Jupiter was the first of the Sun's planets to form, and its inward migration during the primordial phase of the Solar System affected much of the formation history of the other planets. Jupiter's atmosphere consists of 76% hydrogen and 24% helium by mass, with a denser interior. It contains trace elements like carbon, oxygen, sulfur, neon, ammonia, water vapour, phosphine, hydrogen sulfide, and hydrocarbons. Jupiter's helium abundance is 80% of the Sun's, similar to Saturn's composition. The ongoing contraction of Jupiter's interior generates more heat than the planet receives from the Sun. Its internal structure is believed to consist of an outer mantle of fluid metallic hydrogen and a diffuse inner core of denser material. Because of its rapid rate of rotation, one turn in ten hours, Jupiter is an oblate spheroid; it has a slight but noticeable bulge around the equator. The outer atmosphere is divided into a series of latitudinal bands, with turbulence and storms along their interacting boundaries; the most obvious result of this is the Great Red Spot, a giant storm that has been recorded since 1831.
Jupiter's magnetic field is the strongest and second-largest contiguous structure in the Solar System, generated by eddy currents within the fluid, metallic hydrogen core. The solar wind interacts with the magnetosphere, extending it outward and affecting Jupiter's orbit. Jupiter is surrounded by a faint system of planetary rings that were discovered in 1979 by Voyager 1 and further investigated by the Galileo orbiter in the 1990s. The Jovian ring system consists mainly of dust and has three main segments: an inner torus of particles known as the halo, a relatively bright main ring, and an outer gossamer ring. The rings have a reddish colour in visible and near-infrared light. The age of the ring system is unknown, possibly dating back to Jupiter's formation.
In both the ancient Greek and Roman civilizations, Jupiter was named after the chief god of the divine pantheon: Zeus to the Greeks and Jupiter to the Romans.[19] The International Astronomical Union formally adopted the name Jupiter for the planet in 1976 and has since named its newly discovered satellites for the god's lovers, favourites, and descendants.[20] The planetary symbol for Jupiter, , descends from a Greek zeta with a horizontal stroke, ⟨Ƶ⟩, as an abbreviation for Zeus.[21][22]
In Latin, Iovis is the genitive case of Iuppiter, i.e. Jupiter. It is associated with the etymology of Zeus ('sky father'). The English equivalent, Jove, is known to have come into use as a poetic name for the planet around the 14th century.[23]
Jovian is the adjectival form of Jupiter. The older adjectival form jovial, employed by astrologers in the Middle Ages, has come to mean 'happy' or 'merry', moods ascribed to Jupiter's influence in astrology.[24]
The original Greek deity Zeus supplies the root zeno-, which is used to form some Jupiter-related words, such as zenographic.[d]
Jupiter is believed to be the oldest planet in the Solar System, having formed just one million years after the Sun and roughly 50 million years before Earth.[25] Current models of Solar System formation suggest that Jupiter formed at or beyond the snow line: a distance from the early Sun where the temperature was sufficiently cold for volatiles such as water to condense into solids.[26] First forming a solid core, the planet then accumulated its gaseous atmosphere. Therefore, the planet must have formed before the solar nebula was fully dispersed.[27] During its formation, Jupiter's mass gradually increased until it had 20 times the mass of the Earth, approximately half of which was made up of silicates, ices and other heavy-element constituents.[25] When the proto-Jupiter grew larger than 50 Earth masses it created a gap in the solar nebula.[25] Thereafter, the growing planet reached its final mass in 3–4million years.[25][27] Since Jupiter is made of the same elements as the Sun (hydrogen and helium) it has been suggested that the Solar System might have been early in its formation a system of multiple protostars, which are quite common, with Jupiter being the second but failed protostar. But the Solar System never developed into a system of multiple stars and Jupiter does not qualify as a protostar or brown dwarf since it does not have enough mass to fuse hydrogen.[28][29]
According to the "grand tack hypothesis", Jupiter began to form at a distance of roughly 3.5AU (520millionkm; 330millionmi) from the Sun. As the young planet accreted mass, its interaction with the gas disk orbiting the Sun and the orbital resonances from Saturn caused it to migrate inward.[26][30] This upset the orbits of several super-Earths orbiting closer to the Sun, causing them to collide destructively.[31] Saturn would later have begun to migrate inwards at a faster rate than Jupiter until the two planets became captured in a 3:2 mean motion resonance at approximately 1.5AU (220millionkm; 140millionmi) from the Sun.[32] This changed the direction of migration, causing them to migrate away from the Sun and out of the inner system to their current locations.[31] All of this happened over a period of 3–6million years, with the final migration of Jupiter occurring over several hundred thousand years.[30][33] Jupiter's migration from the inner solar system eventually allowed the inner planets—including Earth—to form from the rubble.[34]
There are several unresolved issues with the grand tack hypothesis. The resulting formation timescales of terrestrial planets appear to be inconsistent with the measured elemental composition.[35] Jupiter would likely have settled into an orbit much closer to the Sun if it had migrated through the solar nebula.[36] Some competing models of Solar System formation predict the formation of Jupiter with orbital properties that are close to those of the present-day planet.[27] Other models predict Jupiter forming at distances much farther out, such as 18AU (2.7billionkm; 1.7billionmi).[37][38]
According to the Nice model, the infall of proto-Kuiper belt objects over the first 600 million years of Solar System history caused Jupiter and Saturn to migrate from their initial positions into a 1:2 resonance, which caused Saturn to shift into a higher orbit, disrupting the orbits of Uranus and Neptune, depleting the Kuiper belt, and triggering the Late Heavy Bombardment.[39]
Based on Jupiter's composition, researchers have made the case for an initial formation outside the molecular nitrogen (N2) snow line, which is estimated at 20–30AU (3.0–4.5billionkm; 1.9–2.8billionmi) from the Sun, and possibly even outside the argon snow line, which may be as far as 40AU (6.0billionkm; 3.7billionmi).[40][41] Having formed at one of these extreme distances, Jupiter would then have, over a roughly 700,000-year period, migrated inwards to its current location,[37][38] during an epoch approximately 2–3million years after the planet began to form. In this model, Saturn, Uranus, and Neptune would have formed even further out than Jupiter, and Saturn would also have migrated inwards.[37]
Physical characteristics
Jupiter is a gas giant, meaning its chemical composition is primarily hydrogen and helium. These materials are classified as gasses in planetary geology, a term that does not denote the state of matter. It is the largest planet in the Solar System, with a diameter of 142,984km (88,846mi) at its equator, giving it a volume 1,321 times that of the Earth.[2][42] Its average density, 1.326g/cm3,[e] is lower than those of the four terrestrial planets.[44][45]
Composition
The atmosphere of Jupiter is approximately 76% hydrogen and 24% helium by mass. By volume, the upper atmosphere is about 90% hydrogen and 10% helium, with the lower proportion owing to the individual helium atoms being more massive than the molecules of hydrogen formed in this part of the atmosphere.[46] The atmosphere contains trace amounts of elemental carbon, oxygen, sulfur, and neon,[47] as well as ammonia, water vapour, phosphine, hydrogen sulfide, and hydrocarbons like methane, ethane and benzene.[48] Its outermost layer contains crystals of frozen ammonia.[49] The planet's interior is denser, with a composition of roughly 71% hydrogen, 24% helium, and 5% other elements by mass.[50][51]
The atmospheric proportions of hydrogen and helium are close to the theoretical composition of the primordial solar nebula.[52] Neon in the upper atmosphere consists of 20 parts per million by mass, which is about a tenth as abundant as in the Sun.[53] Jupiter's helium abundance is about 80% that of the Sun due to the precipitation of these elements as helium-rich droplets, a process that happens deep in the planet's interior.[54][55]
Based on spectroscopy, Saturn is thought to be similar in composition to Jupiter, but the other giant planets Uranus and Neptune have relatively less hydrogen and helium and relatively more of the next most common elements, including oxygen, carbon, nitrogen, and sulfur.[56] These planets are known as ice giants because during their formation, these elements are thought to have been incorporated into them as ice; however, they probably contain very little ice.[57]
Size of Jupiter compared to Earth and Earth's Moon
Jupiter is about ten times larger than Earth (11.209R🜨) and smaller than the Sun (0.10276R☉). Jupiter's mass is 318 times that of Earth;[2] 2.5 times that of all the other planets in the Solar System combined. It is so massive that its barycentre with the Sun lies above the Sun's surface at 1.068solar radii from the Sun's centre.[58][59]:6 Jupiter's radius is about one tenth the radius of the Sun,[60] and its mass is one thousandth the mass of the Sun, as the densities of the two bodies are similar.[61] A "Jupiter mass" (MJ or MJup) is used as a unit to describe masses of other objects, particularly extrasolar planets and brown dwarfs. For example, the extrasolar planet HD 209458 b has a mass of 0.69MJ, while the brown dwarf Gliese 229 b has a mass of 60.4MJ.[62][63]
Theoretical models indicate that if Jupiter had over 40% more mass, the interior would be so compressed that its volume would decrease despite the increasing amount of matter. For smaller changes in its mass, the radius would not change appreciably.[64] As a result, Jupiter is thought to have about as large a diameter as a planet of its composition and evolutionary history can achieve.[65] The process of further shrinkage with increasing mass would continue until appreciable stellar ignition was achieved.[66] Although Jupiter would need to be about 75 times more massive to fuse hydrogen and become a star,[67] its diameter is sufficient as the smallest red dwarf may be slightly larger in radius than Saturn.[68]
Jupiter radiates more heat than it receives through solar radiation, due to the Kelvin–Helmholtz mechanism within its contracting interior.[69]:30[70] This process causes Jupiter to shrink by about 1mm (0.039in) per year.[71][72] At the time of its formation, Jupiter was hotter and was about twice its current diameter.[73]
Internal structure
Diagram of Jupiter with its interior, surface features, rings, and inner moons
Before the early 21st century, most scientists proposed one of two scenarios for the formation of Jupiter. If the planet accreted first as a solid body, it would consist of a dense core, a surrounding layer of fluid metallic hydrogen (with some helium) extending outward to about 80% of the radius of the planet,[74] and an outer atmosphere consisting primarily of molecular hydrogen.[72] Alternatively, if the planet collapsed directly from the gaseous protoplanetary disk, it was expected to completely lack a core, consisting instead of a denser and denser fluid (predominantly molecular and metallic hydrogen) all the way to the centre. Data from the Juno mission showed that Jupiter has a diffuse core that mixes into its mantle, extending for 30–50% of the planet's radius, and comprising heavy elements with a combined mass 7–25 times the Earth.[75][76][77] This mixing process could have arisen during formation, while the planet accreted solids and gases from the surrounding nebula.[78] Alternatively, it could have been caused by an impact from a planet of about ten Earth masses a few million years after Jupiter's formation, which would have disrupted an originally compact Jovian core.[76][79]
Outside the layer of metallic hydrogen lies a transparent interior atmosphere of hydrogen. At this depth, the pressure and temperature are above molecular hydrogen's critical pressure of 1.3 MPa and critical temperature of 33K (−240.2°C; −400.3°F).[80] In this state, there are no distinct liquid and gas phases—hydrogen is said to be in a supercritical fluid state. The hydrogen and helium gas extending downward from the cloud layer gradually transitions to a liquid in deeper layers, possibly resembling something akin to an ocean of liquid hydrogen and other supercritical fluids.[69]:22[81][82] Physically, the gas gradually becomes hotter and denser as depth increases.[83][84]
Rain-like droplets of helium and neon precipitate downward through the lower atmosphere, depleting the abundance of these elements in the upper atmosphere.[54][85] Calculations suggest that helium drops separate from metallic hydrogen at a radius of 60,000km (37,000mi) (11,000km (6,800mi) below the cloud tops) and merge again at 50,000km (31,000mi) (22,000km (14,000mi) beneath the clouds).[86] Rainfalls of diamonds have been suggested to occur, as well as on Saturn[87] and the ice giants Uranus and Neptune.[88]
The temperature and pressure inside Jupiter increase steadily inward as the heat of planetary formation can only escape by convection.[55] At a surface depth where the atmospheric pressure level is 1bar (0.10MPa), the temperature is around 165K (−108°C; −163°F). The region where supercritical hydrogen changes gradually from a molecular fluid to a metallic fluid spans pressure ranges of 50–400GPa with temperatures of 5,000–8,400K (4,730–8,130°C; 8,540–14,660°F), respectively. The temperature of Jupiter's diluted core is estimated to be 20,000K (19,700°C; 35,500°F) with a pressure of around 4,000GPa.[89]
Timelapse of Jupiter's cloud system moving over the course of one month (photographed during Voyager 1 flyby in 1979)
The atmosphere of Jupiter is primarily composed of molecular hydrogen and helium, with a smaller amount of other compounds such as water, methane, hydrogen sulfide, and ammonia.[90] Jupiter's atmosphere extends to a depth of approximately 3,000km (2,000mi) below the cloud layers.[89]
Cloud layers
Jupiter is perpetually covered with clouds of ammonia crystals, which may contain ammonium hydrosulfide as well.[91] The clouds are located in the tropopause layer of the atmosphere, forming bands at different latitudes, known as tropical regions. These are subdivided into lighter-hued zones and darker belts. The interactions of these conflicting circulation patterns cause storms and turbulence. Wind speeds of 100 metres per second (360km/h; 220mph) are common in zonal jet streams.[92] The zones have been observed to vary in width, colour and intensity from year to year, but they have remained stable enough for scientists to name them.[59]:6
View of Jupiter's south pole
Enhanced colour view of Jupiter's southern storms
The cloud layer is about 50km (31mi) deep and consists of at least two decks of ammonia clouds: a thin, clearer region on top and a thicker, lower deck. There may be a thin layer of water clouds underlying the ammonia clouds, as suggested by flashes of lightning detected in the atmosphere of Jupiter.[93] These electrical discharges can be up to a thousand times as powerful as lightning on Earth.[94] The water clouds are assumed to generate thunderstorms in the same way as terrestrial thunderstorms, driven by the heat rising from the interior.[95] The Juno mission revealed the presence of "shallow lightning" which originates from ammonia-water clouds relatively high in the atmosphere.[96] These discharges carry "mushballs" of water-ammonia slushes covered in ice, which fall deep into the atmosphere.[97]Upper-atmospheric lightning has been observed in Jupiter's upper atmosphere, bright flashes of light that last around 1.4milliseconds. These are known as "elves" or "sprites" and appear blue or pink due to the hydrogen.[98][99]
The orange and brown colours in the clouds of Jupiter are caused by upwelling compounds that change colour when they are exposed to ultraviolet light from the Sun. The exact makeup remains uncertain, but the substances are thought to be made up of phosphorus, sulfur or possibly hydrocarbons.[69]:39[100] These colourful compounds, known as chromophores, mix with the warmer clouds of the lower deck. The light-coloured zones are formed when rising convection cells form crystallising ammonia that hides the chromophores from view.[101]
Jupiter has a low axial tilt, thus ensuring that the poles always receive less solar radiation than the planet's equatorial region. Convection within the interior of the planet transports energy to the poles, balancing out temperatures at the cloud layer.[59]:54
Great Red Spot and other vortices
Close-up of the Great Red Spot imaged by the Juno spacecraft in true colour. Due to the way Juno takes photographs, stitched image has extreme barrel distortion.
A well-known feature of Jupiter is the Great Red Spot,[102] a persistent anticyclonic storm located 22° south of the equator. It was first observed in 1831,[103] and possibly as early as 1665.[104][105] Images by the Hubble Space Telescope have shown two more "red spots" adjacent to the Great Red Spot.[106][107] The storm is visible through Earth-based telescopes with an aperture of 12cm or larger.[108] The storm rotates counterclockwise, with a period of about six days.[109] The maximum altitude of this storm is about 8km (5mi) above the surrounding cloud tops.[110] The Spot's composition and the source of its red colour remain uncertain, although photodissociated ammonia reacting with acetylene is a likely explanation.[111]
The Great Red Spot is larger than the Earth.[112]Mathematical models suggest that the storm is stable and will be a permanent feature of the planet.[113] However, it has significantly decreased in size since its discovery. Initial observations in the late 1800s showed it to be approximately 41,000km (25,500mi) across. As of 2015[update], the storm was measured at approximately 16,500 by 10,940km (10,250 by 6,800mi),[114] and was decreasing in length by about 930km (580mi) per year.[112][115] In October 2021, a Juno flyby mission measured the depth of the Great Red Spot, putting it at around 300–500 kilometres (190–310 miles).[116]
Juno missions found several cyclone groups at Jupiter's poles. The northern group contains nine cyclones, with a large one in the centre and eight others around it, while its southern counterpart also consists of a centre vortex but is surrounded by five large storms and a single smaller one for a total of 7 storms.[117][118]
Formation of Oval BA from three white ovals
In 2000, an atmospheric feature formed in the southern hemisphere that is similar in appearance to the Great Red Spot, but smaller. This was created when smaller, white oval-shaped storms merged to form a single feature—these three smaller white ovals were formed in 1939–1940. The merged feature was named Oval BA. It has since increased in intensity and changed from white to red, earning it the nickname "Little Red Spot".[119][120]
In April 2017, a "Great Cold Spot" was discovered in Jupiter's thermosphere at its north pole. This feature is 24,000km (15,000mi) across, 12,000km (7,500mi) wide, and 200°C (360°F) cooler than surrounding material. While this spot changes form and intensity over the short term, it has maintained its general position in the atmosphere for more than 15 years. It may be a giant vortex similar to the Great Red Spot, and appears to be quasi-stable like the vortices in Earth's thermosphere. This feature may be formed by interactions between charged particles generated from Io and the strong magnetic field of Jupiter, resulting in a redistribution of heat flow.[121]
Jupiter's magnetic field is the strongest of any planet in the Solar System,[101] with a dipole moment of 4.170 gauss (0.4170mT) that is tilted at an angle of 10.31° to the pole of rotation. The surface magnetic field strength varies from 2 gauss (0.20mT) up to 20 gauss (2.0mT).[122] This field is thought to be generated by eddy currents—swirling movements of conducting materials—within the fluid, metallic hydrogen core. At about 75 Jupiter radii from the planet, the interaction of the magnetosphere with the solar wind generates a bow shock. Surrounding Jupiter's magnetosphere is a magnetopause, located at the inner edge of a magnetosheath—a region between it and the bow shock. The solar wind interacts with these regions, elongating the magnetosphere on Jupiter's lee side and extending it outward until it nearly reaches the orbit of Saturn. The four largest moons of Jupiter all orbit within the magnetosphere, which protects them from solar wind.[69]:69
The volcanoes on the moon Io emit large amounts of sulfur dioxide, forming a gas torus along its orbit. The gas is ionized in Jupiter's magnetosphere, producing sulfur and oxygen ions. They, together with hydrogen ions originating from the atmosphere of Jupiter, form a plasma sheet in Jupiter's equatorial plane. The plasma in the sheet co-rotates with the planet, causing deformation of the dipole magnetic field into that of a magnetodisk. Electrons within the plasma sheet generate a strong radio signature, with short, superimposed bursts in the range of 0.6–30MHz that are detectable from Earth with consumer-grade shortwave radio receivers.[123][124] As Io moves through this torus, the interaction generates Alfvén waves that carry ionized matter into the polar regions of Jupiter. As a result, radio waves are generated through a cyclotronmaser mechanism, and the energy is transmitted out along a cone-shaped surface. When Earth intersects this cone, the radio emissions from Jupiter can exceed the radio output of the Sun.[125]
Jupiter has a faint planetary ring system composed of three main segments: an inner torus of particles known as the halo, a relatively bright main ring, and an outer gossamer ring.[127] These rings appear to be made of dust, whereas Saturn's rings are made of ice.[69]:65 The main ring is most likely made out of material ejected from the satellites Adrastea and Metis, which is drawn into Jupiter because of the planet's strong gravitational influence. New material is added by additional impacts.[128] In a similar way, the moons Thebe and Amalthea are believed to produce the two distinct components of the dusty gossamer ring.[128] There is evidence of a fourth ring that may consist of collisional debris from Amalthea that is strung along the same moon's orbit.[129]
Orbit and rotation
3-hour timelapse showing rotation of Jupiter and orbital motion of the moons
Jupiter is the only planet whose barycentre with the Sun lies outside the volume of the Sun, though by 7% of the Sun's radius.[130][131] The average distance between Jupiter and the Sun is 778millionkm (5.2AU) and it completes an orbit every 11.86years. This is approximately two-fifths the orbital period of Saturn, forming a near orbital resonance.[132] The orbital plane of Jupiter is inclined 1.30° compared to Earth. Because the eccentricity of its orbit is 0.049, Jupiter is slightly over 75millionkm nearer the Sun at perihelion than aphelion,[2] which means that its orbit is nearly circular. This low eccentricity is at odds with exoplanet discoveries, which have revealed Jupiter-sized planets with very high eccentricities. Models suggest this may be due to there being two giant planets in our Solar System, as the presence of a third or more giant planets tends to induce larger eccentricities.[133]
The axial tilt of Jupiter is 3.13°, which is relatively small, so its seasons are insignificant compared to those of Earth and Mars.[134]
Jupiter's rotation is the fastest of all the Solar System's planets, completing a rotation on its axis in slightly less than ten hours; this creates an equatorial bulge easily seen through an amateur telescope. Because Jupiter is not a solid body, its upper atmosphere undergoes differential rotation. The rotation of Jupiter's polar atmosphere is about 5minutes longer than that of the equatorial atmosphere.[135] The planet is an oblate spheroid, meaning that the diameter across its equator is longer than the diameter measured between its poles.[84] On Jupiter, the equatorial diameter is 9,276km (5,764mi) longer than the polar diameter.[2]
Three systems are used as frames of reference for tracking planetary rotation, particularly when graphing the motion of atmospheric features. System I applies to latitudes from 7°N to 7°S; its period is the planet's shortest, at 9h50m30.0s. System II applies at latitudes north and south of these; its period is 9h55m40.6s.[136] System III was defined by radio astronomers and corresponds to the rotation of the planet's magnetosphere; its period is Jupiter's official rotation.[137]
Observation
Jupiter and four Galilean moons seen through an amateur telescope
Jupiter is usually the fourth brightest object in the sky (after the Sun, the Moon, and Venus),[101] although at opposition Mars can appear brighter than Jupiter. Depending on Jupiter's position with respect to the Earth, it can vary in visual magnitude from as bright as −2.94 at opposition down to −1.66 during conjunction with the Sun.[16] The mean apparent magnitude is −2.20 with a standard deviation of 0.33.[16] The angular diameter of Jupiter likewise varies from 50.1 to 30.5 arc seconds.[2] Favourable oppositions occur when Jupiter is passing through the perihelion of its orbit, bringing it closer to Earth.[138] Near opposition, Jupiter will appear to go into retrograde motion for a period of about 121 days, moving backward through an angle of 9.9° before returning to prograde movement.[139]
Because the orbit of Jupiter is outside that of Earth, the phase angle of Jupiter as viewed from Earth is always less than 11.5°; thus, Jupiter always appears nearly fully illuminated when viewed through Earth-based telescopes. It was during spacecraft missions to Jupiter that crescent views of the planet were obtained.[140] A small telescope will usually show Jupiter's four Galilean moons and the cloud belts across Jupiter's atmosphere. A larger telescope with an aperture of 4–6 inches (10–15cm) will show Jupiter's Great Red Spot when it faces Earth.[141][142]
History
Pre-telescopic research
Model in the Almagest of the longitudinal motion of Jupiter (☉) relative to Earth (🜨)
Observation of Jupiter dates back to at least the Babylonian astronomers of the 7th or 8th century BC.[143] The ancient Chinese knew Jupiter as the "Suì Star" (Suìxīng歲星) and established their cycle of 12 earthly branches based on the approximate number of years it takes Jupiter to rotate around the Sun; the Chinese language still uses its name (simplified as 歲) when referring to years of age. By the 4th century BC, these observations had developed into the Chinese zodiac,[144] and each year became associated with a Tai Sui star and god controlling the region of the heavens opposite Jupiter's position in the night sky. These beliefs survive in some Taoistreligious practices and in the East Asian zodiac's twelve animals. The Chinese historian Xi Zezong has claimed that Gan De, an ancient Chinese astronomer,[145] reported a small star "in alliance" with the planet,[146] which may indicate a sighting of one of Jupiter's moons with the unaided eye. If true, this would predate Galileo's discovery by nearly two millennia.[147][148]
A 2016 paper reports that trapezoidal rule was used by Babylonians before 50 BC for integrating the velocity of Jupiter along the ecliptic.[149] In his 2nd century work the Almagest, the Hellenistic astronomer Claudius Ptolemaeus constructed a geocentric planetary model based on deferents and epicycles to explain Jupiter's motion relative to Earth, giving its orbital period around Earth as 4332.38days, or 11.86years.[150]
Ground-based telescope research
Galileo's drawings of Jupiter and its "Medicean Stars" from Sidereus Nuncius
In 1610, Italian polymath Galileo Galilei discovered the four largest moons of Jupiter (now known as the Galilean moons) using a telescope. This is thought to be the first telescopic observation of moons other than Earth's. Just one day after Galileo, Simon Marius independently discovered moons around Jupiter, though he did not publish his discovery in a book until 1614.[151] It was Marius's names for the major moons, however, that stuck: Io, Europa, Ganymede, and Callisto. The discovery was a major point in favour of the heliocentric theory of the motions of the planets by Nicolaus Copernicus; Galileo's outspoken support of the Copernican theory led to him being tried and condemned by the Inquisition.[152]
In the autumn of 1639, the Neapolitan optician Francesco Fontana tested a 22-palm telescope of his own making and discovered the characteristic bands of the planet's atmosphere.[153]
During the 1660s, Giovanni Cassini used a new telescope to discover spots in Jupiter's atmosphere, observe that the planet appeared oblate, and estimate its rotation period.[154] In 1692, Cassini noticed that the atmosphere undergoes a differential rotation.[155]
The Great Red Spot may have been observed as early as 1664 by Robert Hooke and in 1665 by Cassini, although this is disputed. The pharmacist Heinrich Schwabe produced the earliest known drawing to show details of the Great Red Spot in 1831.[156] The Red Spot was reportedly lost from sight on several occasions between 1665 and 1708 before becoming quite conspicuous in 1878.[157] It was recorded as fading again in 1883 and at the start of the 20th century.[158]
Both Giovanni Borelli and Cassini made careful tables of the motions of Jupiter's moons, which allowed predictions of when the moons would pass before or behind the planet. By the 1670s, Cassini observed that when Jupiter was on the opposite side of the Sun from Earth, these events would occur about 17minutes later than expected. Ole Rømer deduced that light does not travel instantaneously (a conclusion that Cassini had earlier rejected),[51] and this timing discrepancy was used to estimate the speed of light.[159][160]
In 1892, E. E. Barnard observed a fifth satellite of Jupiter with the 36-inch (910mm) refractor at Lick Observatory in California. This moon was later named Amalthea.[161] It was the last planetary moon to be discovered directly by a visual observer through a telescope.[162] An additional eight satellites were discovered before the flyby of the Voyager 1 probe in 1979.[f]
In 1932, Rupert Wildt identified absorption bands of ammonia and methane in the spectra of Jupiter.[163] Three long-lived anticyclonic features called "white ovals" were observed in 1938. For several decades, they remained as separate features in the atmosphere that approach each other but never merge. Finally, two of the ovals merged in 1998, then absorbed the third in 2000, becoming Oval BA.[164]
Radiotelescope research
In 1955, Bernard Burke and Kenneth Franklin discovered that Jupiter emits bursts of radio waves at a frequency of 22.2MHz.[69]:36 The period of these bursts matched the rotation of the planet, and they used this information to determine a more precise value for Jupiter's rotation rate. Radio bursts from Jupiter were found to come in two forms: long bursts (or L-bursts) lasting up to several seconds, and short bursts (or S-bursts) lasting less than a hundredth of a second.[165]
Scientists have discovered three forms of radio signals transmitted from Jupiter:
Decametric radio bursts (with a wavelength of tens of metres) vary with the rotation of Jupiter, and are influenced by the interaction of Io with Jupiter's magnetic field.[166]
Decimetric radio emission (with wavelengths measured in centimetres) was first observed by Frank Drake and Hein Hvatum in 1959.[69]:36 The origin of this signal is a torus-shaped belt around Jupiter's equator, which generates cyclotron radiation from electrons that are accelerated in Jupiter's magnetic field.[167]
Jupiter has been visited by automated spacecraft since 1973, when the space probe Pioneer 10 passed close enough to Jupiter to send back revelations about its properties and phenomena.[168][169] Missions to Jupiter are accomplished at a cost in energy, which is described by the net change in velocity of the spacecraft, or delta-v. Entering a Hohmann transfer orbit from Earth to Jupiter from low Earth orbit requires a delta-v of 6.3km/s,[170] which is comparable to the 9.7km/s delta-v needed to reach low Earth orbit.[171]Gravity assists through planetary flybys can be used to reduce the energy required to reach Jupiter.[172]
Beginning in 1973, several spacecraft performed planetary flyby manoeuvres that brought them within the observation range of Jupiter. The Pioneer missions obtained the first close-up images of Jupiter's atmosphere and several of its moons. They discovered that the radiation fields near the planet were much stronger than expected, but both spacecraft managed to survive in that environment. The trajectories of these spacecraft were used to refine the mass estimates of the Jovian system. Radio occultations by the planet resulted in better measurements of Jupiter's diameter and the amount of polar flattening.[59]:47[174]
Six years later, the Voyager missions vastly improved the understanding of the Galilean moons and discovered Jupiter's rings. They also confirmed that the Great Red Spot was anticyclonic. Comparison of images showed that the Spot had changed hues since the Pioneer missions, turning from orange to dark brown. A torus of ionized atoms was discovered along Io's orbital path, which were found to come from erupting volcanoes on the moon's surface. As the spacecraft passed behind the planet, it observed flashes of lightning in the night side atmosphere.[59]:87[175]
The next mission to encounter Jupiter was the Ulysses solar probe. In February 1992, it performed a flyby manoeuvre to attain a polar orbit around the Sun. During this pass, the spacecraft studied Jupiter's magnetosphere, although it had no cameras to photograph the planet. The spacecraft passed by Jupiter six years later, this time at a much greater distance.[173]
In 2000, the Cassini probe flew by Jupiter on its way to Saturn, and provided higher-resolution images.[176]
The New Horizons probe flew by Jupiter in 2007 for a gravity assist en route to Pluto.[177] The probe's cameras measured plasma output from volcanoes on Io and studied all four Galilean moons in detail.[178]
Galileo in preparation for mating with the rocket, 1989
The first spacecraft to orbit Jupiter was the Galileo mission, which reached the planet on December 7, 1995.[65] It remained in orbit for over seven years, conducting multiple flybys of all the Galilean moons and Amalthea. The spacecraft also witnessed the impact of Comet Shoemaker–Levy 9 when it collided with Jupiter in 1994. Some of the goals for the mission were thwarted due to a malfunction in Galileos high-gain antenna.[179]
A 340-kilogram titanium atmospheric probe was released from the spacecraft in July 1995, entering Jupiter's atmosphere on December 7.[65] It parachuted through 150km (93mi) of the atmosphere at a speed of about 2,575km/h (1,600mph)[65] and collected data for 57.6minutes until the spacecraft was destroyed.[180] The Galileo orbiter itself experienced a more rapid version of the same fate when it was deliberately steered into the planet on September 21, 2003. NASA destroyed the spacecraft to avoid any possibility of the spacecraft crashing into and possibly contaminating the moon Europa, which may harbour life.[179]
Data from this mission revealed that hydrogen composes up to 90% of Jupiter's atmosphere.[65] The recorded temperature was more than 300°C (570°F), and the wind speed measured more than 644km/h (>400mph) before the probes vaporized.[65]
Juno preparing for testing in a rotation stand, 2011
NASA's Juno mission arrived at Jupiter on July 4, 2016, with the goal of studying the planet in detail from a polar orbit. The spacecraft was originally intended to orbit Jupiter thirty-seven times over a period of twenty months.[181][77][182] During the mission, the spacecraft will be exposed to high levels of radiation from Jupiter's magnetosphere, which may cause the failure of certain instruments.[183] On August 27, 2016, the spacecraft completed its first flyby of Jupiter and sent back the first-ever images of Jupiter's north pole.[184]
Juno completed 12 orbits before the end of its budgeted mission plan, ending in July 2018.[185] In June of that year, NASA extended the mission operations plan to July 2021, and in January of that year the mission was extended to September 2025 with four lunar flybys: one of Ganymede, one of Europa, and two of Io.[186][187] When Juno reaches the end of the mission, it will perform a controlled deorbit and disintegrate into Jupiter's atmosphere. This will avoid the risk of collision with Jupiter's moons.[188][189]
Cancelled missions and future plans
There is an interest in missions to study Jupiter's larger icy moons, which may have subsurface liquid oceans.[190] Funding difficulties have delayed progress, causing NASA's JIMO (Jupiter Icy Moons Orbiter) to be cancelled in 2005.[191] A subsequent proposal was developed for a joint NASA/ESA mission called EJSM/Laplace, with a provisional launch date around 2020. EJSM/Laplace would have consisted of the NASA-led Jupiter Europa Orbiter and the ESA-led Jupiter Ganymede Orbiter.[192] However, the ESA formally ended the partnership in April 2011, citing budget issues at NASA and the consequences on the mission timetable. Instead, ESA planned to go ahead with a European-only mission to compete in its L1 Cosmic Vision selection.[193] These plans have been realized as the European Space Agency's Jupiter Icy Moon Explorer (JUICE), launched on April 14, 2023,[194] followed by NASA's Europa Clipper mission, launched on October 14, 2024.[195]
Jupiter has 95 known natural satellites,[199] and it is likely that this number would go up due to improved instrumentation.[200] Of these, 79 are less than 10km in diameter.[7] The four largest moons are Ganymede, Callisto, Io, and Europa (in order of decreasing size), collectively known as the "Galilean moons", and are visible from Earth with binoculars on a clear night.[201]
The moons discovered by Galileo—Io, Europa, Ganymede, and Callisto—are among the largest in the Solar System. The orbits of Io, Europa, and Ganymede form a pattern known as a Laplace resonance; for every four orbits that Io makes around Jupiter, Europa makes exactly two orbits and Ganymede makes exactly one. This resonance causes the gravitational effects of the three large moons to distort their orbits into elliptical shapes, because each moon receives an extra tug from its neighbours at the same point in every orbit it makes. The tidal force from Jupiter, on the other hand, works to circularize their orbits.[202]
The eccentricity of their orbits causes regular flexing of the three moons' shapes, with Jupiter's gravity stretching them out as they approach it and allowing them to spring back to more spherical shapes as they swing away. The friction created by this tidal flexing generates heat in the interior of the moons.[203] This is seen most dramatically in the volcanic activity of Io (which is subject to the strongest tidal forces),[203] and to a lesser degree in the geological youth of Europa's surface, which indicates recent resurfacing of the moon's exterior.[204]
The Galilean satellites in false colour. From left to right, in order of increasing distance from Jupiter: Io, Europa, Ganymede, Callisto.
The Galilean satellites Io, Europa, Ganymede, and Callisto (in order of increasing distance from Jupiter) in false colour
Classification
Jupiter's moons were classified into four groups of four, based on their similar orbital elements.[205] This picture has been complicated by the discovery of numerous small outer moons since 1999. Jupiter's moons are divided into several different groups, although there are two known moons which are not part of any group (Themisto and Valetudo).[206]
The eight innermost regular moons, which have nearly circular orbits near the plane of Jupiter's equator, are thought to have formed alongside Jupiter, while the remainder are irregular moons and are thought to be captured asteroids or fragments of captured asteroids. The irregular moons within each group may have a common origin, perhaps as a larger moon or captured body that broke up.[207][208]
The inner group of four small moons all have diameters of less than 200km, orbit at radii less than 200,000km, and have orbital inclinations of less than half a degree.[209]
These four moons, discovered by Galileo Galilei and by Simon Marius in parallel, orbit between 400,000 and 2,000,000km, and are some of the largest moons in the Solar System.
This group of retrograde-orbiting moons has rather indistinct borders, averaging 21,276,000km from Jupiter with an average inclination of 149 degrees.[208]
A dispersed and vaguely distinct retrograde group that covers all the outermost moons.[212]
Interaction with the Solar System
As the most massive of the eight planets, the gravitational influence of Jupiter has helped shape the Solar System. With the exception of Mercury, the orbits of the system's planets lie closer to Jupiter's orbital plane than the Sun's equatorial plane. The Kirkwood gaps in the asteroid belt are mostly caused by Jupiter,[213] and the planet may have been responsible for the Late Heavy Bombardment in the inner Solar System's history.[214]
In addition to its moons, Jupiter's gravitational field controls numerous asteroids that have settled around the Lagrangian points that precede and follow the planet in its orbit around the Sun. These are known as the Trojan asteroids, and are divided into Greek and Trojan "camps" to honour the Iliad. The first of these, 588 Achilles, was discovered by Max Wolf in 1906; since then more than two thousand have been discovered.[215] The largest is 624 Hektor.[216]
The Jupiter family is defined as comets that have a semi-major axis smaller than Jupiter's; most short-period comets belong to this group. Members of the Jupiter family are thought to form in the Kuiper belt outside the orbit of Neptune. During close encounters with Jupiter, they are perturbed into orbits with a smaller period, which then becomes circularized by regular gravitational interactions with the Sun and Jupiter.[217]
Jupiter has been called the Solar System's vacuum cleaner[218] because of its immense gravity well and location near the inner Solar System. There are more impacts on Jupiter, such as comets, than on any other planet in the Solar System.[219] For example, Jupiter experiences about 200 times more asteroid and comet impacts than Earth.[65] Scientists used to believe that Jupiter partially shielded the inner system from cometary bombardment.[65] However, computer simulations in 2008 suggest that Jupiter does not cause a net decrease in the number of comets that pass through the inner Solar System, as its gravity perturbs their orbits inward roughly as often as it accretes or ejects them.[220] This topic remains controversial among scientists, as some think it draws comets towards Earth from the Kuiper belt, while others believe that Jupiter protects Earth from the Oort cloud.[221]
Surveys of early astronomical records and drawings produced eight examples of potential impact observations between 1664 and 1839. However, a 1997 review determined that these observations had little or no possibility of being the results of impacts. Further investigation by this team revealed a dark surface feature discovered by astronomer Giovanni Cassini in 1690 may have been an impact scar.[228]
Jupiter, woodcut from a 1550 edition of Guido Bonatti's Liber Astronomiae
The existence of the planet Jupiter has been known since ancient times. It is visible to the naked eye in the night sky and can be seen in the daytime when the Sun is low.[229] To the Babylonians, this planet represented their god Marduk,[230] chief of their pantheon from the Hammurabi period.[231] They used Jupiter's roughly 12-year orbit along the ecliptic to define the constellations of their zodiac.[230]
The mythical Greek name for this planet is Zeus (Ζεύς), also referred to as Dias (Δίας), the planetary name of which is retained in modern Greek.[232] The ancient Greeks knew the planet as Phaethon (Φαέθων), meaning "shining one" or "blazing star".[233][234] The Greek myths of Zeus from the Homeric period showed particular similarities to certain Near-Eastern gods, including the Semitic El and Baal, the Sumerian Enlil, and the Babylonian god Marduk.[235] The association between the planet and the Greek deity Zeus was drawn from Near Eastern influences and was fully established by the fourth century BC, as documented in the Epinomis of Plato and his contemporaries.[236]
The god Jupiter is the Roman counterpart of Zeus, and he is the principal god of Roman mythology. The Romans originally called Jupiter the "star of Jupiter" (Iuppiter Stella), as they believed it to be sacred to its namesake god. This name comes from the Proto-Indo-Europeanvocative compound *Dyēu-pəter (nominative: *Dyēus-pətēr, meaning "Father Sky-God", or "Father Day-God").[237] As the supreme god of the Roman pantheon, Jupiter was the god of thunder, lightning, and storms, and was called the god of light and sky.[238]
In Vedic astrology, Hindu astrologers named the planet after Brihaspati, the religious teacher of the gods, and called it "Guru", which means the "Teacher".[239][240] In Central Asian Turkic myths, Jupiter is called Erendiz or Erentüz, from eren (of uncertain meaning) and yultuz ("star"). The Turks calculated the period of the orbit of Jupiter as 11 years and 300 days. They believed that some social and natural events connected to Erentüz's movements in the sky.[241] The Chinese, Vietnamese, Koreans, and Japanese called it the "wood star" (Chinese:木星; pinyin:mùxīng), based on the Chinese Five Elements.[242][243][244] In China, it became known as the "Year-star" (Sui-sing), as Chinese astronomers noted that it jumped one zodiac constellation each year (with corrections). In some ancient Chinese writings, the years were, in principle, named in correlation with the Jovian zodiac signs.[144]
↑ This image was taken by the Hubble Space Telescope, using the Wide Field Camera 3, on April 21, 2014. Jupiter's atmosphere and its appearance constantly changes, and hence its current appearance today may not resemble what it was when this image was taken. Depicted in this image, however, are a few features that remain consistent, such as the famous Great Red Spot, featured prominently in the lower right of the image, and the planet's recognizable banded appearance.
1 2 3 4 5 6 Refers to the level of 1 bar atmospheric pressure
↑ Based on the volume within the level of 1 bar atmospheric pressure
Galileo was an American robotic space program that studied the planet Jupiter and its moons, as well as several other Solar System bodies. Named after the Italian astronomer Galileo Galilei, the Galileo spacecraft consisted of an orbiter and an atmospheric entry probe. It was delivered into Earth orbit on October 18, 1989, by Space ShuttleAtlantis on the STS-34 mission, and arrived at Jupiter on December 7, 1995, after gravity assist flybys of Venus and Earth, and became the first spacecraft to orbit Jupiter. The spacecraft then launched the first probe to directly measure its atmosphere. Despite suffering major antenna problems, Galileo achieved the first asteroid flyby, of 951 Gaspra, and discovered the first asteroid moon, Dactyl, around 243 Ida. In 1994, Galileo observed Comet Shoemaker–Levy 9's collision with Jupiter.
A planet is a large, rounded astronomical body that is generally required to be in orbit around a star, stellar remnant, or brown dwarf, and is not one itself. The Solar System has eight planets by the most restrictive definition of the term: the terrestrial planets Mercury, Venus, Earth, and Mars, and the giant planets Jupiter, Saturn, Uranus, and Neptune. The best available theory of planet formation is the nebular hypothesis, which posits that an interstellar cloud collapses out of a nebula to create a young protostar orbited by a protoplanetary disk. Planets grow in this disk by the gradual accumulation of material driven by gravity, a process called accretion.
The Solar System is the gravitationally bound system of the Sun and the objects that orbit it. It formed about 4.6 billion years ago when a dense region of a molecular cloud collapsed, forming the Sun and a protoplanetary disc. The Sun is a typical star that maintains a balanced equilibrium by the fusion of hydrogen into helium at its core, releasing this energy from its outer photosphere. Astronomers classify it as a G-type main-sequence star.
Callisto, or Jupiter IV, is the second-largest moon of Jupiter, after Ganymede. In the Solar System it is the third-largest moon after Ganymede and Saturn's largest moon Titan, and nearly as large as the smallest planet Mercury. Callisto is, with a diameter of 4,821 km, roughly a third larger than Earth's Moon and orbits Jupiter on average at a distance of 1,883,000 km, which is about six times further out than the Moon orbiting Earth. It is the outermost of the four large Galilean moons of Jupiter, which were discovered in 1610 with one of the first telescopes, being visible from Earth with common binoculars.
Europa, or Jupiter II, is the smallest of the four Galilean moons orbiting Jupiter, and the sixth-closest to the planet of all the 95 known moons of Jupiter. It is also the sixth-largest moon in the Solar System. Europa was discovered independently by Simon Marius and Galileo Galilei and was named after Europa, the Phoenician mother of King Minos of Crete and lover of Zeus.
Saturn is the sixth planet from the Sun and the second largest in the Solar System, after Jupiter. It is a gas giant, with an average radius of about nine times that of Earth. It has an eighth the average density of Earth, but is over 95 times more massive. Even though Saturn is almost as big as Jupiter, Saturn has less than a third the mass of Jupiter. Saturn orbits the Sun at a distance of 9.59 AU (1,434 million km), with an orbital period of 29.45 years.
Uranus is the seventh planet from the Sun. It is a gaseous cyan-coloured ice giant. Most of the planet is made of water, ammonia, and methane in a supercritical phase of matter, which astronomy calls "ice" or volatiles. The planet's atmosphere has a complex layered cloud structure and has the lowest minimum temperature of all the Solar System's planets. It has a marked axial tilt of 82.23° with a retrograde rotation period of 17 hours and 14 minutes. This means that in an 84-Earth-year orbital period around the Sun, its poles get around 42 years of continuous sunlight, followed by 42 years of continuous darkness.
Titan is the largest moon of Saturn and the second-largest in the Solar System. It is the only moon known to have an atmosphere denser than the Earth's and is the only known object in space—other than Earth—on which there is clear evidence that stable bodies of liquid exist. Titan is one of seven gravitationally rounded moons of Saturn and the second-most distant among them. Frequently described as a planet-like moon, Titan is 50% larger in diameter than Earth's Moon and 80% more massive. It is the second-largest moon in the Solar System after Jupiter's Ganymede and is larger than Mercury; yet Titan is only 40% as massive as Mercury, because Mercury is mainly iron and rock while much of Titan is ice, which is less dense.
Ganymede, or Jupiter III, is the largest and most massive natural satellite of Jupiter, and in the Solar System. Despite being the only moon in the Solar System with a substantial magnetic field, it is the largest Solar System object without a substantial atmosphere. Like Saturn's largest moon Titan, it is larger than the planet Mercury, but has somewhat less surface gravity than Mercury, Io, or the Moon due to its lower density compared to the three. Ganymede orbits Jupiter in roughly seven days and is in a 1:2:4 orbital resonance with the moons Europa and Io, respectively.
The rings of Jupiter are a system of faint planetary rings. The Jovian rings were the third ring system to be discovered in the Solar System, after those of Saturn and Uranus. The main ring was discovered in 1979 by the Voyager 1 space probe and the system was more thoroughly investigated in the 1990s by the Galileo orbiter. The main ring has also been observed by the Hubble Space Telescope and from Earth for several years. Ground-based observation of the rings requires the largest available telescopes.
Io, or Jupiter I, is the innermost and second-smallest of the four Galilean moons of the planet Jupiter. Slightly larger than Earth's moon, Io is the fourth-largest moon in the Solar System, has the highest density of any moon, the strongest surface gravity of any moon, and the lowest amount of water by atomic ratio of any known astronomical object in the Solar System. It was discovered in 1610 by Galileo Galilei and was named after the mythological character Io, a priestess of Hera who became one of Zeus's lovers.
Juno is a NASA space probe orbiting the planet Jupiter. It was built by Lockheed Martin and is operated by NASA's Jet Propulsion Laboratory. The spacecraft was launched from Cape Canaveral Air Force Station on August 5, 2011 UTC, as part of the New Frontiers program. Juno entered a polar orbit of Jupiter on July 5, 2016, UTC, to begin a scientific investigation of the planet. After completing its mission, Juno was originally planned to be intentionally deorbited into Jupiter's atmosphere, but has since been approved to continue orbiting until contact is lost with the spacecraft.
The magnetosphere of Saturn is the cavity created in the flow of the solar wind by the planet's internally generated magnetic field. Discovered in 1979 by the Pioneer 11 spacecraft, Saturn's magnetosphere is the second largest of any planet in the Solar System after Jupiter. The magnetopause, the boundary between Saturn's magnetosphere and the solar wind, is located at a distance of about 20 Saturn radii from the planet's center, while its magnetotail stretches hundreds of Saturn radii behind it.
The magnetosphere of Jupiter is the cavity created in the solar wind by Jupiter's magnetic field. Extending up to seven million kilometers in the Sun's direction and almost to the orbit of Saturn in the opposite direction, Jupiter's magnetosphere is the largest and most powerful of any planetary magnetosphere in the Solar System, and by volume the largest known continuous structure in the Solar System after the heliosphere. Wider and flatter than the Earth's magnetosphere, Jupiter's is stronger by an order of magnitude, while its magnetic moment is roughly 18,000 times larger. The existence of Jupiter's magnetic field was first inferred from observations of radio emissions at the end of the 1950s and was directly observed by the Pioneer 10 spacecraft in 1973.
The exploration of Jupiter has been conducted via close observations by automated spacecraft. It began with the arrival of Pioneer 10 into the Jovian system in 1973, and, as of 2024, has continued with eight further spacecraft missions in the vicinity of Jupiter and two more en route. All but one of these missions were undertaken by the National Aeronautics and Space Administration (NASA), and all but four were flybys taking detailed observations without landing or entering orbit. These probes make Jupiter the most visited of the Solar System's outer planets as all missions to the outer Solar System have used Jupiter flybys. On 5 July 2016, spacecraft Juno arrived and entered the planet's orbit—the second craft ever to do so. Sending a craft to Jupiter is difficult, mostly due to large fuel requirements and the effects of the planet's harsh radiation environment.
The Jupiter mass, also called Jovian mass, is the unit of mass equal to the total mass of the planet Jupiter. This value may refer to the mass of the planet alone, or the mass of the entire Jovian system to include the moons of Jupiter. Jupiter is by far the most massive planet in the Solar System. It is approximately 2.5 times as massive as all of the other planets in the Solar System combined.
The habitability of natural satellites is the potential of moons to provide habitats for life, though it is not an indicator that they harbor it. Natural satellites are expected to outnumber planets by a large margin and the study of their habitability is therefore important to astrobiology and the search for extraterrestrial life. There are, nevertheless, significant environmental variables specific to moons.
Neptune is the eighth and farthest known planet from the Sun. It is the fourth-largest planet in the Solar System by diameter, the third-most-massive planet, and the densest giant planet. It is 17 times the mass of Earth. Compared to its fellow ice giant Uranus, Neptune is slightly more massive, but denser and smaller. Being composed primarily of gases and liquids, it has no well-defined solid surface, and orbits the Sun once every 164.8 years at an orbital distance of 30.1 astronomical units. It is named after the Roman god of the sea and has the astronomical symbol , representing Neptune's trident.
Energetic Neutral Atom (ENA) imaging is a technology used to create global images of otherwise invisible phenomena in the magnetospheres of planets and throughout the heliosphere.
The exploration of Io, Jupiter's innermost Galilean and third-largest moon, began with its discovery in 1610 and continues today with Earth-based observations and visits by spacecraft to the Jupiter system. Italian astronomer Galileo Galilei was the first to record an observation of Io on January 8, 1610, though Simon Marius may have also observed Io at around the same time. During the 17th century, observations of Io and the other Galilean satellites helped with the measurement of longitude by map makers and surveyors, with validation of Kepler's Third Law of planetary motion, and with measurement of the speed of light. Based on ephemerides produced by astronomer Giovanni Cassini and others, Pierre-Simon Laplace created a mathematical theory to explain the resonant orbits of three of Jupiter's moons, Io, Europa, and Ganymede. This resonance was later found to have a profound effect on the geologies of these moons. Improved telescope technology in the late 19th and 20th centuries allowed astronomers to resolve large-scale surface features on Io as well as to estimate its diameter and mass.
1 2 3 4 Simon, J. L.; Bretagnon, P.; Chapront, J.; Chapront-Touzé, M.; Francou, G.; Laskar, J. (February 1994). "Numerical expressions for precession formulae and mean elements for the Moon and planets". Astronomy and Astrophysics. 282 (2): 663–683. Bibcode:1994A&A...282..663S.
↑ "HORIZONS Planet-center Batch call for January 2023 Perihelion". ssd.jpl.nasa.gov (Perihelion for Jupiter's planet-centre (599) occurs on 2023-Jan-21 at 4.9510113au during a rdot flip from negative to positive). NASA/JPL. Archived from the original on September 7, 2021. Retrieved September 7, 2021.
1 2 3 Sheppard, Scott S. "Moons of Jupiter". Earth & Planets Laboratory. Carnegie Institution for Science. Archived from the original on April 24, 2019. Retrieved December 20, 2022.
↑ de Pater, Imke; Lissauer, Jack J. (2015). Planetary Sciences (2nd updateded.). New York: Cambridge University Press. p.250. ISBN978-0-521-85371-2. Archived from the original on July 17, 2023. Retrieved August 17, 2016.
↑ "Astrodynamic Constants". JPL Solar System Dynamics. February 27, 2009. Archived from the original on March 21, 2019. Retrieved August 8, 2007.
↑ Jones, Alexander (1999). Astronomical papyri from Oxyrhynchus. American Philosophical Society. pp.62–63. ISBN978-0-87169-233-7. It is now possible to trace the medieval symbols for at least four of the five planets to forms that occur in some of the latest papyrus horoscopes ([ P.Oxy. ] 4272, 4274, 4275 [...]). That for Jupiter is an obvious monogram derived from the initial letter of the Greek name.
↑ Bagenal, Fran; Dowling, Timothy E.; McKinnon, William B., eds. (2006). Jupiter: The Planet, Satellites and Magnetosphere. Cambridge University Press. pp.59–75. ISBN0521035457.
↑ Kim, S. J.; Caldwell, J.; Rivolo, A. R.; Wagner, R. (1985). "Infrared Polar Brightening on Jupiter III. Spectrometry from the Voyager 1 IRIS Experiment". Icarus. 64 (2): 233–248. Bibcode:1985Icar...64..233K. doi:10.1016/0019-1035(85)90201-5.
↑ Vdovichenko, V. D.; Karimov, A. M.; Kirienko, G. A.; Lysenko, P. G.; Tejfel’, V. G.; Filippov, V. A.; Kharitonova, G. A.; Khozhenets, A. P. (2021). "Zonal Features in the Behavior of Weak Molecular Absorption Bands on Jupiter". Solar System Research. 55 (1): 35–46. Bibcode:2021SoSyR..55...35V. doi:10.1134/S003809462101010X. S2CID255069821.
↑ Ingersoll, A. P.; Hammel, H. B.; Spilker, T. R.; Young, R. E. (June 1, 2005). "Outer Planets: The Ice Giants"(PDF). Lunar & Planetary Institute. Archived(PDF) from the original on October 9, 2022. Retrieved February 1, 2007.
↑ MacDougal, Douglas W. (2012). "A Binary System Close to Home: How the Moon and Earth Orbit Each Other". Newton's Gravity. Undergraduate Lecture Notes in Physics. Springer New York. pp.193–211. doi:10.1007/978-1-4614-5444-1_10. ISBN978-1-4614-5443-4. the barycentre is 743,000km from the centre of the Sun. The Sun's radius is 696,000km, so it is 47,000km above the surface.
1 2 3 4 5 Burgess, Eric (1982). By Jupiter: Odysseys to a Giant. New York: Columbia University Press. ISBN978-0-231-05176-7.
↑ Davis, Andrew M.; Turekian, Karl K. (2005). Meteorites, comets, and planets. Treatise on geochemistry. Vol.1. Elsevier. p.624. ISBN978-0-08-044720-9.
↑ Burrows, Adam; Hubbard, W. B.; Lunine, J. I.; Liebert, James (July 2001). "The theory of brown dwarfs and extrasolar giant planets". Reviews of Modern Physics. 73 (3): 719–765. arXiv:astro-ph/0103383. Bibcode:2001RvMP...73..719B. doi:10.1103/RevModPhys.73.719. S2CID204927572. Hence the HBMM at solar metallicity and Yα = 50.25 is 0.07 – 0.074 M☉, ... while the HBMM at zero metallicity is 0.092 M☉
↑ von Boetticher, Alexander; Triaud, Amaury H. M. J.; Queloz, Didier; Gill, Sam; Lendl, Monika; Delrez, Laetitia; Anderson, David R.; Collier Cameron, Andrew; Faedi, Francesca; Gillon, Michaël; Gómez Maqueo Chew, Yilen; Hebb, Leslie; Hellier, Coel; Jehin, Emmanuël; Maxted, Pierre F. L.; Martin, David V.; Pepe, Francesco; Pollacco, Don; Ségransan, Damien; Smalley, Barry; Udry, Stéphane; West, Richard (August 2017). "The EBLM project. III. A Saturn-size low-mass star at the hydrogen-burning limit". Astronomy & Astrophysics. 604: 6. arXiv:1706.08781. Bibcode:2017A&A...604L...6V. doi:10.1051/0004-6361/201731107. S2CID54610182. L6.
1 2 Guillot, Tristan; Stevenson, David J.; Hubbard, William B.; Saumon, Didier (2004). "Chapter 3: The Interior of Jupiter". In Bagenal, Fran; Dowling, Timothy E.; McKinnon, William B. (eds.). Jupiter: The Planet, Satellites and Magnetosphere. Cambridge University Press. ISBN978-0-521-81808-7.
1 2 Guillot, Tristan; Stevenson, David J.; Hubbard, William B.; Saumon, Didier (2004). "The interior of Jupiter". In Bagenal, Fran; Dowling, Timothy E.; McKinnon, William B. (eds.). Jupiter. The planet, satellites and magnetosphere. Cambridge planetary science. Vol.1. Cambridge, UK: Cambridge University Press. p.45. Bibcode:2004jpsm.book...35G. ISBN0-521-81808-7. Archived from the original on March 26, 2023. Retrieved March 19, 2023.
↑ Atreya, Sushil K.; Mahaffy, P. R.; Niemann, H. B.; Wong, M. H.; Owen, T. C. (February 2003). "Composition and origin of the atmosphere of Jupiter—an update, and implications for the extrasolar giant planets". Planetary and Space Science. 51 (2): 105–112. Bibcode:2003P&SS...51..105A. doi:10.1016/S0032-0633(02)00144-7.
↑ Ingersoll, Andrew P.; Dowling, Timothy E.; Gierasch, Peter J.; Orton, Glenn S.; Read, Peter L.; Sánchez-Lavega, Agustin; Showman, Adam P.; Simon-Miller, Amy A.; Vasavada, Ashwin R. (2004). Bagenal, Fran; Dowling, Timothy E.; McKinnon, William B. (eds.). "Dynamics of Jupiter's Atmosphere"(PDF). Jupiter. The Planet, Satellites and Magnetosphere. Cambridge planetary science. 1. Cambridge, UK: Cambridge University Press: 105–128. ISBN0-521-81808-7. Archived(PDF) from the original on October 9, 2022. Retrieved March 8, 2022.
↑ Aglyamov, Yury S.; Lunine, Jonathan; Becker, Heidi N.; Guillot, Tristan; Gibbard, Seran G.; Atreya, Sushil; Bolton, Scott J.; Levin, Steven; Brown, Shannon T.; Wong, Michael H. (February 2021). "Lightning Generation in Moist Convective Clouds and Constraints on the Water Abundance in Jupiter". Journal of Geophysical Research: Planets. 126 (2). arXiv:2101.12361. Bibcode:2021JGRE..12606504A. doi:10.1029/2020JE006504. S2CID231728590. e06504.
↑ Strycker, P. D.; Chanover, N.; Sussman, M.; Simon-Miller, A. (2006). A Spectroscopic Search for Jupiter's Chromophores. DPS meeting No. 38, #11.15. American Astronomical Society. Bibcode:2006DPS....38.1115S.
↑ Cardall, C. Y.; Daunt, S. J. "The Great Red Spot". University of Tennessee. Archived from the original on March 31, 2010. Retrieved February 2, 2007.
↑ Simon, Amy A.; Wong, M. H.; Rogers, J. H.; Orton, G. S.; de Pater, I.; Asay-Davis, X.; Carlson, R. W.; Marcus, P. S. (March 2015). Dramatic Change in Jupiter's Great Red Spot. 46th Lunar and Planetary Science Conference. March 16–20, 2015. The Woodlands, Texas. Bibcode:2015LPI....46.1010S.
↑ Brainerd, Jim (November 22, 2004). "Jupiter's Magnetosphere". The Astrophysics Spectator. Archived from the original on January 25, 2021. Retrieved August 10, 2008.
↑ Phillips, Tony; Horack, John M. (February 20, 2004). "Radio Storms on Jupiter". NASA. Archived from the original on February 13, 2007. Retrieved February 1, 2007.
↑ Fieseler, P. D.; Adams, O. W.; Vandermey, N.; Theilig, E. E.; Schimmels, K. A.; Lewis, G. D.; Ardalan, S. M.; Alexander, C. J. (2004). "The Galileo Star Scanner Observations at Amalthea". Icarus. 169 (2): 390–401. Bibcode:2004Icar..169..390F. doi:10.1016/j.icarus.2004.01.012.
↑ Herbst, T. M.; Rix, H.-W. (1999). "Star Formation and Extrasolar Planet Studies with Near-Infrared Interferometry on the LBT". In Guenther, Eike; Stecklum, Bringfried; Klose, Sylvio (eds.). Optical and Infrared Spectroscopy of Circumstellar Matter. ASP Conference Series. Vol.188. San Francisco, Calif.: Astronomical Society of the Pacific. pp.341–350. Bibcode:1999ASPC..188..341H. ISBN978-1-58381-014-9. – See section 3.4.
↑ MacDougal, Douglas W. (December 16, 2012). Newton's Gravity: An Introductory Guide to the Mechanics of the Universe. Springer New York. p.199. ISBN978-1-4614-5444-1.
↑ Michtchenko, T. A.; Ferraz-Mello, S. (February 2001). "Modeling the 5:2 Mean-Motion Resonance in the Jupiter–Saturn Planetary System". Icarus. 149 (2): 77–115. Bibcode:2001Icar..149..357M. doi:10.1006/icar.2000.6539.
↑ Fimmel, Richard O.; Swindell, William; Burgess, Eric (1974). "8. Encounter with the Giant". Pioneer Odyssey (Reviseded.). NASA History Office. Archived from the original on December 25, 2017. Retrieved February 17, 2007.
↑ Chaple, Glenn F. (2009). Jones, Lauren V.; Slater, Timothy F. (eds.). Outer Planets. Greenwood Guides to the Universe. ABC-CLIO. p.47. ISBN978-0-313-36571-3. Archived from the original on March 26, 2023. Retrieved March 19, 2023.
↑ North, Chris; Abel, Paul (October 31, 2013). The Sky at Night: How to Read the Solar System. Ebury Publishing. p.183. ISBN978-1-4481-4130-2.
↑ Seargent, David A. J. (September 24, 2010). "Facts, Fallacies, Unusual Observations, and Other Miscellaneous Gleanings". Weird Astronomy: Tales of Unusual, Bizarre, and Other Hard to Explain Observations. Astronomers' Universe. pp.221–282. ISBN978-1-4419-6424-3.
↑ Xi, Z. Z. (1981). "The Discovery of Jupiter's Satellite Made by Gan-De 2000 Years Before Galileo". Acta Astrophysica Sinica. 1 (2): 87. Bibcode:1981AcApS...1...85X.
↑ Dong, Paul (2002). China's Major Mysteries: Paranormal Phenomena and the Unexplained in the People's Republic. China Books. ISBN978-0-8351-2676-2.
↑ Westfall, Richard S. "Galilei, Galileo". The Galileo Project. Rice University. Archived from the original on January 23, 2022. Retrieved January 10, 2007.
↑ O'Connor, J. J.; Robertson, E. F. (April 2003). "Giovanni Domenico Cassini". University of St. Andrews. Archived from the original on July 7, 2015. Retrieved February 14, 2007.
↑ Fimmel, Richard O.; Swindell, William; Burgess, Eric (August 1974). "Jupiter, Giant of the Solar System". Pioneer Odyssey (Reviseded.). NASA History Office. Archived from the original on August 23, 2006. Retrieved August 10, 2006.
↑ Brown, Kevin (2004). "Roemer's Hypothesis". MathPages. Archived from the original on September 6, 2012. Retrieved January 12, 2007.
↑ Tenn, Joe (March 10, 2006). "Edward Emerson Barnard". Sonoma State University. Archived from the original on September 17, 2011. Retrieved January 10, 2007.
↑ Fortescue, Peter W.; Stark, John; Swinerd, Graham (2003). Spacecraft systems engineering (3rded.). John Wiley and Sons. p.150. ISBN978-0-470-85102-9.
1 2 3 Chan, K.; Paredes, E. S.; Ryne, M. S. (2004). "Ulysses Attitude and Orbit Operations: 13+ Years of International Cooperation". Space OPS 2004 Conference. American Institute of Aeronautics and Astronautics. doi:10.2514/6.2004-650-447.
↑ Lasher, Lawrence (August 1, 2006). "Pioneer Project Home Page". NASA Space Projects Division. Archived from the original on January 1, 2006. Retrieved November 28, 2006.
↑ "Jupiter". NASA/JPL. January 14, 2003. Archived from the original on June 28, 2012. Retrieved November 28, 2006.
↑ Magalhães, Julio (December 10, 1996). "Galileo Probe Mission Events". NASA Space Projects Division. Archived from the original on January 2, 2007. Retrieved February 2, 2007.
↑ Ferraz-Mello, S. (1994). Milani, Andrea; Di Martino, Michel; Cellino, A. (eds.). Kirkwood Gaps and Resonant Groups. Asteroids, Comets, Meteors 1993: Proceedings of the 160th Symposium of the International Astronomical Union, held in Belgirate, Italy, June 14–18, 1993, International Astronomical Union. Symposium no. 160. Dordrecht: Kluwer Academic Publishers. p.175. Bibcode:1994IAUS..160..175F.
↑ Cruikshank, D. P.; Dalle Ore, C. M.; Geballe, T. R.; Roush, T. L.; Owen, T. C.; Cash, Michele; de Bergh, C.; Hartmann, W. K. (October 2000). "Trojan Asteroid 624 Hektor: Constraints on Surface Composition". Bulletin of the American Astronomical Society. 32: 1027. Bibcode:2000DPS....32.1901C.
1 2 Rogers, J. H. (1998). "Origins of the ancient constellations: I. The Mesopotamian traditions". Journal of the British Astronomical Association. 108: 9–28. Bibcode:1998JBAA..108....9R.
↑ Tarnas, R. (2009). "The planets". Archai: The Journal of Archetypal Cosmology. 1 (1): 36–49. CiteSeerX10.1.1.456.5030.
↑ Harper, Douglas (November 2001). "Jupiter". Online Etymology Dictionary. Archived from the original on September 28, 2008. Retrieved February 23, 2007.
Missions are ordered by launch date. Sign † indicates failure en route or before intended mission data returned. ‡ indicates use of the planet as a gravity assist en route to another destination.
This page is based on this Wikipedia article Text is available under the CC BY-SA 4.0 license; additional terms may apply. Images, videos and audio are available under their respective licenses.
