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Comet tail

A comet tail is a projection of material from a comet that often becomes visible when illuminated by the Sun, while the comet passes through the inner Solar System. As a comet approaches the Sun, solar radiation causes the volatile materials within the comet to vaporize and stream out of the comet nucleus, carrying dust away with them.

Tail formation
In the outer Solar System, comets remain frozen and are extremely difficult or impossible to detect from Earth due to their small size. Statistical detections of inactive comet nuclei in the Kuiper belt have been reported from the Hubble Space Telescope observations, but these detections have been questioned, and have not yet been independently confirmed. As a comet approaches the inner Solar System, solar radiation causes the volatile materials within the comet to vaporize and stream out of the nucleus, carrying dust away with them. The streams of dust and gas thus released form a huge, extremely tenuous atmosphere around the comet called the coma, and the force exerted on the coma by the Sun's radiation pressure and solar wind cause an enormous tail to form, which points away from the Sun. The streams of dust and gas each form their own distinct tails, pointing in slightly different directions. The tail of dust is left behind in the comet's orbit in such a manner that it often forms a curved tail called the antitail, only when it seems that it is directed towards the Sun. At the same time, the ion tail, made of gases, always points along the streamlines of the solar wind as it is strongly affected by the magnetic field of the plasma of the solar wind. The ion tail follows the magnetic field lines rather than an orbital trajectory. Parallax viewing from the Earth may sometimes mean the tails appear to point in opposite directions. == Size ==
Size
While the solid nucleus of comets is generally less than 30 km across, the coma may be larger than the Sun, and ion tails have been observed to extend . == Structure of the ion tail ==
Structure of the ion tail
with its tail as seen in October 2025 The structure of the ion tail is the result of complex interactions between the Sun and the comet. Ultraviolet radiation ionize molecules in the coma, forming plasma which in turn induces a magnetosphere around the comet. The comet and its induced magnetic field form an obstacle to solar wind particles. The comet is supersonic relative to the solar wind, so a bow shock is formed upstream of the comet (i.e. facing the Sun), in the flow direction of the solar wind. In this bow shock, large concentrations of cometary ions (called "pick-up ions") congregate and act to "load" the solar magnetic field with plasma. The field lines "drape" around the comet forming the ion tail. == Tail loss ==
Tail loss
If the ion tail loading is sufficient, then the magnetic field lines are squeezed together to the point where, at some distance along the ion tail, magnetic reconnection occurs. This leads to a "tail disconnection event". This event was observed by the STEREO spacecraft. A disconnection event was also seen with C/2009 R1 (McNaught) on May 26, 2010. == Analogues ==
Analogues
Venus possesses a similar tail due to the induced magnetosphere formed by interaction of the solar wind with the venusian atmosphere. On January 29, 2013, ESA scientists reported that the ionosphere of the planet Venus streams outwards in a manner similar to "the ion tail seen streaming from a comet under similar conditions." While Mercury lacks an atmosphere, the MESSENGER mission observed magnesium and sodium flowing off the planet, along the magnetic field lines trailing behind the planet, making them the primary components of Mercury's magnetotail. == Anti-tail ==
Anti-tail
The anti-tail is a needle-like feature that sometimes appears to extend from the coma towards the Sun, and therefore in the opposite direction to the gas and dust tails. The anti-tail typically consists of older dust particles ejected from the nucleus in the preceding weeks which remain close to the comet's orbital plane, forming a thin sheet of material. This material is normally too faint to be observed, but as Earth passes through the plane, the sheet is seen side-on and briefly becomes visible. Under favorable viewing conditions, the relative position of Earth, Sun, and the comet is such that part of the sheet is optically projected in front of the coma, appearing as the characteristic sunward spike. Most comets do not develop sufficiently for an anti-tail to become visible, but notable comets that did display anti-tails include Arend–Roland in 1957, Kohoutek in 1973, Hale–Bopp in 1997, C/1999 H1 (Lee) in 1999, Lulin in 2009, PANSTARRS and C/2022 E3 (ZTF) in 2023, 12P/Pons–Brooks and C/2023 A3 Tsuchinshan–ATLAS in 2024, and 3I/ATLAS in 2025. == References ==
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