Tsunami word problem (waves practice)

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    Word problem
In summary, a tsunami with a wavelength of 100km and a sea surface displacement of 3 meters has been generated 4000km off the shore of California. Its speed is approximately 198m/s and it will take about 20203 seconds to reach the shore. The frequency of the tsunami is 505.1 Hz with a period of 1.97E-3 seconds. As the wave approaches the shore and its depth decreases from 4000m to 10m, the new wavelength is calculated to be 5051m. The amplitude of the wave will change as it goes shallow in order to conserve energy flux, and can be calculated using the formula for water wave power.
  • #1
cmorissette
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Homework Statement


A Tsunami has been generated as a plane wave 4000km off the shore of California. The sea surface displacement is found to be 3 meters and the wavelength of the tsunami is 100km. You can assume a depth of 4000m from the location of wave generation to shore.

a.) Calculate the speed of the wave (assume it is a deep water wave if h/lambda > 1/4 and it is a shallow wave if h/lambda < 1/20) Estimate the time it will take this wave to reach the shore.

b.) calculate the frequency and period of the tsunami

c.) As the wave approcahes the shore its depth decreases from 4000m to 10m. What is it's new wavelength? (the wave period is conserved as the depth changes)

d.) What is the new amplitude of the wave? (you must conserve energy flux)


Homework Equations


shallow water wave velocity Cp = √gh
frequency = Cp/λ
Period = 1/F


The Attempt at a Solution



Part a is pretty easy. IT is a shallow water wave because h/λ < 1/20. The wave velocity is [(g)(h)]^1/2 which equals ~198m/s. Given the offshore distance of 4000000m, it would take a time of (4E6m/197.99m/s)= 20203 s.

PArt b is also straight forward: The frequency is F= Cp/λ which equals (198m/s)/(100000m) = 505.1 Hz. The period T = 1/F or 1.97E-3 s

Part c is what I'm having trouble on. if the wavelength λ=Cp/F and the period is conserved, does that mean the frequency is also conserved? So does this simply become (198m/s)/505.1s = 0.39m? Or do I need to recalculate Cp with a depth of 10m?

Cp= [(g)(10m)]^1/2 = ~10m/s so then wavelength would be (10m/s)(505.1Hz)= 5051m?

Also, I'm not sure about part d. If I were to guess, I would use
E= (1/2)ρga^2
But I can't see how amplitude would change here, because ρ and g are constant!

Help!
 
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  • #2
Better check the calc for frequency in (b); looks like you inverted it or something.
Yes, the speed changes as the water gets shallow.
The amplitude is related to the power and energy of the wave. It says energy is conserved, so you must have the same power in the shallow wave as in the ocean wave. If you don't have a formula for water wave power, you might check
http://en.wikipedia.org/wiki/Wave_power
The power depends on the period and amplitude, so if power stays constant amplitude will change when it goes shallow.
 
Last edited:

1. What is a tsunami?

A tsunami is a series of large waves caused by a sudden disturbance on the ocean floor, such as an earthquake, volcanic eruption, or underwater landslide.

2. How do tsunamis form?

Tsunamis form when a large amount of water is displaced and moves rapidly, creating a series of waves that can travel long distances across the ocean.

3. What are the destructive effects of a tsunami?

Tsunamis can cause widespread devastation, including flooding, strong currents, and destruction of buildings and infrastructure near the coast. They can also lead to loss of life and displacement of communities.

4. How can we prepare for a tsunami?

It is important to have an emergency plan in place and to be aware of evacuation routes in case of a tsunami. In areas prone to tsunamis, warning systems and drills are often in place to help people prepare for and respond to a tsunami.

5. How can scientists predict tsunamis?

Scientists use a variety of methods, including seismometers, tide gauges, and ocean buoys, to detect and measure seismic activity and changes in sea level that could indicate a potential tsunami. This data is then used to create models and forecasts to predict when and where a tsunami may occur.

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