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{{Other|Leonid}}
{{Other|Leonid}}


The '''Leonids''' ([ˈli.əˌnɪdz] ''lee-uh-nids'') are a prolific [[meteor shower]] associated with the [[comet]] [[55P/Tempel-Tuttle|Tempel-Tuttle]]. The Leonids get their name from the location of their [[Radiant (meteor shower)|radiant]] in the [[constellation]] [[Leo (constellation)|Leo]]: the meteors appear to stream from that point in the [[sky]]. The 2009 display peaking on November 17 may produce more than 500 meteors an hour.<ref name="Meteor" /><ref>{{Cite web
The '''Leonids''' ([ˈli.əˌnɪdz] ''lee-uh-nids'') are a prolific [[meteor shower]] associated with the [[comet]] [[55P/Tempel-Tuttle|Tempel-Tuttle]]. The Leonids get their name from the location of their [[Radiant (meteor shower)|radiant]] in the [[constellation]] [[Leo (constellation)|Leo]]: the meteors appear to radiate from that point in the [[sky]]. The 2009 display peaking on November 17 may produce more than 500 meteors an hour.<ref name="Meteor" /><ref>{{Cite web
| title = Strong Leonid Meteor Shower Predicted for 2009
| title = Strong Leonid Meteor Shower Predicted for 2009
| publisher = Space.com
| publisher = Space.com
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</ref>
</ref>


[[Earth]] moves through the meteoroid stream of [[wiktionary:Particle|particles]] left from the passages of the [[comet]]. The stream comprises solid particles, known as [[meteoroid]]s, ejected by the comet as its frozen gases [[evaporate]] under the heat of the [[Sun]] which begins to warm the comet as it comes within the orbit of [[Jupiter]]. A typical particle is no bigger than fine [[dust]]. The main source of light of a [[meteor]] is caused by the solar wind, which fragments and atomizes the dust,<ref>[http://www.space.com/scienceastronomy/astronomy/leonids_science_021112.html Space.com] The Power of a Shooting Star</ref> and the resulting spray of microscopic debris collides with individual atoms of the atmosphere ionizing the air. The air molecules recombine and cool by giving off [[photons]]. Larger particles leave a stream of smaller particles and form a tail, which can leave a glowing trail in the atmosphere. Leonids in particular are well known for having such bright meteors. The meteoroids left by the comet are organized in trails in orbits similar to though different from that of the comet. They are differentially disturbed by the planets, in particular [[Jupiter]] (see also a full explanation by [http://cdsads.u-strasbg.fr/abs/1999JIMO...27...85M McNaught & Asher (1999)]). The ensemble of the trails compose the meteoroid stream. Old trails are spatially not dense and compose the meteor shower background (a few meteors per minute), happening around November 17, but changing every year.<ref>you may check every year at the [http://www.imo.net/calendar IMO website]</ref> Conversely, young trails are spatially very dense and the cause of [[meteor storms]] when the Earth enters one of these structures. Usual counts during a storm exceed 1000 meteors per hour,<ref>after correction, see: [http://www.imo.net/observations the IMO pages]</ref> to be compared to the annual background (1 to 2 meteors per hour) and the shower background (a few per hour).
[[Earth]] moves through the meteoroid stream of [[wiktionary:Particle|particles]] left from the passages of a [[comet]]. The stream comprises solid particles, known as [[meteoroid]]s, ejected by the comet as its frozen gases [[evaporate]] under the heat of the [[Sun]] when it is close enough - typically closer than Jupiter's orbit. The Leonids are a fast moving stream which come close to or cross the path of the Earth and impact the Earth at 72 km/s.<ref>[http://www.space.com/scienceastronomy/astronomy/leonids_science_021112.html Space.com] The Power of a Shooting Star</ref> Leonids in particular are well known for having bright [[meteor]]s or [[fireball]]s which may be 9mm across and have 85g of mass and punch into the atmosphere like a car hitting at 60mph. An annual Leonid shower may deposit 12 or 13 tons of particles across the entire planet. Sometimes these trails of meteoroids cause meteor showers and sometimes meteor storms.
The meteoroids left by the comet are organized in trails in orbits similar to though different from that of the comet. They are differentially disturbed by the planets, in particular [[Jupiter]] and sunlight/solar wind (see also a full explanation by [http://cdsads.u-strasbg.fr/abs/1999JIMO...27...85M McNaught & Asher (1999)]). Old trails are spatially not dense and compose the meteor shower with a few meteors per minute. In the case of the Leonids that tends to peak around November 17, but some are spread through several days on either side and the specific peak changing every year.<ref>you may check every year at the [http://www.imo.net/calendar IMO website]</ref> Conversely, young trails are spatially very dense and the cause of [[meteor storms]] when the Earth enters one. Usual counts during a storm exceed 1000 meteors per hour,<ref>after correction, see: [http://www.imo.net/observations the IMO pages]</ref> to be compared to the annual background (1 to 2 meteors per hour) and the shower background (a few per hour).


==History==
==History==

Revision as of 19:16, 24 December 2009

A famous depiction of the 1833 meteor storm, produced in 1889 for the Adventist book Bible Readings for the Home Circle.

The Leonids ([ˈli.əˌnɪdz] lee-uh-nids) are a prolific meteor shower associated with the comet Tempel-Tuttle. The Leonids get their name from the location of their radiant in the constellation Leo: the meteors appear to radiate from that point in the sky. The 2009 display peaking on November 17 may produce more than 500 meteors an hour.[1][2][3]

Earth moves through the meteoroid stream of particles left from the passages of a comet. The stream comprises solid particles, known as meteoroids, ejected by the comet as its frozen gases evaporate under the heat of the Sun when it is close enough - typically closer than Jupiter's orbit. The Leonids are a fast moving stream which come close to or cross the path of the Earth and impact the Earth at 72 km/s.[4] Leonids in particular are well known for having bright meteors or fireballs which may be 9mm across and have 85g of mass and punch into the atmosphere like a car hitting at 60mph. An annual Leonid shower may deposit 12 or 13 tons of particles across the entire planet. Sometimes these trails of meteoroids cause meteor showers and sometimes meteor storms.

The meteoroids left by the comet are organized in trails in orbits similar to though different from that of the comet. They are differentially disturbed by the planets, in particular Jupiter and sunlight/solar wind (see also a full explanation by McNaught & Asher (1999)). Old trails are spatially not dense and compose the meteor shower with a few meteors per minute. In the case of the Leonids that tends to peak around November 17, but some are spread through several days on either side and the specific peak changing every year.[5] Conversely, young trails are spatially very dense and the cause of meteor storms when the Earth enters one. Usual counts during a storm exceed 1000 meteors per hour,[6] to be compared to the annual background (1 to 2 meteors per hour) and the shower background (a few per hour).

History

Woodcut print depicts the shower as seen at Niagara Falls, New York. Mechanics' Magazine said this illustration was made by an editor named Pickering "who witnessed the scene."

The Leonids are famous because their meteor showers, or storms, can be, and have been in a few cases, among the most spectacular. Because of the superlative storm of 1833 and the recent developments in scientific thought the Leonids have had a major effect on the development of the scientific study of meteors which had previously been thought to be atmospheric phenomena. The meteor storm of 1833 was of truly superlative strength. One estimate is over one hundred thousand meteors an hour,[7] but another, done as the storm abated, estimated in excess of two hundred thousand meteors an hour[8] over the entire region of North America east of the Rocky Mountains. It was marked by the Native Americans, slaves and owners, and many others. That same 1833 shower, near Independence, Missouri, was taken as a sign to push the growing Mormon community out of the area.[9]

Accounts of the 1866 repeat of the Leonids counted hundreds per minute/a few thousand per hr in Europe.[10] Later work identified the meteoroids from the 1733 passage of Comet Temple-Tuttle.[11] The Leonids were again seen in 1867, when moonlight reduced the rates to 1000 per hour. Another strong appearance of the Leonids in 1868 reached an intensity of 1000 per hour in dark skies. It was in 1866-7 that information on Comet Temple-Tuttle was gathered pointing it out as the source of the meteor shower.[12] When the storms failed to return in 1899, it was generally thought that the dust had moved on and storms were a thing of the past. Then, in 1966 a spectacular storm was seen over the Americas. Leading up to the 1998 return, an airborne observing campaign was organized to mobilize modern observing techniques by Peter Jenniskens at NASA Ames Research Center. This resulted in spectacular footage from the 1999, 2001 and 2002 storms producing up to 3,000 Leonid meteors per hour.[1] Initially, the exact location of the dust was unknown. A graph published in Sky and Telescope adapted from Comet 55P/Tempel-Tuttle and the Leonid Meteors(1996, see p. 6) shows relative positions of the Earth and Tempel-Tuttle and marks where Earth encountered dense dust. This showed that the particles are behind and outside the path of the comet, but paths resulting in powerful storms were very near paths of nearly no activity. The work of David Asher, Armagh Observatory and Robert H. McNaught, Siding Spring Observatory, and independently of Esko Lyytinen in Finland, following on from the pioneering research by Kondrat'eva, Reznikov and colleagues at Kazan, is considered by most meteor experts as the breakthrough in modern analysis of meteor storms. Whereas previously it was hazardous to guess if there would be a storm or little activity, the predictions of Asher and McNaught timed bursts in activity down to five minutes. However, the relative brightness of the meteors is still not understood. The double spikes in Leonid activity in 2001 and in 2002 were due to the passage of the comet's dust ejected in 1767 and 1866.[13] The 1833 storm was not due to the recent passage of the comet, but from a direct hit with the 1800 dust[14] and the 1966 storm was from the 1899 passage of the comet.[15] Examples of other streams accounting for spikes in activity include the 2004 June Bootids. Peter Jenniskens has published predictions for the next 50 years.[16]

However, a close encounter with Jupiter is expected to perturb the comet's path, and many streams, making storms of historic magnitude unlikely for many decades.[17]

Year Leonids active between Peak of shower
2008 November 14 - 22 Nov. 17, 2008[1]
2009 November 10-21 Nov. 17, 2009 ZHRmax ranging from 300 to 400 predicted per hour[18][19]
  • "There are no guarantees in meteor work ... observers should be alert as often as conditions allow throughout the shower, in case something unexpected happens, this year 2009 the best viewing spots will be Southern Asia, Northern and Eastern Australia."[19]

See also

References

  1. ^ a b c "Return of the Leonids". NASA. Dec. 4, 2008. Retrieved 2009-10-21. {{cite web}}: Check date values in: |date= (help)
  2. ^ "Strong Leonid Meteor Shower Predicted for 2009". Space.com. 4 December 2008. Retrieved 2009-10-22. The 2009 display will not rate as a meteor storm, which has over 1,000 meteors an hour.
  3. ^ Lopez, Mike (December 7, 2008). "Watch Out for Leonids 2009 Meteor Shower". Retrieved 2009-10-22.
  4. ^ Space.com The Power of a Shooting Star
  5. ^ you may check every year at the IMO website
  6. ^ after correction, see: the IMO pages
  7. ^ Space.com The 1833 Leonid Meteor Shower: A Frightening Flurry
  8. ^ Leonid MAC Brief history of the Leonid shower
  9. ^ McCullough, David, Truman, 1992, p. 22
  10. ^ The Revelation of Bahá'u'lláh, Vol 2 by Adib Taherzadeh, Appendix I: The Star-fall of 1866
  11. ^ Leonid dust trail positions in 1866 Armagh Observatory
  12. ^ Observing the Leonids Gary W. Kronk
  13. ^ Meteor Orbs.org Predictions & Observations of Lunar Meteor impacts
  14. ^ Armagh Observatory Leonid dust trail positions in 1833
  15. ^ Armagh Observatory Leonid dust trail positions in 1966
  16. ^ Jenniskens P., Meteor Showers and their Parent Comets. Cambridge University Press, Cambridge, UK, 790 pp.
  17. ^ a list of predictions can be found here and here
  18. ^ Fazekas, Andrew (November 16, 2009). "Leonid Meteor Shower: Best Sky Show Tonight". National Geographic News.
  19. ^ a b "IMO Meteor Shower Calendar 2009". The International Meteor Organization. 1997–2009. Retrieved 2009-10-21. {{cite web}}: Text "International Meteor Organization" ignored (help)CS1 maint: date format (link)