Posted: February 27th, 2023

Calculating Tsunami Velocities

Assignment 3 – Calculating Tsunami Velocities – Due Monday, Feb 20 by

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0:59 am

This assignment must be completed and uploaded to the Assignments HW 3 folder on d2l NO LATER than Monday, Feb 20 at 10:59 am to get credit for assignment 3. The graph you create and a description of what the graph shows is a key part of this assignment. Please get help if you are having trouble.

We learned that it took about 15 minutes for the first tsunami waves to reach the shores of Northern Sumatra after the magnitude 9.2 earthquake that happened off the coast of Sumatra on December 24th, 2004. It created one of the most devastating tsunamis ever, killing 2

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0,000 people and decimating coastal. So how fast do tsunamis travel?

Tsunamis are what we call “barotropic gravity waves,” which means the entire water column is moving, and is driven by the acceleration due to gravity. Think of it like this: when you throw a ball up into the air, gravity acts upon it to pull it back toward the ground. Similarly, when a mass of water is pushed upward above a subduction zone, that water will be pulled back down due to gravity. But there is also an outward component, causing the water to move out in all directions, like seismic waves from an earthquake.

Here’s how we calculate how fast a tsunami will travel:

c =

where c = the speed of the tsunami, g = acceleration due to gravity (9.8 m/s2), and H is the height of the water column that is pushed up by the rebounding plate (in other words, the depth of water). To figure out how fast a tsunami will travel, one only needs to know the depth of the water in which the tsunami occurred, and plug this into the above equation as H.

Part 1. Imagine a tsunami occurs in the Pacific Ocean in water that is about 4,000 meters deep:

How fast will that tsunami travel? We must set up our equation c= . We simply plug in the value for acceleration due to gravity (g), which is a constant (see above), and the depth of the water (H). We multiply those values, then take the square root to get the velocity in m/s2. We always want to work in meters for H so it is consistent with the units of m/s2 we use for g.

Part 2. Now that you know how to calculate tsunami depth, you are going to use the table below to calculate tsunami velocities for tsunamis in various locations (note: some locations may not be places we expect tsunamis to happen – that is ok). Enter the depth in meters (remember, there are 1,000 meters in a km) and the velocities you calculate in the table. You can round to nearest whole numbers. (7 pts)

 Location Water Depth (km) Water Depth (m) Tsunami Velocity (m/s) East Pacific Rise 1.4 Mid Atlantic Ridge 2.5 West coast of Japan 1.75 Java Sea (Indonesia) .046 South China Sea 5.6 Mariana Trench 11 Indian Ocean 8

Part 3. Graph your results as a scatter plot (on graph paper or using a graphing program). Label the axes – recall the independent variable goes on the x-axis. Be sure the graph is included as part of this document when uploading to d2l. (4 pts)

Part 4. Explain the graph – what is it showing? (2 pts)

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