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Solar corona

Outermost layer of the Sun's atmosphere

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Total Solar eclipse in France.
Luc Viatour · CC BY-SA 3.0

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Through Sun, Solar wind and Spectroscopy

The solar corona lies above the photosphere and chromosphere and extends out to the edge of the solar atmosphere where it merges with the solar wind. The chromosphere and corona are separated by a thin, highly dynamic transition region. The outer edge of solar atmosphere where the corona transitions into the solar wind is defined by the Alfvén surface which forms an irregularly shaped boundary around the Sun at heights ranging from about 10 to 20 solar radii (7000000 to 14000000 km) above the photosphere.

Coronal light is typically obscured by diffuse sky radiation and glare from the solar disk, but can be easily seen by the naked eye when the sun is completely or totally blocked in a solar eclipse, or with a specialized coronagraph. Spectroscopic measurements indicate strong ionization in the corona and a plasma temperature in excess of 1000000 kelvins, much hotter than the surface of the Sun.

The solar corona is populated by structures such as prominences, coronal loops, and helmet streamers.

Observational history

In 1724, French-Italian astronomer Giacomo F. Maraldi recognized that the aura visible during a solar eclipse belongs to the Sun, not to the Moon. In 1809, Spanish astronomer José Joaquín de Ferrer published his own observations of the solar eclipse that happened three years earlier at Kinderhook, New York and also proposed that the corona was part of the Sun and not of the Moon; his reports is where the term 'corona' first appears coined by himself.

English astronomer Norman Lockyer identified the first element unknown on Earth in the Sun's chromosphere, which was called helium (from Greek helios 'sun'). French astronomer Jules Jenssen noted, after comparing his readings between the 1871 and 1878 eclipses, that the size and shape of the corona changes with the sunspot cycle. In 1930, Bernard Lyot invented the "coronograph" (now "coronagraph"), which allows viewing the corona without a total eclipse. In 1952, American astronomer Eugene Parker proposed that the solar corona might be heated by myriad tiny nanoflares, miniature brightenings resembling solar flares that would occur all over the surface of the Sun.

The high temperature of the Sun's corona gives it unusual spectral features, which led some in the 19th century to suggest that it contained a previously unknown element, "coronium". Instead, these spectral features have since been explained by highly ionized iron (Fe-XIV, or Fe13+). Bengt Edlén, following the work of Walter Grotrian in 1939, first identified the coronal spectral lines in 1940 (observed since 1869) as transitions from low-lying metastable levels of the ground configuration of highly ionised metals (the green Fe-XIV line from Fe13+ at 5303Å, but also the red Fe-X line from Fe9+ at 6374Å).

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