Күн бетіндегі ұзын тіл тәрізді құрылымдар

Structure extending off of the Sun's surface

In solar physics, a prominence, sometimes referred to as a filament,efn|When viewed against the background of space (off limb), they are referred to as prominences; when viewed against the Sun's surface (on disk), they are referred to as filaments. roughly of solar radius.

The first detailed description of a solar prominence was in 14th century Laurentian Codex, describing the solar eclipse of May 1, 1185. They were described as "flame like tongues of live embers". Prominences were first photographed during the solar eclipse of July 18, 1860, by Angelo Secchi. From these photographs, altitude, emissivity, and many other important parameters were able to be derived for the first time. During the solar eclipse of August 18, 1868, spectroscopes were for the first time able to detect the presence of emission lines from prominences. The detection of a hydrogen line confirmed that prominences were gaseous in nature. Pierre Janssen was also able to detect an emission line corresponding to an at the time unknown element now known as helium. The following day, Janssen confirmed his measurements by recording the emission lines from the now unobstructed Sun, a task that had never been done before. Using his new techniques, astronomers were able to study prominences daily.

Historically, any feature that was visible extending above the surface of the sun, including solar spicules, coronal loops, and some coronal mass ejections, was considered a solar prominence. Today, due to a better understanding of the diversity of these phenomena, most of these are classified separately, and the word prominence is primarily used to refer to larger and cooler features. There are a number of different prominence classification schemes in use today. One of the most widely used and basic schemes classifies prominences based on the magnetic environment in which they had formed. There are three classes:
Active region prominences, or active region filaments, form within the relatively strong magnetic fields at the centers of active regions. Active region prominences have lifetimes ranging from hours to days and erupt more often than prominences belonging to the other classes. As a consequence of being located within active regions, active region prominences are usually found in low heliographic latitudes. Intermediate prominences, or intermediate filaments, form between a weak unipolar plage regions and active regions. Quiescent prominences, or quiescent filaments, form in the weak background magnetic field far from any active regions. Unlike active region prominences, quiescent prominences are relatively stable and can have lifetimes ranging from weeks to months, hence the name quiescent.

Prominences form in magnetic structures known as filament channels where they are thermally shielded from the surrounding corona and supported against gravity. These channels are found in the chromosphere and lower corona above divisions between regions of opposite photospheric magnetic polarity known as polarity inversion lines (PIL). The presence of a filament channel is a necessary condition for the formation of a prominence, but a filament channel can exist without containing a prominence. Multiple prominences may form and erupt from within one filament channel over the channel's lifetime. The magnetic field making up the filament channel is predominantly horizontal, pointing in the same direction on both sides of the PIL (see ). Prominence material does not occupy the entire width of the filament channel; a tunnel like region less dense than the corona, known as a coronal cavity, occupies the volume between the prominence and the overlying magnetic arcade. These streamers may reach a solar radius or more above the Sun's surface. At least 70% of prominence eruptions are associated with an ejection of coronal material into the solar wind known as a coronal mass ejection.