The branch of astrophysics that investigates the interior structure of the Sun by
studying its surface wave oscillations. See also
→ asteroseismology and → stellar pulsation.
The surface of the Sun vibrates much like a bell.
A piano has 88 keys or musical tones, whereas the Sun has millions of notes.
These vibrations are the result of internal pressure waves that reflect
off the → photosphere and repeatedly cross the solar interior. They are
detected through the → Doppler shift
of absorption lines formed in the photosphere.
Because these vibrations make the solar surface move up and down,
analysis of the surface patterns is used to study conditions far below the
Sun’s surface. The mean period of the vibrations is about five minutes, which corresponds
to a speed of 0.5 km s-1 or a frequency of about 3 mHz.
See also → p mode.
Etymology (EN): From → helio- + → seismology.