Understanding the Physics of Tsunamis

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SUMMARY

The speed of a tsunami is calculated using the formula c = sqrt(G * d), where G is the gravitational constant (9.8 m/sec²) and d is the ocean depth in meters. Tsunamis behave as shallow-water waves, which differentiates them from normal surface ocean waves. The velocity of these waves is derived from the shallow-water phase and group velocity equations. For further understanding, refer to the linear theory of ocean surface waves as detailed in the provided resources.

PREREQUISITES
  • Understanding of gravitational constant (G) and its value (9.8 m/sec²)
  • Knowledge of wave mechanics, specifically shallow-water wave theory
  • Familiarity with ocean depth measurements and their impact on wave speed
  • Basic mathematical skills for manipulating equations
NEXT STEPS
  • Study the derivation of the shallow-water wave equations from the linear theory of ocean surface waves
  • Explore the differences between shallow-water waves and deep-water waves
  • Research the impact of ocean depth on tsunami wave height and behavior
  • Examine case studies of tsunami events to analyze wave speed and height in real scenarios
USEFUL FOR

Students of physics, oceanographers, and anyone interested in understanding tsunami dynamics and wave mechanics.

lagrange
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I read that the speed of a tsunami is given by

c = sqrt(G * d)

where G is the gravitational constant 9.8 m/sec^2 and
d is ocean depth in meters.

How is this derived? I had always thought that wave speed was a constant depending only on the medium.

Also, is there some fundamental mechanical difference between a tsunami and a "normal" surface ocean wave?
 
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Do you also know the formula for the height of the wave. (Of course in respect to the clifs stepping.)
 
Hello lagrange,

The behaviour of tsunami is the behaviour of shallow-water waves.
Therefor the velocity of the waves is given by the equation for the shallow-water phase- and group velocity.

Here you'll find the linear theory of ocean surface waves:
http://oceanworld.tamu.edu/resources/ocng_textbook/chapter16/chapter16_01.htm

The shallow-water velocity equation (16.8) and (16.11) in this paper are derived using the equations (16.5)and (16.6).

More about ocean waves and tsunami:
http://oceanworld.tamu.edu/resources/ocng_textbook/chapter17/chapter17_02.htm
 

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