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Tsunami: Hazard, Mitigation and Warning Ishmael C. Narag Officer-in-Charge Seismological Observation and Earthquake Prediction Division PHIVOLCS-DOST School Teachers’ Seminar-Training on Natural Hazards Awareness and Preparedness 24 April 2007 PHIVOLCS

3.2 understanding tsunami

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Page 1: 3.2 understanding tsunami

Tsunami:Hazard, Mitigation and Warning

Ishmael C. NaragOfficer-in-Charge

Seismological Observation and Earthquake Prediction DivisionPHIVOLCS-DOST

School Teachers’ Seminar-Training on Natural Hazards Awareness and Preparedness

24 April 2007PHIVOLCS

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• A series of waves generated by various geological processes

Tsunami Hazard

• Japanese term meaning “harbor waves”

• ”

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Tidal Wave / Storm Surge

• Tsunami waves are not “tidal waves”– Gravitational attraction

between earth and a heavenly body (e.g. moon, sun & other planets)

• Wind-generated waves– Surfs

– Storm surges

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Tsunami

• Danger continues for hours

• High fatality hazard

• Global impact blind to political boundaries

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Recent Tsunami in the Philippines

1976 Moro Gulf Tsunami

1992 Eastern Mindanao Tsunami

1994 Mindoro Tsunami

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The Science of Tsunami

• Generation

• Propagation

• Inundation

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Tsunami Generation

• Generally byEARTHQUAKES

• Less commonly by Sub-aerial to SubmarineLANDSLIDES

• Infrequently byVOLCANIC ERUPTIONS

• Very rarely byMETEORITE IMPACTS

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Tsunami Generation

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Tsunami Propagation

• Speed depends on

Water Depth

– Fast in deep ocean (>1000 kph)

– Slows near shore (30-50 kph)

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Tsunami Propagation

• Height depends on Water Depth

– Small in deep ocean (few cm to 1 m)

– Grows near shore (can be > 30 m)

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Run-up & Inundation

• Last stage of the evolution of a tsunami

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Scientific Development

• Run-up data used to improve models

• New generation of inundation models– Better inundation maps– Tsunami wave-height

forecasting

• Distributed global historical databases

• Paleotsunami studies– More complete and

longer tsunami histories– Improved hazard ID &

risk assessment

• Slump-generated tsunamis

• Real-time deep ocean data– New monitoring

strategies– Direct confirmation of

tsunami

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Tsunami Hazard Assessment

• Compile complete catalogue for earthquakes and tsunamis. Understand local and regional geology and tectonics

• Identify most hazardous tsunami source areas and its tsunami-generating mechanism (earthquake, landslide, volcanic eruption)

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Tsunami Hazard Assessment

• Identify most vulnerable coastal locations from sources (historical or expected)

• For these coastal locations, conduct modelling for inundation and run-up to determine impact

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Tsunami in the PhilippinesTsunami in the Philippines

• About 44 earthquakes from 1589 to present generated tsunamis.

• Enclosed bays are the usual sites where tsunami waves are observed.

• Some areas have more than one tsunami reports (ex. Songsong Bay, Manila Bay, Calauag Bay, CaragaBay, Moro Gulf area)

• Minimum earthquake magnitude is 5.4.

• Largest tsunamis occurred in the Zamboanga-Cotabato-Sarangani areas

Reference: Bautista, 2002

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Tsunami Deposits

• Geologic materials (including grain sizes from boulders to mud) deposited above mean sea level during the passage of a tsunami.

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Tsunami Deposits

• Landward limit of inundation

• Direction of flow over an area

• Infer the passage of prehistoric tsunamis and the occurrence of an earthquake.

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Tsunami Deposits

• Identify ancient tsunami deposits

– Difference in faciesbetween tsunami and storm deposits

• Post-depositional alteration

– Depositional extent

– Thickness

– Internal structure

• Understand tsunami hydraulics

– Where tsunami might transport sediments

– Depth and velocity of flow

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Tsunami Warning System

• Sensors / Instrumentation for seismic and tidal data

– Seismographs

– Wet Sensors

– Tide Gauge

– Pressure Gauge

– Deep-sea bottom pressure gauge

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Deep-ocean Assessment and Reporting of Tsunamis

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Lubang Island Setup

Concrete Pier

The height of stainless tube and elevation of probes and collecting vessel could be adjusted to set the tsunami heightmeasurement level H(I.e. 1 m, 3 m, 6 m or 10 m)

Water collecting

vessel

Stainless Tube

Air Vent

Tsunami Water Intake

H

Electric Cable

Sea Water

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PHIVOLCS Proposed Deployment of Tsunami

Wet Sensors

1 m

5 m10 m

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Tsunami Warning System

• Data Transmission /Retrieval System

– Radio

– Microwave

– Landline

– Satellite

– Internet

• Data Evaluation– Earthquake Location &

Magnitude Estimate

– Coastal amplitude forecast

• Emergency Communications for Info Dissemination

– Sirens

– Emergency Alert Systems

– Radios

– Telephones/Hotlines

– Wire

– Data Systems

– Satellite

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Warning Guidance

• Very Rapid Earthquake Evaluation

• Very Rapid Sea Level Evaluation

– Early Detection

– Wave Forecast

– Warning Disseminated to the last kilometer

• Rapid (as soon as possible)

• Accurate (minimize false warnings)

• Reliable (continuous operation)

• Effective (to save lives)

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Two Tsunami Threats

• LOCAL/REGIONAL TSUNAMI

• Generated nearby

• Strikes shore quickly (within minutes)

• Highest Run-ups

• Damage only to limited areas

• DISTANT / PACIFIC-WIDE TSUNAMI

• Generated far away

• Strikes shore later (5+ hours for official evacuation)

• Widespread Damage

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Two Tsunami Threats

• LOCAL/REGIONAL TSUNAMI

• Philippine National Seismic Network

• DISTANT / PACIFIC-WIDE TSUNAMI

• Pacific Tsunami Warning Center (PTWC)

• Northwest Pacific Tsunami Information Center (NWPTIC)

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Two Tsunami Threats

• Chile

• Alaska

• Aleutian Islands

• Marianas

• Japan

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Distant Tsunami

1960 Chilean Earthquake & Tsunami1960 Chilean Earthquake & Tsunami

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PHIVOLCS Tsunami Alert Levels (distant earthquakes)

• life threatening tsunami generated near epicenter

• IMMEDIATE EVACUATIONof areas projected to be affected

• NDCC flow of info• Community-based

alarms• Media, military

• Major shallow earthquake in Pacific (magnitude > 7.0)

• Waiting for confirmation of tsunami

• Information released to general public

• BE READY, wait for further information

• NO EVACUATION ORDER!

• Confirmed tsunami near epicentral area

• wave heights NON-LIFE threatening

• WATCH in effect,

• NO EVACUATION!

• Observe precautionary measures near coastline- stay away from the coastline

Go!!Watch/observe Ready

Level 3Level 2Level 1

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False Warnings

• False Warnings will occur– Small, non-destructive

tsunami observed

– Expensive: In 1994, false warning in Hawaii cost $50M

– High number of false alarms reduces credibility

– Evacuations place citizens at greater risk

• Balance number of false warnings with missed events

– No warning system, no false warnings

• Prepare & educate public, media and emergency officials

– Statistics

– Reliability

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1993 Okushiri TsunamiAonae Peninsula

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Aonae Peninsula – Rebuilding

• 10 years & > $600 M later– Memorial Park

– Memorial Hall

– Elevate (3 m fill) and/or relocate town

– 10-m high platform at harbor

– Sloping (not stairs) covered evacuation routes

– Four water gates

– Concrete sea-walls

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Aonae Peninsula - Rebuilding

1993

2000

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Lessons Learned

• Education is essential for local tsunamis

– Hard sell

– All hazards approach

• Land use management is least expensive way to mitigate tsunami damage

– Rebuild or Relocate?

• Surveys of tsunami damage immediately after the tsunami provides vital data for numerical model development and education

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Tsunami: Education and Safety

• Inundation Maps

• Tsunami Evacuation Procedures

• Tsunami Educational Materials

• Tsunami Markers

• Tsunami Awareness Month

– Tsunami Safety Drills

– Essay Contests

• Tsunami Museums

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Pacific Tsunami Museum

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Pacific Tsunami Museum

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Tsunami Damage

• Run-Up & Inundation

• Ground Subsidence

• Wave-related damage

– Best case: Quickly rising tide

– Worse case: Wall of turbulent water with rocks and debris

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Damage Scenario

• Trees and posts are uprooted from their locations

• Cars and boats are inundated;

• Tsunami debris can cause injuries during inland & back flows

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Damage Scenario

• Sea water is murky and may cause health complications when ingested.

• Water in wells become salty and not potable

• Agricultural lands are rendered useless for two years.

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Signs of an Impending Tsunami

• Large off-shore earthquake

• Unusual rise or fall of coastal waters

• Exposure of corals and underwater rocks

• Sound of approaching train

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Safety Procedures

• If any news of a nearby earthquake, stay alert and be ready to move to higher ground;

• If you feel an earthquake wherein you cannot stand, immediately move to higher ground;

• If the water receded, immediately move to higher ground;

• Never attempt to watch an approaching tsunami;

• Listen to instructions and do not return until authorities issue an all’s-clear bulletin;

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Structural Countermeasures

• Sea walls at breakwaters

• Tide control gates

• Flood gates

• Elevated Structure

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Non-structural Countermeasures

• Planting of trees and preservation of mangrove

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Non-structural Countermeasures

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Non-structural Countermeasures

• Sufficient road networks & paths to elevated areas

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Non-structural Countermeasures

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Non-structural Countermeasures

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Non-structural Countermeasures

• Regulation of coastal population

• Peace and security of the area

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Issues on Land Use Planning

� Uncoordinated special

purpose plans such as for

transportation or economic

development with hazard

planning

� Location of the hazard

does not seem to have

impacted the land use

allocation decision

making process

� Definitions of hazard

zones vary in accordance

with technique

Safety related criteria < Economically viable project

Private and other government agencies

would perform beyond their mandates

and capabilities;

Evacuation routes are non-

existent or unmaintained and are

located in hazard zones

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• Restrict land use by strategically controlling development

• Support land-use plans through capital improvement planning and budgeting

• Existing land-use restrictions can be modified

Land Planning Measures

• Designate tsunami hazard areas for open-space use (agriculture, parks, recreation);

� Acquire tsunami hazard areas for open-space use

Very low-density residential useClustering of development

Extension of water supply, public facilities etc.

Keep development at a minimum in hazard areas

floodplain restrictions, hillside and landslide control, environmental, scenic, recreational and wildlife-protection requirements

�Simple acquisition

�Development rights

�Leasing

�Land exchange

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Land Use Planning

• Tsunami effects must be addressed if administration decides to build in hazard zones;

• Damage to life and property may be due to:

– Simple flooding

– Force of waves

– Horizontal currents such as drawdown

� Organization and

arrangement of three

primary elements :

�Structures

�Elevated Open Spaces

�Roads & Alleys

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Inventory of Physical Conditions

• Opportunities & Limitations

– Areas of high and low relief

– Dangerous to other calamities

– Characteristics of the coastline (narrow bays, steep cliffs, etc)

– Soil condition

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Review of the Plan

• Requirements for the implementation of the plans

• Conform to the site’s physical characteristics;

• Expected cost and benefits of the plan

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THANK YOU

FOR

LISTENING

PHIVOLCS: http://[email protected]