Tiny fluctuations in a star's brightness and surface, akin to a bell ringing, used for asteroseismology.Stellar oscillation refers to the natural resonant vibrations of a star, similar to how a bell rings after being struck. These oscillations cause tiny periodic changes in a star's brightness, surface velocity, and temperature. By studying these oscillations, astronomers can infer the internal structure and composition of stars, a field known as asteroseismology.
The first solar oscillations were detected in the 1960s by Robert Leighton and colleagues, and the field of asteroseismology expanded to other stars in the 1990s with space missions like WIRE and later CoRoT and Kepler.
Oscillations are driven by internal processes such as convection, magnetic activity, or tidal forces from companions. They propagate through the star as sound waves (p-modes) or surface gravity waves (g-modes). The frequencies of these modes depend on the star's density, temperature, and rotation, allowing astronomers to model its interior like a musical instrument.
Asteroseismology is used to determine the ages, masses, and radii of stars, which is crucial for calibrating stellar evolution models and characterizing exoplanet host stars.
The Sun oscillates with a dominant period of about 5 minutes, and these oscillations can be used to map the Sun's internal rotation profile.




