Comet: Difference between revisions

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Roughly six percent of the [[near-Earth asteroid]]s are thought to be [[Extinct comets|extinct nuclei of comets]] that no longer experience outgassing,<ref name=dormant>{{cite journal |doi=10.1016/j.icarus.2006.02.016 |arxiv=astro-ph/0603106v2.pdf |year=2006 |title=The size–frequency distribution of dormant Jupiter family comets |last1=Whitman |first1=K |last2=Morbidelli |first2=A |last3=Jedicke |first3=R |journal=Icarus |volume=183 |pages=101|bibcode = 2006Icar..183..101W }}</ref> including [[14827 Hypnos]] and [[3552 Don Quixote]].
Roughly six percent of the [[near-Earth asteroid]]s are thought to be [[Extinct comets|extinct nuclei of comets]] that no longer experience outgassing,<ref name=dormant>{{cite journal |doi=10.1016/j.icarus.2006.02.016 |arxiv=astro-ph/0603106v2.pdf |year=2006 |title=The size–frequency distribution of dormant Jupiter family comets |last1=Whitman |first1=K |last2=Morbidelli |first2=A |last3=Jedicke |first3=R |journal=Icarus |volume=183 |pages=101|bibcode = 2006Icar..183..101W }}</ref> including [[14827 Hypnos]] and [[3552 Don Quixote]].


===Coma and tail===
==Coma==
[[File:Hubble's Last Look at Comet ISON Before Perihelion.jpg|thumb|[[Hubble Space Telescope|Hubble]]'s Last Look at Comet ISON Before [[Perihelion]].<ref>{{cite news|title=Hubble's Last Look at Comet ISON Before Perihelion|url=http://www.spacetelescope.org/images/opo1347a/|accessdate=20 November 2013|newspaper=ESA/Hubble Press Release}}</ref> ]]
[[File:Hubble's Last Look at Comet ISON Before Perihelion.jpg|thumb|[[Hubble Space Telescope|Hubble]]'s Last Look at Comet ISON Before [[Perihelion]].<ref>{{cite news|title=Hubble's Last Look at Comet ISON Before Perihelion|url=http://www.spacetelescope.org/images/opo1347a/|accessdate=20 November 2013|newspaper=ESA/Hubble Press Release}}</ref> ]]
The streams of [[Comet dust|dust]] and gas thus released form a huge and extremely thin 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 pointing away from the Sun.<ref>{{cite book |url=http://books.google.co.uk/books?id=4zjv84hHNPcC&pg=PA66#v=onepage&q&f=false |page=66 |title=A Complete Manual of Amateur Astronomy: Tools and Techniques for Astronomical Observations |isbn=9780486152165 |last1=Clay Sherrod |first1=P. Clay |last2=Koed |first2=Thomas L. |year=2003}}</ref>
{{main|Coma (cometary)}}
In the outer [[Solar System]], comets remain frozen and inactive 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 observations by the [[Hubble Space Telescope]]<ref name="Cochran1995">{{cite journal |bibcode=1995ApJ...455..342C |title=The Discovery of Halley-sized Kuiper Belt Objects Using the Hubble Space Telescope |author1=Cochran |first1=Anita L. |last2=Levison |first2=Harold F. |last3=Stern |first3=S. Alan |last4=Duncan |first4=Martin J. |volume=455 |year=1995 |pages=342 |journal=Astrophysical Journal v.455 |doi=10.1086/176581|arxiv = astro-ph/9509100 }}</ref><ref name="Cochran1998">{{cite journal |doi=10.1086/311515 |title=The Calibration of the Hubble Space Telescope Kuiper Belt Object Search:Setting the Record Straight |year=1998 |last1=Cochran |first1=Anita L. |last2=Levison |first2=Harold F. |last3=Tamblyn |first3=Peter |last4=Stern |first4=S. Alan |last5=Duncan |first5=Martin J. |journal=The Astrophysical Journal |volume=503 |pages=L89|arxiv = astro-ph/9806210 |bibcode = 1998ApJ...503L..89C }}</ref> but these detections have been questioned.<ref name="Brown1997">
{{cite journal |doi=10.1086/311009 |title=An Analysis of the Statistics of the \ITAL]Hubble Space Telescope\/ITAL] Kuiper Belt Object Search |year=1997 |last1=Brown |first1=Michael E. |last2=Kulkarni |first2=Shrinivas R. |last3=Liggett |first3=Timothy J. |journal=The Astrophysical Journal |volume=490 |pages=L119|bibcode = 1997ApJ...490L.119B }}</ref><ref name="Jewitt1996">{{cite journal |bibcode=1996AJ....112.1225J |title=The Mauna Kea-Cerro-Tololo (MKCT) Kuiper Belt and Centaur Survey |author1=Jewitt |first1=David |last2=Luu |first2=Jane |last3=Chen |first3=Jun |volume=112 |year=1996 |pages=1225 |journal=Astronomical Journal v.112 |doi=10.1086/118093}}</ref> 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 [[Comet dust|dust]] and gas thus released form a huge and extremely thin 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 pointing away from the Sun.<ref>{{cite book |url=http://books.google.co.uk/books?id=4zjv84hHNPcC&pg=PA66#v=onepage&q&f=false |page=66 |title=A Complete Manual of Amateur Astronomy: Tools and Techniques for Astronomical Observations |isbn=9780486152165 |last1=Clay Sherrod |first1=P. Clay |last2=Koed |first2=Thomas L. |year=2003}}</ref>


The coma is generally made of {{H2O}} and [[dust]], with water making up to 90% of the [[volatiles]] that outflow from the nucleus when the comet is within {{convert|3|to|4|AU}} of the Sun.<ref name=Combi2004>{{cite journal |bibcode=2004come.book..523C |url=http://www.lpi.usra.edu/books/CometsII/7023.pdf |title=Gas dynamics and kinetics in the cometary coma: Theory and observations |last1=Combi |first1=Michael R. |last2=Harris |first2=Walter M. |last3=Smyth |first3=William H. |year=2004 |pages=523 |journal=Comets II}}</ref> The {{H2O}} parent molecule is destroyed primarily through [[photodissociation]] and to a much smaller extent [[photoionization]], with the solar wind playing a minor role in the destruction of water compared to [[photochemistry]].<ref name=Combi2004/> Larger dust particles are left along the comet's orbital path whereas smaller particles are pushed away from the Sun into the comet's tail by [[radiation pressure|light pressure]].<ref>{{cite web |url=http://migall.fastmail.fm/astronomy/solar_system/small_bodies/hale_bop/jpl/define.htm |title=Comet Definitions |publisher=Michael Gallagher |last=Morris |first=Charles S. |accessdate=31 August 2013}}</ref>
The coma is generally made of {{H2O}} and [[dust]], with water making up to 90% of the [[volatiles]] that outflow from the nucleus when the comet is within {{convert|3|to|4|AU}} of the Sun.<ref name=Combi2004>{{cite journal |bibcode=2004come.book..523C |url=http://www.lpi.usra.edu/books/CometsII/7023.pdf |title=Gas dynamics and kinetics in the cometary coma: Theory and observations |last1=Combi |first1=Michael R. |last2=Harris |first2=Walter M. |last3=Smyth |first3=William H. |year=2004 |pages=523 |journal=Comets II}}</ref> The {{H2O}} parent molecule is destroyed primarily through [[photodissociation]] and to a much smaller extent [[photoionization]], with the solar wind playing a minor role in the destruction of water compared to [[photochemistry]].<ref name=Combi2004/> Larger dust particles are left along the comet's orbital path whereas smaller particles are pushed away from the Sun into the comet's tail by [[radiation pressure|light pressure]].<ref>{{cite web |url=http://migall.fastmail.fm/astronomy/solar_system/small_bodies/hale_bop/jpl/define.htm |title=Comet Definitions |publisher=Michael Gallagher |last=Morris |first=Charles S. |accessdate=31 August 2013}}</ref>
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Both the coma and tail are illuminated by the Sun and may become visible when a comet passes through the inner Solar System, the dust reflecting sunlight directly and the gases glowing from [[ion]]isation.<ref name="le">{{cite web |url=http://www.le.ac.uk/ph/faulkes/web/planets/r_pl_comets.html |title=Comets |publisher=University of Leicester |last1=Brinkworth |first1=Carolyn |last2=Thomas |first2=Claire |accessdate=31 July 2013}}</ref> 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.<ref>{{cite book |url=http://books.google.co.uk/books?id=caYpAQAAMAAJ |page=75 |title=A field guide to the stars and planets |isbn=9780395934326 |last=Pasachoff |first=Jay M |year=2000}}</ref> Occasionally a comet may experience a huge and sudden outburst of gas and dust, during which the size of the coma greatly increases for a period of time. This happened in 2007 to [[17P/Holmes|Comet Holmes]].<ref name="atmosphere">{{cite web |last=Jewitt |first=David |url=http://www2.ess.ucla.edu/~jewitt/holmes.html |title=Comet Holmes Bigger Than The Sun |publisher=Institute for Astronomy at the University of Hawaii |accessdate=31 July 2013}}</ref>
Both the coma and tail are illuminated by the Sun and may become visible when a comet passes through the inner Solar System, the dust reflecting sunlight directly and the gases glowing from [[ion]]isation.<ref name="le">{{cite web |url=http://www.le.ac.uk/ph/faulkes/web/planets/r_pl_comets.html |title=Comets |publisher=University of Leicester |last1=Brinkworth |first1=Carolyn |last2=Thomas |first2=Claire |accessdate=31 July 2013}}</ref> 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.<ref>{{cite book |url=http://books.google.co.uk/books?id=caYpAQAAMAAJ |page=75 |title=A field guide to the stars and planets |isbn=9780395934326 |last=Pasachoff |first=Jay M |year=2000}}</ref> Occasionally a comet may experience a huge and sudden outburst of gas and dust, during which the size of the coma greatly increases for a period of time. This happened in 2007 to [[17P/Holmes|Comet Holmes]].<ref name="atmosphere">{{cite web |last=Jewitt |first=David |url=http://www2.ess.ucla.edu/~jewitt/holmes.html |title=Comet Holmes Bigger Than The Sun |publisher=Institute for Astronomy at the University of Hawaii |accessdate=31 July 2013}}</ref>

===Tails===
{{main|Comet tail}}
[[File:Comet Parts.jpg|thumb|150px|right|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]]{{main|Coma (cometary)}}
In the outer [[Solar System]], comets remain frozen and inactive 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 observations by the [[Hubble Space Telescope]]<ref name="Cochran1995">{{cite journal |bibcode=1995ApJ...455..342C |title=The Discovery of Halley-sized Kuiper Belt Objects Using the Hubble Space Telescope |author1=Cochran |first1=Anita L. |last2=Levison |first2=Harold F. |last3=Stern |first3=S. Alan |last4=Duncan |first4=Martin J. |volume=455 |year=1995 |pages=342 |journal=Astrophysical Journal v.455 |doi=10.1086/176581|arxiv = astro-ph/9509100 }}</ref><ref name="Cochran1998">{{cite journal |doi=10.1086/311515 |title=The Calibration of the Hubble Space Telescope Kuiper Belt Object Search:Setting the Record Straight |year=1998 |last1=Cochran |first1=Anita L. |last2=Levison |first2=Harold F. |last3=Tamblyn |first3=Peter |last4=Stern |first4=S. Alan |last5=Duncan |first5=Martin J. |journal=The Astrophysical Journal |volume=503 |pages=L89|arxiv = astro-ph/9806210 |bibcode = 1998ApJ...503L..89C }}</ref> but these detections have been questioned.<ref name="Brown1997">
{{cite journal |doi=10.1086/311009 |title=An Analysis of the Statistics of the \ITAL]Hubble Space Telescope\/ITAL] Kuiper Belt Object Search |year=1997 |last1=Brown |first1=Michael E. |last2=Kulkarni |first2=Shrinivas R. |last3=Liggett |first3=Timothy J. |journal=The Astrophysical Journal |volume=490 |pages=L119|bibcode = 1997ApJ...490L.119B }}</ref><ref name="Jewitt1996">{{cite journal |bibcode=1996AJ....112.1225J |title=The Mauna Kea-Cerro-Tololo (MKCT) Kuiper Belt and Centaur Survey |author1=Jewitt |first1=David |last2=Luu |first2=Jane |last3=Chen |first3=Jun |volume=112 |year=1996 |pages=1225 |journal=Astronomical Journal v.112 |doi=10.1086/118093}}</ref> 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 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 type II or dust tail.<ref name="le"/> At the same time, the ion or type I tail, made of gases, always points directly away from the Sun because this gas is more strongly affected by the solar wind than is dust, following magnetic field lines rather than an orbital trajectory.<ref>{{cite book |url=http://books.google.co.uk/books?id=S4xDhVCxAQIC&pg=PA422#v=onepage&q&f=false |page=422 |title=The Cambridge Guide to the Solar System |isbn=9781139494175 |last=Lang |first=Kenneth R. |year=2011}}</ref> On occasions - such as when the Earth passes through a comet's orbital plane, and we see the track of the comet edge-on, a tail pointing in the opposite direction to the ion and dust tails may be seen – the [[antitail]]. <ref>{{cite web |title=PanSTARRS: The Anti Tail Comet |url=http://apod.nasa.gov/apod/ap130629.html |publisher=NASA |date=29 June 2013 |accessdate=31 July 2013}}</ref> (The dust tail of the comet prior to its rounding of the sun, is collinear with the dust tail post the rounding of the sun).
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 type II or dust tail.<ref name="le"/> At the same time, the ion or type I tail, made of gases, always points directly away from the Sun because this gas is more strongly affected by the solar wind than is dust, following magnetic field lines rather than an orbital trajectory.<ref>{{cite book |url=http://books.google.co.uk/books?id=S4xDhVCxAQIC&pg=PA422#v=onepage&q&f=false |page=422 |title=The Cambridge Guide to the Solar System |isbn=9781139494175 |last=Lang |first=Kenneth R. |year=2011}}</ref> On occasions - such as when the Earth passes through a comet's orbital plane, and we see the track of the comet edge-on, a tail pointing in the opposite direction to the ion and dust tails may be seen – the [[antitail]]. <ref>{{cite web |title=PanSTARRS: The Anti Tail Comet |url=http://apod.nasa.gov/apod/ap130629.html |publisher=NASA |date=29 June 2013 |accessdate=31 July 2013}}</ref> (The dust tail of the comet prior to its rounding of the sun, is collinear with the dust tail post the rounding of the sun).

Revision as of 21:29, 11 December 2013

9P/Tempel collides with Deep Impact's impactor
Comet Holmes (17P/Holmes) in 2007, showing blue ion tail on right

A comet is an icy

solar radiation and the solar wind
upon the nucleus of the comet. Comet nuclei range from a few hundred metres to tens of kilometres across and are composed of loose collections of ice, dust, and small rocky particles. The coma and tail are much larger, and if sufficiently bright may be seen from the Earth without the aid of a telescope. Comets have been observed and recorded since ancient times by many different cultures.

Comets have a wide range of

.

Comets are distinguished from

.

As of July 2013[update] there were 4,894 known comets,

Great Comets
".

Etymology

The word comet derives from the Old English cometa from the Latin comēta or comētēs. That, in turn, is a latinisation of the Greek κομήτης ("wearing long hair"), and the Oxford English Dictionary notes that the term (ἀστὴρ) κομήτης already meant "long-haired star, comet" in Greek. Κομήτης was derived from κομᾶν ("to wear the hair long"), which was itself derived from κόμη ("the hair of the head") and was used to mean "the tail of a comet".[7][8]

The astronomical symbol for comets is (), consisting of a small disc with three hairlike extensions.[9]

Physical characteristics

Nucleus

Nucleus of Comet 103P/Hartley with jets streaming out; photography by a visiting space probe. The nucleus is about 2 km in length.
C/2011 W3 (Lovejoy) heads into the Sun
Comet Borrelly exhibits jets, but has no surface ice.
Comet Wild 2
exhibits jets on light side and dark side, stark relief, and is dry.

The solid, core structure of a comet is known as the nucleus. Cometary nuclei are composed of an amalgamation of

Fred Whipple's model.[11] However, some comets may have a higher dust content, leading them to be called "icy dirtballs".[12]

The surface of the nucleus is generally dry, dusty or rocky, suggesting that the ices are hidden beneath a surface crust several metres thick. In addition to the gases already mentioned, the nuclei contain a variety of

asteroids and comets.[16][17]

The outer surfaces of cometary nuclei have a very low

organic compounds. Solar heating drives off lighter volatile compounds, leaving behind larger organic compounds that tend to be very dark, like tar or crude oil. The low reflectivity of cometary surfaces enables them to absorb the heat necessary to drive their outgassing processes.[19]

Properties of some comets
Name Dimensions
km
Density
g/cm3
Mass
kg[20]
Halley's Comet 15 × 8 × 8[21] 0.6[22] 3×1014
Tempel 1 7.6 × 4.9[23] 0.62[24] 7.9×1013
19P/Borrelly 8 × 4×4 0.3[24] 2×1013
81P/Wild 5.5 × 4.0 × 3.3[25] 0.6[24] 2.3×1013

Comet nuclei with radii of up to 30 kilometres (19 mi) have been observed,

P/2007 R5 is probably only 100–200 metres in diameter.[28] A lack of smaller comets being detected despite the increased sensitivity of instruments has lead some to suggest that there is a real lack of comets smaller than 100 metres (330 ft) across.[29] Known comets have been estimated to have an average density of 0.6 g/cm3.[24] Because of their low mass, comet nuclei do not become spherical under their own gravity and therefore have irregular shapes.[30]

Roughly six percent of the

extinct nuclei of comets that no longer experience outgassing,[31] including 14827 Hypnos and 3552 Don Quixote
.

Coma

The streams of dust and gas thus released form a huge and extremely thin 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 pointing away from the Sun.[33]

The coma is generally made of H2O and dust, with water making up to 90% of the volatiles that outflow from the nucleus when the comet is within 3 to 4 astronomical units (450,000,000 to 600,000,000 km; 280,000,000 to 370,000,000 mi) of the Sun.[34] The H2O parent molecule is destroyed primarily through photodissociation and to a much smaller extent photoionization, with the solar wind playing a minor role in the destruction of water compared to photochemistry.[34] Larger dust particles are left along the comet's orbital path whereas smaller particles are pushed away from the Sun into the comet's tail by light pressure.[35]

Although the solid nucleus of comets is generally less than 60 kilometres (37 mi) across, the coma may be thousands or millions of kilometres across, sometimes becoming larger than the Sun.

17P/Holmes briefly had a tenuous dust atmosphere larger than the Sun.[37] The Great Comet of 1811 also had a coma roughly the diameter of the Sun.[38] Even though the coma can become quite large, its size can actually decrease about the time it crosses the orbit of Mars around 1.5 astronomical units (220,000,000 km; 140,000,000 mi) from the Sun.[38] At this distance the solar wind becomes strong enough to blow the gas and dust away from the coma, enlarging the tail.[38] Ion tails have been observed to extend one astronomical unit (150 million km) or more.[37]

Both the coma and tail are illuminated by the Sun and may become visible when a comet passes through the inner Solar System, the dust reflecting sunlight directly and the gases glowing from

Tails

Coma (cometary)

In the outer

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 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 type II or dust tail.

antitail. [46]
(The dust tail of the comet prior to its rounding of the sun, is collinear with the dust tail post the rounding of the sun).

The observation of antitails contributed significantly to the discovery of solar wind.[47] The ion tail is formed as a result of the ionisation by solar ultra-violet radiation of particles in the coma. Once the particles have been ionized, they attain a net positive electrical charge, which in turn gives rise to an "induced magnetosphere" around the comet. The comet and its induced magnetic field form an obstacle to outward flowing solar wind particles. Because the relative orbital speed of the comet and the solar wind is supersonic, a bow shock is formed upstream of the comet 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, such that the field lines "drape" around the comet forming the ion tail.[48]

Encke's Comet
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,

Encke's Comet was completely severed while the comet passed through a coronal mass ejection. This event was observed by the STEREO space probe.[49]

In 1996, comets were found to emit

In 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."[52][53]

Jets

Gas and Snow Jets from Comet Hartley 2

Orbital characteristics

Most comets are

elliptical orbits that take them close to the Sun for a part of their orbit and then out into the further reaches of the Solar System for the remainder.[54] Comets are often classified according to the length of their orbital periods
: The longer the period the more elongated the ellipse.

Short period

aphelion; for example, the aphelion of Halley's Comet is a little beyond the orbit of Neptune. Comets whose aphelia are near a major planet's orbit are called its "family".[57] Such families are thought to arise from the planet capturing formerly long-period comets into shorter orbits.[58]

At the shorter extreme,

Encke's Comet has an orbit that does not reach the orbit of Jupiter, and is known as an Encke-type comet. Short-period comets with orbital periods shorter than 20 years and low inclinations (up to 30 degrees) are called "Jupiter-family comets".[59][60] Those like Halley, with orbital periods of between 20 and 200 years and inclinations extending from zero to more than 90 degrees, are called "Halley-type comets".[61][62] As of 2013, only 72 Halley-type comets have been observed, compared with 470 identified Jupiter-family comets.[63]

Recently discovered

main-belt comets form a distinct class, orbiting in more circular orbits within the asteroid belt.[64]

Because their elliptical orbits frequently take them close to the giant planets, comets are subject to further gravitational perturbations.[65] Short-period comets display a tendency for their aphelia to coincide with a gas giant's orbital radius, with the Jupiter family of comets being the largest.[60] It is clear that comets coming in from the Oort cloud often have their orbits strongly influenced by the gravity of giant planets as a result of a close encounter. Jupiter is the source of the greatest perturbations, being more than twice as massive as all the other planets combined. These perturbations can deflect long-period comets into shorter orbital periods.[66][67]

Based on their orbital characteristics, short-period comets are thought to originate from the

Jan Hendrik Oort who hypothesised its existence).[69] Vast swarms of comet-like bodies are believed to orbit the Sun in these distant regions in roughly circular orbits. Occasionally the gravitational influence of the outer planets (in the case of Kuiper belt objects) or nearby stars (in the case of Oort cloud objects) may throw one of these bodies into an elliptical orbit that takes it inwards toward the Sun to form a visible comet. Unlike the return of periodic comets, whose orbits have been established by previous observations, the appearance of new comets by this mechanism is unpredictable.[70]

Long period

Orbits of the Kohoutek Comet (red) and the Earth (blue), illustrating the high eccentricity of its orbit and its rapid motion when close to the Sun.
Hyperbolic
comet discoveries
[71]
Year #
2013 8
2012 10
2011 12
2010 4
2009 8
2008 7
2007 12

Long-period comets have highly

apoapsis
distances of nearly 70,000 AU with orbital periods estimated around 6 million years.

C/2011 L4
(PANSTARRS) (bottom)

Single-apparition or non-periodic comets are similar to long-period comets because they also have

unstable maximum boundary of 230,000 AU (1.1 parsecs (3.6 light-years)).[75] Only a few hundred comets have been seen to achieve a hyperbolic orbit (e > 1) when near perihelion[76] that using a heliocentric unperturbed two-body best-fit
suggests they may escape the Solar System.

No comets with an

.

Some authorities use the term "periodic comet" to refer to any comet with a periodic orbit (that is, all short-period comets plus all long-period comets),[78] whereas others use it to mean exclusively short-period comets.[72] Similarly, although the literal meaning of "non-periodic comet" is the same as "single-apparition comet", some use it to mean all comets that are not "periodic" in the second sense (that is, to also include all comets with a period greater than 200 years).

Early observations have revealed a few genuinely hyperbolic (i.e. non-periodic) trajectories, but no more than could be accounted for by perturbations from Jupiter. If comets pervaded

interstellar space, they would be moving with velocities of the same order as the relative velocities of stars near the Sun (a few tens of kms per second). If such objects entered the Solar System, they would have positive specific orbital energy and would be observed to have genuinely hyperbolic trajectories. A rough calculation shows that there might be four hyperbolic comets per century within Jupiter's orbit, give or take one and perhaps two orders of magnitude.[79]

Lost

A number of periodic comets discovered in earlier decades or previous centuries are now

LINEAR in 2001.[80]

Comets in other star systems

A V star, in 1987.[82][83] A total of 10 such exocomet systems have been identified as of 2013, using the absorption spectrum caused by the large clouds of gas emitted by comets when passing close to their star.[81][82]

Effects of comets

Connection to meteor showers

As a result of outgassing, comets leave in their wake a trail of solid debris too large to be swept away by

Halley's comet is the source of the Orionid shower in October.[85]


Comets and impact on life

Many comets and asteroids collided into Earth in its early stages. Many scientists believe that comets bombarding the young Earth about 4 billion years ago brought the vast quantities of water that now fill the Earth's oceans, or at least a significant portion of it. Other researchers have cast doubt on this theory.[86] The detection of organic molecules in significant quantities in comets has led some to speculate that comets or meteorites may have brought the precursors of life—or even life itself—to Earth.[87]

It is suspected that comet impacts have, over long timescales, also delivered significant quantities of water to the Earth's

lunar ice.[88] Comet and meteoroid impacts are also believed responsible for the existence of tektites and australites.[89]

In 2013 it was suggested that impacts between rocky and icy surfaces, such as comets, had the potential to create the amino acids that make up proteins through shock synthesis.[90]

Fate of comets

Departure (ejection) from Solar System

If a comet is traveling fast enough, it may leave the Solar System; such is the case for hyperbolic comets. To date, comets are only known to be ejected by interacting with another object in the Solar System, such as Jupiter.[91]

Volatiles exhausted

Jupiter-family comets and long-period comets appear to follow very different fading laws. The JFCs are active over a lifetime of about 10,000 years or ~1,000 orbits whereas long-period comets fade much faster. Only 10% of the long-period comets survive more than 50 passages to small perihelion and only 1% of them survive more than 2,000 passages.[31] Eventually most of the volatile material contained in a comet nucleus evaporates away, and the comet becomes a small, dark, inert lump of rock or rubble that can resemble an asteroid.[92] Some asteroids in elliptical orbits are now identified as extinct comets.[93] Roughly six percent of the near-Earth asteroids are thought to be extinct nuclei of comets that no longer emit gas.[31]

Breakup

Breaking up of 73P/Schwassmann–Wachmann in 1995. This animation covers three days.

The nucleus of some comets may be fragile, a conclusion supported by the observation of comets splitting apart.

3D/Biela in 1846 and 73P/Schwassmann–Wachmann from 1995 to 2006.[97] Greek historian Ephorus reported that a comet split apart as far back as the winter of 372–373 BC.[98] Comets are suspected of splitting due to thermal stress, internal gas pressure, or impact.[99]

Comets 42P/Neujmin and 53P/Van Biesbroeck appear to be fragments of a parent comet. Numerical integrations have shown that both comets had a rather close approach to Jupiter in January 1850, and that, before 1850, the two orbits were nearly identical.[100]

Some comets have been observed to break up during their perihelion passage, including great comets

meteor showers were seen in 1872 and 1885 when the comet should have been visible. A lesser meteor shower, the Andromedids, occurs annually in November, and it is caused when the Earth crosses the orbit of Biela's Comet.[101]

Collisions

Brown spots mark impact sites of Comet Shoemaker–Levy on Jupiter

Some comets meet a more spectacular end – either falling into the Sun[102] or smashing into a planet or other body. Collisions between comets and planets or moons were common in the early Solar System: some of the many craters on the Moon, for example, may have been caused by comets. A recent collision of a comet with a planet occurred in July 1994 when Comet Shoemaker–Levy 9 broke up into pieces and collided with Jupiter.[103]

Nomenclature

The names given to comets have followed several different conventions over the past two centuries. Prior to the early 20th century, most comets were simply referred to by the year when they appeared, sometimes with additional adjectives for particularly bright comets; thus, the "

Great January comet of 1910
".

Edmund Halley
for successfully calculating its orbit. Photo of 1910

After

Edmund Halley demonstrated that the comets of 1531, 1607, and 1682 were the same body and successfully predicted its return in 1759, that comet became known as Halley's comet.[104] Similarly, the second and third known periodic comets, Encke's Comet[105] and Biela's Comet,[106] were named after the astronomers who calculated their orbits rather than their original discoverers. Later, periodic comets were usually named after their discoverers, but comets that had appeared only once continued to be referred to by the year of their apparition.[107]

In the early 20th century, the convention of naming comets after their discoverers became common, and this remains so today. A comet can be named its discoverers, or an instrument or program that helped to find it.[107]

History of study

Early observations and thought

the Battle of Hastings in 1066 (Bayeux Tapestry
).

From ancient sources, such as Chinese oracle bones, it is known that their appearances have been noticed by humans for millennia.[108] Until the sixteenth century, comets were usually considered bad omens of deaths of kings or noble men, or coming catastrophes, or even interpreted as attacks by heavenly beings against terrestrial inhabitants.[109][110]

Aristotle believed that comets were atmospheric phenomena, due to the fact that they could appear outside of the Zodiac and vary in brightness over the course of a few days.[111] Pliny the Elder believed that comets were connected with political unrest and death.[112]

In the 16th century Tycho Brahe demonstrated that comets must exist outside the Earth's atmosphere by measuring the parallax of the Great Comet of 1577 from observations collected by geographically separated observers. Within the precision of the measurements, this implied the comet must be at least four times more distant than from the Earth to the Moon.[113][114]

Orbital studies

The orbit of the comet of 1680, fitted to a parabola, as shown in Isaac Newton's Principia

inverse square law of universal gravitation must trace out an orbit shaped like one of the conic sections, and he demonstrated how to fit a comet's path through the sky to a parabolic orbit, using the comet of 1680 as an example.[115]

In 1705,

Joseph Lalande, and Nicole-Reine Lepaute, who predicted the date of the comet's 1759 perihelion to within one month's accuracy.[117] When the comet returned as predicted, it became known as Halley's Comet (with the latter-day designation of 1P/Halley). It will next appear in 2061.[118]

Studies of physical characteristics

"From his huge vapouring train perhaps to shake
Reviving moisture on the numerous orbs,
Thro' which his long ellipsis winds; perhaps
To lend new fuel to declining suns,
To light up worlds, and feed th' ethereal fire."

The Seasons (1730; 1748)[119]

Isaac Newton described comets as compact and durable solid bodies moving in oblique orbit and their tails as thin streams of vapor emitted by their nuclei, ignited or heated by the Sun. Newton suspected that comets were the origin of the life-supporting component of air.[120]

As early as the 18th century, some scientists had made correct hypotheses as to comets' physical composition. In 1755, Immanuel Kant hypothesized that comets are composed of some volatile substance, whose vaporization gives rise to their brilliant displays near perihelion.[121] In 1836, the German mathematician Friedrich Wilhelm Bessel, after observing streams of vapor during the appearance of Halley's Comet in 1835, proposed that the jet forces of evaporating material could be great enough to significantly alter a comet's orbit, and he argued that the non-gravitational movements of Encke's Comet resulted from this phenomenon.[122]

In 1950,

Giotto probe and the Soviet Union's Vega 1 and Vega 2) that flew through the coma of Halley's Comet in 1986, photographed the nucleus, and observed jets of evaporating material.[124]

Spacecraft missions

View from the impactor in its last moments before hitting the comet in the Deep Impact missioni
NASA is developing a comet harpoon for returning samples to Earth.

Debate continues about how much ice is in a comet. In 2001, the Deep Space 1 spacecraft obtained high-resolution images of the surface of Comet Borrelly. It was found that the surface of comet Borrelly is hot and dry, with a temperature of between 26 to 71 °C (79 to 160 °F), and extremely dark, suggesting that the ice has been removed by solar heating and maturation, or is hidden by the soot-like material that covers Borrelly's.[125]

In July 2005, the

Comet Tempel 1 to study its interior. The mission yielded results suggesting that the majority of a comet's water ice is below the surface and that these reservoirs feed the jets of vaporised water that form the coma of Tempel 1.[126] Renamed EPOXI, it made a flyby of Comet Hartley 2
on November 4, 2010.

Data from the Stardust mission show that materials retrieved from the tail of Wild 2 were crystalline and could only have been "born in fire," at extremely high temperatures of over 1,000 °C (1,830 °F).[127][128] Although comets formed in the outer Solar System, radial mixing of material during the early formation of the Solar System is thought to have redistributed material throughout the proto-planetary disk,[129] so comets also contain crystalline grains that formed in the hot inner Solar System. This is seen in comet spectra as well as in sample return missions. More recent still, the materials retrieved demonstrate that the "comet dust resembles asteroid materials".[130] These new results have forced scientists to rethink the nature of comets and their distinction from asteroids.[131]

The Rosetta probe is presently en route to Comet Churyumov–Gerasimenko; in 2014 it will go into orbit around the comet and place a small lander on its surface.[132]

Examples

  • Comet C/2006 P1 (McNaught) taken from Victoria, Australia 2007
    Comet
    C/2006 P1
    (McNaught) taken from Victoria, Australia 2007
  • The Great Comet of 1882 is a member of the Kreutz group
    The
    Kreutz group
  • Great Comet 1861
    Great Comet 1861

Great comets

Approximately once a decade, a comet becomes bright enough to be noticed by a casual observer, leading such comets to be designated as

Great Comets.[98]

Woodcut of the Great Comet of 1577

Predicting whether a comet will become a great comet is notoriously difficult, as many factors may cause a comet's brightness to depart drastically from predictions.[133] Broadly speaking, if a comet has a large and active nucleus, will pass close to the Sun, and is not obscured by the Sun as seen from the Earth when at its brightest, it has a chance of becoming a great comet. However, Comet Kohoutek in 1973 fulfilled all the criteria and was expected to become spectacular but failed to do so.[134] Comet West, which appeared three years later, had much lower expectations but became an extremely impressive comet.[135]

The late 20th century saw a lengthy gap without the appearance of any great comets, followed by the arrival of two in quick succession—

C/2006 P1 (McNaught), which became visible to naked eye observers in January 2007. It was the brightest in over 40 years.[136]

Sungrazing comets

Kreutz Sungrazer
with a prominent tail, plunging towards the Sun

A sungrazing comet is a comet that passes extremely close to the Sun at perihelion, generally within a few million kilometres.

tidal forces they experience often lead to their fragmentation.[138]

About 90% of the sungrazers observed with

Kreutz group, which all originate from one giant comet that broke up into many smaller comets during its first passage through the inner Solar System.[139] The remainder contains some sporadic sungrazers, but four other related groups of comets have been identified among them: the Kracht, Kracht 2a, Marsden, and Meyer groups. The Marsden and Kracht groups both appear to be related to Comet 96P/Machholz, which is also the parent of two meteor streams, the Quadrantids and the Arietids.[140]

Unusual comets

See also Fate of comets.

Of the thousands of known comets, some exhibit unusual properties. Encke's Comet orbits from outside the asteroid belt to just inside the orbit of the planet

Comet Shoemaker–Levy 2 was originally designated asteroid 1990 UL3.[143]

Observation

X-ray emission from Hyakutake, as seen by the ROSAT satellite.

A comet may be discovered photographically using a wide-field

amateur astronomer to discover a sungrazing comet online by downloading images accumulated by some satellite observatories such as SOHO.[28] SOHO's 2000th comet was discovered by Polish amateur astronomer Michał Kusiak on 26 December 2010.[144]

Comets & Culture

Comet Hale-Bopp, as seen in Pazin, Croatia
1997.

The depiction of comets in

In times past, bright comets often inspired panic and hysteria in the general population, being thought of as bad omens. More recently, during the passage of Halley's Comet in 1910, the Earth passed through the comet's tail, and erroneous newspaper reports inspired a fear that cyanogen in the tail might poison millions,[146] whereas the appearance of Comet Hale–Bopp in 1997 triggered the mass suicide of the Heaven's Gate cult.[147]

In science fiction, the impact of comets has been depicted as a threat overcome by technology and heroism (Deep Impact, 1998), or as a trigger of global apocalypse (Lucifer's Hammer, 1979) or of waves of zombies (Night of the Comet, 1984).[145] In Jules Verne's Off on a Comet a group of people are stranded on a comet orbiting the Sun, while a large manned space expedition visits Halley's Comet in Sir Arthur C. Clarke's novel 2061: Odyssey Three.[148]

See also

Template:Wikipedia books

References

Notes

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Sources

Further reading

External links

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