The Sun's lower atmosphere, where boiling plasma generates the electric fields.The chromosphere is the Sun's lower atmosphere, sitting just above the visible surface (the photosphere) and below the corona. It is a thin, translucent layer where plasma boils and churns, generating the electric fields that shape much of the Sun's magnetic activity. Though invisible to the naked eye except during a total solar eclipse (when it appears as a reddish rim), it is a dynamic region where temperatures rise from about 6,000 K at the bottom to over 20,000 K at the top, defying simple expectations of cooling with altitude.
The chromosphere was first observed during solar eclipses in the 19th century; its name (from Greek 'chroma', color) was coined by Angelo Secchi in the 1860s. The discovery of its spectrum's emission lines, particularly hydrogen, came later with the development of spectroscopy.
The chromosphere is heated by a combination of magnetic field interactions and mechanical waves. Convection in the photosphere pushes plasma upward, creating spicules—jets of gas that shoot into the chromosphere and beyond. These spicules, along with magnetic reconnection events, transfer energy into the chromosphere, ionizing hydrogen and making it glow in characteristic red light (the H-alpha line). The electric fields generated by this boiling plasma play a key role in driving solar activity, including flares and the heating of the corona above.
Studying the chromosphere helps predict solar flares and space weather, which can disrupt satellites, power grids, and communication systems on Earth.
The chromosphere's reddish glow during an eclipse is so bright that it was once mistaken for a planet or a hole in the Moon's shadow.















