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Doppler effect

(PD) Image: John R. Brews
Boat traveling against waves experiences Doppler effect.

The Doppler effect (or Doppler shift, or Doppler's principle), named after Christian Doppler who proposed it in 1842, is the change in frequency of a wave for an observer moving relative to the source of the wave. It is commonly heard when a vehicle sounding a siren or horn approaches, passes, and recedes from an observer. The received frequency is higher (compared to the emitted frequency) during the approach, it is identical at the instant of passing by, and it is lower during the recession.

The relative increase in frequency can be explained using the figure. Waves blowing ashore with velocity c are spaced a distance λ apart. The frequency with which a crest appears at a fixed location is f_w:

$f_{w}=c/\lambda \ .$

The boat going to sea is running at velocity v in the opposite direction to the waves. Consequently the boat moves relative to the crests at a speed v+c. That means a crest is met at intervals of time τ:

$\lambda =(v+c)\tau \ .$

In other words, the frequency with which the boat bumps over a crest f_b is:

$f_{b}={\frac {1}{\tau }}={\frac {1}{\lambda /(v+c)}}=f_{w}{\frac {v+c}{c}}=f_{w}\left(1+{\frac {v}{c}}\right)\ .$

so evidently f_b is a higher frequency than the frequency f_w of the waves themselves. This increase in frequency is the Doppler effect, and it is often expressed as the shift in frequency f_d, the Doppler shift, namely:

$f_{d}=f_{b}-f_{w}=f_{w}{\frac {v}{c}}\ .$

Of course, if the boat runs inshore with the wave, the opposite happens: it takes the boat longer between crests, and the frequency with which the boat bumps over a crest is lower than the actual frequency of the waves.