Practical Applications of the Doppler Effect
In the 160 years or so since Doppler first described the wave phenomenon that would cement his place in history, several practical applications of the Doppler effect have emerged to serve society. In all of these applications, the same basic thing is happening: A stationary transmitter shoots waves at a moving object. The waves hit the object and bounce back. The transmitter (now a receiver) detects the frequency of the returned waves. Based on the amount of the Doppler shift, the speed of the object can be determined. Let's look at a few specific examples.
The handheld radar guns used by police to check for speeding vehicles rely on the Doppler effect. Here's how they work:
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- A police officer takes a position on the side of the road.
- The officer aims his radar gun at an approaching vehicle. The gun sends out a burst of radio waves at a particular frequency.
- The radio waves strike the vehicle and bounce back toward the radar gun.
- The radar gun measures the frequency of the returning waves. Because the car is moving toward the gun, the frequency of the returning waves will be higher than the frequency of the waves initially transmitted by the gun. The faster the car's speed, the higher the frequency of the returning wave.
- The difference between the emitted frequency and the reflected frequency is used to determine the speed of the vehicle. A computer inside the gun performs the calculation instantly and displays a speed to the officer.
Meteorologists use a similar principle to read weather events. In this case, the stationary transmitter is located in a weather station and the moving object being studied is a storm system. This is what happens:
- Radio waves are emitted from a weather station at a specific frequency.
- The waves are large enough to interact with clouds and other atmospheric objects. The waves strike objects and bounce back toward the station.
- If the clouds or precipitation are moving away from the station, the frequency of the waves reflected back decreases. If the clouds or precipitation are moving toward the station, the frequency of the waves reflected back increases.
- Computers in the radar electronically convert Doppler shift data about the reflected radio waves into pictures showing wind speeds and direction.
Doppler images are not the same as reflectivity images. Reflectivity images also rely on radar, but they are not based on changes in wave frequency. Instead, a weather station sends out a beam of energy, then measures how much of that beam is reflected back. This data is used to form the precipitation intensity images we see all the time on weather maps, where blue is light precipitation and red is heavy precipitation.
A traditional echocardiogram uses sound waves to produce images of the heart. In this procedure, a radiologist uses a transducer to transmit and receive ultrasound waves, which are reflected when they reach the edge of two structures with different densities. The image produced by an echocardiogram shows the edges of heart structures, but it cannot measure the speed of blood flowing through the heart. Doppler techniques must be incorporated to provide this additional information. In a Doppler echocardiogram, sound waves of a certain frequency are transmitted into the heart. The sound waves bounce off blood cells moving through the heart and blood vessels. The movement of these cells, either toward or away from the transmitted waves, results in a frequency shift that can be measured. This helps cardiologists determine the speed and direction of blood flow in the heart.