Graphing sound waves at the bottom of the ocean

In summary, sonar is used to measure the distance to the ocean bottom by sending a pulse of sound waves and listening for the echo. The graph provided shows the delay time as the ship crosses 60 km of ocean, with the ocean bottom having negative values of y. The average speed of sound in ocean water is 1500 m/s.
  • #1
MyNewPony
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Homework Statement



Ships measure the distance to the ocean bottom with sonar. A pulse of sound waves is aimed at the ocean bottom, then sensitive microphones listen for the echo. The graph shows the delay time as a function of the ship's position as it crosses 60 km of ocean.

Draw a graph of the ocean bottom. Let the ocean surface define y = 0 and ocean bottom have negative values of y. This way your graph will be a picture of the ocean bottom. The speed of sound in ocean water varies slightly with temperature, but you can use 1500 m/s as an average value.

http://session.masteringphysics.com/problemAsset/1071083/10/20.P46.jpg

Homework Equations



v = d/t

The Attempt at a Solution



I'm not how to interpret the graph given. Do the time values represent how long it takes for the waves to get to the bottom? Or do they represent how long it takes for the waves to reach the bottom and echo back?
 
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  • #2
MyNewPony said:
Or do they represent how long it takes for the waves to reach the bottom and echo back?

Doesn't it say:
ProblemStatement said:
A pulse of sound waves is aimed at the ocean bottom, then sensitive microphones listen for the echo.
 
  • #3
If it is the latter, then the distance from the ship to the ocean bottom can be calculated by multiplying the time by the speed of sound in water. This would result in a graph with negative values for y, as instructed. However, if it is the former, then the graph would show the distance from the ship to the ocean bottom directly, with no need for calculations. Either way, the graph would show a gradual decrease in the distance as the ship moves across the ocean, indicating a gradual sloping of the ocean bottom. The varying time values could also indicate changes in the depth of the ocean bottom, as the ship may encounter different types of terrain or structures along its path. Additional data and measurements would be needed to accurately determine the shape and features of the ocean bottom.
 

Related to Graphing sound waves at the bottom of the ocean

What is the purpose of graphing sound waves at the bottom of the ocean?

The purpose of graphing sound waves at the bottom of the ocean is to study the characteristics of underwater sound propagation. This can provide valuable information about the ocean environment, marine life, and potential sources of noise pollution.

How are sound waves graphed at the bottom of the ocean?

To graph sound waves at the bottom of the ocean, scientists use a hydrophone, which is a specialized microphone that can detect and record underwater sound. The hydrophone is lowered to the ocean floor and connected to a recording device, which produces a graph of the sound waves.

What can be learned from graphing sound waves at the bottom of the ocean?

By graphing sound waves at the bottom of the ocean, scientists can learn about the speed, intensity, and direction of sound propagation. They can also identify different types of sounds, such as marine animal calls, ship noise, or natural phenomena. This information can help us better understand the ocean and its inhabitants.

How do sound waves behave at the bottom of the ocean?

Sound waves at the bottom of the ocean behave differently than in air due to the differences in density and pressure. They can travel much faster and over longer distances, but can also be affected by temperature, salinity, and other properties of the water. By graphing these sound waves, scientists can better understand how they behave and interact with the ocean environment.

What are the potential uses of graphing sound waves at the bottom of the ocean?

Graphing sound waves at the bottom of the ocean has many potential uses, such as mapping the seafloor, tracking marine animals, detecting underwater earthquakes or volcanic activity, and monitoring human activities like shipping and oil exploration. This information can also aid in the development of better sonar technology and underwater communication systems.

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