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Comet tail

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Subject: Halley's Comet, Comet, Comets, Antitail, 209P/LINEAR
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Comet tail

Diagram of a comet showing the dust trail, the dust tail (or antitail) and the ion gas tail, which is formed by the solar wind flow. NASA
Comet Holmes (17P/Holmes) in 2007 showing blue ion tail on right
Comet Lovejoy from orbit

A comet tail and coma are illuminated by the Sun and may become visible from Earth when a comet passes through the inner Solar System, the dust reflecting sunlight directly and the gases glowing from ionisation. Most comets are too faint to be visible without the aid of a telescope, but a few each decade become bright enough to be visible to the naked eye.

The streams of dust and gas each form their own distinct tail, 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.[1]

While the solid nucleus of comets is generally less than 50 km across, the coma may be larger than the Sun, and ion tails have been observed to extend 3.8 astronomical units (570 million km, or 355 million mi).[2] The observation of antitails contributed significantly to the discovery of solar wind.[3] The ion tail is the result of ultraviolet radiation ejecting electrons off particles in the coma. Once the particles have been ionised, they form a plasma which in turn induces a magnetosphere around the comet. The comet and its induced magnetic field form an obstacle to outward flowing 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.[4] (This is similar to the formation of planetary magnetospheres.)

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."[5][6]

Tail formation

A comet's orbit showing the different directions of the gas and dust tails as the comet passes the Sun

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,[7][8] but these detections have been questioned,[9][10] 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.

Tail loss

Comet Encke loses its tail

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".[4] This has been observed on a number of occasions, notable among which was on the 20th. April 2007 when the ion tail of comet Encke was completely severed as the comet passed through a coronal mass ejection.[11] This event was observed by the STEREO spacecraft.[12] A disconnection event was also seen with C/2009 R1 (McNaught) on May 26, 2010.[13]


  1. ^ McKenna, M. (20 May 2008). "Chasing an Anti-Tail". "Astronomy Sketch of the Day". Retrieved 2009-02-25. 
  2. ^ Yeomans, Donald K. (2005). "Comet". World Book Online Reference Center.  
  3. ^ Biermann, L. (1963). "The plasma tails of comets and the interplanetary plasma".  
  4. ^ a b Carroll, B. W.; Ostlie, D. A. (1996). An Introduction to Modern Astrophysics.  
  5. ^ Staff (January 29, 2013). "When A Planet Behaves Like A Comet".  
  6. ^ Kramer, Miriam (January 30, 2013). "Venus Can Have 'Comet-Like' Atmosphere".  
  7. ^ Cochran, A. L.; Levison, H. F.; Stern, S. A.; Duncan, J. (1995). "The Discovery of Halley-sized Kuiper Belt Objects Using the Hubble Space Telescope".  
  8. ^ Cochran, A. L.; Levison, H. F.; Tamblyn, P.; Stern, S. A.; Duncan, J. (1998). "The Calibration of the Hubble Space Telescope Kuiper Belt Object Search: Setting the Record Straight".  
  9. ^ Brown, Michael E.; Kulkarni, S. R.; Liggett, T. J. (1997). "An Analysis of the Statistics of the Hubble Space Telescope Kuiper Belt Object Search".  
  10. ^  
  11. ^ "The Sun Rips Off a Comet's Tail". Science@NASA. 2007-10-01. Retrieved 2009-10-20. 
  12. ^ Eyles, C. J.; Harrison, R. A.; Davis, C. J.; Waltham, N. R.; Shaughnessy, B. M.; Mapson-Menard, H. C. A.; Bewsher, D.; Crothers, S. R.; Davies, J. A.; Rochus, P. (2009). "The Heliospheric Imagers Onboard the STEREO Mission".  
  13. ^ "Comet C/2009 R1 (McNaught) - Animation & Images". Remanzacco Observatory. May 30, 2010. Retrieved 2011-06-07. 

External links

  • Comets at DMOZ
  • Comets Page at NASA's Solar System Exploration
  • Source of useful comet-related material on the Web
  • Did you know that if you condensed the entire 100 thousand mile long tail of a comet such as Hale-Bopp to the density of water, it would not even fill a swimming pool?
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