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JOM (journal)
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JOM
Former names
Journal of Metals
ISO 4 abbreviation
Find out here
Discipline
Materials science
Language
English
Edited by
Justin A. Scott, Maureen Byko
Publication details
Publisher
The Minerals, Metals & Materials Society (TMS), Springer Science+Business Media
Publication history
1949–present
Frequency
Monthly
Impact factor
(2016)
1.860
Indexing
ISSN
1047-4838 (print)
1543-1851 (web)
Links
Journal homepage
Web-enhanced JOM archive (1997 to 2011)
JOM is a technical journal devoted to exploring the many aspects of materials, science and engineering published monthly by The Minerals, Metals & Materials Society (TMS) (a member-based professional society).[1] JOM reports scholarly work that explores the many aspects of materials science and engineering within the broad topical areas of light metals, structural materials, functional materials, extraction and processing, and materials processing and manufacturing. JOM strives to balance the interests of the laboratory and the marketplace by reporting academic, industrial, and government-sponsored work from around the world.
History[edit]
From 1949 through 1988, the journal was named Journal of Metals. With materials systems becoming commonplace and with the journal frequently covering composites, plastics, and other materials, its name was changed to JOM. It is published by TMS, which is headquartered in Pittsburgh, Pennsylvania.[2]
Many articles can be viewed free, online at Springerlink.[3]
References[edit]
Jump up ^ "JOM-Springer". Springer Science+Business Media. Retrieved 9 May 2017.
Jump up ^ Charles R. Lord (1 January 2000). Guide to Information Sources in Engineering. Libraries Unlimited. p. 83. ISBN 978-1-56308-699-1. Retrieved 26 December 2015.
Jump up ^ "About JOM". The Minerals, Metals & Materials Society (TMS). Retrieved 9 July 2007.
External links[edit]
JOM home page
Open-access JOM articles

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Extraterrestrial skies
From Wikipedia, the free encyclopedia
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For the view from above the astronomical object's surface, see Extraterrestrial atmospheres.
This article possibly contains original research. Please improve it by verifying the claims made and adding inline citations. Statements consisting only of original research should be removed. (November 2013) (Learn how and when to remove this template message)
A historic extraterrestrial sky—the Earth viewed from the Moon, Apollo 8 mission, Lunar orbit, December 24, 1968
In astronomy, an extraterrestrial sky is a view of outer space from the surface of a planet other than Earth.
The only extraterrestrial sky that has been directly observed and photographed by astronauts is that of the Moon. The skies of Titan, Mars, and Venus have been observed by space probes designed to land on the surface and transmit images back to Earth.
Characteristics of extraterrestrial skies appear to vary substantially due to a number of factors. An extraterrestrial atmosphere, if present, has a large bearing on visible characteristics. The atmosphere's density and chemical composition can contribute to differences in colour, opacity (including haze) and the presence of clouds. Astronomical objects may also be visible and can include natural satellites, rings, star systems and nebulas and other planetary system bodies.
For skies that have not been directly or indirectly observed, their appearance can be simulated based on known parameters, such as the position of astronomical objects relative to the surface and atmospheric composition.
Contents
1 Luminosity and angular diameter of the Sun
2 Horizon
3 Mercury
3.1 The Sun from Mercury
3.2 Other planets seen from Mercury
4 Venus
5 The Moon
5.1 The Sun from the Moon
5.2 The Earth from the Moon
5.3 Eclipses from the Moon
6 Mars
6.1 The color of the Martian sky
6.2 The Sun from Mars
6.3 Mars's moons as seen from Mars
6.4 Earth from Mars
6.5 Venus from Mars
6.6 The outer planets
6.7 The skies of Mars's moons
7 The Asteroid Belt
7.1 87 Sylvia and its moons Romulus and Remus
7.2 243 Ida and its moon Dactyl
8 Jupiter
8.1 Jupiter's moons as seen from Jupiter
8.2 The skies of Jupiter's moons
9 Saturn
9.1 The skies of Saturn's moons
9.1.1 The rings from Saturn's moons
9.1.2 The sky of Titan
9.1.3 The sky of Enceladus
10 Uranus
11 Neptune
11.1 The sky of Triton
12 Trans-Neptunian Objects
12.1 Pluto and Charon
12.2 50000 Quaoar and its moon Weywot
13 Comets
14 Extrasolar planets
14.1 Basics
14.2 View from nearby stars (0 – 10 ly)
14.3 View from more distant stars (10 ly – )
14.4 Recent developments
15 See also
16 Notes
17 References
18 Further reading
19 External links
Luminosity and angular diameter of the Sun[edit]
Main article: Angular diameter
The Sun's apparent magnitude changes according to the inverse square law, therefore, the difference in magnitude as a result of greater or lesser distances from different celestial bodies can be predicted by the following formula:
intensity ∝ 1 distance 2 {\displaystyle {\text{intensity}}\ \propto \ {\frac {1}{{\text{distance}}^{2}}}\,}
Where "distance" can be in km, au, or any other appropriate unit.
To illustrate, since Pluto is 40 au away from the Sun on average, it follows that the parent star would appear to be 1,600 times dimmer than it is on Earth.
Though a terrestrial observer would find a dramatic decrease in available sunlight in these environments, the Sun would still be bright enough to cast shadows even as far as the hypothetical Planet Nine, possibly located 1,200 AU away, and would still outshine the full Moon.
The change in angular diameter of the sun with distance is illustrated in the diagram below:
Diagram for the formula of the angular diameter
The angular diameter of a circle whose plane is perpendicular to the displacement vector between the point of view and the centre of said circle can be calculated using the formula[1]
δ = 2 arctan  ( d 2 D ) , {\displaystyle \delta =2\arctan \left({\frac {d}{2D}}\right),}
in which δ {\displaystyle \delta } is the angular diameter, and d {\displaystyle d} and D {\displaystyle D} are the actual diameter of and the distance to the object. When D ≫ d {\displaystyle D\gg d} , we have δ ≈ d / D {\displaystyle \delta \approx d/D} , and the result obtained is in radians.
For a spherical object whose actual diameter equals d a c t , {\displaystyle d_{\mathrm {act} },} and where D {\displaystyle D} is the distance to the centre of the sphere, the angular diameter can be found by the formula
δ = 2 arcsin  ( d a c t 2 D ) {\displaystyle \delta =2\arcsin \left({\frac {d_{\mathrm {act} }}{2D}}\right)}
The difference is due to the fact that the apparent edges of a sphere are its tangent points, which are closer to the observer than the centre of the sphere. For practical use, the distinction is only significant for spherical objects that are relatively close, since the small-angle approximation holds for x ≪ 1 {\displaystyle x\ll 1} :[2]
arcsin  x ≈ arctan  x ≈ x {\displaystyle \arcsin x\approx \arctan x\approx x} .
Differences in how the sun appears can be visualized with this chart:
Comparison of angular diameter of the Sun, Moon and planets. To get a true representation of the sizes, view the image at a distance of 103 times the width of the "Moon: max." circle. For example, if this circle is 10 cm wide on your monitor, view it from 10.3 m away.
Horizon[edit]
On terrestrial planets and other solid celestial bodies with negligible atmospheric effects, the distance to the horizon for a "standard observer" varies as the square root of the planet's radius. Thus, the horizon on Mercury is 62% as far away from the observer as it is on Earth, on Mars the figure is 73%, on the Moon the figure is 52%, on Mimas the figure is 18%, and so on. For smaller, non-spherical objects, the observer's height must be taken into account when calculating the distance to the horizon.
Mercury[edit]
Because Mercury has little or no atmosphere, a view of the planet's skies would be no different from viewing space from orbit. Mercury has a southern pole star, α Pictoris, a magnitude 3.2 star. It is fainter than Earth's Polaris (α Ursae Minoris).[3]
The Sun from Mercury[edit]
On average, the visible diameter of the Sun on Mercury is 2.5 times as large as it appears from Earth, and its total brightness is more than 6 times as great. Because of the planet's eccentric orbit, the Sun's apparent size in the sky would vary from 2.2 times that from Earth at aphelion (with total brightness 4.8 times as great), to 3.2 times at perihelion (with total brightness 10.2 times as great).
Mercury has a 3:2 spin–orbit resonance. This means that although a sidereal day (the period of rotation) lasts around 58.7 Earth days, a solar day (the length between two meridian transits of the Sun) lasts around 176 Earth days. (In contrast, the difference between Earth's sidereal and solar days is only 4 minutes.)
The large eccentricity of Mercury's orbit coupled with the long length of a Mercurian day results in an unusual effect in which the Sun appears to briefly reverse its usual east-to-west motion once every Mercurian year. The on-sky distance over which the Sun appears to be travelling in this reversed (west-to-east) direction is slightly larger than the apparent size of the Sun itself. Thus, while the effect is visible wherever one happens to be on Mercury, there are certain points on Mercury's surface where an observer would be able to see the Sun rise, reverse and set, and then rise again, all within the same Mercurian day.[4]
The apparent motion reverses because approximately four (Earth) days prior to perihelion, the angular speed of Mercury's orbit exactly equals its rotational velocity, so that the Sun's apparent motion ceases. At perihelion, Mercury's orbital angular velocity slightly exceeds the rotational velocity, so the Sun appears to be retrograde. Four days after perihelion, the Sun's normal apparent motion resumes. Because of its spin–orbit resonance, Mercury presents one of two spots of its surface to the Sun on alternate perihelia. One of these subsolar points is Caloris Planitia ("hot basin"), appropriately named because an observer near its centre would see the Sun loop around the zenith once per Mercurian day, and hence experience a very hot day indeed.
Other planets seen from Mercury[edit]
After the Sun, the second-brightest object in the Mercurian sky is Venus, which is much brighter than for terrestrial observers. The reason for this is that when Venus is closest to Earth, it is between the Earth and the Sun, so we see only its night side. Indeed, even when Venus is brightest in the Earth's sky, we are actually seeing only a narrow crescent. For a Mercurian observer, on the other hand, Venus is closest when it is in opposition to the Sun and is showing its full disk. The apparent magnitude of Venus is as bright as −7.7.[5]
The Earth and the Moon are also very prominent, their apparent magnitudes being about −5[5] and −1.2, respectively. The maximum apparent distance between the Earth and the Moon is about 15′. All other planets are visible just as they are on Earth, but somewhat less bright at opposition.
The zodiacal light is probably more prominent than it is from Earth.
Venus[edit]
The atmosphere of Venus is so thick that the Sun is not distinguishable in the daytime sky, and the stars are not visible at night. Color images taken by the Soviet Venera probes suggest that the sky on Venus is orange.[6] If the Sun could be seen from Venus's surface, the time from one sunrise to the next (a solar day) would be 116.75 Earth days. Because of Venus's retrograde rotation, the Sun would appear to rise in the west and set in the east.[7]
An observer aloft in Venus's cloud tops, on the other hand, would circumnavigate the planet in about four Earth days and see a sky in which Earth and the Moon shine brightly (about magnitudes −6.6[5] and −2.7, respectively) at opposition. Mercury would also be easy to spot, because it is closer and brighter, at up to magnitude −2.7,[5] and because its maximum elongation from the Sun is considerably larger (40.5°) than when observed from Earth (28.3°).
The Moon[edit]
Earth from the Moon
(October 12, 2015)
The Moon's atmosphere is negligibly thin, essentially vacuum, so its sky is always black, as in the case of Mercury. However, the Sun is so bright that it is impossible to see stars during the daytime, unless the observer is well shielded from sunlight (direct or reflected from the ground). The Moon has a southern polar star, δ Doradus, a magnitude 4.34 star. It is better aligned than Earth's Polaris (α Ursae Minoris), but much fainter.
The Sun from the Moon[edit]
The Sun looks the same from the Moon as it does from Earth's orbit, somewhat brighter than it does from the Earth's surface, and colored pure white, due to the lack of atmospheric scattering and absorption.
Since the Moon's axial tilt relative to its orbit around the Sun is nearly zero, the Sun traces out almost exactly the same path through the Moon's sky over the course of a year. As a result, there are craters and valleys near the Moon's poles that never receive direct sunlight, and there may exist mountains and hilltops that are never in shadow (see Lunar south pole and Peak of eternal light).
The Earth from the Moon[edit]
Apollo 17 commander Eugene Cernan on the Moon, with Earth visible in the sky
Among the most prominent features of the Moon's sky is Earth. Earth's angular diameter (1.9°) is four times the Moon's as seen from Earth, although because the Moon's orbit is eccentric, Earth's apparent size in the sky varies by about 5% either way (ranging between 1.8° and 2.0° in diameter). Earth shows phases, just like the Moon does for terrestrial observers. The phases, however, are opposite; when the terrestrial observer sees the full Moon, the lunar observer sees a "new Earth", and vice versa. Earth's albedo is three times as high as that of the Moon (due in part to its whitish cloud cover), and coupled with the wider area, the full Earth glows over 50 times brighter than the full Moon at zenith does for the terrestrial observer. This Earth light reflected on the Moon's un-sunlit half is bright enough to be visible from Earth, even to the unaided eye – a phenomenon known as earthshine.
As a result of the Moon's synchronous rotation, one side of the Moon (the "near side") is permanently turned towards Earth, and the other side, the "far side", mostly cannot be seen from Earth. This means, conversely, that Earth can only be seen from the near side of the Moon and would always be invisible from the far side. If the Moon's rotation were purely synchronous, Earth would not have any noticeable movement in the Moon's sky. However, due to the Moon's libration, Earth does perform a slow and complex wobbling movement. Once a month, as seen from the Moon, Earth traces out an approximate oval 18° in diameter. The exact shape and orientation of this oval depend on one's location on the Moon. As a result, near the boundary of the near and far sides of the Moon, Earth is sometimes below the horizon and sometimes above it.
Eclipses from the Moon[edit]
From space, the Moon's shadow during the solar eclipse of March 9, 2016 appears as a dark spot moving across the Earth.
Earth and the Sun sometimes meet in the lunar sky, causing an eclipse. On Earth, one would see a lunar eclipse, when the Moon passes through the Earth's shadow; meanwhile on the Moon, one would see a solar eclipse, when the Sun goes behind the Earth. Since the apparent diameter of the Earth is four times as large as that of the Sun, the Sun would be hidden behind the Earth for hours. Earth's atmosphere would be visible as a reddish ring. During the Apollo 15 mission, an attempt was made to use the Lunar Roving Vehicle's TV camera to view such an eclipse, but the camera or its power source failed after the astronauts left for Earth.[8]
Terrestrial solar eclipses, on the other hand, would not be as spectacular for lunar observers because the Moon's umbra nearly tapers out at the Earth's surface. A blurry dark patch would barely be visible. The effect would be comparable to the shadow of a golf ball cast by sunlight on an object 4.572 m (15 ft) away. Lunar observers with telescopes might be able to discern the umbral shadow as a black spot at the center of a less dark region (penumbra) traveling across the full Earth's disk. It would look essentially the same as it does to the Deep Space Climate Observatory.
In summary, whenever an eclipse of some sort is occurring on Earth, an eclipse of another sort is occurring on the Moon. Eclipses occur for observers on both Earth and the Moon whenever the two bodies and the Sun align in a straight line, or syzygy.
Mars[edit]
See also: Astronomy on Mars
Mars has only a thin atmosphere; however, it is extremely dusty and there is much light that is scattered about. The sky is thus rather bright during the daytime and stars are not visible. The Martian northern pole star is Deneb[9] (although the actual pole is somewhat offset in the direction of Alpha Cephei).
The color of the Martian sky[edit]
Sunset (animated) – Gale crater (April 15, 2015)
Mars sky at noon, as imaged by Mars Pathfinder (June 1999)
Mars sky at sunset, as imaged by Mars Pathfinder (June 1999)
Mars sky at sunset, as imaged by the Spirit rover (May 2005)
Mars sky at sunset, as imaged by the Curiosity rover (February 2013; sun simulated by artist)
Generating accurate true-color images from Mars's surface is surprisingly complicated.[10] To give but one aspect to consider, there is the Purkinje effect: the human eye's response to color depends on the level of ambient light; red objects appear to darken faster than blue objects as the level of illumination goes down. There is much variation in the color of the sky as reproduced in published images, since many of those images have used filters to maximize their scientific value and are not trying to show true color. For many years, the sky on Mars was thought to be more pinkish than it is now believed to be.
It is now known that during the Martian day, the sky is a butterscotch color.[11] Around sunset and sunrise, the sky is rose in color, but in the vicinity of the setting Sun it is blue. This is the opposite of the situation on Earth. Twilight lasts a long time after the Sun has set and before it rises because of the dust high in Mars's atmosphere.
On Mars, Rayleigh scattering is usually a very weak effect; the red color of the sky is caused by the presence of iron(III) oxide in the airborne dust particles. These particles are larger in size than gas molecules, so most of the light is scattered by Mie scattering. Dust absorbs blue light and scatters longer wavelengths (red, orange, yellow).
The Sun from Mars[edit]
See also: Timekeeping on Mars
The Sun as seen from Mars appears to be 5⁄8 the size as seen from Earth (0.35°), and sends 40% of the light, approximately the brightness of a slightly cloudy afternoon on Earth.
On June 3, 2014, the Curiosity rover on Mars observed the planet Mercury transiting the Sun, marking the first time a planetary transit has been observed from a celestial body besides Earth.[12]
Mars's moons as seen from Mars[edit]
Phobos transits the Sun, as seen by Mars Rover Opportunity on March 10, 2004
Planet Mercury transiting the Sun as viewed by the Curiosity rover on Mars (June 3, 2014)[12]
Mars has two small moons: Phobos and Deimos. From the Martian surface, Phobos has one-third to one-half the angular diameter of the Sun while Deimos is barely more than a dot (only 2′ angular diameter). The orbital period of Phobos is so much shorter than the Martian day that the apparent motion of Phobos is in reverse: it rises in the west and sets in the east. Phobos orbits so close (in a low-inclination equatorial orbit) that it cannot be seen north of 70.4°N or south of 70.4°S latitude; high-latitude observers would also notice a decrease in Phobos's apparent size, the additional distance being non-negligible. Phobos's apparent size varies by up to 45% as it passes overhead, due to its proximity to Mars's surface. For an equatorial observer, for example, Phobos is about 0.14° upon rising and swells to 0.20° by the time it reaches the zenith. It crosses the sky swiftly, in about 4.24 hours, every 11.11 hours. Deimos rises in the east and sets in the west, like a "normal" moon, although its appearance to the naked eye would be starlike (angular diameter between 1.8′ and 2.1′). Its brightness would vary between that of Venus and of the star Vega (as seen from Earth). Being relatively close to Mars, Deimos cannot be seen from Martian latitudes greater than 82.7°. Finally, Deimos's orbital period of about 30.3 hours exceeds the Martian rotation period (of about 24.6 hours) by such a small amount that it rises every 5.5 days and takes 2.5 days between rising and setting for an equatorial observer. Thus Phobos crosses the Martian sky nearly 12 times in the time it takes Deimos to cross it just once.
Phobos and Deimos can both eclipse the Sun as seen from Mars, although neither can completely cover its disk and so the event is in fact a transit, rather than an eclipse. For a detailed description of such events see the articles Transit of Phobos from Mars and Transit of Deimos from Mars.
Earth from Mars[edit]
The Earth is visible from Mars as a double star; the Moon would be visible alongside it as a fainter companion. The maximum visible distance between the Earth and the Moon would be about 25′, at inferior conjunction of the Earth and the Sun (for the terrestrial observer, this is the opposition of Mars and the Sun). Near maximum elongation (47.4°), the Earth and Moon would shine at apparent magnitudes −2.5 and +0.9, respectively.[5][13]
Earth and the Moon as viewed from Mars, 205 million kilometers / 127 million miles away (MRO; HiRISE; November 20, 2016)[14]
Curiosity's first view of the Earth and the Moon from the surface of Mars (January 31, 2014)[15]
Venus from Mars[edit]
Venus as seen from Mars (when near the maximum elongation from the Sun of 31.7°) would have an apparent magnitude of about −3.2.[5]
The outer planets[edit]
Compared with their view from Earth, the outer planets (Jupiter, Saturn, Uranus and Neptune) would appear slightly brighter during opposition, but slightly dimmer during conjunction. This effect is most noticeable for Jupiter, and results from Mars' larger orbit compared with that of Earth causing larger variations of interplanetary distance.
The skies of Mars's moons[edit]
From Phobos, Mars appears 6,400 times larger and 2,500 times brighter than the full Moon as seen from Earth, and appears as a sphere of angular diameter roughly 42°—taking up a quarter of the width of a celestial hemisphere.
From Deimos, Mars appears 1,000 times larger and 400 times brighter than the full Moon as seen from Earth, and appears as a sphere of angular diameter roughly 16.5°—taking up an eleventh of the width of a celestial hemisphere.
The Asteroid Belt[edit]
The asteroid belt is sparsely populated and most asteroids are very small, so that an observer situated on one asteroid would be unlikely to be able to see another without the aid of a telescope. Occasional "close approaches" do occur, but these are spread out over eons.
Some asteroids that cross the orbits of planets may occasionally get close enough to a planet or asteroid so that an observer from that asteroid can make out the disc of the nearby object without the aid of binoculars or a telescope. For example, in September 2004, 4179 Toutatis came about four times the distance from the Earth that the Moon does. At the closest point in its encounter, the Earth would have appeared about the same size as the Moon appears from Earth. The Moon would also be easily visible as a small shape in Toutatis's sky at that time.
Asteroids with unusual orbits also offer a lot to the imagination. For instance, the asteroid (or more likely, extinct comet) 3200 Phaethon has one of the most eccentric orbits: its distance from the Sun varies between 0.14 and 2.4 AU. At perihelion, the Sun would loom over 7 times larger than it does in our sky, and blast the surface with over 50 times as much energy; at aphelion, the Sun would shrink to less than half its apparent diameter on Earth, and give little more than a sixth as much illumination.
87 Sylvia and its moons Romulus and Remus[edit]
The asteroid 87 Sylvia is one of the largest main-belt asteroids and the first asteroid observed to have two moons. These moons, Romulus and Remus, would appear roughly the same size. Romulus, the farther one, would be about 0.89° across, slightly bigger than the closer but smaller Remus, which would be about 0.78° across. Because Sylvia is far from spherical, these values can vary by about a little more than 10%, depending on where the observer is on Sylvia's surface. Since the two asteroidal moons appear to orbit (as best we can tell) in the same plane, they would occult each other once every 2.2 days. When the season is right, twice during Sylvia's 6.52 year orbital period, they would eclipse the Sun, which, at 0.15° across, is much smaller than when seen from Earth (0.53°). From Remus, the inner moon, Sylvia is huge, roughly 30°×18° across, while its view of Romulus varies between 1.59 and 0.50° across. From Romulus, Sylvia measures 16°×10° across, while Remus varies between 0.62° and 0.19°.
243 Ida and its moon Dactyl[edit]
Simulated view of Dactyl from Ida
The asteroid 243 Ida was visited by the Galileo spacecraft on its way to Jupiter. It discovered a small moon named Dactyl. Although the exact orbital characteristics of Dactyl are not fully known, it was 90 kilometers from Ida when Galileo passed by. This would mean that from Ida, Dactyl would appear as large as 1.76 degrees across, which is huge for such a small moon (1.4 km).
Jupiter[edit]
Although no images from within Jupiter's atmosphere have ever been taken, artistic representations typically assume that the planet's sky is blue, though dimmer than Earth's, because the sunlight there is on average 27 times fainter, at least in the upper reaches of the atmosphere. The planet's narrow rings might be faintly visible from latitudes above the equator. Further down into the atmosphere, the Sun would be obscured by clouds and haze of various colors, most commonly blue, brown, and red. Although theories abound on the cause of the colors, there is currently no unambiguous answer.[16]
From Jupiter, the Sun appears to cover only 5 arcminutes, less than a quarter of its size as seen from Earth.
Jupiter's moons as seen from Jupiter[edit]
Simulated view of Io, Europa, and the rings of Jupiter seen from their parent planet[17]
Aside from the Sun, the most prominent objects in Jupiter's sky are the four Galilean moons. Io, the nearest to the planet, would be slightly larger than the full moon in Earth's sky, though less bright, and would be the largest moon in the Solar System as seen from its parent planet. The higher albedo of Europa would not overcome its greater distance from Jupiter, so it would not outshine Io. In fact, the low solar constant at Jupiter's distance (3.7% Earth's) ensures that none of the Galilean satellites would be as bright as the full moon is on Earth; from Io to Callisto their apparent magnitudes would be: −11.2, −9.7, −9.4, and −7.0.[citation needed]
Water vapor plume on Europa (artist concept) (December 12, 2013)[18]
Ganymede, the largest moon and third from Jupiter, is almost as bright as Io and Europa, but appears only half the size of Io. However, its great size means that it appears about 2″ larger than Europa. Also, a triple conjunction of Io, Europa and Ganymede would be impossible, because the Laplace resonance that they share prevents this. When two of the Galilean moons are aligned, the third is never less than 90 degrees to the left or right of these moons in its orbit. Callisto, still further out, would appear only a quarter the size of Io.
None of the surface features on Jupiter's moons would appear as prominent as the lunar maria do when the Moon is viewed from Earth. Dark and light patches would be visible on Io's surface due to the coloration of sulfur that covers Io, and the largest volcanoes would be designated by dark points, but the lack of large, contrasting features results in a poor view of it. Europa, however, would appear as a completely featureless white disc. Even when viewed from nearby, most spacecraft images use contrast enhancements to clearly show the cracks in the Europan ice, which are only about 10–15 percent darker than the rest of the surface. Vague dark and light patches would be visible on Ganymede, whereas Callisto is much too distant for any features to be made out.
All four Galilean moons stand out because of the swiftness of their motion, compared to the Moon. They are all also large enough to fully eclipse the Sun.[19] Because Jupiter's axial tilt is minimal, and the Galilean moons all orbit in the plane of Jupiter's equator, solar eclipses are quite common.
Jupiter's small inner moons appear only as starlike points except Amalthea, which can occasionally appear as large as Callisto. However, they would all be brighter than any star, ranging from magnitudes −1.5 to −4.9. The outer moons would be invisible except for Himalia, which would appear as a dim, starlike point to the naked eye (magnitude +5.5) only under favorable circumstances (if its periapsis happens to coincide exactly with its full phase).
The skies of Jupiter's moons[edit]
Artist's impression of an Interplanetary Spaceship on the Jovian moon Europa, after 2020; a part of the Interplanetary Transport System currently in funded development, under the name BFR, by SpaceX
None of Jupiter's moons have more than traces of atmosphere, so their skies are black or very nearly so. For an observer on one of the moons, the most prominent feature of the sky by far would be Jupiter. For an observer on Io, the closest large moon to the planet, Jupiter's apparent diameter would be about 20° (38 times the visible diameter of the Moon, covering 1% of Io's sky). An observer on Metis, the innermost moon, would see Jupiter's apparent diameter increased to 68° (130 times the visible diameter of the Moon, covering 18% of Metis's sky). A "full Jupiter" over Metis shines with about 4% of the Sun's brightness (light on Earth from a full moon is 400 thousand times dimmer than sunlight).
Because the inner moons of Jupiter are in synchronous rotation around Jupiter, the planet always appears in nearly the same spot in their skies (Jupiter would wiggle a bit because of the non-zero eccentricities). Observers on the sides of the Galilean satellites facing away from the planet would never see Jupiter, for instance.
From the moons of Jupiter, solar eclipses caused by the Galilean satellites would be spectacular, because an observer would see the circular shadow of the eclipsing moon travel across Jupiter's face.[20]
Saturn[edit]
NASA's Cassini spacecraft photographs the Earth and Moon (visible bottom-right) from Saturn (July 19, 2013)
The sky in the upper reaches of Saturn's atmosphere is blue (from imagery of the Cassini mission at the time of its September 2017 demise), but the predominant color of its cloud decks suggests that it may be yellowish further down. Observations from spacecraft show that seasonal smog develops in Saturn's southern hemisphere at its perihelion due to its axial tilt. This could cause the sky to become yellowish at times. As the northern hemisphere is pointed towards the sun only at aphelion, the sky there would likely remain blue. The rings of Saturn are almost certainly visible from the upper reaches of its atmosphere. The rings are so thin that from a position on Saturn's equator, they would be almost invisible. However, from anywhere else on the planet, they could be seen as a spectacular arc stretching across half the celestial hemisphere.[16]
Simulated view of Saturn's rings seen from its equator
Simulated view of Saturn's rings seen from a latitude above its equator
Saturn's moons would not look particularly impressive in its sky, as most are fairly small, and the largest are a long way from the planet. Even Titan, the largest moon of Saturn, appears only half the size of Earth's moon, and only grows as bright as −7. In fact, Titan is the dimmest of Saturn's moons due to its great distance and low albedo; Mimas, Enceladus, Tethys, Dione, and Rhea are all brighter, at magnitudes −7.8, −7.9, −8.8, −8, and −7.8, respectively. Here are the approximate angular diameters of the main moons (for comparison, Earth's moon has an average angular diameter of 31′): Mimas: 7–11′, Enceladus: 7–9′, Tethys: 12–15′, Dione: 10–12′, Rhea: 8–11′, Titan: 14–15′, Iapetus: 1′. Most of the inner moons would appear as bright, starlike points (with the exception of Janus, which would appear 7 arcseconds across at its zenith), although most would shine brighter than any star; for example, Janus and Epimetheus would both shine as bright as magnitude −6. Meanwhile, none of the outer moons would be visible except Phoebe, which nears the naked eye limit (6.2–6.6) even at full phase.
Saturn has a southern polar star, δ Octantis, a magnitude 4.3 star. It is much fainter than Earth's Polaris (α Ursae Minoris).
The skies of Saturn's moons[edit]
Since the inner moons of Saturn are all in synchronous rotation, the planet always appears in the same spot in their skies. Observers on the sides of those satellites facing away from the planet would never see Saturn.
In the skies of Saturn's inner moons, Saturn is an enormous object. For instance, Saturn seen from Pan has an apparent diameter of ~50°, 104 times larger than our Moon and occupying 11% of Pan's sky. Because Pan orbits along the Encke division within Saturn's rings, they are visible from anywhere on Pan, even on its side facing away from Saturn.
The rings from Saturn's moons[edit]
Saturn's rings would not be prominent from most of the moons. This is because the rings, though wide, are not very thick, and most of the moons orbit almost exactly (within 1.5°) in the planet's ring plane. Thus, the rings are edge-on and practically invisible from the inner moons. From the outer moons, starting with Iapetus, a more oblique view of the rings would be available, although the greater distance would make Saturn appear smaller in the sky; from Phoebe, the largest of Saturn's irregular moons, Saturn would appear only as big as the full Moon does from Earth. The play of distance and angle is quite sensitive to the values used, but calculations show the best view of the rings would be achieved from the inner moon Mimas, which lies a full 1.5° off Saturn's equatorial plane and is fairly near the rings. At their widest opening, when Mimas is at its maximum distance from Saturn's equatorial plane, the edges of the rings (from B to A) would be separated by 2.7 degrees. The co-orbitals Epimetheus and Janus would also get a good view, with maximum opening angles ranging between 1.5 and 2.9°. Tethys gets the next best view, with nearly half a degree. Iapetus achieves 15.47°, which is more than any of the outer moons can claim.
The sky of Titan[edit]
Image of the surface of Titan from the Huygens probe
Titan is the only moon in the solar system to have a thick atmosphere. Images from the Huygens probe show that the Titanean sky is a light tangerine color. However, an astronaut standing on the surface of Titan would see a hazy brownish/dark orange color. As a consequence of its greater distance from the Sun and the opacity of its atmosphere, the surface of Titan receives only about 1⁄3000 of the sunlight Earth does – daytime on Titan is thus only as bright as twilight on the Earth. It seems likely that Saturn is permanently invisible behind orange smog, and even the Sun would only be a lighter patch in the haze, barely illuminating the surface of ice and methane lakes. However, in the upper atmosphere, the sky would have a blue color and Saturn would be visible.[21] With its thick atmosphere and methane rain, Titan is the only celestial body other than Earth upon which rainbows could form. However, given the extreme opacity of the atmosphere in visible light, the vast majority would be in the infrared.[22]
The sky of Enceladus[edit]
An artist's conception of Enceladus's sky
Seen from Enceladus, Saturn would have a visible diameter of almost 30°, sixty times more than the Moon visible from Earth. Moreover, since Enceladus rotates synchronously with its orbital period and therefore keeps one face pointed toward Saturn, the planet never moves in Enceladus's sky (albeit with slight variations coming from the orbit's eccentricity), and cannot be seen from the far side of the satellite.
Saturn's rings would be seen from an angle of only 0.019° and be almost invisible, but their shadow on Saturn's disk would be clearly distinguishable. Like our own Moon from Earth, Saturn itself would show regular phases. From Enceladus, the Sun would have a diameter of only 3.5 minutes of arc, one-ninth that of the Moon as seen from Earth.
An observer located on Enceladus could also observe Mimas (the biggest satellite located inside Enceladus's orbit) transit in front of Saturn every 72 hours, on average. Its apparent size would be at most 26 minutes of arc, about the same size as the Moon seen from Earth. Pallene and Methone would appear nearly star-like (maximum 30 seconds of arc). Tethys, visible from Enceladus's anti-Saturnian side, would reach a maximum apparent size of about 64 minutes of arc, about twice that of the Moon as seen from the Earth.
Uranus[edit]
Judging by the color of its atmosphere, the sky of Uranus is probably a light blue, i.e. cyan color. It is unlikely that the planet's rings can be seen from its surface, as they are very thin and dark. Uranus has a northern polar star, Sabik (η Ophiuchi), a magnitude 2.4 star. Uranus also has a southern polar star, 15 Orionis, an unremarkable magnitude 4.8 star. Both are fainter than Earth's Polaris (α Ursae Minoris), although Sabik only slightly.[16]
Simulated view of Ariel in the sky of Uranus
Uranus is unusual in that the obliquity of its ecliptic is 82° (angle between the orbital and rotational poles). The North Pole of Uranus points to somewhere near η Ophiuchi (in Earth's southern celestial hemisphere), about 15° northeast of Antares, and its South Pole halfway between Betelgeuse and Aldebaran. Uranus's "tropics" lie at 82° latitude and its "Arctic circles" at 8° latitude. On December 17, 2007, the Sun passed the Uranian celestial equator to the North and in 2029 the North Pole of Uranus will be nearly pointed at the Sun.
None of Uranus's moons would appear as large as a full moon on Earth from the surface of their parent planet, but the large number of them would present an interesting sight for observers hovering above the cloudtops. The angular diameters of the five large moons are as follows (for comparison, Earth's moon measures on average 31′ for terrestrial observers): Miranda, 11–15′; Ariel, 20–23′; Umbriel, 15–17′; Titania, 11–13′; Oberon, 8–9′. Unlike on Jupiter and Saturn, many of the inner moons can be seen as disks rather than starlike points; the moons Portia and Juliet can appear around the size of Miranda at times, and a number of other inner moons appear larger than Oberon. Several others range from 6′ to 8′. The outer irregular moons would not be visible to the naked eye.
However, the low light levels at such a great distance from the sun ensure that the moons appear very dim; the brightest, Ariel, would only shine at magnitude −7.4, more than 100 times dimmer than the moon as seen from Earth. Meanwhile, the outer large moon Oberon would only be as bright as magnitude −4.9, about the same as Venus despite its proximity.
Neptune[edit]
Simulated view of Triton in the sky of Neptune.
Judging by the color of its atmosphere, the sky of Neptune is probably an azure or sky blue, similar to Uranus'. As in the case of Uranus, it is unlikely that the planet's rings can be seen from its surface, as they are very thin and dark.
Aside from the Sun, the most impressive object in Neptune's sky is its large moon Triton, which would appear slightly smaller than a full Moon on Earth. It moves more swiftly than our Moon, because of its shorter period (5.8 days) compounded by its retrograde orbit. The smaller moon Proteus would show a disk about half the size of the full Moon. Surprisingly, Neptune's small inner moons all cover, at some point in their orbits, more than 10′ in Neptune's sky. At some points, Despina's angular diameter rivals that of Ariel from Uranus and Ganymede from Jupiter. Here are the angular diameters for Neptune's moons (for comparison, Earth's moon measures on average 31′ for terrestrial observers): Naiad, 7–13′; Thalassa, 8–14′; Despina, 14–22′; Galatea, 13–18′; Larissa, 10–14′; Proteus, 12–16′; Triton, 26–28′. An alignment of the inner moons would likely produce a spectacular sight. Neptune's large outer satellite, Nereid, is not large enough to appear as a disk from Neptune, and is not noticeable in the sky, as its brightness at full phase varies from magnitude 2.2–6.4, depending on which point in its eccentric orbit it happens to be. The other irregular outer moons would not be visible to the naked eye, although a dedicated telescopic observer could potentially spot some at full phase.
As with Uranus, the low light levels cause the major moons to appear very dim. The brightness of Triton at full phase is only −7.11, despite the fact that Triton is more than 4 times as intrinsically bright as our moon and orbits much closer to Neptune.
The sky of Triton[edit]
Simulated view of Neptune in the sky of Triton
Triton, Neptune's largest moon, has an atmosphere, but it is so thin that its sky is still black, possibly with some pale haze at the horizon. Because Triton orbits with synchronous rotation, Neptune always appears in the same position in its sky. Triton's rotation axis is inclined 130° to Neptune's orbital plane and thus points within 40° of the Sun twice per Neptunian year, much like Uranus's. As Neptune orbits the Sun, Triton's polar regions take turns facing the Sun for 82 years at a stretch, resulting in radical seasonal changes as one pole, then the other, moves into the sunlight.
Neptune itself would span 8 degrees in Triton's sky, though with a maximum brightness roughly comparable to that of the full moon on Earth it would appear only about 1⁄256 as bright as the full moon, per unit area. Due to its eccentric orbit, Nereid would vary considerably in brightness, from fifth to first magnitude; its disk would be far too small to see with the naked eye. Proteus would also be difficult to resolve at just 5–6 arcminutes across, but it would never be fainter than first magnitude, and at its closest would rival Canopus.
Trans-Neptunian Objects[edit]
A trans-Neptunian object is any minor planet in the Solar System that orbits the Sun at a greater average distance (semi-major axis) than Neptune, 30 astronomical units (AU).
Pluto and Charon[edit]
Pluto, accompanied by its largest moon Charon, orbits the Sun at a distance usually outside the orbit of Neptune except for a twenty-year period in each orbit.
From Pluto, the Sun is point-like to human eyes, but still very bright, giving roughly 150 to 450 times the light of the full Moon from Earth (the variability being due to the fact that Pluto's orbit is highly elliptical, stretching from just 4.4 billion km to over 7.3 billion km from the Sun).[23] Nonetheless, human observers would find a large decrease in available light.
Pluto's atmosphere consists of a thin envelope of nitrogen, methane, and carbon monoxide gases, all of which are derived from the ices of these substances on its surface. When Pluto is close to the Sun, the temperature of Pluto's solid surface increases, causing these ices to sublimate into gasses. This atmosphere also produces a noticeable blue haze that is visible at sunset and possibly other times of the Plutonian day.[24]
Pluto and Charon are tidally locked to each other. This means that Charon always presents the same face to Pluto, and Pluto also always presents the same face to Charon. Observers on the far side of Charon from Pluto would never see the dwarf planet; observers on the far side of Pluto from Charon would never see the moon. Every 124 years, for several years it is mutual-eclipse season, during which Pluto and Charon each alternatively eclipse the Sun for the other at intervals of 3.2 days.
View from Hydra. Pluto and Charon (right); Nix (left) (artist concept).
View from Pluto. Sun (right-top); Charon (left) (artist concept).
View from Pluto of Charon and the Sun (artist concept).
Pluto by moonlight (artist concept).
Pluto – Norgay Montes (left-foreground); Hillary Montes (left-skyline); Sputnik Planitia (right)
Near-sunset view includes several layers of atmospheric haze.
50000 Quaoar and its moon Weywot[edit]
The asteroid Quaoar is a Kuiper belt object with a circular orbit and moderate inclination. From its surface and at the average distance between its perihelion and aphelion the Sun would have an angular diameter of 44.2″ (arcseconds) comparable to the maximum diameter of Venus of 63.0″; the human eye has a resolution of 72″, so the Sun from Quaoar's surface would appear as a point. The Sun's apparent magnitude would be −18.56, in comparison the magnitude of the Moon at full phase is −12.74, so the Sun would appear on Quaoar as a point of light 212 times brighter than a full Moon on Earth. The amount of light depends on the atmosphere: if present the amount of light received at noon would be similar to the light at dusk or dawn on Earth.
Quaoar's moon Weywot has an angular diameter of 15.9′ (arcminutes) at apoapsis and 21.4′ at periapsis, in comparison the Moon's angular diameter varies between 29.4′ and 33.5′. In comparison to the size of the Sun from Quaoar's surface Weywot would appear much bigger: 15.9′ is equal to 954″ or 21.6 times the diameter of the Sun as seen from Quaoar. Most solar eclipses would be total and a partial eclipse would be extremely rare. At full phase Weywot's visual magnitude is −3.24 somewhere between Jupiter's maximum magnitude (−2.94) and Venus's minimum magnitude (−3.82), in comparison the Moon at full phase is 6,301 times brighter than Weywot.
Quaoar's umbra extends 5,180,390 km and at the distance of Weywot's apoapsis it would have a diameter of 1,106.5 km or 15 times Weywot's diameter. In comparison, Earth's umbra at the Moon's position is 2.65 times wider. Weywot's inclination is not determined yet, it's either 14° or 30°, if we assume the smaller value then Weywot's center at apoapsis can be up to 4,121 km above or below Quaoar's equatorial plane, this mean for most of the time Weywot is outside of the umbra completely.
Comets[edit]
The sky of a comet changes dramatically as it nears the Sun. During perihelion, a comet's ices begin to sublime from its surface, forming tails of gas and dust, and a coma. An observer on a comet nearing the Sun might see the stars slightly obscured by a milky haze, which could create halo effects around the Sun and other bright objects.
Extrasolar planets[edit]
Basics[edit]
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For observers on extrasolar planets, the constellations would differ depending on the distances involved. The view of outer space of exoplanets can be extrapolated from open source software such as Celestia or Stellarium, and it appears that due to parallax, distant stars change their position less than nearby ones. For alien observers, the Sun would be visible to the naked human eye only at distances below 20[25] – 27[26] parsec (60–90 ly).[nb 1] Whenever the sun is observed from another star, it always appears on the opposite coordinates in the sky. Thus an observer located near a star with RA at 4 hr and declination −10 would see the sun located at RA: 16 hr, dec: +10. A consequence of observing the universe from other stars is that stars that may appear bright in our own sky may appear dimmer in other skies and vice versa.
View from nearby stars (0 – 10 ly)[edit]
If the Sun were to be observed from the Alpha Centauri system, the nearest star system to ours, it would appear to be a 0.46 magnitude star in the constellation Cassiopeia, and would create a "/W" shape instead of the "W" as seen from Earth. Due to the proximity of the Alpha Centauri system, the constellations would, for the most part, appear similar. However, there are some notable differences with the position of other nearby stars; for example, Sirius would appear about one degree from the star Betelgeuse in the constellation Orion. Also, Procyon would appear in the constellation Gemini, about 13 degrees below Pollux.
Looking towards the sky around Orion from Alpha Centauri with Sirius near Betelgeuse, Procyon in Gemini, and the Sun between Perseus and Cassiopeia generated by Celestia
A planet around either α Centauri A or B would see the other star as a very bright secondary. For example, an Earth-like planet at 1.25 astronomical units from α Cen A (with a revolution period of 1.34 years) would get Sun-like illumination from its primary, and α Cen B would appear 5.7 to 8.6 magnitudes dimmer (−21.0 to −18.2), 190 to 2,700 times dimmer than α Cen A but still 150 to 2,100 times brighter than the full Moon. Conversely, an Earth-like planet at 0.71 AU from α Cen B (with a revolution period of 0.63 years) would get Sun-like illumination from its primary, and α Cen A would appear 4.6 to 7.3 magnitudes dimmer (−22.1 to −19.4), 70 to 840 times dimmer than α Cen B but still 470 to 5,700 times brighter than the full Moon. In both cases the secondary sun would, in the course of the planet's year, appear to circle the sky. It would start off right beside the primary and end up, half a period later, opposite it in the sky (at "full"). After another half period, it would complete the cycle. Other planets orbiting one member of a binary system would enjoy similar skies. The angular separation between the two stars would not be exactly the same after one orbit of the planet however, because during that time the parent star will have completed part of its orbit around the other star in the system.
View from more distant stars (10 ly – )[edit]
From 40 Eridani, 16 light years away, the Sun would be an average looking star of about apparent magnitude 3.3 in the constellation Serpens Caput. At this distance most of the stars nearest to us would be in different locations to those in our sky, including Alpha Centauri, Sirius, and Procyon.
From a planet orbiting Aldebaran, 65 light years away, our Sun would be seen as an insignificant 6.4 magnitude star between Ophiuchus and Scorpius (more specifically, it would in the vicinity of Phi Ophiuchi and 24 Scorpii). Constellations made of bright, distant stars would look somewhat similar (such as Orion and Scorpius) but much of the night sky would seem unfamiliar to someone from Earth. Even Orion would appear somewhat different; viewed from this position, Alnilam and Mintaka would appear to be on top of each other, only 15 arcminutes apart, thus reducing the belt to two stars. Also Bellatrix would be much closer to the belt, making the "chest" somewhat smaller.
Recent developments[edit]
In May 2017, glints of light from Earth, seen as twinkling from an orbiting satellite a million miles away, were found to be reflected light from ice crystals in the atmosphere.[27][28] The technology used to determine this may be useful in studying the atmospheres of distant worlds, including those of exoplanets.
See also[edit]
Exosphere
Large Magellanic Cloud#View from the LMC
Sky
Notes[edit]
Jump up ^ These numbers are extrapolated from the fact that the human eye can generally see up to magnitude 6.5 on Earth, while it can see up to magnitude 7 under the best possible conditions.
References[edit]
Jump up ^ This can be derived using the formula for the length of a cord found at http://mathworld.wolfram.com/CircularSegment.html
Jump up ^ http://www.mathstat.concordia.ca/faculty/rhall/mc/arctan.pdf
Jump up ^ "Thin Atmosphere of Mercury, Formation and Composition – Windows to the Universe". www.windows.ucar.edu.
Jump up ^ Seligman, Courtney. "The Rotation of Mercury". cseligman.com. Retrieved October 18, 2015.
^ Jump up to: a b c d e f Yakov Perelman; Arthur Shkarovsky-Raffe (2000). Astronomy for Entertainment. University Press of the Pacific. ISBN 0-89875-056-3.
Jump up ^ "Venera 13 – Missions – NASA Solar System Exploration". NASA Solar System Exploration.
Jump up ^ "The Terrestrial Planets". The Planetary Society. Archived from the original on August 21, 2011. Retrieved August 3, 2007.
Jump up ^ "Return to Orbit". www.hq.nasa.gov.
Jump up ^ Burgess, E. & Singh, G., To the Red Planet Columbia University Press 1978; see review in Astrophysics and space SCI. V.201, NO. 1/FEB(I), P.160, 1993
Jump up ^ "Phil Plait's Bad Astronomy: Misconceptions: What Color is Mars?". www.badastronomy.com.
Jump up ^ "Archived copy". Archived from the original on August 10, 2004. Retrieved April 23, 2005.
^ Jump up to: a b Webster, Guy (June 10, 2014). "Mercury Passes in Front of the Sun, as Seen From Mars". NASA. Retrieved June 10, 2014.
Jump up ^ "Earth and Moon as Viewed from Mars". Earth Observatory. 2003-05-08. Retrieved 2008-06-03. (JPL Horizons shows: 0.9304AU from Earth; Phase 43%; Sun Elongation 43°)
Jump up ^ St. Fleur, Nicholas (January 9, 2017). "Looking at Your Home Planet from Mars". New York Times. Retrieved January 9, 2017.
Jump up ^ Revkin, Andrew C. (February 6, 2014). "Martian View of Our Pale Dot". New York Times. Retrieved February 9, 2014.
^ Jump up to: a b c Fran Bagenal (2005). "Class 17 – Giant Planets". Laboratory for Atmospheric and Space Physics. Retrieved September 5, 2008.
Jump up ^ This and other simulated images on this page were made with the Celestia space simulation software.
Jump up ^ Cook, Jia-Rui C.; Gutro, Rob; Brown, Dwayne; Harrington, J.D.; Fohn, Joe (December 12, 2013). "Hubble Sees Evidence of Water Vapor at Jupiter Moon". NASA. Retrieved December 12, 2013.
Jump up ^ "Pre-eclipse of the Sun by Callisto from the center of Jupiter". JPL Solar System Simulator. June 3, 2009. Retrieved June 4, 2008.
Jump up ^ Jim Thommes. "Jupiter Moon Shadow Transit". Jim Thommes Astrophotography. Retrieved September 3, 2008.
Jump up ^ Pascal, René. "POV-Ray renderings of Huygens descending to Titan". www.beugungsbild.de.
Jump up ^ "Rainbows on Titan". NASA. Retrieved October 8, 2011.
Jump up ^ Plait, Phil (March 15, 2012). "BAFact math: How bright is the Sun from Pluto?". Discover Magazine. Retrieved July 6, 2015.
Jump up ^ "New Horizons shows Pluto sporting blue skies and red water ice".
Jump up ^ "Vmag<6.5". SIMBAD Astronomical Database. Retrieved 2010-06-25.
Jump up ^ John E. Bortle (February 2001). "The Bortle Dark-Sky Scale". Sky & Telescope. Retrieved 2009-11-18.
Jump up ^ St. Fleur, Nicholas (19 May 2017). "Spotting Mysterious Twinkles on Earth From a Million Miles Away". New York Times. Retrieved 20 May 2017.
Jump up ^ Marshak, Alexander; Várnai, Tamás; Kostinski, Alexander (15 May 2017). "Terrestrial glint seen from deep space: oriented ice crystals detected from the Lagrangian point". Geophysical Research Letters. 44 (10): 5197–5202. Bibcode:2017GeoRL..44.5197M. doi:10.1002/2017GL073248. Retrieved 20 May 2017.
Further reading[edit]
Carroll, Michael (2007). Space art : how to draw and paint planets, moons, and landscapes of alien worlds. New York: Watson-Guptil Publications. ISBN 9780823048762.
Carroll, Michael (2010). Drifting on Alien Winds Exploring the Skies and Weather of Other Worlds. New York, NY: Springer Science+Business Media, LLC. ISBN 9781441969170.
Barnett, Lincoln (December 20, 1954). "The Starry Universe". Life: 44–64. Retrieved April 12, 2013.
Perelman, Y. (2000). "Lunar heavens". Astronomy for entertainment. Honolulu: University Press of the Pacific. pp. 78–84. ISBN 9780898750560.
External links[edit]
Astronauts on the planets
Essay on the possible sky colours of alien worlds.
JPL Solar System Simulator
Phases of Charon as seen from Pluto
The Starry Universe – Life Magazine (December 20, 1954).
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text:
Uranium mining in Australia
From Wikipedia, the free encyclopedia
Jump to: navigation, search
Ranger Uranium Mine, number 3 pit
Quarterly expenditure ($millions) on uranium exploration since 1988
Annual Australian production of uranium (thousand tonnes) since 1989
Radioactive ores were first extracted at Radium Hill in 1906, and Mount Painter in South Australia in the 1930s, to recover radium for medical use. Several hundred kilograms of uranium were also produced.[1] Of the world's proven estimated uranium reserves (5,404,000 tonnes), 31% are held in Australia (1,673,000 tonnes), ahead of the second largest, Kazakhstan (12.1% or 651,800 tonnes).[2] In terms of production, Canada is the largest supplier to export markets, followed by Kazakhstan and Australia.[3] Uranium mined in Australia is mainly for export. Australia exported 50,235 tonnes of uranium oxide concentrate in the five years to 2008, worth A$2.9 billion.[1]
Following the Japanese Fukushima nuclear disaster in early 2011, many countries are scaling back their nuclear power production, with some setting deadlines for a complete shutdown of all nuclear power reactors. It is expected that this may impact on demand for Australian Uranium. However, State governments have now approved mine development in Western Australia and Queensland. But as of 2013 uranium prices are very low, and it is unlikely that any new projects will enter active development until the market improves.
Historically, many prospective Australian uranium mines have been constrained by active antinuclear opposition. For several decades uranium mining has been a major part of the Australian political landscape, with opposition groups citing the wide ranging environmental impacts, indigenous land access and nuclear proliferation as reasons for ceasing or restricting the industry. The debate has resulted in limitations on mining and export activities, with Federal and State governments occasionally backflipping on public policy.
As of 2015, there are three operational sites for uranium mining in Australia: Olympic Dam (BHP), Ranger (ERA), and Four Mile (Quasar Resources Pty Ltd and Alliance Resources Ltd).[4]
Contents
[hide]
1 History
2 Map
3 Markets
4 Government policy and politics
4.1 Recent legislative changes
4.2 Opposition
5 Regulation of uranium mining in Australia
5.1 Federal law
5.2 State and Territory laws
5.2.1 NSW
5.2.2 Northern Territory
5.2.3 Queensland
5.2.4 South Australia
5.2.5 Victoria
5.2.6 Western Australia
6 Mines
7 See also
8 References
9 External links
History[edit]
Uranium mine at Mt. Gee from the early 20th century
Radium Hill minesite c.1954
The presence of a uranium resource in Australia had been known since the 1890s.[1] Uranium was mined at Radium Hill in South Australia from 1906 and a refinery at Hunter's Hill near Sydney processed the Radium Hill ore between 1911 and 1915 for radium bromide and uranium. Radium was used for medical research and also mined at Mount Painter (adjacent to Mount Gee) in South Australia.[5]
Serious uranium exploration started in 1944 after requests from the United States and United Kingdom governments, and in 1948 tax concessions were offered by the Commonwealth for successful discoveries. A £1,800,000 uranium treatment complex operated by the Government of South Australia at Port Pirie commenced operations in August 1955, processing ore from Radium Hill and Wild Dog Hill (Myponga), south of Adelaide. The complex supplied the UK - USA Combined Development Agency and closed in February 1962.[6][7]
Uranium deposits were found at Rum Jungle (NT) in 1949 and a mining operation run by the Commonwealth commenced there in 1954. Further discoveries were made at South Alligator River (NT) in 1953, Mary Kathleen (Qld) in 1954, and Westmoreland (Qld) in 1956. In 1954 Radium Hill reopened as a uranium mine and mining operations started at several other sites in the late 1950s.
By 1964, production had mostly ended due to depleted reserves and filled contracts. Export sales during this initial phase included 7,730 tonnes of uranium to the USA and UK for their nuclear weapons programs. Other sales related to the power generation in overseas countries.
A second wave of exploration activity in the late 1960s occurred with the development of nuclear energy for electricity production. 60 deposits had been identified up to the late 1970s. The Ranger deposit was discovered in 1969, Nabarlek and Koongarra in 1970, and Jabiluka in 1971.
The first of many government inquiries into the industry was tabled in 1976 as the "Ranger Uranium Environmental Inquiry" (also known as the "Fox Report"), and addressed the question of whether Australia should mine and export uranium.[8] Mining operations ceased while the inquiry was underway but recommenced in 1977 after the government took up a 42% share of Ranger Uranium Mines Pty Ltd.[1] In 1979 the Commonwealth sold its share in the still to be built Ranger operation and at the same time established Energy Resources of Australia Ltd to own and operate the mine. Ranger finally opened for production in 1981.
The Nabarlek (NT) mine operated for four months in 1979. Milling of stockpiled ore commenced in 1980 and produced 10,858 tonnes of uranium oxide up to 1988 with sales to Japan, Finland and France, for civil power generation.
Mary Kathleen closed in late 1982 becoming the site of Australia's first major uranium mine site rehabilitation project. This was completed in 1985. A similar site rehabilitation project at Rum Jungle also took place in the 1980s.[1]
Olympic Dam (SA) at Roxby Downs started operations in 1988, operated by Western Mining Corporation. A large underground mine, it was mainly focussed on copper production, with uranium, gold and silver as by-products. Western Mining Corp was taken over by BHP Billiton in 2005.[1]
Historically, many prospective Australian uranium mines have been constrained by active antinuclear opposition, but state governments have now approved mine development in Western Australia and Queensland. But it is unlikely that any new projects will enter active development until the market improves. As of 2013 uranium prices are very low. Cameco placed the Kintyre project on hold until market prices improve and Paladin has stated that its project proposals (Bigrlyi, Angela/Pamela, Manyingee, Oobagooma, and Valhalla/Skal) need higher uranium market prices before they can proceed. Toro wants to take the Wiluna proposal to the development phase, but has not been successful in attracting equity investors. When market prices go up again, so that mine development is justified, most projects would need at least five years to proceed to production.[9]
Map[edit]
Perth
Darwin
Alice Springs
Brisbane
Sydney
Adelaide
Melbourne
Hobart
Port Hedland
Broome
Ranger
Olympic Dam
Beverley
Nabarlek
Rum Jungle
Mary Kathleen
Radium Hill

Westmoreland
Port Pirie
Hunter's Hill
Four Mile
Yeelirie
Lake Maitland
Kintyre
Angela
Oobagooma
Manyingee
Mulga Rock
Mount Gee
Naperby
Bigrlyi
Koongarra

Mt. Fitch
Honeymoon
Major uranium mines and deposits in Australia[1][10]
Active mine Deposit/possible future minesite Closed mines/plants City/town
(May 2009)
Markets[edit]
Generally, there is only one commercial use for uranium: as the source material for nuclear power generation. In February 2009 there were 436 operational nuclear power plants worldwide, with a total generating capacity of nearly 372 gigawatts of electricity.[11] Another 64 nuclear power reactors are expected to be commissioned over the next six years.
There are no nuclear power generation plants operating in Australia and therefore no domestic demand. The High Flux Australian Reactor at Lucas Heights, New South Wales operated from 1958 to 2007. The OPAL research reactor is currently in operation at Lucas Heights.
Australian uranium is mined and sold only for electrical power generation or nuclear research, Almost all the uranium is exported under strict International Atomic Energy Agency safeguards.
Government policy and politics[edit]
See also: List of inquiries into uranium mining in Australia
Uranium mining in Australia has been highly political, particularly for the Australian Labor Party(ALP) at both state and federal level. Development of projects has often been stymied by a succession of inquiries and the politicisation of the issuing of mining and export licences.
The biennial ALP National conference in 1982 debated the issue vigorously. At the 1984 Conference, the newly elected federal Labor government under Bob Hawke introduced the so-called "Three mine policy".[12] The policy confined Australian uranium mining activities to the three sites already operational: Ranger, Nabarlek and Olympic Dam with a moratorium on new mines opening. Subsequently reserves at Nabarlek were depleted and the Beverley Uranium Mine became the notional third mine.
The coalition won the 1996 Federal election under John Howard and promptly abandoned the policy.
On 28 April 2007, the Howard government adopted a new uranium strategy which aimed to immediately remove "unnecessary constraints impeding the expansion of uranium mining, such as overlapping and cumbersome regulations relating to the mining and transport of uranium ore" and repeal prohibitions on further nuclear industrial development which had been established in 1999 under the Environment Protection and Biodiversity Conservation (EPBC) Act 1999.[13]
The same day, the Labor party abandoned its "no new mines" policy, while maintaining its opposition to other forms of nuclear industrial development in Australia.[14]
After returning to government in 2008, the ALP approved a fourth uranium mine in July 2009: the Four Mile uranium mine in South Australia, thus ending its 25-year-old policy.[15] Federal Resources Minister Martin Ferguson subsequently declared that increased uranium mining in Australia was inevitable.[16]
State governments opposed to uranium mining have been able to stop the issuing of mining permits, sometimes against the policy of the incumbent Federal government. As of December 2015, the current position of the affected states and territories is as follows:
South Australia (ALP): supports mining[17]
Western Australia (Lib/NP coalition): supports mining[18]
Queensland (ALP): opposed to mining[19]
New South Wales (Lib/NP): supports exploration, opposed to mining[20]
Northern Territory: under the control of the Commonwealth
Victoria (Lib/NP): opposed to mining[21]
Tasmania (Lib/NP): supports mining[22]
Recent legislative changes[edit]
The Western Australian ban on uranium mining was removed in 2008.[11]
Queensland's ban on uranium mining was revoked in 2012, when Premier Campbell Newman back-flipped on a pre-election promise.[21] In March 2015 the Palaszczuk government announced that it would be reinstating the ban.[19]
The New South Wales Government passed the Mining Legislation Amendment (Uranium Exploration) Act 2012 No 16 on 4 April 2012. The Act was proclaimed on 14 September 2012. The Act removed the ban on uranium exploration to help gain an understanding of what uranium and uranium-bearing mineral resources may exist in the State. The ban on uranium mining remains in place.[20]
Opposition[edit]
Dr Helen Caldicott
Kevin Buzzacott in Adelaide 2014
Opposition to uranium mining has been considerable in Australia, and notable anti-uranium activists have included Dr Helen Calidicott, Kevin Buzzacott, Jacqui Katona, Yvonne Margarula, and Jillian Marsh.[23][24][25]
In November 2011, Prime Minister Julia Gillard called on the ALP to reverse its policy at the ALP national conference, to allow export of Australian uranium to India. India has not signed the nuclear non-proliferation treaty.
While being welcomed at the time by State and Federal governments as a major boost to the economy, the proposed Olympic Dam expansion of mining operations did attract criticism. In 2010, local traditional owners and Indigenous communities protested the proposed expansion.[26] In July 2012, more than 400 people joined a "Lizard's Revenge march" to the Olympic Dam site. The anti-nuclear activists, including Elder Kevin Buzzacott, protested against the mine expansion and the uranium industry. They say the company and the government have put short-term economic gain ahead of environmental and health concerns. Organiser Nectaria Calan said police harassed protesters, demanding identification and controlling access to and from their campsite.[27] In August 2012, BHP Billiton announced that the expansion was being postponed indefinitely pending investigation of a "new and cheaper design".[28][29]
In 2016, BHP Billiton’s asset president, Jacqui McGill, announced that the expansion plans would move ahead, “through low-risk, capital efficient underground expansions.”[30]
Regulation of uranium mining in Australia[edit]
Federal law[edit]
Mining or milling uranium ore is defined as a 'nuclear action' in Environment Protection and Biodiversity Conservation Act 1999, s.22(1)(d). This means that an EPBC Act approval is required for uranium mining from the Federal Environment Minister if a corporation or the Commonwealth or a Commonwealth agency is to take a nuclear action that has, will have or is likely to have a significant impact on the environment (s.21(1)).
State and Territory laws[edit]
NSW[edit]
Until 2012, the Uranium Mining and Nuclear Facilities (Prohibitions) Act 1986 (NSW) prohibited uranium mining in NSW. In 2012 the O'Farrell government proposed the repeal of selected provisions of this Act, by means of the Mining Legislation Amendment (Uranium Exploration) Bill 2012, which passed on 28 March 2012, and received Royal Assent on 4 April 2012. The UMNFP Act had made it an offence to prospect for, or to mine, uranium in NSW. (s.7) The 2012 Bill removed the general prohibition on prospecting for uranium in New South Wales. It also enables exploration licences and associated permits (but no other licences or authorities) to be granted under the Mining Act 1992 to prospect for uranium, to apply the State environmental planning policy applicable to other mineral exploration to uranium prospecting, vests all uranium in NSW in the Crown and excludes compensation for that vesting. The UMNFP Act still prohibits State authorities from constructing or operating nuclear reactors for the production of electricity (s.9).
Northern Territory[edit]
Queensland[edit]
Mining uranium was banned in Queensland from 1989 to 2012. The ban was repealed by the Newman government, then the Palaszczuk government in 2015 announced that it would be reinstated.[31][32]
South Australia[edit]
Radiation Protection and Control Act 1982 (SA) (ss. 5, 27).
Roxby Downs (Indenture Ratification) Act 1982 (see: Schedule)
On March 19, 2015 the South Australian government established The Nuclear Fuel Cycle Royal Commission to investigate the expansion of uranium mining and exploration of new uranium deposits in South Australia.[33] On November 15, 2016 the government decided to support all five uranium mining related recommendations made by the commission.[34]
Victoria[edit]
Nuclear Activities (Prohibitions) Act 1983 - s.5: Prohibition against exploration etc. for uranium or thorium
Western Australia[edit]
Uranium (Yeelirrie) Agreement Act 1978 see alsohttp://www.dmp.wa.gov.au/9997.aspx
In 2017, Western Australia’s Environment Minister, Albert Jacob, gave approval for the Wiluna Project, owned by Toro Energy. The company will apply for federal approval later this year.[35] The state also gave approval to Canadian based company Cameco for the right to mine the Yeelirrie mine.[36]
Mines[edit]
Mary Kathleen mine, 2011
About 96% of known deposits are at six sites: Olympic Dam (the world's largest known uranium deposit), Ranger, Jabiluka, Koongarra, Kintyre and Yeelirrie.[1]
For a more comprehensive list, see List of uranium mines.
Closed/depleted
Radium Hill
Nabarlek Uranium Mine
Rum Jungle Mine
Mary Kathleen mine
Operating
Olympic Dam mine
Ranger Uranium Mine
Beverley Uranium Mine
Four Mile uranium mine
Honeymoon Uranium Mine
Known deposits/possible future minesites
See also: Uranium in Western Australia
Mount Gee uranium deposit
Jabiluka uranium deposit
Kintyre uranium deposit
Yeelirrie uranium project
Angela uranium deposit
Wiluna uranium deposit
See also[edit]
Australia portal
Energy portal
Anti-nuclear movement in Australia
Australian Uranium Association
Environmental issues in Australia
Fallout and Follow Me (1977 play)
Gavin Mudd
List of countries by uranium reserves
Nuclear industry in South Australia
Nuclear power in Australia
Supervising Scientist
Treaty on the Non-Proliferation of Nuclear Weapons
Uranium mining in Kakadu National Park
World Uranium Hearing
References[edit]
^ Jump up to: a b c d e f g h "Australia's Uranium and Nuclear Power Prospects". World Nuclear Association. August 2011. Retrieved 4 October 2011.
Jump up ^ OECD. Uranium 2009: Resources, Production and Demand. OECD NEA Publication 6891. 2010
Jump up ^ "World Uranium Mining". World Nuclear Association. May 2010. Retrieved 25 June 2010.
Jump up ^ "Australian Uranium - Australian Uranium Market Overview". www.australianuranium.com.au. Retrieved 2017-02-22.
Jump up ^ radiumhill.org.au website
Jump up ^ "Uranium deposits in Australia". Government of South Australia Primary Industries and Resources. 13 March 2009. Retrieved 26 July 2009.
Jump up ^ "Port Pirie Uranium Treatment Complex, SA". www.sea-us.org.au. Retrieved 26 July 2009.
Jump up ^ Major Commonwealth Inquiries and Reports relating to Uranium Mining
Jump up ^ "Uranium supply: a troubled market". Nuclear Engineering International. 3 October 2013.
Jump up ^ Google Earth keyhole map of Uranium sites
^ Jump up to: a b Michael Lampard. "Uranium Outlook to 2013-14". ABARE. Retrieved 26 July 2009.
Jump up ^ "Prospect or suspect – uranium mining in Australia". Australian Academy of Science. September 2002. Retrieved 24 July 2009.
Jump up ^ "Prime Minister of Australia - Media Release - Uranium Mining and Nuclear Energy: A Way Forward for Australia". 2007-06-07. Archived from the original on 7 June 2007. Retrieved 2016-04-01.
Jump up ^ Mascher, Sharon (2007). "Too Hot to Handle? Uranium and Nuclear Power in Australia's Energy Mix" (PDF). Australian Resources and Energy Law Journal. Retrieved 2016-04-01.
Jump up ^ Peter Van Onselen (18 July 2009). "The good oil: Peter Garrett knows his job". The Australian. Archived from the original on 19 July 2009. Retrieved 25 July 2009.
Jump up ^ Paul Robinson and Maria Hatzakis (21 July 2009). "Qld uranium mining 'inevitable'". ABC News. Retrieved 27 July 2009.
Jump up ^ "Mine objections 'short-sighted'". ABC News. 15 July 2009. Retrieved 25 July 2009.
Jump up ^ "Barnett lifts WA uranium ban". WA Today. 17 November 2008. Retrieved 25 July 2009.
^ Jump up to: a b "Qld uranium mining ban on again". 2015-03-15. Retrieved 2015-08-18.
^ Jump up to: a b "Uranium Exploration" New South Wales Government - Trade & Investment, Australia. Accessed 2014-07-03.
^ Jump up to: a b "Newman lifts uranium mining ban in Queensland" ABC News, October 22, 2012 (Retrieved 2013-12-12).
Jump up ^ "Door opens for uranium explorers in Tasmania" Sydney Morning Herald, 2007-09-24. Retrieved 2013-12-12.
Jump up ^ Aborigines count cost of mine(25 May 2004) By Phil Mercer, BBC correspondent in Darwin, BBC NEWS / ASIA-PACIFIC
Jump up ^ Anti-uranium demos in Australia(5 April 1998)BBC World Service
Jump up ^ Anti-nuke protests(16 July 1997)By Jennifer Thompson, Green Left Weekly
Jump up ^ "Protesters issue warning on Olympic Dam expansion". Green Left Weekly. 2016-09-06. Retrieved 2017-02-22.
Jump up ^ Sarah Martin (16 July 2012). "Police accused over Olympic Dam protest". The Australian.
Jump up ^ http://www.abc.net.au/news/2012-08-22/bhp-billiton-profit-falls-a-third/4215638
Jump up ^ "BHP given more time on Olympic Dam expansion". ABC News. 2012-11-13. Retrieved 2017-02-22.
Jump up ^ "BHP announces scaled back Olympic Dam expansion plans". ABC News. 2016-07-08. Retrieved 2017-02-22.
Jump up ^ "Investor confidence shaken after QLD uranium mining ban". Australian Mining. Retrieved 2015-12-07.
Jump up ^ "No uranium mining please, we're Queenslanders". Brisbane Times. Retrieved 2015-12-07.
Jump up ^ "Home | Nuclear Fuel Cycle Royal Commission". nuclearrc.sa.gov.au. Retrieved 2017-02-22.
Jump up ^ "South Australia government responds to Royal Commission". www.world-nuclear-news.org. Retrieved 2017-02-22.
Jump up ^ "Western Australia about to get its first uranium mine | MINING.com". MINING.com. 2017-01-09. Retrieved 2017-02-22.
Jump up ^ http://asia.nikkei.com/Markets/Commodities/West-Australian-uranium-mines-win-approval-as-prices-rise
External links[edit]
Australian atlas of minerals resources, mines & processing centres
Australia’s uranium resources, geology and development of deposits Geoscience Australia
Australian Map of Nuclear and Uranium Sites
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Lists
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