Radio Propagation Codexery

Doppler effect

Frequency shift due to relative motion between source and observer.

Doppler effect

The Doppler effect (also called Doppler shift) describes how the frequency or period of a wave changes for an observer who is moving relative to the wave’s source. Christian Doppler first proposed the idea in 1842. A familiar example is the change in pitch of a vehicle’s sound as it approaches and then moves away: the pitch is higher during approach, the same at the moment it passes, and lower as it recedes.

When a sound source moves toward an observer, each successive wave cycle starts from a point closer to the observer than the last. This shortens the time between cycles, raising the frequency. If the source moves away, each cycle starts from a farther point, lengthening the time between cycles and lowering the frequency.

For waves that travel through a medium—like sound—the motion of the observer, the source, and the medium all matter. For waves that travel in a vacuum, such as electromagnetic or gravitational waves, only the relative velocity between observer and source is relevant.

The relationship between observed frequency and emitted frequency for waves in a medium depends on the wave’s speed in that medium, the receiver’s speed relative to the medium, and the source’s speed relative to the medium. If the receiver moves toward the source, its speed is added to the wave speed; if away, subtracted. If the source moves toward the receiver, its speed is subtracted from the wave speed; if away, added. The observed frequency decreases as the distance between source and receiver increases. The wave’s speed is set by the medium, not by the source’s motion.

If a source approaches an observer at an angle, the observed frequency starts higher than the emitted frequency, then decreases steadily as the source gets closer. It becomes equal to the emitted frequency when the source is perpendicular to the line of sight (though the wave was emitted at the closest point, and by the time it is received, the source and observer are no longer at that point). The frequency continues to drop as the source recedes. When the observer is very close to the source’s path, the shift from high to low pitch is abrupt; when far from the path, the shift is gradual.

If a stationary observer faces a wave source moving at or above the wave’s speed, the Doppler equation gives an infinite or negative frequency, so it does not apply.

Named after
Christian Doppler
Year proposed
1842
First tested for sound
1845
Tested by
Buys Ballot
Independently discovered for electromagn
1848
Discoverer of electromagnetic effect
Hippolyte Fizeau
Experimental study in britain
John Scott Russell (1848)

Lore & Background

Christian Doppler first proposed the effect in 1842 in his treatise 'Über das farbige Licht der Doppelsterne und einiger anderer Gestirne des Himmels' (On the coloured light of the binary stars and some other stars of the heavens). The hypothesis was tested for sound waves by Buys Ballot in 1845, who confirmed that the pitch was higher when the source approached and lower when it receded. Hippolyte Fizeau independently discovered the same phenomenon on electromagnetic waves in 1848; in France, the effect is sometimes called 'effet Doppler-Fizeau', though that name was not adopted elsewhere. In Britain, John Scott Russell made an experimental study of the Doppler effect in 1848.

For waves propagating in a medium such as sound, the observed frequency depends on the velocities of the source and receiver relative to that medium. The relationship is given by a formula where the observed frequency changes based on whether the source and receiver are moving toward or away from each other. If the source approaches the observer at an angle, the observed frequency decreases monotonically from a higher pitch through equality when perpendicular to the motion, to a lower pitch as it recedes. When the observer is very close to the path, the transition is abrupt; when far, it is gradual.

If the source moves at or above the wave speed, the Doppler equation predicts an infinite or negative frequency and becomes inapplicable. For sound, a source moving faster than the speed of sound creates a shock wave and a sonic boom. Lord Rayleigh predicted that if an observer moved from a stationary source at twice the speed of sound, a musical piece would be heard in correct tempo and pitch but played backwards.

Reader's Guide

The Doppler effect has significant practical applications across multiple fields. In astronomy, it is used to measure the speed at which stars and galaxies approach or recede, producing blueshift or redshift. This allows detection of binary stars, measurement of rotational speeds, and discovery of exoplanets. The effect typically occurs on a very small scale, not noticeable to the unaided eye. Among nearby stars, the largest radial velocities relative to the Sun are +308 km/s (receding) and −260 km/s (approaching). The cosmological redshift of the expanding universe is considered separate from Doppler motion or gravitational redshifts.

In radar, the Doppler effect is used to measure the velocity of moving objects, such as cars detected by police radar guns. A radar beam fired at a moving target experiences a wavelength change: increasing when the target recedes, decreasing when it approaches. For example, a police radar operating at 24.15 GHz detecting a vehicle at 30 m/s measures a Doppler shift of about 4.83 kHz. The proximity fuze, developed during World War II, relies on Doppler radar to detonate explosives at the correct time.

A common everyday example is the siren of a passing emergency vehicle, which sounds higher in pitch when approaching and lower when receding. The pitch remains constant if the vehicle approaches directly, then jumps to a lower pitch upon passing. The radial speed varies with the angle between the line of sight and the vehicle's velocity.

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