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The possibility is of particular interest to [[human]]s as it is easily [[inference|inferred]] that the more similar a planet is to Earth, the more likely it is of sustaining Earth-like complex [[extraterrestrial life]] and more importantly, [[civilization]]. As such it has long been speculated and the subject expressed in [[science]], [[philosophy]], [[science fiction]] and [[popular culture]].
The possibility is of particular interest to [[human]]s as it is easily [[inference|inferred]] that the more similar a planet is to Earth, the more likely it is of sustaining Earth-like complex [[extraterrestrial life]] and more importantly, [[civilization]]. As such it has long been speculated and the subject expressed in [[science]], [[philosophy]], [[science fiction]] and [[popular culture]].

Before the scientific search for and study of [[extrasolar planet]]s, the possibility was argued through philosophy and science fiction. The [[Mediocrity principle]] suggests that planets like the Earth should be common and in an infinite universe, while the [[Rare Earth hypothesis]] suggests that they are extremely rare. Philosophers have pointed out that the size of the universe is such that a near identical planet must exists somewhere, such theories include the philosophy of [[Multiverse]] and the [[Twin Earth thought experiment]].


Advocates of [[space colonization]] have long sought an Earth Analog as a "second home" while advocates for [[space and survival]] would regard such a planet as a potential "new home".
Advocates of [[space colonization]] have long sought an Earth Analog as a "second home" while advocates for [[space and survival]] would regard such a planet as a potential "new home".


Some scientific theories speculate that Earth analogs may have existed in our Solar System in the past. In the future, [[technology]] may be used by humans to artificially produce an Earth analog. In theory, [[terraforming]], [[virtual reality]] or [[simulated reality]] could potentially create such a world. [[Multiverse]] theory suggests that an Earth analog could exist in another universe or even another version of the Earth itself in a [[Parallel universe (fiction)|parallel universe]].
Some scientific theories speculate that Earth analogs, such as ancient Mars and Venus may have existed in our Solar System in the past and that in the distant future Titan may naturally become one or that [[technology]] may be used to artificially produce one by means of [[terraforming]], [[virtual reality]] or [[simulated reality]].


Technological advances in [[extrasolar planet]] detection are rapidly refining the probabilities of a real discovery, not just in this universe, but in the present [[Milky Way galaxy]]. Although the distribution and attributes of the studied planets are still very much unknown, current calculations suggest that they may be relatively common in the universe. 2011 estimates by the NASA's [[Jet Propulsion Laboratory]] (JPL) based on observations from the [[Kepler (spacecraft)|Kepler mission]] determined that about "1.4 to 2.7 percent" of all [[sun]]-like [[star]]s are expected to have earthlike planets "within the [[habitable zone]]s of their stars". This means there are "two billion" of them in our own Milky Way galaxy alone and assuming that all galaxies have a similar number as the Milky Way, in the 50 billion galaxies in the [[observable universe]] there may be as many as a [[sextillion]].<ref name="ChoiCQ">{{cite web |last1=Choi |first1=Charles Q. |url=http://www.space.com/11188-alien-earths-planets-sun-stars.html |title=New Estimate for Alien Earths: 2 Billion in Our Galaxy Alone |date=21 March 2011 |publisher=[[Space.com]] |accessdate=2011-04-24}}</ref>
Technological advances in [[extrasolar planet]] detection are rapidly refining the probabilities of a real discovery, not just in this universe, but in the present [[Milky Way galaxy]]. Although the distribution and attributes of the studied planets are still very much unknown, current calculations suggest that they may be relatively common in the universe. 2011 estimates by the NASA's [[Jet Propulsion Laboratory]] (JPL) based on observations from the [[Kepler (spacecraft)|Kepler mission]] determined that about "1.4 to 2.7 percent" of all [[sun]]-like [[star]]s are expected to have earthlike planets "within the [[habitable zone]]s of their stars". This means there are "two billion" of them in our own Milky Way galaxy alone and assuming that all galaxies have a similar number as the Milky Way, in the 50 billion galaxies in the [[observable universe]] there may be as many as a [[sextillion]].<ref name="ChoiCQ">{{cite web |last1=Choi |first1=Charles Q. |url=http://www.space.com/11188-alien-earths-planets-sun-stars.html |title=New Estimate for Alien Earths: 2 Billion in Our Galaxy Alone |date=21 March 2011 |publisher=[[Space.com]] |accessdate=2011-04-24}}</ref>


The [[mediocrity principle]] suggests that there is a chance that serendipitous events may have allowed an Earth-like planet to form elsewhere that would allow the emergence of complex, multi-cellular life. Philosophers have pointed out that the size of the universe is such that a near identical planet must exists somewhere, such theories include the philosophy of [[Multiverse]] and the [[Twin Earth thought experiment]]. However, the [[Rare Earth hypothesis]] asserts that if the strictest criteria are applied, a true Earth Analog, should such a planet exist may be so far away that humans may never locate it.
The more recent serious scientific findings have greatly influenced the scope of the fields of [[astrobiology]], models of [[planetary habitability]] and [[Search for Extraterrestrial Intelligence]]. [[NASA]] and the [[SETI Institute]] have proposed categorising the increasing number of Earth-like planets found using a measure called the [[Earth Similarity Index]] (ESI) based on mass, radius and temperature.<ref>http://www.wired.co.uk/news/archive/2011-11/21/exoplanet-indices</ref><ref>Stuart Gary [http://www.abc.net.au/news/2011-11-22/new-recipe-in-search-for-alien-life/3686408/ New approach in search for alien life] ABC Online. November 22, 2011</ref> According to this measure, the confirmed planets most similar to Earth are [[Gliese 667C c]] (0.85)<ref>http://phl.upr.edu/projects/habitable-exoplanets-catalog/data</ref>, [[Kepler 22b]]<ref>[http://phl.upr.edu/library/notes/updatesonexoplanetsduringthefirstkeplerscienceconference Updates on Exoplanets during the First Kepler Science Conference]</ref> and [[HD 85512 b]] (0.79), [[Gliese 581 d]] (0.74), [[Mars]] and [[Gliese 581c]] (0.70).<ref>Dirk Schulze-Makuch, Abel Méndez, Alberto G. Fairén, Philip von Paris, Carol Turse, Grayson Boyer, Alfonso F. Davila, Marina Resendes de Sousa António, David Catling, and Louis N. Irwin. Astrobiology. doi:10.1089/ast.2010.0592. October 21, 2011</ref>

The more recent serious scientific findings have greatly influenced the scope of the fields of [[astrobiology]], models of [[planetary habitability]] and [[Search for Extraterrestrial Intelligence]]. Astrobiologists assert that Earth analogs would most likely be found in a stellar [[habitable zone]] in which liquid water could exist, providing also the conditions for supporting life. Some astrobiologists, such as [[Dirk Schulze-Makuch]] have theorised that a sufficiently massive [[natural satellite]] may form a [[habitable moon]] similar to Earth. [[NASA]] and the [[SETI Institute]] have proposed categorising the increasing number of Earth-like planets found using a measure called the [[Earth Similarity Index]] (ESI) based on mass, radius and temperature.<ref>http://www.wired.co.uk/news/archive/2011-11/21/exoplanet-indices</ref><ref>Stuart Gary [http://www.abc.net.au/news/2011-11-22/new-recipe-in-search-for-alien-life/3686408/ New approach in search for alien life] ABC Online. November 22, 2011</ref> According to this measure, the confirmed planets most similar to Earth are [[Gliese 667C c]] (0.85)<ref>http://phl.upr.edu/projects/habitable-exoplanets-catalog/data</ref>, [[Kepler 22b]]<ref>[http://phl.upr.edu/library/notes/updatesonexoplanetsduringthefirstkeplerscienceconference Updates on Exoplanets during the First Kepler Science Conference]</ref> and [[HD 85512 b]] (0.79), [[Gliese 581 d]] (0.74), [[Mars]] and [[Gliese 581c]] (0.70).<ref>Dirk Schulze-Makuch, Abel Méndez, Alberto G. Fairén, Philip von Paris, Carol Turse, Grayson Boyer, Alfonso F. Davila, Marina Resendes de Sousa António, David Catling, and Louis N. Irwin. Astrobiology. doi:10.1089/ast.2010.0592. October 21, 2011</ref>


==History==
==History==
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===Terrestrial===
===Terrestrial===
[[Image:Mars Viking 21i093.png|thumb|Although cold and dry, much of the surface and topography of Mars bears similarities to that of arid regions on Earth]]
Another criteria often cited is that an Earth analog must be terrestrial, that is, it should possess a similar surface geology - a [[planetary surface]] composed of similar surface materials. The closest known example is Mars and Titan and while there are similarities in their types of landforms and surface compositions there are also significant differences.
Another criteria often cited is that an Earth analog must be terrestrial, that is, it should possess a similar surface geology - a [[planetary surface]] composed of similar surface materials. The closest known example is Mars and Titan and while there are similarities in their types of landforms and surface compositions there are also significant differences.


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A true Earth analog therefore might need to have formed through similar processes, having possessed an atmosphere, volcanic interactions with the surface, past or present liquid water and lifeforms.
A true Earth analog therefore might need to have formed through similar processes, having possessed an atmosphere, volcanic interactions with the surface, past or present liquid water and lifeforms.

The [[Geography of Mars]] and [[List of geological features on Titan|of Titan]] in particular appear to include many features similar to Earth.


===Temperature===
===Temperature===
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[[File:Kepler-22b System Diagram.jpg|thumb|[[Kepler-22b]], located in the habitable zone of a Sun-like star may be the best exoplanetary candidate for extraterrestrial surface water discovered to date, but is significantly larger than Earth and its actual composition is unknown]]
[[File:Kepler-22b System Diagram.jpg|thumb|[[Kepler-22b]], located in the habitable zone of a Sun-like star may be the best exoplanetary candidate for extraterrestrial surface water discovered to date, but is significantly larger than Earth and its actual composition is unknown]]
{{main|Habitable zone}}
{{main|Habitable zone}}
{{main|Mars Ocean Hypothesis}}
The concept of the Liquid Water Zone (or habitable zone) defines a region where water can exist on the surface and based on the properties of both the Earth and Sun. Under this model, Earth orbits roughly at the centre of this zone or in the "Goldilocks" position. The Earth is the only planet in the universe confirmed to possess large bodies of surface water. Venus, is on the hot side of the zone while Mars is on the cold side, neither are known to have persistent surface water, though evidence exists that Mars and it is speculated that Venus did have in their ancient pasts. Thus extrasolar planets (or moon) in the Goldilocks position with substantial atmospheres may more possess oceans and water clouds like those on Earth.
The concept of the Liquid Water Zone (or habitable zone) defines a region where water can exist on the surface and based on the properties of both the Earth and Sun. Under this model, Earth orbits roughly at the centre of this zone or in the "Goldilocks" position. The Earth is the only planet in the universe confirmed to possess large bodies of surface water. Venus, is on the hot side of the zone while Mars is on the cold side, neither are known to have persistent surface water, though evidence exists that Mars and it is speculated that Venus did have in their ancient pasts. Thus extrasolar planets (or moon) in the Goldilocks position with substantial atmospheres may more possess oceans and water clouds like those on Earth.


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However planets remarkably Earth-like may be found using less strict criteria. For example under certain conditions, such as strong greenhouse effect, atmospheric pressure or gravity, a planet could theoretically possess surface lakes and oceans without being strictly within the habitable zone. Indeed, Saturn's moon Titan is the only other body in the Solar System known to have surface liquid, however it is hydrocarbons rather than water. Other worlds may be similar to Earth, but have a largely dry or icy surface but with atmospheric water vapour, [[ground water]] or subsurface ocean, much like some arid and polar regions on Earth.
However planets remarkably Earth-like may be found using less strict criteria. For example under certain conditions, such as strong greenhouse effect, atmospheric pressure or gravity, a planet could theoretically possess surface lakes and oceans without being strictly within the habitable zone. Indeed, Saturn's moon Titan is the only other body in the Solar System known to have surface liquid, however it is hydrocarbons rather than water. Other worlds may be similar to Earth, but have a largely dry or icy surface but with atmospheric water vapour, [[ground water]] or subsurface ocean, much like some arid and polar regions on Earth.


==Candidates in the Solar System==
Early in the history of astronomy, [[Venus]] (and to a lesser extent [[Mars]] and [[Neptune]]) were thought to be Earth-like planets and some even conceptualised them to be home to extraterrestrial civilisation. Although these were later found to be misconceptions.

Still, scientists continue to find similarities with Mars and postulate that both ancient Venus and Mars could have been quite Earth-like.

===Mars===
{{see also|Water on Mars|Life on Mars|Colonization of Mars|Terraforming of Mars}}
[[File:Mars Earth Comparison.png|thumb|right|Size comparison of [[Earth]] and Mars.]]
Mars, the second closest planet, appears to have had and still have some similarities to Earth. Like Earth, Mars has an [[Atmosphere of Mars|atmosphere]] with a [[greenhouse effect]], [[Geography of Mars|geographical similarities]] including [[polar ice cap]]s, similar rotation, [[Volcanism on Mars|volcanic activity]] and evidence of [[Water on Mars|water]]. As such, Mars remains a candidate for [[Life on Mars|extraterrestrial life]]. It also makes human [[colonization of Mars]] a subject of much research.

However Mars is much smaller and lacks a magnetosphere and its year is almost twice as long. Its freezing climate, lower gravity and thin but toxic carbon dioxide atmosphere all make it hostile to Earth life.

====Ancient Mars====
[[Image:AncientMars.jpg|thumb|left|An artist's impression of ancient Mars and its oceans based on [[Mars Ocean Hypothesis#Observational evidence|geological data]]]]
Ancient Mars may have been quite Earth-like with a similar climate and liquid water.

=====Mars Ocean Hypothesis=====
{{main|Mars Ocean Hypothesis}}
The Mars Ocean Hypothesis states that nearly a third of the [[Geography of Mars|surface]] of [[Mars]] was covered by an ocean of liquid [[Water (molecule)|water]] early in the planet’s [[Geology of Mars|geologic history]].<ref name=Clifford>Clifford, S. M. and T. J. Parker, 2001: [http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6WGF-457CXN8-4&_user=126524&_rdoc=1&_fmt=&_orig=search&_sort=d&view=c&_acct=C000010360&_version=1&_urlVersion=0&_userid=126524&md5=f78bbc3ae211391e23070bd03d8e1dc6 The Evolution of the Martian Hydrosphere: Implications for the Fate of a Primordial Ocean and the Current State of the Northern Plains], Icarus 154, 40-79.</ref>
The Mars Ocean Hypothesis states that nearly a third of the [[Geography of Mars|surface]] of [[Mars]] was covered by an ocean of liquid [[Water (molecule)|water]] early in the planet’s [[Geology of Mars|geologic history]].<ref name=Clifford>Clifford, S. M. and T. J. Parker, 2001: [http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6WGF-457CXN8-4&_user=126524&_rdoc=1&_fmt=&_orig=search&_sort=d&view=c&_acct=C000010360&_version=1&_urlVersion=0&_userid=126524&md5=f78bbc3ae211391e23070bd03d8e1dc6 The Evolution of the Martian Hydrosphere: Implications for the Fate of a Primordial Ocean and the Current State of the Northern Plains], Icarus 154, 40-79.</ref>
This primordial ocean, dubbed Oceanus Borealis,<ref name=Baker>Baker, V. R., R. G. Strom, V. C. Gulick, J. S. Kargel, G. Komatsu and V. S. Kale, 1991: Ancient oceans, ice sheets and the hydrological cycle on Mars, Nature, 352, 589-594.</ref> would have filled the [[Vastitas Borealis]] basin in the northern hemisphere, a region which lies 4–5&nbsp;km (2.5–3 miles) below the mean planetary elevation, at a time period of approximately 3.8 billion years ago. Evidence for this ocean includes geographic features resembling ancient shorelines, and the chemical properties of the Martian soil and atmosphere. Early Mars would have required a denser atmosphere and warmer climate to allow liquid water to remain at the surface.<ref name=ReadandLewis>Read, Peter L. and S. R. Lewis, “The Martian Climate Revisited: Atmosphere and Environment of a Desert Planet”, Praxis, Chichester, UK, 2004.</ref>
This primordial ocean, dubbed Oceanus Borealis,<ref name=Baker>Baker, V. R., R. G. Strom, V. C. Gulick, J. S. Kargel, G. Komatsu and V. S. Kale, 1991: Ancient oceans, ice sheets and the hydrological cycle on Mars, Nature, 352, 589-594.</ref> would have filled the [[Vastitas Borealis]] basin in the northern hemisphere, a region which lies 4–5&nbsp;km (2.5–3 miles) below the mean planetary elevation, at a time period of approximately 3.8 billion years ago. Evidence for this ocean includes geographic features resembling ancient shorelines, and the chemical properties of the Martian soil and atmosphere. Early Mars would have required a denser atmosphere and warmer climate to allow liquid water to remain at the surface.<ref name=ReadandLewis>Read, Peter L. and S. R. Lewis, “The Martian Climate Revisited: Atmosphere and Environment of a Desert Planet”, Praxis, Chichester, UK, 2004.</ref>


A younger Venus is believed to have possessed Earth-like oceans,<ref>{{cite journal
===Venus===
{{see|Atmosphere of Venus|Volcanism on Venus|Terraforming of Venus}}
Venus is sometimes called Earth's "sister planet" (see below) due to the similar size, gravity, and bulk composition. Like Earth it has an [[Atmosphere of Venus|atmosphere]] with a [[greenhouse effect]] and [[cloud]]s, [[rain]] and is [[Volcanism on Venus|volcanically active]]. A younger Venus is believed to have possessed Earth-like oceans,<ref>{{cite journal
|author=Hashimoto, G. L.; Roos-Serote, M.; Sugita, S.; Gilmore, M. S.; Kamp, L. W.; Carlson, R. W.; Baines, K. H.
|author=Hashimoto, G. L.; Roos-Serote, M.; Sugita, S.; Gilmore, M. S.; Kamp, L. W.; Carlson, R. W.; Baines, K. H.
|title=Felsic highland crust on Venus suggested by Galileo Near-Infrared Mapping Spectrometer data
|title=Felsic highland crust on Venus suggested by Galileo Near-Infrared Mapping Spectrometer data
Line 160: Line 144:
|pages=E00B24
|pages=E00B24
|bibcode=2008JGRE..11300B24H
|bibcode=2008JGRE..11300B24H
}}</ref> but these evaporated as the temperature rose. This may be due to the fact that Venus, owing to its slow rotation, does not have a significant magnetic field, allowing the constituent atoms of the water to be blown away by the [[solar wind]].<ref>{{citation | last = | first = | title =Caught in the wind from the Sun | date =July 12, 2008}}</ref> However, the extreme heat on present day Venus, combined with the crushing atmosphere composed of toxic carbon dioxide and sulfuric acid rain makes the surface hostile to Earth life. The possibility that a habitable niche exists in the lower and middle cloud layers of Venus can not yet be excluded.<ref>{{citation
}}</ref> but these evaporated as the temperature rose. This may be due to the fact that Venus, owing to its slow rotation, does not have a significant magnetic field, allowing the constituent atoms of the water to be blown away by the [[solar wind]].<ref>{{citation | last = | first = | title =Caught in the wind from the Sun | date =July 12, 2008}}</ref>
| last1=Cockell | first1=C. S.
| title=Life on Venus
| journal=Planetary and Space Science
| volume=47 | issue=12 | pages=1487–1501
| month=December | year=1999
| doi=10.1016/S0032-0633(99)00036-7
| bibcode=1999P&SS...47.1487C }}</ref>

===Saturn's moon Titan===
[[File:Titan multi spectral overlay.jpg|right|thumb|Saturn's moon Titan]]
{{see|Life on Titan|Lakes of Titan|Colonization of Titan}}

[[Saturn]]'s moon [[Titan (moon)|Titan]] has some Earth-like properties. Titan's geography has similarities to Earth and is known to have a dense [[celestial body atmosphere|atmosphere]],<ref Name=NasaNews>
{{cite web
|title=News Features: The Story of Saturn
|url=http://saturn.jpl.nasa.gov/news/features/saturn-story/moons.cfm
|work=Cassini-Huygens Mission to Saturn & Titan
|publisher=NASA & [[Jet Propulsion Lab|JPL]]
|accessdate=2007-01-08
}}</ref> with [[cloud]]s and [[rain]] and the only object other than Earth for which clear evidence of stable bodies of surface liquid has been found.<ref name=NatureDefinitive>{{cite journal|title=The lakes of Titan|author=Stofan, E. R.|coauthors= ''et al.''|issue=1 |volume=445|pages=61–64|journal=Nature|year=2007|doi= 10.1038/nature05438|pmid=17203056|bibcode = 2007Natur.445...61S }}</ref>

The possibility of [[life on Titan]] is a subject of ongoing research.

In billions of years, Titan may become Earth-like as the solar system's habitable zone moves farther out.

However Titan is much smaller than Earth, it has a lower gravity and its composition including its toxic methane atmosphere and [[anti-greenhouse effect]] is hostile to Earth life.

==Extrasolar Earth analog==
[[File:Planet Kepler-22b.jpg|thumb|left|220px|Artist's rendering of Kepler-22b, a possible Earth analog which orbits a sun-like star some 600 light years away.]]

The [[mediocrity principle]] suggests that there is a chance that serendipitous events may have allowed an Earth-like planet to form elsewhere that would allow the emergence of complex, multi-cellular life. However, the [[Rare Earth hypothesis]] asserts that if the strictest criteria are applied, such a planet, if it exists may be so far away that humans may never locate it.


===Axial Tilt and Rotation===
Because the [[Solar System]] proved to be devoid of an Earth analog, the search has widened to [[extrasolar planet]]s. Astrobiologists assert that Earth analogs would most likely be found in a stellar [[habitable zone]] in which liquid water could exist, providing the conditions for supporting life. Some astrobiologists, such as [[Dirk Schulze-Makuch]] have theorised that a sufficiently massive [[natural satellite]] may form a [[habitable moon]] similar to Earth.
[[Image:AxialTiltObliquity.png|thumb|right|Earth's axial tilt is 23.44°.]]
The [[Axial Tilt]] of Earth is believed to play a large role in stabilising climate and is the cause of seasonal changes in climate. The Earth's axial tilt varies between 22.1° and 24.5° and is stabilized by the Moon. In addition to this steady decrease there are much smaller short term (18.6 years) variations, known as [[nutation]], mainly due to the changing plane of the moon's orbit. This can shift the Earth's axial tilt by plus or minus 0.005 degree.


The closest axial tilt of a terrestrial planet is [[astronomy on Mars|Mars]]. Though its tilt is within a similar range, its range is also less stable, believed to be between 11° and 49° as a result of gravitational perturbations from other planets.<ref>{{cite journal | last = Touma | first = Jihad | coauthors = Wisdom, Jack | bibcode=1993Sci...259.1294T | title = The Chaotic Obliquity of Mars | journal = Science | volume = 259 | pages = 1294–7 | year = 1993 | doi = 10.1126/science.259.5099.1294 | pmid = 17732249 | issue = 5099}}</ref> Mars like Earth experiences seasons. Venus, however has a miniscule axial tilt.
A 2011 estimate by the NASA's [[Jet Propulsion Laboratory]] (JPL), based on observations from the [[Kepler (spacecraft)|Kepler mission]], determined that about "1.4 to 2.7 percent" of all sun-like stars are expected to have earth-like planets "within the [[habitable zone]]s of their stars". This means there are "two billion" such worlds in the Milky Way galaxy. Assuming that all galaxies have a similar number as the Milky Way, in the 50 billion known galaxies there may be as many as one [[sextillion]].<ref name="ChoiCQ"/>


[[Earth's rotation]] creates a day/night cycle. The day of Mars is very similar to Earth's while other terrestrial planets, such as Venus and Mercury have extremely long days in comparison due to [[tidal forces]].
Perhaps one of the most promising Earth analogs to date, [[Kepler-22b]] was confirmed December 5, 2011.<ref name="bbc20111205">BBC NEWS, "Kepler 22-b: Earth-like planet confirmed" 12/5/2011 http://www.bbc.co.uk/news/science-environment-16040655</ref> orbiting the habitable zone of a sun-like main sequence star. At 2.4 times the size of Earth {{Citation needed|date=February 2012}}it has an estimated surface temperature around 22 degrees Celsius, however the nature of the planet is still unknown.


==Terraforming==
==Terraforming==

Revision as of 04:37, 9 March 2012

The planet Earth

An Earth analog (also referred to as a Twin Earth, Earth Twin, Second Earth, Alien Earth, Earth 2 or Earth-like planet) is a theoretical other planet (or world) with conditions similar to Earth.

The possibility is of particular interest to humans as it is easily inferred that the more similar a planet is to Earth, the more likely it is of sustaining Earth-like complex extraterrestrial life and more importantly, civilization. As such it has long been speculated and the subject expressed in science, philosophy, science fiction and popular culture.

Advocates of space colonization have long sought an Earth Analog as a "second home" while advocates for space and survival would regard such a planet as a potential "new home".

Some scientific theories speculate that Earth analogs, such as ancient Mars and Venus may have existed in our Solar System in the past and that in the distant future Titan may naturally become one or that technology may be used to artificially produce one by means of terraforming, virtual reality or simulated reality.

Technological advances in extrasolar planet detection are rapidly refining the probabilities of a real discovery, not just in this universe, but in the present Milky Way galaxy. Although the distribution and attributes of the studied planets are still very much unknown, current calculations suggest that they may be relatively common in the universe. 2011 estimates by the NASA's Jet Propulsion Laboratory (JPL) based on observations from the Kepler mission determined that about "1.4 to 2.7 percent" of all sun-like stars are expected to have earthlike planets "within the habitable zones of their stars". This means there are "two billion" of them in our own Milky Way galaxy alone and assuming that all galaxies have a similar number as the Milky Way, in the 50 billion galaxies in the observable universe there may be as many as a sextillion.[1]

The mediocrity principle suggests that there is a chance that serendipitous events may have allowed an Earth-like planet to form elsewhere that would allow the emergence of complex, multi-cellular life. Philosophers have pointed out that the size of the universe is such that a near identical planet must exists somewhere, such theories include the philosophy of Multiverse and the Twin Earth thought experiment. However, the Rare Earth hypothesis asserts that if the strictest criteria are applied, a true Earth Analog, should such a planet exist may be so far away that humans may never locate it.

The more recent serious scientific findings have greatly influenced the scope of the fields of astrobiology, models of planetary habitability and Search for Extraterrestrial Intelligence. Astrobiologists assert that Earth analogs would most likely be found in a stellar habitable zone in which liquid water could exist, providing also the conditions for supporting life. Some astrobiologists, such as Dirk Schulze-Makuch have theorised that a sufficiently massive natural satellite may form a habitable moon similar to Earth. NASA and the SETI Institute have proposed categorising the increasing number of Earth-like planets found using a measure called the Earth Similarity Index (ESI) based on mass, radius and temperature.[2][3] According to this measure, the confirmed planets most similar to Earth are Gliese 667C c (0.85)[4], Kepler 22b[5] and HD 85512 b (0.79), Gliese 581 d (0.74), Mars and Gliese 581c (0.70).[6]

History

Around 400BC, Philolaus proposed that there existed a Counter-Earth, a counter-balance of the same mass to prevent the universe from being flung apart.

Between 1858 and 1920, Mars was believed by many, including some scientists, to be very similar to Earth, only drier with a thick atmosphere, similar axial tilt, orbit and seasons as well as a Martian civilisation that had built great Martian canals. These theories were advanced by Giovanni Schiaparelli, Percival Lowell and others. As such Mars in fiction portrayed the red planet as similar to Earth but with a desert like landscape. Images and data from the Mariner and Viking space probes, however, portrayed the planet as a dead cratered world. Although with continuing discoveries many Earth comparisons remained. The Mars Ocean Hypothesis, having had its seeds sown from the Viking missions and popularised during the 1980s,[7] speculation began that Mars was once much more Earth-like and could have actually given origin to life.

Likewise, until the 1960s, Venus was believed by many, including some scientists, to be a warmer version of Earth with a thick atmosphere and either hot and dusty or humid with water clouds and oceans. Venus in fiction was often portrayed as having similarities to Earth and many speculated about Venusian civilisation. These beliefs were dispelled in the 1960s as the first space probes gathered more accurate scientific data on the planet and found that Venus is a hellish world with the surface temperature around 900 °F (482 °C) under the atmosphere 92 times thicker the Earth's.

Attributes and Criteria

The probability of finding an Earth analog depends mostly on the attributes which are expected to be similar, and these vary greatly. Generally it is considered that it would be a terrestrial planet and there have been several scientific studies aimed at finding such planets. Often implied but not limited to are such criteria as planet size, star size and type (i.e. Solar analog), orbital distance and stability, axial tilt and rotation, similar geography, oceans, air and weather conditions, strong magnetosphere and even the presence Earth-like complex life (possibly through convergent evolution or parallel evolution). If there is complex life, there could be some forests covering much of the land. If there is intelligent life, some parts of land could be covered in cities. Some things that are assumed of such a planet may be unlikely due to Earth's own history. For instance the Earth's atmosphere was not always oxygen-rich and this is a biosignature from the emergence of photosynthetic life. The formation, presence, influence on these characteristics of the moon (such as tidal forces) may also pose a problem in finding an Earth analog.

Size

Size Comparisons: Kepler-20e[8] and Kepler-20f[9] with Venus and Earth.

Size is often thought to be an effective measure as planets of Earth's size are thought more likely to be terrestrial in nature and be capable of retaining a significant atmosphere.

The closest planets and natural satellites to Earth's size are:

Name Earth Masses (Me) Earth Radii (Re) Note
Kepler-22b < 36 2.4 Much larger. Within the HZ of solar analog.
Gliese 667 Cc 4.5 - Within the HZ of red dwarf. Significantly less massive than Kepler-22b.
55 Cancri e 8.63 2 much larger
Kepler-9d ? 1.64 larger
COROT-7b <9 1.58 larger
Kepler-10b 4.56 1.416 larger
Kepler-20f < 14.3[9] 1.03[9] slightly larger and likely more massive
Earth 1 1
Venus 0.815 0.949 slightly smaller
Kepler-20e < 3.08[8] 0.87[8] smaller
KOI-961.01 0.78[10] smaller
KOI-961.02 0.73[10] smaller
KOI-961.03 0.57[10] much smaller
Mars 0.107 0.533 much smaller
Ganymede 0.025 0.413 much smaller
Titan 0.0225 0.404 much smaller

This comparison indicates that size alone is a poor measure, particularly in terms of habitability. Temperature must also be considered as Venus and the planets of Kepler-20 (discovered in 2011[11][12]), COROT-7b and the three planets of KOI-961 (confirmed in 2012) are incredibly hot and Mars, Ganymede and Titan are frigid worlds, resulting also in wide variety of surface and atmospheric conditions. The mass of the Solar System's moons are a tiny fraction of that of Earth whereas the mass of extrasolar planets are very difficult to accurately measure. However discoveries of Earth-sized exoplanets are important as they may indicate the probable frequency and distribution of Earth-like planets. One of the first steps to finding more Earth-like planets may be shortlisting candidates of similar size and then comparing their temperatures to that of Earth.

Terrestrial

Although cold and dry, much of the surface and topography of Mars bears similarities to that of arid regions on Earth

Another criteria often cited is that an Earth analog must be terrestrial, that is, it should possess a similar surface geology - a planetary surface composed of similar surface materials. The closest known example is Mars and Titan and while there are similarities in their types of landforms and surface compositions there are also significant differences.

Many of Earth's surface materials and landforms are formed as a result of interaction with water (such as clay and sedimentary rocks) or as a byproduct of organic life (such as limestone or coal), interaction with the atmosphere, volcanically or artificially.

A true Earth analog therefore might need to have formed through similar processes, having possessed an atmosphere, volcanic interactions with the surface, past or present liquid water and lifeforms.

The Geography of Mars and of Titan in particular appear to include many features similar to Earth.

Temperature

There are several factors that can determine planetary temperatures and therefore several measures that can draw direct comparisons to that of the Earth in planets where atmospheric conditions are unknown.. Equilibrium temperature is used for planets without atmospheres. With atmospheres, a greenhouse effect is assumed. Finally surface temperature is used. Each of these temperatures is of course affected by climate which is influenced by the orbit and rotation (or tidal locking) of the planet, each which introduces further variabilities.

Below is a comparison of the confirmed planets with the closest known temperatures to Earth.

Temperature
comparisons
Venus Earth Kepler 22b Mars
Global
Equilibrium
Temperature
307 K
34 °C
93 °F
255 K
−18 °C
−0.4 °F
262 K
−11 °C
22.2 °F
206 K
−67 °C
−88.6 °F
+ Venus'
GHG effect
737 K
464 °C
867 °F
+ Earth's
GHG effect
288 K
15 °C
59 °F
295 K
22 °C
71.6 °F
+ Mars'
GHG effect
210 K
−63 °C
−81 °F
Tidally
locked
Almost No Unknown No
Global
Bond Albedo
0.9 0.29 Unknown 0.25
Refs.[13][14][15]

Solar Analog

Another criteria of an Earth Analog is that it should orbit a Solar Analog, that is, a star much like our own sun, similar photometrically or in terms of spectral type. It follows that the composition of a planet around a Solar Twin with similar metallicity might have a similar composition to Earth. Also this would help eliminate stellar extremes and variability that may be applicable to other types of stars.

While planets have been discovered orbiting similar stars to the Sun, most are gas giant or Super-Earth sized, and additionally many of these planetary systems have proven to be surprisingly different to our own.

Kepler-22, the parent star of Kepler-22b is slightly smaller and cooler than the Sun.

This measure is not entirely reliable as Mars and Venus also orbit the Sun but have different compositions and properties.

Surface-water and hydrological cycle

Water covers 70% of Earth's surface and is required by all known life.
Kepler-22b, located in the habitable zone of a Sun-like star may be the best exoplanetary candidate for extraterrestrial surface water discovered to date, but is significantly larger than Earth and its actual composition is unknown

The concept of the Liquid Water Zone (or habitable zone) defines a region where water can exist on the surface and based on the properties of both the Earth and Sun. Under this model, Earth orbits roughly at the centre of this zone or in the "Goldilocks" position. The Earth is the only planet in the universe confirmed to possess large bodies of surface water. Venus, is on the hot side of the zone while Mars is on the cold side, neither are known to have persistent surface water, though evidence exists that Mars and it is speculated that Venus did have in their ancient pasts. Thus extrasolar planets (or moon) in the Goldilocks position with substantial atmospheres may more possess oceans and water clouds like those on Earth.

Some argue that a true Earth Analog must not only have a similar position of its planetary system but also orbit a Solar Analog and have a near circular orbit such that it remains continually habitable like the Earth.

The best candidates to date by these measure is Kepler-22b, it orbits a Sun-like star in a similar position within the habitable zone, however it is much larger than Earth and its composition is currently unknown. Our Solar System has shown that just being in the habitable zone does not guarantee that a planet is "Earth-like".

In addition to surface water, a true Earth-Analog would require a mix of oceans or lakes and areas not covered by water, or land.

However planets remarkably Earth-like may be found using less strict criteria. For example under certain conditions, such as strong greenhouse effect, atmospheric pressure or gravity, a planet could theoretically possess surface lakes and oceans without being strictly within the habitable zone. Indeed, Saturn's moon Titan is the only other body in the Solar System known to have surface liquid, however it is hydrocarbons rather than water. Other worlds may be similar to Earth, but have a largely dry or icy surface but with atmospheric water vapour, ground water or subsurface ocean, much like some arid and polar regions on Earth.

The Mars Ocean Hypothesis states that nearly a third of the surface of Mars was covered by an ocean of liquid water early in the planet’s geologic history.[16] This primordial ocean, dubbed Oceanus Borealis,[17] would have filled the Vastitas Borealis basin in the northern hemisphere, a region which lies 4–5 km (2.5–3 miles) below the mean planetary elevation, at a time period of approximately 3.8 billion years ago. Evidence for this ocean includes geographic features resembling ancient shorelines, and the chemical properties of the Martian soil and atmosphere. Early Mars would have required a denser atmosphere and warmer climate to allow liquid water to remain at the surface.[18]

A younger Venus is believed to have possessed Earth-like oceans,[19] but these evaporated as the temperature rose. This may be due to the fact that Venus, owing to its slow rotation, does not have a significant magnetic field, allowing the constituent atoms of the water to be blown away by the solar wind.[20]

Axial Tilt and Rotation

Earth's axial tilt is 23.44°.

The Axial Tilt of Earth is believed to play a large role in stabilising climate and is the cause of seasonal changes in climate. The Earth's axial tilt varies between 22.1° and 24.5° and is stabilized by the Moon. In addition to this steady decrease there are much smaller short term (18.6 years) variations, known as nutation, mainly due to the changing plane of the moon's orbit. This can shift the Earth's axial tilt by plus or minus 0.005 degree.

The closest axial tilt of a terrestrial planet is Mars. Though its tilt is within a similar range, its range is also less stable, believed to be between 11° and 49° as a result of gravitational perturbations from other planets.[21] Mars like Earth experiences seasons. Venus, however has a miniscule axial tilt.

Earth's rotation creates a day/night cycle. The day of Mars is very similar to Earth's while other terrestrial planets, such as Venus and Mercury have extremely long days in comparison due to tidal forces.

Terraforming

Artist's conception of a terraformed Venus, a potential Earth analog

Terraforming (literally, "Earth-forming") of a planet, moon, or other body is the hypothetical process of deliberately modifying its atmosphere, temperature, surface topography or ecology to be similar to those of Earth to make it habitable by terran organisms.

Due to proximity and similarity in size, Mars and to a lesser extent Venus are seen as the most likely candidates for terraforming.

References

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  2. ^ http://www.wired.co.uk/news/archive/2011-11/21/exoplanet-indices
  3. ^ Stuart Gary New approach in search for alien life ABC Online. November 22, 2011
  4. ^ http://phl.upr.edu/projects/habitable-exoplanets-catalog/data
  5. ^ Updates on Exoplanets during the First Kepler Science Conference
  6. ^ Dirk Schulze-Makuch, Abel Méndez, Alberto G. Fairén, Philip von Paris, Carol Turse, Grayson Boyer, Alfonso F. Davila, Marina Resendes de Sousa António, David Catling, and Louis N. Irwin. Astrobiology. doi:10.1089/ast.2010.0592. October 21, 2011
  7. ^ NASA - Mars Ocean Hypothesis
  8. ^ a b c NASA Staff (20 December 2011). "Kepler: A Search For Habitable Planets - Kepler-20e". NASA. Retrieved 2011-12-23.
  9. ^ a b c NASA Staff (20 December 2011). "Kepler: A Search For Habitable Planets - Kepler-20f". NASA. Retrieved 2011-12-23.
  10. ^ a b c Major, Jason (Jan 11, 2012). "KEPLER SPOTS TINIEST TRIO OF EXOPLANETS". Discovery News. Retrieved 2012-01-12.
  11. ^ Johnson, Michele (20 December 2011). "NASA Discovers First Earth-size Planets Beyond Our Solar System". NASA. Retrieved 2011-12-20.
  12. ^ Hand, Eric (20 December 2011). "Kepler discovers first Earth-sized exoplanets". Nature. doi:10.1038/nature.2011.9688.
  13. ^ "NASA, Mars: Facts & Figures". Retrieved 2010-01-28.
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  15. ^ Mallama, A. (2007). "The magnitude and albedo of Mars". Icarus. 192 (2): 404–416. Bibcode:2007Icar..192..404M. doi:10.1016/j.icarus.2007.07.011.
  16. ^ Clifford, S. M. and T. J. Parker, 2001: The Evolution of the Martian Hydrosphere: Implications for the Fate of a Primordial Ocean and the Current State of the Northern Plains, Icarus 154, 40-79.
  17. ^ Baker, V. R., R. G. Strom, V. C. Gulick, J. S. Kargel, G. Komatsu and V. S. Kale, 1991: Ancient oceans, ice sheets and the hydrological cycle on Mars, Nature, 352, 589-594.
  18. ^ Read, Peter L. and S. R. Lewis, “The Martian Climate Revisited: Atmosphere and Environment of a Desert Planet”, Praxis, Chichester, UK, 2004.
  19. ^ Hashimoto, G. L.; Roos-Serote, M.; Sugita, S.; Gilmore, M. S.; Kamp, L. W.; Carlson, R. W.; Baines, K. H. (2008). "Felsic highland crust on Venus suggested by Galileo Near-Infrared Mapping Spectrometer data". Journal of Geophysical Research, Planets. 113: E00B24. Bibcode:2008JGRE..11300B24H. doi:10.1029/2008JE003134.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  20. ^ Caught in the wind from the Sun, July 12, 2008
  21. ^ Touma, Jihad (1993). "The Chaotic Obliquity of Mars". Science. 259 (5099): 1294–7. Bibcode:1993Sci...259.1294T. doi:10.1126/science.259.5099.1294. PMID 17732249. {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)