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Tsunamis

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Title: Tsunamis


1
Tsunamis
EPS 131Introduction to Physical Oceanography
  • Presented by
  • Saira Hashmi
  • Oct. 14th,2005

2
Overview
  • Tsunami - what is it?
  • Tsunami Formation
  • What is the Physics behind them?
  • Warning systems?
  • Examples of Tsunamis
  • Animations/Simulations
  • Conclusion
  • References
  • Questions

3
Tsunami- what is it?
  • Definition
  • Unusually large wave in a harbour (Japanese)
  • Series of water waves generated by huge and
    sudden perturbation (e.g. earthquakes, slides,
    volcanoes, asteroids)
  • Characteristics
  • Wave period 2-200 minutes
  • Run-up heights O(10-100 m)(Flooding of
    shoreline)
  • Speed

4
Tsunami Formation
5
Tsunami Formation
  • Tsunamis can be generated when the sea floor
    suddenly displaces the overlying water
    vertically.
  • Tectonic earthquakes are a kind of earthquake
    that can cause that.
  • When they occur beneath the sea, the water above
    the deformed area is displaced from its
    equilibrium position.
  • Waves are formed as the displaced water mass,
    acting under the force of gravity, tries to
    regain equilibrium.
  • When large areas of the sea floor elevate or
    subside, a tsunami can be created.
  • Large vertical movements of the earth's crust can
    occur at plate boundaries, at the faults.

6
Tsunami Formation
  • As a tsunami leaves the deep ocean and travels
    toward the shallow coast, it transforms.
  • A tsunami moves at a speed related to the water
    depth, therefore the tsunami slows as the water
    depth decreases.
  • The tsunami's energy flux, being dependent on
    both its wave speed and wave height, remains
    nearly constant.
  • As a result, the tsunami's speed decreases as it
    travels into shallower water, and its height
    increases.
  • When it reaches the coast, it may appear as a
    rapidly rising or a series of breaking waves.

7
Tsunami Formation
  • As a tsunami reaches the shore, it begins to lose
    energy .
  • It Slows down and height increases when
    approaching shallow coast
  • Tsunamis reach the coast with tremendous amounts
    of energy.
  • Destructive power is due to speed and force with
    which they strike the coastal area.
  • Tsunamis are stronger and retain height longer
    than waves generated by wind.

8
Whats the Physics behind the Waves
http//observe.arc.nasa.gov/nasa/exhibits/tsunami/
tsun_hit2.html
9
Warning Systems
10
PUBLIC WARNING SYSTEMcan you tell if a tsunami
is coming?
  • The U. S. ESSA operates warning systems.
  • Its PTWC in Hawaii is the regional operational
    center for tsunami information in the Pacific
  • A Tsunami Watch Bulletin is released when an
    earthquake occurs with a magnitude of 6.75 or
    greater on the Richter scale.
  • A Tsunami Warning Bulletin is released when
    information from tidal stations indicates that a
    potentially destructive tsunami exists.
  • This system is not very reliable. For example,
    Honolulu was evacuated in 1948 on a false alarm
    at a cost of more than 30 million dollars.

11
Examples of Tsunamis
12
Simulations/ Animations
13
Wave Propagation simulation
http//www.pgc.nrcan.gc.ca/press/images/2003JB0025
21-animation.gif
14
Conclusion
  • Tsunamis..
  • Are uncontrollable phenomenon
  • Causes extensive loss of life
  • Damage property
  • Public warning systems provide some measures of
    protection.

15
Reference
  • Online . http//pubs.usgs.gov/publications/text/
    historical.htm 1 February 2005
  • "Elastic Rebound" . "Pacific Earthquake
    Engineering Research Center" . Online .
    http//peer.berkeley.edu/jrodgers/EQDef/eqdef2.ht
    m 5 March 2005
  • "2004 Indian Ocean earthquake" . "Wikipedia" .
    Online . http//en.wikipedia.org/wiki/2004_India
    n_Ocean_Earthquake 20 February 2005
  • "Tsunami" . "Wikipedia" . Online .
    http//en.wikipedia.org/wiki/Tsunami 20 February
    2005
  • "USGS Earthquake Hazards Program-Latest
    Earthquakes" . "US Geological Survey" . Online
    . http//earthquake.usgs.gov/eqinthenews/2004/ussl
    av/ 5 March 2005
  • "26 December 2004 Tsunam" . "National Institute
    of Oceanography, India" . Online .
    http//www.nio.org/jsp/tsunami.jsp 5 March 2005
  • "Tsunami! The WWW Tsunami Information Resource"
    . "Earth and Space Sciences (Geology and
    Geophysics) at UW" . Online .
    http//www.ess.washington.edu/tsunami/toc.html 5
    March 2005
  • "Sumatra Earthquake 26 December 2004" . "British
    Geological Survey" . Online .
    http//www.earthquakes.bgs.ac.uk/latest_info.htm
  • "USGS Earthquake Hazards Program-Latest
    Earthquakes" . "US Geological Survey" . Online
    . http//earthquake.usgs.gov/eqinthenews/2004/ussl
    av/ 5 March 2005
  • "26 December 2004 Tsunam" . "National Institute
    of Oceanography, India" . Online .
    http//www.nio.org/jsp/tsunami.jsp 5 March 2005
  • "Tsunami! The WWW Tsunami Information Resource"
    . "Earth and Space Sciences (Geology and
    Geophysics) at UW" . Online .
    http//www.ess.washington.edu/tsunami/toc.html 5
    March 2005
  • "Sumatra Earthquake 26 December 2004" . "British
    Geological Survey" . Online .
    http//www.earthquakes.bgs.ac.uk/latest_info.htm

16
Questions
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