The oscillation rate of gravitational waves, which can reveal properties of the emitting source.Gravitational wave frequency is the rate at which the ripples in spacetime oscillate as they pass a detector. These waves are produced by accelerating massive objects, such as merging black holes or neutron stars, and their frequency is directly tied to the motion of the source. For example, a binary system of two compact objects spiraling together emits waves whose frequency increases as the orbit shrinks, eventually sweeping upward in a characteristic 'chirp' before the merger.
The concept was central to predictions made by Albert Einstein in 1916, but the first direct detection of gravitational waves with a measurable frequency occurred in 2015 by the LIGO collaboration.
The frequency of a gravitational wave is set by the orbital or rotational period of the emitting system. For a binary, the wave frequency is twice the orbital frequency, and it evolves as the system loses energy through radiation. Detectors like LIGO measure the stretching and squeezing of space, and by tracking how the frequency changes over time, physicists can infer the masses, spins, and distance of the sources.
Gravitational wave frequency analysis is used to identify and characterize astrophysical events, enabling multi-messenger astronomy and tests of general relativity.
The frequency of gravitational waves from the first detected merger, GW150914, swept from about 35 Hz to 250 Hz in less than a second, corresponding to a pitch audible to humans if converted to sound.










