Science Made Simple: Anatomy of Our Sun

Core

This is where the Sun generates its energy. The temperature in the core is around 15 million degrees Celsius (27 million degrees Fahrenheit). This, combined with the huge pressure and density of the plasma force hydrogen nuclei to fuse together, creating helium and releasing vast quantities of energy in the process. Every second, the Sun converts four million tonnes of matter into energy in this way, which begins a slow journey towards the surface.

Radiative zone

This is the layer above the core. Although not as dense as the core, the plasma is still packed so tightly in the radiative zone that convection cannot take place. Instead, the energy created in the core diffuses slowly through the plasma. It takes photons around 170,000 years to pass through the radiative zone: The photons travel at the speed of light, but can travel only a few millimeters at a time before they are absorbed by an atom and then re-emitted in any direction. At the top of the zone, the temperature is around two million degrees Celsius (3.6 million degrees Fahrenheit). At the base, next to the Sun’s core, the temperature is around seven million degrees Celsius (12.6 million degrees Fahrenheit).

Convective zone

This lies between the deeper, radiative zone and the photosphere. The convective zone is 200,000 km (124,000 mi) deep. While the top layer is the same temperature as the photosphere (between 4,500 – 6,000 degrees Celsius or 8,100 – 10,800 degrees Fahrenheit), the base of the convective zone reaches two million degrees Celsius. Plasma at the base of the zone is heated rapidly. This makes it buoyant and so it rises rapidly, creating a turbulent convection pattern, rather like a boiling pan of water – only 200,000 km deep and surrounding the entire Sun.

Tachocline

This is the boundary between the convective zone and the radiative zone. Below the tachocline, the Sun rotates like a solid body. Above it, the Sun rotates at different speeds according to its latitude. The change of rotation speed across the tachocline is very fast and this results in shearing forces that are thought to be important in the creation of the magnetic fields that lead to sunspots.

Photosphere

This is the visible ‘surface’ of the Sun. Almost all radiation from the Sun is emitted from this thin layer of several 100 km thickness, which lies at the upper boundary of the convection zone. It is where the energy generated in the core can finally move freely through space. The temperature of the photosphere varies from place to place but lies between 4,500 and 6,000 degrees Celsius.

Chromosphere

This is the layer above the photosphere, where the density of plasma drops dramatically. In general, the chromosphere is roughly 1000–2000 kilometers (600-1,200 miles) thick, with a temperature that rises from around 4,000 to about 25,000 degrees Celsius (7,200 to 45,000 degrees Fahrenheit). Spires of chromospheric gas, known as spicules, can reach up to a height of 10,000 km (62,00 mi).

Transition region

This is a thin, irregular layer that separates the relatively cool chromosphere from the much hotter corona. Across the transition zone, the temperature of the solar plasma soars to nearly a million degrees Celsius (1.8 million degrees Fahrenheit). While the convection zone and partly also the solar photosphere are dominated by flows that are capable of moving regions of strong magnetic flux around, the transition region and corona are dominated by the magnetic field which forces the plasma to move predominantly along field lines.

Corona

This is the Sun’s outer atmosphere and extends to millions of kilometers into outer space. It is most easily seen during a total solar eclipse. The plasma in the corona is extremely hot at more than one million degrees Celsius, yet is very rarefied. Its density is typically just one trillionth of the density of the photosphere. The solar wind originates in the corona.

Prominence

These are large structures, often thousands of kilometers in extent. They are made of tangled magnetic field lines that keep dense concentrations of solar plasma suspended above the Sun’s surface and often take the form of loops that arch up from the chromosphere. They can persist for several weeks or even months.

Solar flare

This is a sudden release of energy. A flare is usually created when the magnetic field lines that make sunspots transform themselves rapidly into more stable configurations. This is a bit like a stretched elastic band breaking and releasing all of its stored energy as it snaps back into position. The energy released by solar flares strongly influences the behavior of the solar wind.

Sunspots

These are temporary features on the photosphere. They look like dark patches against the brighter region of the photosphere because they are about 1,000 degrees cooler and so do not emit so much light. They are caused by magnetic fields breaking through the photosphere of the Sun and cooling the gas there. Sunspots can be anything from a few tens of kilometers across to larger than 150,000 km (93,000 mi).

Granulation

These are convective patterns that occur in the photosphere. Each granule is about 1,000 km (620 mi)wide and consists of hot plasma rising in its center. As it releases its energy into space, the plasma cools and this makes it flow to the sides of the granule and sink back down into the photosphere. Individual granules persist for about 20 minutes, after this new ones in slightly different places develop.

Coronal mass ejections

These are vast eruptions of billions of tonnes of plasma and magnetic fields from the Sun’s corona. They travel out from the Sun at speeds of hundreds to thousands of kilometers per second, and if sent into the pathway of the Earth, can create geomagnetic storms.

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