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Tsunamis. What is a tsunami ?. A tsunami is a very long ocean wave generated by sudden displacement of the sea floor or of the oceanic mass The displacement of an equivalent volume of water generates the tsunami. Terminology. The term “tsunami” is a Japanese word meaning “harbour wave” - PowerPoint PPT Presentation
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Tsunamis
What is a tsunami ?
A tsunami is a very long ocean wave generated by sudden displacement of the sea floor or of the oceanic mass
The displacement of an equivalent volume of water generates the tsunami
Terminology
The term “tsunami” is a Japanese word meaning “harbour wave”
It was so named because the wave is harmless until it enters a harbour
It is frequently called a “tidal wave”, but it has nothing to do with tides
Hazards and risks of tsunamis
Tsunamis can hit with little or no warning
4,000 people have been killed between 1990 and 2000
The most prone areas are those associated with earthquakes and volcanoes (mainly subduction zones)
1990-2000
26 December 2004: ¼ million fatalities
Locally-generated tsunamis
The subduction zone of Cascadia has potential for very large offshore quakes (M 8)
There is a great danger of locally-generated tsunamis here, since they travel so fast
Many large cities are found on the coast
Structure of a wave
Wavelength, , can exceed 200 km
normal ocean waves have wavelengths of about 100 m
trough; peak; wave height, h; amplitude
From Murck et al. (1996)
Velocities and energies
Velocity = 3.132 x (water depth)½
where water depth is in meters and velocity is in meters/second (1 m/s = 3.6 km/hr)
Wave energy h2 (approximately)
Velocities in deep water
Tsunamis travel very quickly relative to normal ocean waves
This is particularly the case in open water, where velocities increase with water depth
Velocities can reach 1,000 km/hr in open ocean (normal ocean wave: ~90 km/hr)
Thus, velocities are about 10 times higher for tsunamis
Shallow water
In shallow water, the tsunami waves pile up
As a result, velocities and wavelengths decrease...
…but at the same time, amplitudes can increase enormously...
Amplitudes
In deep water, wave amplitudes are generally less than 1 meter…
…but in shallow water, amplitudes can reach 40 meters or more above normal sea level
Arrival of a tsunami on a coast
The wave will break when its height exceeds ~one seventh (1/7) of its wavelength…
…so some very long waves actually may not break
initially, there may be a rise or fall (drawdown) in sea level (which may attract people, to their great misfortune)
Long wavelengths and the coast
Due to its long wavelength, it may take a long time for a tsunami wave to crest
The wave then may remain high for several minutes
And it may take a while (hours) for the crests of successive waves to reach the shore…so don’t go surfing !
Wave runup - complicated
This depends on several factors:
water depth
sea floor profile
shape of coastline (focussing of energy, tsunamis travelling up rivers
An example of wave focussing at Krakatau, 1883
Causes of tsunamis - all involve displacement of water
Earthquakes
Volcanic activity
Landslides
Meteorite impacts
Earthquakes
Mainly vertical crustal movements…
…so strike-slip faults perhaps less hazardous…
...although these too can trigger mass movements such as landslides
Types of faults
Earthquakes
In general, the larger the quake, the larger the tsunami…but not a perfect correlation
Some anomalously large tsunamis generated from small quakes…
...energy released at longer periods than can be registered on normal seismometers ?
Shallow quakes
Quake energy seismic moment = slip x fault area x rigidity of rocks
For a given quake magnitude, if displacement is large, then rigidity may be low
This may indicate that the shallow parts of subduction zones are frictionally weak (unconsolidated sediments, fractures, fluids, etc.)
Submarine landslides
Another contributing factor to large tsunamis may be submarine landslides:
-generated by shaking associated with the earthquake
-cause additional displacement of water, thus a larger and more complicated tsunami event
Subduction association
Tsunamis typically are associated with earthquakes generated at subduction zones
Rupture of sea floor surface
Sediment slumps into subduction trench
Volcanic activity
Displacement of rock
Submarine caldera collapse (e.g., along faults) (Krakatau 1883)
Entrance of pyroclastic flows into water (Krakatau 1883)
Subaerial lateral collapse, generating debris avalanches which enter water (Unzen 1792)
Landslides
Landslides often are generated by quakes or volcanoes
also occur on subduction trench slopes (steep)
also can occur in enclosed bodies of water (lakes, bays, reservoirs, etc.) (rockfalls, slumps of unconsolidated material, etc.)
Landslides
Enormous submarine landslides can occur on the flanks of ocean islands (e.g., Hawaii, Canaries)
The wave washup can approach 400 meters in some cases
Canary Islands
Meteorite impacts
Too terrible to contemplate !!!
Hundreds to thousands of meters in height ?
Terminal Cretaceous event
Read and find out !
4 case histories
Alaska 1964 (earthquake-generated)
Krakatau 1883 (caldera-generated)
Unzen 1792 (landslide-generated)
Grand Banks 1929 (submarine landslide-generated
1964 Alaska quake and tsunami
Prince William Sound
epicenter
Old Valdez
1964 events
27 March 1964, 5:36 PM local time (early evening, people in their homes)
Magnitude 9.2 quake…largest ever recorded in North America…second largest ever
Shaking lasted 4-5 minutes (to compare, the 1906 San Francisco event lasted 45-60 seconds
Tectonic setting
Subduction in the Aleutian region results in very large quakes
Between 1899-1965:
7 quakes with M 8
60 quakes with M 7
Tsunami generation
In this region, tsunamis are generated by two mechanisms:
1) large vertical movements of the sea floor along faults (local and distant tsunamis)
2) slumping of material, both underwater and from land to water, by ground shaking
Nature of the 1964 tsunami
106 people were killed by the wave, 114 people total (consider the small coastal population of the area)
The extensive ground deformation caused by the quake triggered tsunamis
Destructive force of the wave
Avalanches and landslides were generated
Some of these generated locally damaging tsunamis
The force of such a wave can be seen in this picture
Boat runups
Carried inland by tsunami waves, boats acted as battering rams, efficiently destroying buildings
Here is a beached boat at Seward after the events
Submarine sliding at Valdez, Seward, and Whittier
These towns were built on unconsolidated sediments
Seismic shaking ruptured petroleum storage tanks in these towns, causing fires
The shaking also initiated submarine landslides, causing tsunami waves
Effects at Valdez
The landslides carried burning oil out into the bays…
…while the tsunamis returned the burning oil to the harbours and townsites, exacerbating the fires
Old and new Valdez
Unconsolidated sediments
Wave runup
This is Valdez Inlet after the main tsunami hit
Here the wave runup was the highest, reaching 67 meters
At Kodiak, tsunami effects were made worse by tectonic subsidence (faulting)
Wave runup
Valdez
It took 2-3 minutes to generate the tsunami from the landslide
30 people died
$ 15 million US in damage
Distant effects
As you can see, the wave affected the entire Pacific basin
The tsunami was hugely destructive along the west coast of Canada and the US (but only 16 dead)
Each colour band represents a 1-hour tsunami travel time increment
The eruption of Krakatau 1883
Krakatau is a volcano located between Java and Sumatra
It is mainly a submarine volcano, with its top sticking out of the water
Krakatau
Caldera collapse
The cataclysmic eruption occurred on 26-27 August 1883
A submarine caldera was formed
Displacement of material during collapse generated a series of devastating tsunamis
Two views of the caldera margin on Rakata, one soon after the eruption and the other in 1979
This is Anak Krakatau, which emerged through the sea in 1928. It is within the caldera
Tsunami
36,000 people were killed by the tsunami along the coasts of Java and Sumatra
At least 3 great waves occurred
165 coastal villages were destroyed by the waves
The largest waves were recorded by tide gauges up to 7,000 km away on the Arabian Peninsula
Tsunami
Coral blocks up to 600 tons were carried inland…
…these served efficiently as natural battering rams
Runup heights reached 40 meters
Maximum runup heights in meters (from Simkin and Fiske, 1983)
Telok Betong
buoy
Shaded grey is submerged area
red=boat
yellow=buoy
blue=hill
Telok Betong
From Simkin and Fiske (1983)
Before...
…and after
hill
The District Hall in Telok Betong. The tsunami stopped just before this building, sparing the people cowering inside
The hill near Telok Betong. The lower part of the hill has been cleansed of its vegetation by the tsunami
Boat runup…the Berouw...
This boat, named the Berouw, was carried 2.5 km inland at Telok Betong by the wave, which reached 24 m in height
…and inland emplacement of its mooring buoy
This is the Berouw’s mooring buoy, also carried inland
It is now a visually pleasing monument overlooking Telok Betong
Refraction diagram of the tsunami, showing transport times in minutes
From Simkin and Fiske (1983)
Krakatau
26 December 2004 earthquake and tsunami
From Brumbaugh (1999)
Magnitude 9.0-9.3
A warning to Indonesians:
Kerry Sieh’s poster and efforts to educate people beforehand
Plate tectonics of the eastern Indian Ocean region
Courtesy USGS
From Lay et al 2005, Science
Tectonics and previous great earthquakes
From Lay et al 2005, ScienceCumulative energy from global seismicity
From Liu et al 2005, Science
Tsunami runups (blue) and maximum tsunami heights (black) in Sri Lanka
Global propagation of the 26 December 2004 tsunami based on a model by Titov et al 2005 in
Science
Tsunami wave heights around the world (from Titov et al 2005 Science)
Unzen volcano, Japan: 1792 collapse of Mt. Mayuyama
In addition to its recent lava dome and pyroclastic flow activity (1990-1995), the volcano also has collapsed catastrophically in the past
Mt. Mayuyama
scar
islands
Pyroclastic debris, 1991-1995
The 21 May 1792 collapse
A debris avalanche occurred from Mt. Mayuyama in 1792 about 1 month after lava stopped flowing from Fugen-dake (site of recent activity)
The avalanche was triggered by two quakes
Fugen-dake
Mt. Mayuyama
Tsunamis
The debris avalanche entered the Ariake Sea, generating a tsunami
The wave killed between 14,000 and 15,000 people in coastal communities
Geological map, showing 1792 debris avalanche deposit
The debris avalanche deposit
Extent of the 1792 debris avalanche deposit and the scar on Mt. Mayuyama
Note the islands
From Siebert et al. (1987)
An artist’s rendition of the 1792 events
Before...…and after
scar
deposit
New islands
18 November 1929 Grand Banks tsunami
This tsunami was caused by a M 7.2 quake on the Grand Banks
The quake triggered a submarine landslide which resulted in the tsunami
1: 1700 quake
3: M9.5 Chilean quake in 1960
4: M9.2 Alaskan quake in 1964
2: 1929 Grand Banks quake
1: 1700 quake
3: M9.5 Chilean quake in 1960
4: M9.2 Alaskan quake in 1964
2: 1929 Grand Banks quake
The 1929 landslide
The volume of the landslide was approximately 200 km3 (big !)
It flowed at speeds up to 70 km/hr
The flow cut 12 trans-Atlantic cables in 28 places
The 1929 tsunami
The height of the tsunami reached 5 meters in height
The wave struck the south coast of the Burin Peninsula on Newfoundland
Between 27 and 29 people drowned
Tsunami hazards
Extensive flooding
Action of wave on coastal structures, both natural and built
The incredible force of the waves can remobilize huge objects
The event may create drawdown
Effects of tsunami drawdown
Release of dissolved gases (CH4, CO2, H2S)
previously contained in shallow sediments
Potential ignition of gases by their rapid expulsion
As a result, a wave of noxious and burning gases may engulf people BEFORE the wall of water arrives
Mitigation efforts
Warning times
Every ~750 km of travel distance is equal to about 1 hour of warning time
So, as discussed above, there is very little warning time for tsunami generated by local sources, compared to those from distant sources
Quake-generated tsunamis
In general, the size of the quake is an approximate indication of the size of the tsunami
But this guide doesn’t always work
To determine the amount and orientation of crustal displacement at the surface, the moment magnitude is more useful than the Richter magnitude
Moment magnitudes
(fault slip) x (fault area) x (rigidity of rox)
The point is that we cannot always rely on quake magnitude to determine the magnitude of the tsunami
Hawaii is particularly vulnerable, being in the middle of the Pacific
Warning systems
Mainly based on earthquake data
Pacific-wide warnings: require at least 1 hour warning time
More local networks require warning times less than 1 hour…this is difficult
A proposed system of real-time detectors
Response to tsunami
Requires good emergency planning and preparation…
…an educated and trained public…
…which has access to information…
…so the dissemination of this info needs to be efficient and reliable
Personal mitigation
Run (don’t walk) to higher ground
Tell your family and friends
Never go to the beach to watch tsunamis
Sign in the lobby of a Hawaiian hotel:
IN CASE OF TSUNAMI:
Remain calm
Pay your bill
Run like hell
Hazard maps
As we have seen for earthquakes and volcanoes, hazard maps are critically useful pieces of information
Here are two examples, the first from Hawaii, and the second from Eureka, California
Note inundation areas and arrows for evacuation centres
Eureka
Eureka, Calif.
Eureka, California
Located in northwestern California, and is part of Cascadia
Hazards from tsunamis, liquefaction, ground shaking associated with liquefaction, etc.
But don’t forget...
Many areas and towns do not have such maps
Tsunamis -reading
Billings, L.G., 1915. Some personal experiences with earthquakes. National Geographic, v. 27, no. 1, January 1915, pp. 57-71.
González, F.J., 1999. Tsunami! Scientific American, May, 1999.
Niven, L., and J. Pournelle, 1983. Lucifer’s Hammer. New York, Fawcett Crest, 629 pp.
Simkin, T., and R.S. Fiske, eds, 1983. Krakatau 1883, the volcanic eruption and its effects. Washington, D.C., Smithsonian Institution Press, pp. 69-81.
Tsunamis - web
Canada: http://atlas.nrcan.gc.ca/site/english/maps/environment/naturalhazar
ds/naturalhazards1999/tsunamis
http://www.pep.bc.ca/hazard_preparedness/Tsunami_Preparedness_Information.html
U.S.: http://www.ess.washington.edu/tsunami/index.html
http://www.tsunami.noaa.gov/
U.K.: http://www.nerc-bas.ac.uk/tsunami-risks/