Also found in: Dictionary, Thesaurus, Medical, Wikipedia.


chromosphere (krōˈməsfērˌ) [Gr.,=color sphere], layer of rarefied, transparent gases in the solar atmosphere; it measures 6,000 mi (9,700 km) in thickness and lies between the photosphere (the sun's visible surface) and the corona (its outer atmosphere).

Composition and Characteristics of the Chromosphere

The flash spectrum has been a valuable tool in the study of the chromosphere. This spectrum is obtained before a solar eclipse reaches totality and is formed from the thin arc of the sun disappearing behind the moon's disk. An analysis of the emission lines gives information about the heights of the chromosphere and the heights at which various elements exist in it. Using the flash spectrum, scientists have found that the chromosphere is composed primarily of hydrogen, which causes its visible pinkish tint, and of sodium, magnesium, helium, calcium, and iron in lesser amounts. The chromosphere consists of three distinct layers that, moving outward from the sun's surface, decrease in density and increase abruptly in temperature. The lower chromosphere is about 10,800℉ (6,000℃), the middle rises to 90,000℉ (50,000℃), and the upper part, merging into the lower corona, reaches 1,800,000℉ (1,000,000℃).

Solar Activity Originating in the Chromosphere

Spicules and Plages

At 600 mi (1,000 km) above the photosphere, the chromosphere separates into cool, high-density columns, called spicules, and hot, low-density material. The spicules, each about 500 mi (800 km) in diameter, shoot out at 20 mi per sec (32 km per sec) and rise as high as 10,000 mi (16,000 km) before falling back. Any point on the sun will erupt a spicule about once every 24 hr and there may be up to 250,000 of them at any instant.

Other types of solar activity are found to occur in the chromosphere. The elements of each layer are sometimes distributed in bright, cloudlike patches called plages, or flocculi, and in general are located along the same zones as sunspots and fluctuate with the same 11-yr cycle; the relationship between the two is not yet understood.

Quiescent and Eruptive Prominences

Most spectacular of the solar features are the streams of hot gas, called prominences, that shoot out thousands or even hundreds of thousands of miles from the sun's surface at velocities as great as 250 mi per sec (400 km per sec). Two major classifications are the quiescent and the eruptive prominences. Quiescent prominences bulge out from the surface about 20,000 mi (32,000 km) and can last days or weeks. Eruptive prominences are thin flames of gas often reaching heights of 250,000 mi (400,000 km); they occur most frequently in the zones containing sunspots. Dark strandlike objects called filaments were discovered on the disk and were originally thought to be a special kind of feature. These are now known to be prominences seen against the bright background of the photosphere.

Until the middle of the 19th cent. prominences could be viewed extending from the edge of the sun's disk only during a solar eclipse. However, in 1868 a method of observing them with a spectroscope at any clear time of day was developed, and in 1930 the invention of the coronagraph allowed them to be continuously photographed.

Solar Flares

Another phenomenon occurring in the chromosphere is the solar flare, a sudden and intense brightening in a plage that rises to great brilliance in a few minutes, then fades dramatically in a half hour to several hours. This feature is also associated with sunspots and is thought to be triggered by the sudden collapse of the magnetic field in the plage. A flare releases the energy equivalent of a billion hydrogen bombs and is the most energetic of solar events. The ultraviolet and X-ray radiation from larger flares can disrupt magnetic compasses and navigation and radio signals as well as affect the electrical grid on the earth and can damage satellites and space probes. Cosmic rays and solar wind particles from some flares interact in the polar regions, creating brilliant auroral displays (see aurora).
The Columbia Electronic Encyclopedia™ Copyright © 2022, Columbia University Press. Licensed from Columbia University Press. All rights reserved.


(kroh -mŏ-sfeer) The stratum of a star's atmosphere immediately above the photosphere and below the corona. The chromosphere is considerably less dense than the photosphere, and its gases are characterized by an emission rather than an absorption spectrum. The best-studied chromosphere is that of the Sun.

In the solar chromosphere the temperature rises over a few thousand kilometers from about 4000 K at the temperature minimum to around 50 000 K at the transition region (see Sun). The rise in temperature (which continues in the transition region and inner corona) was once thought to be the result of ascending shock waves, but this mechanism does not tally with detailed observations of the coronae of the Sun and other stars. It is now believed that magnetic heating is responsible (see corona).

The solar chromosphere is visible under natural circumstances only when the photosphere is totally eclipsed by the Moon (see eclipse). It is then seen in profile at the Sun's limb. It may, however, be observed at times other than totality with the aid of a spectroheliograph/spectrohelioscope or a telescope equipped with a suitable narrow-band interference filter. See also chromospheric network; flash spectrum; spicules.

Chromospheres of other stars are studied by observing their strong ultraviolet emission lines or the narrow optical emission lines seen in the center of their photospheric broad absorption lines. In many stars of similar spectral type to the Sun, the chromospheric emission changes with a period of several years, indicating the presence of a cycle of activity akin to the solar cycle (see sunspot cycle). Chromospheric brightness is related to speed of rotation, being greater for stars that rotate rapidly (either because they are young or because of the effect of a companion – see RS Canum Venaticorum star).

Collins Dictionary of Astronomy © Market House Books Ltd, 2006


A transparent, tenuous layer of gas that rests on the photosphere in the atmosphere of the sun.
McGraw-Hill Dictionary of Scientific & Technical Terms, 6E, Copyright © 2003 by The McGraw-Hill Companies, Inc.


Astronomy a gaseous layer of the sun's atmosphere extending from the photosphere to the corona and visible during a total eclipse of the sun
Collins Discovery Encyclopedia, 1st edition © HarperCollins Publishers 2005
References in periodicals archive ?
During a solar eclipse, the flash spectrum associated with the chromosphere of the Sun becomes readily visible [2-5].
While hydrogen-[alpha] emissions are responsible for the red glow of the chromosphere visible during an eclipse, this region of the Sun also emits a weak continuous spectrum [56] which has drawn the attention of solar observers for more than 100 years [140-147].
In order to further increase this scale height to the levels observed, it was hypothesized that the chromosphere had to be heated, either through turbulent motion, wave motion, magnetic fields, or 5-minute oscillations [277, p.
I watched it thus, for over a minute,' he later wrote, 'but it gradually merged into the background darkness as it moved farther away, and was irretrievably lost just before 13h.19m.' The explanation, he proposed, 'would seem to be that the planet was being projected against a low intensity suffusion of light (not visually apparent) from the lower chromosphere.' (12)
Models based on this picture successfully predict the intensity and color of light emitted by a variety of atoms in the sun's chromosphere. But they cannot readily match measurements of the intensity of certain wavelengths of infrared light emitted by carbon monoxide molecules.
It's unclear whether they are a new type of blast or a hotter analog to "Ellerman bombs," which are created when a small, U-shaped magnetic loop in the chromosphere dips down into the photosphere, pinches off, and dumps its energy.
Since then, great attention has been given to identifying the lines which are contained within the flash spectrum of the chromosphere, particularly through the efforts of astronomers like John Evershed [9,10] and Donald Menzel [11,12].
Other satellites include SOHO, the Solar and Heliospheric Observatory, which has been operating for 15 years, observing the chromosphere (a thin outer layer of the Sun's atmosphere) the corona and the transition region between the two.
Usually comets do not survive because of the Sun's over powering heat but this one apparently did, and disappeared in the chromosphere, evaporating in the 100,000-degree (Kelvin) heat.
it may also lift charged particles from the sun's dense lower atmosphere, or chromosphere. These particles fill the series of closely spaced magnetic loops that form an arcade high in the corona.