Gravitational wave detection measures spacetime ripples using instruments like LISA to test general relativity.Gravitational wave detection involves measuring tiny ripples in spacetime caused by massive accelerating objects, such as merging black holes or neutron stars. These ripples were predicted by Einstein's general relativity in 1916 and were first directly detected in 2015 by the LIGO observatories. The detection of gravitational waves has opened a new window on the universe, allowing us to observe events that emit no light, such as black hole mergers, and to test general relativity under extreme conditions.
The first direct detection of gravitational waves was announced in 2016 by the LIGO Scientific Collaboration, from a binary black hole merger. The concept of using interferometry was pioneered in the 1960s, and the idea for LISA was proposed in the 1980s.
Gravitational waves stretch and compress spacetime as they pass, changing the distances between test masses. Detectors like LIGO and Virgo use laser interferometry: a laser beam is split and sent down two perpendicular arms, reflected by mirrors, and recombined. A passing gravitational wave causes a tiny difference in the arm lengths (on the order of 10^-18 meters), which shows up as a change in the interference pattern. Space-based detectors like LISA will use the same principle but with much longer arms (millions of kilometers) to detect lower-frequency waves from sources like supermassive black hole mergers.
Gravitational wave detectors are used to study astrophysical phenomena like black hole mergers, neutron star collisions, and supernovae, and to measure the expansion rate of the universe (the Hubble constant) independently of other methods.
The LIGO detectors are so sensitive that they can measure a change in distance smaller than the size of a proton over a 4-kilometer arm length.

















