICATIONS OF TSUNAMI WARNING SYSTEM CN C T RSDI A DIRECCION DE TELEMATICA (DIRTEL) OBSERVATORIO DE HONOLULU HAWAII (PTWC) C T AFTN S CORPORACION PERUANA DE AEROPUERTOS (CORPAC) T AFTN RDSI DIRECCION DE HIDROGRAFIA Y NAVEGACION DE LA MARINA (DHN) C T R RDSI AFTN CN S A CN C T S A CN C T A C T RDSI S R C T RDSI S C T RDSI C T DIRECCION DE CAPITANIAS UNIDADES INSTITUTO GEOFISICO INSTITUTO NACIONAL EMPRESA NACIONAL AUTORIDAD PORTUARIA INFORMACIÓN Y DEPENDENCIAS DEL PERU DE DEFENSA CIVIL DE PUERTOS NACIONAL (DIMINMAR) DEL LITORAL (IGP) (INDECI) (ENAPU) (APN) C T R T R T TERMINALES MEDIOS DE DIFUSIÓN MARITIMOS COMUNICACIÓN AUTORIDADES Y Y BUQUES (RADIO TV) COMITES CIVILES NAVEGANDO C = Correo electrónico T = Teléfono R = Radio RDSI = Red Digital de Servicio Integrado AFTN = Aeronautical Fixed Telecomunication Network Satelital CN = Comunicaciones Navales S = Teléfono Satelital A = Sistema Troncalizado
7 MONITORING AND COMMUNICATION ELEMENTS LOCATION OF LOCAL EARTHQUAKES IGP TSUNAMI ARRIVAL TIMES CHART TELESEISMIC LOCATION NEIC DART BUOYS (NOOA) CISN (California seismic network) OCEAN STATION- GPS GEODESIC STATION MILOS (IRD-DHN) TREMORS SYSTEM (Ecu Per Chi) SNAT SISTEMA DE COMUNICACIÓN RSDI (Red Digital de Servicios Integrados) SOFTWARE PARA DETERMINACION COMMUNICATION DE OCURRENCIA Y MEDIA: TV: CNN, TIEMPO DE CANAL ARRIBO DE N channel TSUNAMI TSUNAMI NUMERICAL MODELLING COMIT, TUNAMI, WIN ITDB Sist Int Alert Tsun Hawai AFTN (aerop) SATELLITE PHONE FAX-PHONE MOVIL PHONE COMMUNICATION MEDIA: RADIO: CPN- RPP SEISMIC MONITORING SISTEMA TREMORS ANTENA COMPUTADORA ESTACION SISMICA N E Ingreso de datos al Sist. TREMORS Z SISMOMETRO DE BANDA ANCHA CON TRES COMPONENTES ) (TELEFONO) SISTEMA DE ALERTA
8 SEA LEVEL MONITORING: DART BUOY SYSTEM SEA LEVEL STATION MONITORING FACILITY PERUVIAN TIDAL NETWORK 10 TIDAL STATIONS WITH LEVEL SENSOR OF RADAR TYPE (MICROWAVE 26 GHz). DATA COMMUNICATION DATA COMMUNICATION IN REAL TIME
9 GPS GEODESIC STATION (DHN-IRD) An application in the field of prevention of natural disasters would be the implementation of a tsunami early warning using GPS signals in real time. When there is a great earthquake, tectonic stresses relax and change the position of geodesic point (located in San Lorenzo island). We can measure this sudden changes in the geographical coordinates: latitude, longitude and altitude. If the variation exceeds a certain threshold, the alert would be given for. SOFTWARE FOR DETERMINATION OF TSUNAMI AND FAST CALCULATION OF ARRIVAL TIMES
10 TSUNAMI NUMERICAL MODELING: WIN ITDB TSUNAMI NUMERICAL MODELING TUNAMI-N2
11 TSUNAMI NUMERICAL MODELING: COMMTT EXAMPLE CHILEAN TSUNAMI, FEB 27, 2010 PREVENTION MEASURES
12 Tsunami Workshops; Training in Schools, Universities and publics/privates institutions Information about Tsunamis published in the Web-site of DHN General information: definition, iti origin, generation,history of peruvian tsunamis Information about national and international tsunami warning system. Downloadable information: videos, simulations, journal, Inundation maps Preliminar report of Tsunamis
13 INUNDATION MAPS DHN is elaborating and publishing in the web the tsunami inundation maps of every important city located in the peruvian coasts. It s downloadable information. There are 98 inundation maps. EL SISTEMA DE ALERTA DE TSUNAMI MÁS EFICAZ ES LA EDUCACIÓN DE LA POBLACIÓN COSTERA! GRACIAS!
INTEGRANDO DATOS MARINOS Y MODELOS AL SERVICIO DE LA OPERATIVA PORTUARIA: EL SISTEMA SAMPA DEL PUERTO DE ALGECIRAS
INTEGRANDO DATOS MARINOS Y MODELOS AL SERVICIO DE LA OPERATIVA PORTUARIA: EL SISTEMA SAMPA DEL PUERTO DE ALGECIRAS Operational Oceanography on the Strait of Gibraltar SAMPA and TRADE Teams Physical environment
Magnitude 8.8 OFFSHORE MAULE, CHILE
A great 8.8-magnitude struck central Chile early Saturday. The quake hit 200 miles (325 kilometers) southwest of the capital Santiago. The epicenter was just 70 miles (115 kilometers) from Concepcion,
NATIONAL CIVIL PROTECTION SYSTEM ONEMI. Evolution Current Development Future Challenges
NATIONAL CIVIL PROTECTION SYSTEM ONEMI Evolution Current Development Future Challenges CHILE 1 A nation exposed to all kind of hazards Volcanic Eruptions Wild Fires Tidal waves/ Tsunamis Quakes/ Earthquakes
WWNWS2/3/2-XV Meeting 2 15 July 2010 Agenda Item 3.2. MSI Self Assessment NAVAREA XV. Submitted by CHILE SUMMARY
WWNWS WWNWS2/3/2-XV Meeting 2 15 July 2010 Agenda Item 3.2 MSI Self Assessment NAVAREA XV Submitted by CHILE SUMMARY Executive Summary: NAVAREA XV provides the paper of MSI self assessment for WWNWS2 Action
RED SISMICA DE PUERTO RICO PROTOCOLO DE INFORMACION PARA TERREMOTO/TSUNAMIS PR/IV
RED SISMICA DE PUERTO RICO PROTOCOLO DE INFORMACION PARA TERREMOTO/TSUNAMIS PR/IV EL FENOMENO LLAMADO TSUNAMI CICLO DE LOS DESASTRES MITIGACION RECUPERACION Short term Long Term Eliminate / Reduce impact
Department of Commerce National Oceanic & Atmospheric Administration National Weather Service
Department of Commerce National Oceanic & Atmospheric Administration National Weather Service NATIONAL WEATHER SERVICE WESTERN REGION SUPPLEMENT 17-2003 APPLICABLE TO NWSI 10-701 MARCH 16, 2015 Operations
DRAFT TSUNAMI WARNING INFORMATION DISSEMINATION PROTOCOL FOR TRINIDAD AND TOBAGO (CDEMA PARTICIPATING STATE)
DRAFT TSUNAMI WARNING INFORMATION DISSEMINATION PROTOCOL FOR TRINIDAD AND TOBAGO (CDEMA PARTICIPATING STATE) ODPM 6/3/2011 CONTENTS 1. Acronyms 2. Standard operating procedures A: (SOP A): 3. Standard
Honduras. Tuesday, October 3, 2000 Depart San Jose, Costa Rica, arrive in Tegucigalpa, Honduras.
Honduras Tuesday, October 3, 2000 Depart San Jose, Costa Rica, arrive in Tegucigalpa, Honduras. Puerto Cortes Caribbean Sea GUATEMALA San Pedro Sula HONDURAS EL SALVADOR Pacific Ocean San Lorenzo NICARAGUA
Improved Warnings for Natural Hazards: A Prototype System for Southern California
Improved Warnings for Natural Hazards: A Prototype System for Southern California Yehuda Bock Research Geodesist Scripps Institution of Oceanography University of California San Diego, La Jolla, Calif.
Ring of Fire. (15 minutes) Earthquakes and volcanoes occur in relationship to each other.
Ring of Fire Lesson Concept Link Earthquakes and volcanoes occur in relationship to each other. Lesson 6.12 develops concepts about preparation for earthquakes in terms of home or school damage or lack
The Seismic Alert System of Mexico (SASMEX) and their Alert Signals broadcast Broadcast results Results Paper Title Line 1
The Seismic Alert System of Mexico (SASMEX) and their Alert Signals broadcast Broadcast results Results Paper Title Line 1 J. M. Espinosa-Aranda, A. Cuéllar, G. Ibarrola, R. Islas & A. García, Centro de
Pacific Tsunami Warning Center (NOAA) International Tsunami Information Center (NOAA-UNESCO/IOC)
TSUNAMI WARNING OPERATIONS: SEA LEVEL MONITORING TIDE TOOL: DISPLAY AND DECODE OF SEA LEVEL DATA TRANSMITTED OVER THE WMO GLOBAL TELECOMMUNICATIONS SYSTEM (vers 8.11, June 2010) Pacific Tsunami Warning
Geospatial Information for disaster risk reduction and natural resources management. Rolando Ocampo Alcántar
Geospatial Information for disaster risk reduction and natural resources management Rolando Ocampo Alcántar Content Background Geospatial Information for Disaster Management Risk Atlas Information Exchange
EARTHQUAKES. Compressional Tensional Slip-strike
Earthquakes-page 1 EARTHQUAKES Earthquakes occur along faults, planes of weakness in the crustal rocks. Although earthquakes can occur anywhere, they are most likely along crustal plate boundaries, such
Exploring plate motion and deformation in California with GPS
Exploring plate motion and deformation in California with GPS Student worksheet Cate Fox-Lent, UNAVCO master teacher; Andy Newman, Georgia Institute of Technology; Shelley Olds, UNAVCO; and revised by
Magnitude 7.2 GUERRERO, MEXICO
A powerful magnitude-7.2 earthquake shook central and southern Mexico on Friday. The earthquake occurred at a depth of 24 km (15 miles). Its epicenter was in the western state of Guerrero, near the seaside
How To Make A Report On The Hydrographic Activities Of The Republic Of Cuba
Report on the activities of the Hydrographic and Geodetic Service of the Republic of Cuba National Hydrography and Geodetic Office 2011 I. INTRODUCTION: As part of the accomplishment of actions derived
Regents Questions: Plate Tectonics
Earth Science Regents Questions: Plate Tectonics Name: Date: Period: August 2013 Due Date: 17 Compared to the oceanic crust, the continental crust is (1) less dense and more basaltic (3) more dense and
TECTONICS ASSESSMENT
Tectonics Assessment / 1 TECTONICS ASSESSMENT 1. Movement along plate boundaries produces A. tides. B. fronts. C. hurricanes. D. earthquakes. 2. Which of the following is TRUE about the movement of continents?
Sea Level Monitoring in Mexico
GLOSS GE XII - November 2011 Sea Level Monitoring in Mexico Elaborated by: Jorge Zavala-Hidalgo Instituto de Geofísica Universidad Nacional Autónoma de México Circuito exterior s/n 04510 México, D.F. México
Name: Date: Class: Finding Epicenters and Measuring Magnitudes Worksheet
Example Answers Name: Date: Class: Finding Epicenters and Measuring Magnitudes Worksheet Objective: To use seismic data and an interactive simulation to triangulate the location and measure the magnitude
Disaster Risk Reduction through people centered National Multi-hazard Early Warning System in the context of Maldives
Disaster Risk Reduction through people centered National Multi-hazard Early Warning System in the context of Maldives Abdul Muhusin, Deputy Director Department of Meteorology, Maldives Fourth Technical
Real Time Flood Alert System (RTFAS) for Puerto Rico
Prepared in cooperation with the Puerto Rico Emergency Management Agency (PREMA) Real Time Flood Alert System (RTFAS) for Puerto Rico Overview The Real Time Flood Alert System is a web-based computer program,
Disaster Management Cycle
GIS TOOL FOR CALCULATING REPAIR COST OF BUILDINGS DUE TO EARTHQUAKE EFFECTS (CCRE CISMID) Miguel Estrada Carlos Zavala Fernando Lazares Jorge Morales Japan Peru Center for Earthquake Engineering Research
Plotting Earthquake Epicenters an activity for seismic discovery
Plotting Earthquake Epicenters an activity for seismic discovery Tammy K Bravo Anne M Ortiz Plotting Activity adapted from: Larry Braile and Sheryl Braile Department of Earth and Atmospheric Sciences Purdue
Chincha and Cañete, Peru, Based
Reconstruction of Ica, Pisco, Chincha and Cañete, Peru, Based on Updated Hazard Maps Julio Kuroiwa Professor emeritus National University of Engineering and UNDP Reconstruction Program/Sustainable Cities.
Lessons learned from the tsunami disaster caused by the 2011 Great East Japan Earthquake and improvements in JMA's tsunami warning system
Lessons learned from the tsunami disaster caused by the 2011 Great East Japan Earthquake and improvements in JMA's tsunami warning system October 2013 Japan Meteorological Agency Lessons learned from the
Lecture 12 Earthquake Magnitude
Lecture 12 Earthquake Magnitude Locating Earthquakes Last time, we learned that we could obtain a rough estimate of the distance in miles to an earthquake epicenter by multiplying the S - P time interval
Earthquakes. Earthquakes: Big Ideas. Earthquakes
Earthquakes Earthquakes: Big Ideas Humans cannot eliminate natural hazards but can engage in activities that reduce their impacts by identifying high-risk locations, improving construction methods, and
Chapter 7 Earthquake Hazards Practice Exam and Study Guide
Chapter 7 Earthquake Hazards Practice Exam and Study Guide 1. Select from the following list, all of the factors that affect the intensity of ground shaking. a. The magnitude of the earthquake b. Rather
Glossary. continental crust: the sections of crust, the outermost layer of the earth, that include the continents
aftershock: an earthquake that follows a larger earthquake or main shock and originates in or near the rupture zone of the larger earthquake. Generally, major earthquakes are followed by a number of aftershocks
Assessment of Impact of the December 26, 2004 Tsunami In Aceh Province Indonesia
Assessment of Impact of the December 26, 2004 Tsunami In Aceh Province Indonesia Jay H. Samek, David L. Skole, and Walter Chomentowski December 30, 2004 Center for Global Change and Earth Observations
TsunamiReady Program Definitions
TsunamiReady Program Definitions 24-Hour Warning Point (WP): A communication facility at a state or local level, operating 24 hours a day, which has the capability to receive NWS alerts and warnings, plus
Beacon to Beacon Northern & Southern Maps
Beacon to Beacon Northern & Southern Maps Disclaimer: When using the Beacon to Beacon Guide booklets and/or the maps contained therein for commercial or non-commercial purposes, the Department of Transport
THE 2004 SUMATRA EARTHQUAKE AND INDIAN OCEAN TSUNAMI: WHAT HAPPENED AND WHY
Page 6 The Earth Scientist THE 2004 SUMATRA EARTHQUAKE AND INDIAN OCEAN TSUNAMI: WHAT HAPPENED AND WHY Seth Stein and Emile A. Okal Dept of Geological Sciences, Northwestern University, Evanston Illinois
4.14 Netherlands. Interactive flood risk map of a part of the province of Gelderland in the Netherlands. Atlas of Flood Maps
4.14 Netherlands The Netherlands is flood prone for about 60% of its surface. 95 so-called dike-rings protect the polders from being flooded from the North Sea, rivers or lakes. The protection level has
Soil Dynamics and Earthquake Engineering
Soil Dynamics and Earthquake Engineering 31 (2011) 154 162 Contents lists available at ScienceDirect Soil Dynamics and Earthquake Engineering journal homepage: www.elsevier.com/locate/soildyn The seismic
Geosciences - Programme subject in programme for Specialization in General Studies
Geosciences - Programme subject in programme for Specialization in General Studies Dette er en oversettelse av den fastsatte læreplanteksten. Læreplanen er fastsatt på Bokmål Laid down as a regulation
DETECTION METHOD OF METEOTSUNAMI EVENTS AND CHARACTERIZATION OF HARBOUR OSCILLATIONS IN WESTERN MEDITERRANEAN. Abstract
DETECTION METHOD OF METEOTSUNAMI EVENTS AND CHARACTERIZATION OF HARBOUR OSCILLATIONS IN WESTERN MEDITERRANEAN Gaël André 1, Marta Marcos 2, Camille Daubord 3 Abstract A detection algorithm aimed at analysing
Predicting Coastal Hazards: A Southern California Demonstration
Predicting Coastal Hazards: A Southern California Demonstration Patrick Barnard United States Geological Survey Coastal and Marine Geology Team Santa Cruz, CA Southern California Multi-hazards Demonstration
3D Visualization of Seismic Activity Associated with the Nazca and South American Plate Subduction Zone (Along Southwestern Chile) Using RockWorks
3D Visualization of Seismic Activity Associated with the Nazca and South American Plate Subduction Zone (Along Southwestern Chile) Using RockWorks Table of Contents Figure 1: Top of Nazca plate relative
Tsunami Practice Questions and Answers Revised November 2008
Tsunami Practice Questions and Answers Revised November 2008 1. What happened on 26 December 2004 off the west coast of Sumatra? 2. What is the final estimate of the magnitude of the Sumatra 26 December
Transform Boundaries
Lecture 7 Plates and Mantle Plumes Transform Boundaries Transform boundaries occur where one segment of rigid lithosphere slides horizontally past another in response to stresses in the lithosphere. The
The earthquake source
Global seismology: The earthquake source Reading: Fowler p111-140 and Bolt Appendix G Earthquake location Earthquake focus: Latitude, longitude, depth Earthquake epicenter: Latitude, longitude Earthquakes
TIDES. 1. Tides are the regular rise and fall of sea level that occurs either once a day (every 24.8 hours) or twice a day (every 12.4 hours).
TIDES What causes tides? How are tides predicted? 1. Tides are the regular rise and fall of sea level that occurs either once a day (every 24.8 hours) or twice a day (every 12.4 hours). Tides are waves
Georgia Performance Standards Framework for Natural Disasters 6 th Grade
The following instructional plan is part of a GaDOE collection of Unit Frameworks, Performance Tasks, examples of Student Work, and Teacher Commentary. Many more GaDOE approved instructional plans are
Real time earthquake monitoring for early warning of tsunamis
Real time earthquake monitoring for early warning of tsunamis 2 nd R.S.Dattatrayam India Meteorological Department Ministry of Earth Sciences New Delhi-110003 nd India Disaster Management Congress 4-6
PROCESS OF DELEGATION UNDER THE GRANT METHOD FOR THE PORT OF MANTA. Delegation of the Multipurpose Deepwater Terminal Logistic Activity Zone, LAZ
PROCESS OF DELEGATION UNDER THE GRANT METHOD FOR THE PORT OF MANTA Delegation of the Multipurpose Deepwater Terminal Logistic Activity Zone, LAZ Delegation under the grant method for the Multipurpose Deepwater
DEVELOPMENT OF THE FORECAST PROPAGATION DATABASE FOR NOAA s SHORT-TERM INUNDATION FORECAST FOR TSUNAMIS (SIFT)
NOAA Technical Memorandum OAR PMEL-139 DEVELOPMENT OF THE FORECAST PROPAGATION DATABASE FOR NOAA s SHORT-TERM INUNDATION FORECAST FOR TSUNAMIS (SIFT) Edison Gica 1,2 Mick C. Spillane 1,2 Vasily V. Titov
Tsunami: Reduction Of Impacts through three Key Actions (TROIKA)
ITS 2001 Proceedings, Session 1, Number 1-1 247 Tsunami: Reduction Of Impacts through three Key Actions (TROIKA) Eddie N. Bernard NOAA/Pacific Marine Environmental Laboratory, Seattle, Washington, U.S.A.
How To Help The Environment
CIIFEN Activities 2012 Rodney Martínez Güingla [email protected] Workshop on Climate Change in Mediterranean and Caribbean Seas: Guayaquil, Ecuador, 08-11 May 2011 MISSION To promote, coordinate and
HAZARD MAPPING, RISK ASSESSMENT, AND INSURANCE COVERAGE OF NATURAL CATASTROPHE RISK
SESSION III HAZARD MAPPING, RISK ASSESSMENT, AND INSURANCE COVERAGE OF NATURAL CATASTROPHE RISK Mr. Sumarjono Insurance Bureau of The Ministry of Finance of the Republic of Indonesia Geological Position
Evolving a new Geodetic Positioning Framework: An Australian Perspective
Evolving a new Geodetic Positioning Framework: An Australian Perspective G. Johnston, J. Dawson Outline Introduction Precise Positioning National Geospatial Reference Systems Asia Pacific Reference Frame
Draft 8/1/05 SYSTEM First Rev. 8/9/05 2 nd Rev. 8/30/05 EMERGENCY OPERATIONS PLAN
Draft 8/1/05 SYSTEM First Rev. 8/9/05 2 nd Rev. 8/30/05 EMERGENCY OPERATIONS PLAN I. INTRODUCTION A. PURPOSE - The University of Hawaii System Emergency Operations Plan (EOP) provides procedures for managing
Investigation 6: What happens when plates collide?
Tectonics Investigation 6: Teacher Guide Investigation 6: What happens when plates collide? In this activity, students will use the distribution of earthquakes and volcanoes in a Web GIS to learn about
Chapter 5: Earthquakes
Chapter 5: Earthquakes 1. Experiencing an Earthquake firsthand 2. The Science of Ghost Forests and Megaearthquakes 3. Faults, Earthquakes, and Plate Tectonics 4. Seismic Waves and Earthquake Detection
Storm tide is the water level rise during a storm due to the combination of storm surge and the astronomical tide.
INTRODUCTION TO STORM SURGE Introduction to Storm Surge BOLIVAR PENINSULA IN TEXAS AFTER HURRICANE IKE (2008) What is Storm Surge? Inland Extent Storm surge can penetrate well inland from the coastline.
GNSS permanent stations as the part of integrated geodetic system in Estonia
GNSS permanent stations as the part of integrated geodetic system in Estonia Karin Kollo (MSc) Department of Geodesy Estonian Land Board United Nations/Croatia Workshop on the applications of Global Navigation
EARTH SCIENCE ACTIVITY #1 Tsunami in a Bottle
EARTH SCIENCE ACTIVITY #1 Tsunami in a Bottle Grades 3 and Up This activity is one of several in a basic curriculum designed to increase student knowledge about earthquake science and preparedness. The
Storm tide is the water level rise during a storm due to the combination of storm surge and the astronomical tide.
INTRODUCTION TO STORM SURGE Introduction to Storm Surge National Hurricane Center Storm Surge Unit BOLIVAR PENINSULA IN TEXAS AFTER HURRICANE IKE (2008) What is Storm Surge? Inland Extent Storm surge can
PACIFIC CATASTROPHE RISK ASSESSMENT AND FINANCING INITIATIVE
PACIFIC CATASTROPHE RISK ASSESSMENT AND FINANCING INITIATIVE NIUE SEPTEMBER 11 COUNTRY RISK PROFILE: NIUE Niue is expected to incur, on average,.9 million USD per year in losses due to earthquakes and
Coastal Areas emergency alert system FAQs
Coastal Areas emergency alert system FAQs What is the Stinger? The Stinger Mobile Alert System was developed by a local business in partnership with Hastings Civil Defence and GNS science for use in the
User s Guide. Zuniga Point. Point Loma
User s Guide Welcome to the Location File for San Diego Bay, located in the southwestern corner of the U.S. San Diego Bay has an excellent natural harbor, which has made it a busy commercial port. San
Possible Inundation Map of Coastal Areas of Gujarat with a Tsunamigenic Earthquake
Indian Minerals, Vol.61(3-4) & 62 (1-4), (July, 2007 - December, 2008); pp. 59-64 Possible Inundation Map of Coastal Areas of Gujarat with a Tsunamigenic Earthquake A. P. Singh 1*, U. Bhonde 1, B. K. Rastogi
Corredores de Comercio del NAFTA Laredo, Texas: Puente Comercial de las Américas
Corredores de Comercio del NAFTA Laredo, Texas: Puente Comercial de las Américas The Objective of recent trade missions to Central and South America: To position Laredo, Texas as a logistics hub, to promote
Name Date Class. By studying the Vocabulary and Notes listed for each section below, you can gain a better understanding of this chapter.
CHAPTER 7 VOCABULARY & NOTES WORKSHEET Earthquakes By studying the Vocabulary and Notes listed for each section below, you can gain a better understanding of this chapter. SECTION 1 Vocabulary In your
Seismic Waves Practice
1. Base your answer to the following question on the diagram below, which shows models of two types of earthquake waves. Model A best represents the motion of earthquake waves called 1) P-waves (compressional
DYNAMIC CRUST: Unit 4 Exam Plate Tectonics and Earthquakes
DYNAMIC CRUST: Unit 4 Exam Plate Tectonics and Earthquakes NAME: BLOCK: DATE: 1. Base your answer to the following question on The block diagram below shows the boundary between two tectonic plates. Which
ABSG Consulting, Tokyo, Japan Email: [email protected] 2. Professor, Kogakuin University, Tokyo, Japan 3
Application of Earthquake Early Warning System and Real-time Strong-motion Monitoring System to Earthquake Disaster Mitigation of a High-Rise Building in Tokyo, Japan Tomohiro Kubo 1, Yoshiaki Hisada 2,
The Dynamic Crust 2) EVIDENCE FOR CRUSTAL MOVEMENT
The Dynamic Crust 1) Virtually everything you need to know about the interior of the earth can be found on page 10 of your reference tables. Take the time to become familiar with page 10 and everything
The benefits of satellite telecom systems for civil protection
The benefits of satellite telecom systems for civil protection Pascale SOURISSE President 15-17 avenue de Ségur 75007 Paris, France www.eurospace.org T+33-1-44420070 F+33-1-44420079 1 The benefits of satellite
Earthquake Hazards and Risks
Page 1 of 7 EENS 3050 Tulane University Natural Disasters Prof. Stephen A. Nelson Earthquake Hazards and Risks This page last updated on 28-Aug-2013 Earthquake Risk Many seismologists have said that "earthquakes
CHAPTER 7. EMERGENCY SERVICES
CHAPTER 7. EMERGENCY SERVICES Although better forecasts and warning processes have helped save lives by providing more lead time to evacuate, the tremendous growth of development and human population in
EL Civics Objective 16 (Emergencies) Level: Beginning Low & Beginning High Task #1: Identify Emergencies & Disasters
EL Civics Objective 16 (Emergencies) Level: Beginning Low & Beginning High Task #1: Identify Emergencies & Disasters Language & Literacy Objectives: 1. Identify what constitutes an emergency or disaster,
Chapter Overview. Bathymetry. Measuring Bathymetry. Echo Sounding Record. Measuring Bathymetry. CHAPTER 3 Marine Provinces
Chapter Overview CHAPTER 3 Marine Provinces The study of bathymetry charts ocean depths and ocean floor topography. Echo sounding and satellites are efficient bathymetric tools. Most ocean floor features
CRS 610 Ventura County Flood Warning System Website
CRS 610 Ventura County Flood Warning System Website Purpose This document gives instructions and a description of the information available via the Ventura County Watershed Protection District s (VCWPD)
Head 168 HONG KONG OBSERVATORY
Controlling officer: the Director of the Hong Kong Observatory will account for expenditure under this Head. Estimate... $203.4m Establishment ceiling (notional annual mid-point salary value) representing
EARTHQUAKE MAGNITUDE
EARTHQUAKE MAGNITUDE Earliest measure of earthquake size Dimensionless number measured various ways, including M L local magnitude m b body wave magnitude M s surface wave magnitude M w moment magnitude
Earthquake Magnitude Calculator for the AS-1 Seismograph 1
Magnitude calculator for the AS-1 Page 1 of 23 Earthquake Magnitude Calculator for the AS-1 Seismograph 1 Lawrence W. Braile and Saptarshi Dasgupta, Purdue University SKIP TO CALCULATORS Introduction:
Earthquake detection systems can sound the alarm in the moments before a big tremor strikes time enough to save lives
SEISMOLOGY Earthquake detection systems can sound the alarm in the moments before a big tremor strikes time enough to save lives By Richard Allen in brief Earthquake early-warning networks detect the earliest
The Hong Kong Polytechnic University. Subject Description Form
The Hong Kong Polytechnic University Subject Description Form Subject Code Subject Title LSGI3350A Hydrographic Surveying Credit Value 3 Level 3 Pre-requisite / Co-requisite/ Exclusion Objectives Nil This
ABSTRACT INTRODUCTION PURPOSE
EVALUATION OF TSUNAMI DISASTER BY THE 2011 OFF THE PACIFIC COAST OF TOHOKU EARTHQUAKE IN JAPAN BY USING TIME SERIES SATELLITE IMAGES WITH MULTI RESOLUTION Hideki Hashiba Associate Professor Department
GPS Use in U.S. Critical Infrastructure. and Emergency Communications. Presented to the
GPS Use in U.S. Critical Infrastructure and Emergency Communications Presented to the DOT, DoD, and DHS United States Technical Training Institute (USTTI) Presenter Monty Graham Program Manager GPS Jamming
Tsunami Inundation Maps
1946 1964 Today Tomorrow Tsunami Inundation Maps For Emergency Response Planning Available at www.tsunami.ca.gov Multi-year project covers all low-lying populated coastal areas 20 counties and over 75
Earthquakes. www.earthquakes.bgs.ac.uk
Earthquakes www.earthquakes.bgs.ac.uk Introduction Earthquakes are among the most deadly natural hazards. There are around 100 earthquakes each year of a size that could cause serious damage. They strike
Step 2: Learn where the nearest divergent boundaries are located.
What happens when plates diverge? Plates spread apart, or diverge, from each other at divergent boundaries. At these boundaries new ocean crust is added to the Earth s surface and ocean basins are created.
TRAINING SYSTEM AND INFORMATION NETWORK FOR EARTHQUAKE DISASTER MITIGATION
TRAINING SYSTEM AND INFORMATION NETWORK FOR EARTHQUAKE DISASTER MITIGATION T. Saito 1, N. Hurukawa 2, T.Yokoi 2, T. Hara 2, B. Shibazaki 2, Y. Fujii 2, S. Koyama 2, T. Kashima 2 and T. Mukai 2 1 International
DECISION SUPPORT SYSTEM FOR SEISMIC RISKS
DECISION SUPPORT SYSTEM FOR SEISMIC RISKS María J. Somodevilla [email protected] Angeles B. Priego [email protected] Esteban Castillo [email protected] Ivo H. Pineda [email protected] Darnes Vilariño
Interactive Plate Tectonics
Interactive Plate Tectonics Directions: Go to the following website and complete the questions below. http://www.learner.org/interactives/dynamicearth/index.html How do scientists learn about the interior
Communications Systems Used in the USA TARNS. Chris Hill, Meteorologist in Charge (ret) National Weather Service Seattle, Washington, USA
Communications Systems Used in the USA TARNS Chris Hill, Meteorologist in Charge (ret) National Weather Service Seattle, Washington, USA Washington Faces Many Non-Weather Hazards Earthquakes Tsunamis Terrorism
Earthquake Disaster Recovery Plan in TMG
Earthquake Disaster Recovery Plan in TMG Pre-disaster Management Measures by District and Recovery from Expected Earthquake Directly Underneath Tokyo Planning Section Urban Development Projects Division
WWNWS3/3/2-XV Meeting 3 29 August 2011 Agenda Item 3.2. MSI Self Assessment NAVAREA XV. Submitted by Chile SUMMARY
WWNWS WWNWS3/3/2-XV Meeting 3 29 August 2011 Agenda Item 3.2 MSI Self Assessment NAVAREA XV Submitted by Chile SUMMARY Executive Summary: NAVAREA XV provides the paper of MSI self assessment for WWNWS3
