1. Larry Braile, braile@purdue.edu, web.ics.purdue.edu/~braile Sheryl Braile NSTA, Boston, 2008 (Despite the popularity of this image, tsunami waves do not normally look like this.) Tsunami! Understanding the Generation, Propagation, and Hazards of Tsunamis This PowerPoint Presentation (last modified March 14, 2008) : http://web.ics.purdue.edu/~braile/edumod/tsunami/Tsunami!.ppt

2. Tsunamis can be generated by: 1. Large Earthquakes (megathrust events such as Sumatra, Dec. 26, 2004) 2. Underwater or near-surface volcanic eruptions (Krakatoa, 1883) 3. Comet or asteroid impacts (evidence for tsunami deposits from the Chicxulub impact 65 mya) 4. Large landslides that extend into water (Lituya Bay, AK, 1958) 5. Large undersea landslides (evidence for prehistoric undersea landslides in Hawaii and off the east coast of North America)

3. Schematic plate tectonic setting for tsunami generation NOAA Commonly, in mega-thrust earthquakes, a very large area of the ocean floor is uplifted TRENCH

4. Earthquake generation of tsunami (note: tsunami wave in the animation should be asymmetrical with a first peak traveling to the right and a first trough traveling to the left) http://ffden-2.phys.uaf.edu/645fall2003_web.dir/elena_suleimani/generation_small.mov http://web.ics.purdue.edu/~braile/edumod/tsunami/TsunamiFiles.htm Animation

5. Exploring Planet Earth Blind Thrust Fault Earthquake Rupture Animation (Northridge, 1994) Brad Aagaard, USGS http://pasadena.wr.usgs.gov/office/baagaard/research/animations/animations.html The fault rupture will be visible in the animation. Displacements (magnified 3000 times) will be visible by the movement of the mesh from the model. The amplitude of motions and seismic waves is color coded according to ground velocity. Note the rupture along the fault over time from the deepest extent of the fault. http://web.ics.purdue.edu/~braile/new/AagaardBlindThrustAnimation.ppt

6. Blind Thrust Fault Earthquake Rupture Animation – Brad Aagaard, USGS http://pasadena.wr.usgs.gov/office/baagaard/research/animations/animations.html The fault rupture will be visible in the animation. Displacements (magnified 3000 times) will be visible by the movement of the mesh from the model. The amplitude of seismic waves is color coded according to ground velocity.

7. http://pasadena.wr.usgs.gov/office/baagaard/research/animations/animations.html Earthquake Rupture

8. DescriptorMagnitudeAverage Annually Great8 and higher1 ¹ Major7 - 7.917 ² Strong6 - 6.9134 ² Moderate5 - 5.91319 ² Light4 - 4.913,000 (est.) Minor3 - 3.9130,000 (est.) Very Minor2 - 2.91,300,000 (est.) ¹ Based on observations since 1900. ² Based on observations since 1990. Worldwide earthquakes per year (from USGS):

9. Worldwide earthquakes per year: Frequency-magnitude relationship suggests that magnitude 9+ events will occur about once per decade, statistically; since 1900, the actual number is ~once per 20 years.

10. Tsunami Statistics (NOAA): http://wcatwc.arh.noaa.gov/tsustats.pdfhttp://wcatwc.arh.noaa.gov/tsustats.pdf Tsunami Statistics (NOAA): http://wcatwc.arh.noaa.gov/tsustats.pdfhttp://wcatwc.arh.noaa.gov/tsustats.pdf (Dec. 26, 2004 tsunami resulted in over 200,000 deaths) Tsunami Statistics

11. Tsunami wave propagation characteristics – note that as water depth becomes smaller, waves slow down, become shorter wavelength, and have larger amplitude. When the water is 10 m deep, what is the separation of the waves in minutes? NOAA

12. Animation courtesy of Dr. Dan Russell, Kettering University http://www.gmi.edu/~drussell/demos.html Water waves animation Direction of propagation

13. Tsunami velocity and amplitude equations (These are plane layer [flat ocean bottom] equations) 1.Wave velocity controlled by water depth: v = (g x d) 1/2 where v is velocity, d is water depth and g is the acceleration of gravity = 9.8 m/s 2 ; so, velocity decreases in shallower water. 2.Wave height (amplitude) increases (conservation of energy) in shallow water: A S = A D x (V D /V S ) 1/2 where A S = amplitude in shallow water, A D = amplitude in deep water, V S = velocity in shallow water, and V D = velocity in deep water.

14. Geist, Titov and Synolakis, Tsunami: Wave of Change, Scientific American, January, 2006. Wave Heights – Satellite observation versus calculated model – open ocean, deep water ~1600 km; ~2.2 hours of waves at 750 km/hr

15. Tsunami Wave Tank 1. “SnapLock Select” plastic underbed storage box 118 x 51 x 13 cm (45” x 21” 5”) from Walmart, K-Mart, etc. (or Sterilite #1996), remove handles, fill holes with silicon sealer. 2. Plexiglass 53 x 48 x 0.5 cm (21” x 19” x 3/16”) [could use sand for “coastal area” instead of plexiglass]. 3.Two 30 cm plastic rulers with clay base, 30 cm apart. 4.Fill to 8 cm deep with water.

16. Tsunami Wave Tank

17. Tsunami Wave Tank (close-up of ruler and plexiglass – note slope representing shallowing of water depth adjacent to coast)

18. Tsunami Wave Tank – Video of Wave Tank Download Tank.mov from: http://web.ics.purdue.edu/~braile/edumod/tsunami/TsunamiFiles.htm

19. Tsunami Wave Tank – Video of Waves Water Drop – Point source, circular spreading of energy: Download WaterDrop3.mov and WaterDrop4Measure.mov from: http://web.ics.purdue.edu/~braile/edumod/tsunami/TsunamiFiles.htm 1. What are the characteristics of the waves generated by the water drop? 2. Measure the velocity of the wave using a stopwatch (distance from center to side of tank in cm, divided by time in seconds). 3. Can you observe reflected waves. 4. Why do the waves eventually disappear?

20. Tsunami Wave Tank – Video of Waves Line Source (plane wave) – No spreading of energy: Download PlaneWave1.mov from: http://web.ics.purdue.edu/~braile/edumod/tsunami/TsunamiFiles.htm 1. What are the characteristics of the waves generated by the line source? 2. Measure the velocity of the wave using a stopwatch (follow one wave crest from first ruler to the second – 30 cm divided by time). 3. What is the wave height? 4. What is the wave length? 5. Do the waves get smaller with distance of propagation? 6. What type of water wave in the ocean is similar to these waves?

21. Ocean Waves

22. Tsunami Wave Tank – Video of Waves Tsunami – Line source and entire water column disturbed: Download Tsunami2.mov from: http://web.ics.purdue.edu/~braile/edumod/tsunami/TsunamiFiles.htm 1.What are the characteristics of the waves generated by the tsunami source? 2. Measure the velocity of the wave using single frame advance (follow one wave crest from first ruler to the second – 30 cm divided by time). 3. What is the wave height? 4. What is the wave length? 5. What happens to the wave as it propagates into shallow water?

23. Tsunami Wave Tank – Video of Waves Tsunami – Line source and entire water column disturbed: Download Tsunami4Measure.mov from: http://web.ics.purdue.edu/~braile/edumod/tsunami/TsunamiFiles.htm (Use pause and single frame advance to observe wave characteristics) ~5.8 s ~6.2 s  Note Long Wavelength  Note Wave Cresting 

24. Tsunami Wave Tank Materials Wave generation sources; drop into water or oscillate up and down on water surface to create waves: Golf ball, plastic golf ball (or table tennis ball), eye dropper, clay, wood, styrofoam strips 48 x 10 x 2.5 cm (19” x 3.75” x 1”)

25. Geist, Titov and Synolakis, Tsunami: Wave of Change, Scientific American, January, 2006. 26 Dec. 2004 Tsunami max. wave height and arrival time

26. Seismic Eruption software: http://www.geol.binghamton.edu/faculty/jones/http://www.geol.binghamton.edu/faculty/jones/ Indonesia area historical earthquakes files, download from: http://web.ics.purdue.edu/~braile/edumod/tsunami/TsunamiFiles.htm

27. Seismic Eruption software: http://www.geol.binghamton.edu/faculty/jones/http://www.geol.binghamton.edu/faculty/jones/ Sumatra earthquake and aftershocks files, download from: http://web.ics.purdue.edu/~braile/edumod/tsunami/TsunamiFiles.htm

28. Tsunami simulation (Note focusing of energy to west and east of the earthquake rupture area) http://staff.aist.go.jp/kenji.satake/animation.gif

29. Tsunami simulations Open Quick Time simulations (see these websites) http://www.pmel.noaa.gov/tsunami/ http://www.pmel.noaa.gov/tsunami/Mov/TITO V-INDO2004.mov http://es.ucsc.edu/~ward/indo.mov Note distance of propagation and reflection of waves Thailand-Wave.wmv from http://www.asiantsunamivideos.com/http://www.asiantsunamivideos.com/ Tsunami videos:

31. Chedi Resort, Phuket, Thailand, wave height ~4+ m (?, from estimates of water level from beach umbrellas on grassy area above the beach)

32. Banda Aceh, Sumatra, before tsunami http://geo-world.org/tsunami/

33. Banda Aceh, Sumatra, after tsunami Also: http://www.digitalglobe.com/http://www.digitalglobe.com/

34. Tsunami Teacher Resource Kit (17 MB pdf) from ITIC (International Tsunami Information Centre) http://www.tsunamiwave.info/ Tsunami Resources

35. Tsunamis – Wall of Water activities (University of Texas, Institute of Geophysics) http://www.ig.utexas.edu/outreach/cataclysms/modules.htm

36. IRIS Posters: http://www.iris.edu/about/publications.htm#phttp://www.iris.edu/about/publications.htm#p

37. Larry Braile, braile@purdue.edu, web.ics.purdue.edu/~braile Sheryl Braile NSTA, Boston, 2008 (Despite the popularity of this image, tsunami waves do not normally look like this.) Tsunami! Understanding the Generation, Propagation, and Hazards of Tsunamis This PowerPoint Presentation (last modified March 14, 2008) : http://web.ics.purdue.edu/~braile/edumod/tsunami/Tsunami!.ppt