AstronomyThe Sun

Layers of the Sun

Energy made in the core moves out through the radiative and convective zones to the glowing photosphere.

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From luminosity, size and temperature you know the Sun's surface is about $5800$ K and gives off $3.83 \times 10^{26}$ W. That energy is made deep inside and takes a long, slow path out. Along the way it passes through layers, each named for how energy moves through it.

The Sun from the inside out (rounded values from standard solar models and NASA).
LayerWhereTemperatureWhat happens
Corecenter to $0.25\,R_\odot$about 15 million Knuclear fusion makes the energy
Radiative zone$0.25$ to $0.7\,R_\odot$7 million to 2 million Klight carries energy out, absorbed and re-emitted again and again
Convective zone$0.7\,R_\odot$ to the surface2 million K to about 6000 Khot gas rises, cools and sinks, like boiling water
Photospherethe visible "surface," a few hundred km thickabout 5800 Klight finally escapes to space
Chromospherea thin layer above itthousands to tens of thousands of Ka reddish glow seen during eclipses
Coronamillions of km outover 1 million Kvery thin, very hot gas; the pearly halo of a total eclipse

Why it works

Energy always flows from hot to cold, outward from the 15-million-kelvin core. Deep inside, the gas is so dense that light travels only a tiny distance before being absorbed and sent off in a random direction, so energy drifts outward through the radiative zone over tens of thousands of years or more. Farther out, the gas is cool enough that light gets trapped more easily, and it becomes faster to move energy by carrying hot gas upward: convection. At the photosphere the gas is thin enough for light to fly straight out. The Sun is hot plasma all the way through; the photosphere is just the depth we can see down to.

Key idea

Core (fusion), radiative zone (energy carried by light), convective zone (energy carried by moving gas), photosphere (the visible surface), chromosphere and corona (the atmosphere). The Sun is gas all the way down, with no solid surface.
A cutaway of the Sun. The zigzag in the radiative zone stands for light's slow random walk; the loops in the convective zone are rising and sinking gas.

Worked example

Worked example: How deep is the boiling?

The convective zone starts at $0.7$ of the Sun's radius of $696{,}000$ km. How thick is it?
  1. Its thickness is $1 - 0.7 = 0.3$ of the radius.
  2. $0.3 \times 696{,}000 = 208{,}800$ km, about 16 Earths lined up across.

Answer: About $209{,}000$ km.

Common mistake

Photos make the Sun look like a ball with a crisp surface, and people often picture something solid underneath. There is no solid surface: the Sun is gas (plasma) from the corona to the center. The edge looks sharp only because the photosphere, where the gas turns from opaque to clear, is just a few hundred kilometers thick, tiny next to the Sun's radius. Check: a spacecraft falling in would never land on anything; it would just meet hotter, denser gas.
Temperature and density inside the Sun, on log scales. Both rise steeply toward the center.

Practice

Pass with 3 right answers, the last 2 in a row. Each right answer earns 1 XP.

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Sources and further reading

  • OpenStax, Astronomy 2e, section 15.1, The Structure and Composition of the Sun
  • OpenStax, Astronomy 2e, section 16.3, The Solar Interior: Theory
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