ANATOMY OF A TSUNAMI - University of Calgary in Alberta · The Sumatra Andaman Island Earthquake of...
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ANATOMY OF A TSUNAMIJ. Fernando*, A. Braun**, R. Galapatti***, S.C. Wirasinghe**, J. Ruwanpura**
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OUTLINE
•The Sumatra Andaman Island Earthquake
•The Indian Ocean Tsunami
•Impact on Sri Lanka's Coast and Ecosystems
•Tsunami Warning Systems
•Mitigation Strategies and Better Planning
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The Sumatra Andaman Island Earthquake of Dec. 26, 2004
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The Sumatra Andaman Island Earthquake of Dec. 26, 2004
– Facts: Sunday, Dec 26 0:58:53 UTC
– >> 6:58:53 local time
– Location: 3.307N 95.947E, depth=30 km
– 250 km SW from Banda Aceh, Indonesia
– Magnitude 9.0-9.3: 2nd, 4th largest EQ since 1900
– Slip of up to 15-20 meters
– 1200 km long fault plane
– Southern fault – fast rupture, northern fault – slow
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The Indian Ocean Tsunami
– Travels with the speed of up to 800 km/h
– Speed depends on water depth
– Wavelength 100-250 km
– Waveheight depends on water depth
– Over open ocean waveheight = 20-60 cm
– Wave and height observed by satellite altimetry
Courtesy of K. Satake
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The Indian Ocean Tsunami
Courtesy of W. Smith, NOAA
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The Indian Ocean Tsunami
Inundation levels based on different wave heights
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The Indian Ocean Tsunami
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Impact on Sri Lanka's Coast and Ecosystems
•North-south striking fault caused linear wavefront reaching Sri Lanka
•Reached Sri Lanka's east coast frontally at 8:50 AM
•Damage/wave height was a function of local bathymetry
•Sand dunes in the southeast and far northeast coast protected coast
•Man-made and natural gaps in dunes led to wave penetration
•Vegetation protects, coconut trees did not suffer, but palmyrah trees did
•Mangroves protect estuaries, but not found in energetic wave climates
•Displacement of sand and sediments, saltwater intrusion into aquifers
•However, the ecosystem damage was light to moderate
•Internal and external functions are still intact
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Impact on Sri Lanka's Coast and Ecosystems
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Impact on Sri Lanka's Coast and Ecosystems
Dead Palmyrah Trees in Mullaitivu
Breached spit in Bentota
R/H/42/TEroded face of Hambantota dunes
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Tsunami Warning Systems
NOAA Dart – Pacific, new stations in the Atlantic
•GITEWS – Indian Ocean, 2 stations (currently not operational)
•USIOTWS – Indian Ocean, planned
•Detect sea level variations of 1 cm
•Contain 1) detection system, 2) communication system,
•and 3) warning system including social aspects
•How fast can we issue a warning and to whom?
•How reliable must the information be?
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Mitigation Strategies and Better Planning
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Mitigation Strategies and Better Planning
Detect - Local Seismic NetworkUniform (0,10)
Detect - Global Seismic NetworkUniform (0,10)
TsunamiUniform (0,3)
Process Seismic Info.
Uniform (0,2)
Info. Received by Analyst
Uniform (0,5)
Radio SignalUniform (0,1)
Process Seismic Info.
Uniform (0,2)
Validate with Global NetworkUniform (1,5)
Detected by Tsunami Warning
SystemUniform (5,20)
Detect - Tide Gauge System
Uniform (5,20)
Perform Seismic Analysis
Uniform (2,5)
Info. Received by TWC
Uniform (0,5)
Issue an AlertUniform (1,3)
Issue a Decision on EQ
Uniform (1,3)
Info Received - National
Uniform (0,5)
Issue a Detailed Analysis
Uniform (1,3)
Detect EQ - Human
Uniform (0,10)
Tsunami AnalysisUniform (2,5)
Detect - HumanUniform (5,20)
Info. Received - Local
Uniform (1,10)
Process Info - Human
Uniform (0,20)
Telephone SignalUniform (1,30)
Internet SignalUniform (0,2)
Inform Local Authorities for
PreparationUniform (5,30)
Dummy
Human Info Validated - Local
Uniform (3,10)
Satellite SignalUniform (0,2)
Tsunami Simulation Analysis
Uniform (5,10)
Start
Inform National Centre
Uniform (0,5)
National Office Makes a Decision
Uniform (0,5)
Inform Local Authorities for
InitiationUniform (5,30)
Evacuation Start
FS/FF
FS/FF
FS/FF
FS
FS
FS FS
FS FS FS
FS
FS
FS FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
FS
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Conclusions