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Venus
Venus
is the second planet from the Sun, orbiting it every 224.7 Earth days.[12] It has the longest rotation period (243 days) of any planet in the Solar System
Solar System
and rotates in the opposite direction to most other planets (meaning the Sun
Sun
would rise in the west and set in the east).[13] It does not have any natural satellites. It is named after the Roman goddess of love and beauty. It is the second-brightest natural object in the night sky after the Moon, reaching an apparent magnitude of −4.6 – bright enough to cast shadows at night and, rarely, visible to the naked eye in broad daylight.[14][15] Orbiting within Earth's orbit, Venus
Venus
is an inferior planet and never appears to venture far from the Sun; its maximum angular distance from the Sun (elongation) is 47.8°. Venus
Venus
is a terrestrial planet and is sometimes called Earth's "sister planet" because of their similar size, mass, proximity to the Sun, and bulk composition. It is radically different from Earth
Earth
in other respects. It has the densest atmosphere of the four terrestrial planets, consisting of more than 96% carbon dioxide. The atmospheric pressure at the planet's surface is 92 times that of Earth, or roughly the pressure found 900 m (3,000 ft) underwater on Earth. Venus
Venus
is by far the hottest planet in the Solar System, with a mean surface temperature of 735 K (462 °C; 863 °F), even though Mercury is closer to the Sun. Venus
Venus
is shrouded by an opaque layer of highly reflective clouds of sulfuric acid, preventing its surface from being seen from space in visible light. It may have had water oceans in the past,[16][17] but these would have vaporized as the temperature rose due to a runaway greenhouse effect.[18] The water has probably photodissociated, and the free hydrogen has been swept into interplanetary space by the solar wind because of the lack of a planetary magnetic field.[19] Venus's surface is a dry desertscape interspersed with slab-like rocks and is periodically resurfaced by volcanism. As one of the brightest objects in the sky, Venus
Venus
has been a major fixture in human culture for as long as records have existed. It has been made sacred to gods of many cultures, and has been a prime inspiration for writers and poets as the morning star and evening star. Venus
Venus
was the first planet to have its motions plotted across the sky, as early as the second millennium BC.[20] As the closest planet to Earth, Venus
Venus
has been a prime target for early interplanetary exploration. It was the first planet beyond Earth visited by a spacecraft ( Mariner 2
Mariner 2
in 1962), and the first to be successfully landed on (by Venera 7
Venera 7
in 1970). Venus's thick clouds render observation of its surface impossible in visible light, and the first detailed maps did not emerge until the arrival of the Magellan orbiter in 1991. Plans have been proposed for rovers or more complex missions, but they are hindered by Venus's hostile surface conditions.

Contents

1 Physical characteristics

1.1 Geography 1.2 Surface geology 1.3 Internal structure 1.4 Atmosphere
Atmosphere
and climate 1.5 Magnetic field
Magnetic field
and core

2 Orbit and rotation 3 Observation

3.1 Phases 3.2 Transits 3.3 Pentagram of Venus 3.4 Daylight apparitions 3.5 Ashen light

4 Studies

4.1 Early studies 4.2 Ground-based research 4.3 Exploration

5 In culture

5.1 Symbol

6 Habitability 7 See also 8 Notes 9 References 10 External links

10.1 Cartographic resources

Physical characteristics

Size comparison with Earth

Venus
Venus
is one of the four terrestrial planets in the Solar System, meaning that it is a rocky body like Earth. It is similar to Earth
Earth
in size and mass, and is often described as Earth's "sister" or "twin".[21] The diameter of Venus
Venus
is 12,103.6 km (7,520.8 mi)—only 638.4 km (396.7 mi) less than Earth's—and its mass is 81.5% of Earth's. Conditions on the Venusian surface differ radically from those on Earth
Earth
because its dense atmosphere is 96.5% carbon dioxide, with most of the remaining 3.5% being nitrogen.[22] Geography Main article: Mapping of Venus The Venusian surface was a subject of speculation until some of its secrets were revealed by planetary science in the 20th century. Venera landers in 1975 and 1982 returned images of a surface covered in sediment and relatively angular rocks.[23] The surface was mapped in detail by Magellan in 1990–91. The ground shows evidence of extensive volcanism, and the sulfur in the atmosphere may indicate that there have been some recent eruptions.[24][25] About 80% of the Venusian surface is covered by smooth, volcanic plains, consisting of 70% plains with wrinkle ridges and 10% smooth or lobate plains.[26] Two highland "continents" make up the rest of its surface area, one lying in the planet's northern hemisphere and the other just south of the equator. The northern continent is called Ishtar Terra
Ishtar Terra
after Ishtar, the Babylonian goddess of love, and is about the size of Australia. Maxwell Montes, the highest mountain on Venus, lies on Ishtar
Ishtar
Terra. Its peak is 11 km (7 mi) above the Venusian average surface elevation.[27] The southern continent is called Aphrodite Terra, after the Greek goddess of love, and is the larger of the two highland regions at roughly the size of South America. A network of fractures and faults covers much of this area.[28] The absence of evidence of lava flow accompanying any of the visible calderas remains an enigma. The planet has few impact craters, demonstrating that the surface is relatively young, approximately 300–600 million years old.[29][30] Venus
Venus
has some unique surface features in addition to the impact craters, mountains, and valleys commonly found on rocky planets. Among these are flat-topped volcanic features called "farra", which look somewhat like pancakes and range in size from 20 to 50 km (12 to 31 mi) across, and from 100 to 1,000 m (330 to 3,280 ft) high; radial, star-like fracture systems called "novae"; features with both radial and concentric fractures resembling spider webs, known as "arachnoids"; and "coronae", circular rings of fractures sometimes surrounded by a depression. These features are volcanic in origin.[31] Most Venusian surface features are named after historical and mythological women.[32] Exceptions are Maxwell Montes, named after James Clerk Maxwell, and highland regions Alpha Regio, Beta Regio, and Ovda Regio. The latter three features were named before the current system was adopted by the International Astronomical Union, the body which oversees planetary nomenclature.[33] The longitudes of physical features on Venus
Venus
are expressed relative to its prime meridian. The original prime meridian passed through the radar-bright spot at the centre of the oval feature Eve, located south of Alpha Regio.[34] After the Venera
Venera
missions were completed, the prime meridian was redefined to pass through the central peak in the crater Ariadne.[35][36] Surface geology Main articles: Geology of Venus
Geology of Venus
and Volcanology of Venus

False-colour image of Maat Mons
Maat Mons
with a vertical exaggeration of 22.5

Much of the Venusian surface appears to have been shaped by volcanic activity. Venus
Venus
has several times as many volcanoes as Earth, and it has 167 large volcanoes that are over 100 km (62 mi) across. The only volcanic complex of this size on Earth
Earth
is the Big Island of Hawaii.[31]:154 This is not because Venus
Venus
is more volcanically active than Earth, but because its crust is older. Earth's oceanic crust is continually recycled by subduction at the boundaries of tectonic plates, and has an average age of about 100 million years,[37] whereas the Venusian surface is estimated to be 300–600 million years old.[29][31] Several lines of evidence point to ongoing volcanic activity on Venus. During the Soviet Venera
Venera
program, the Venera
Venera
9 orbiter obtained spectroscopic evidence of lightning on Venus,[38] and the Venera
Venera
12 descent probe obtained additional evidence of lightning and thunder.[39][40] The European Space Agency's Venus Express
Venus Express
in 2007 detected whistler waves further confirming the occurrence of lightning on Venus.[41][42] One possibility is that ash from a volcanic eruption was generating the lightning. Another piece of evidence comes from measurements of sulfur dioxide concentrations in the atmosphere, which dropped by a factor of 10 between 1978 and 1986, jumped in 2006, and again declined 10-fold.[43] This may mean that levels had been boosted several times by large volcanic eruptions.[44][45] In 2008 and 2009, the first direct evidence for ongoing volcanism was observed by Venus
Venus
Express, in the form of four transient localized infrared hot spots within the rift zone Ganis Chasma,[46][n 1] near the shield volcano Maat Mons. Three of the spots were observed in more than one successive orbit. These spots are thought to represent lava freshly released by volcanic eruptions.[47][48] The actual temperatures are not known, because the size of the hot spots could not be measured, but are likely to have been in the 800–1,100 K (527–827 °C; 980–1,520 °F) range, relative to a normal temperature of 740 K (467 °C; 872 °F).[49]

Impact craters on the surface of Venus
Venus
(false-colour image reconstructed from radar data)

Almost a thousand impact craters on Venus
Venus
are evenly distributed across its surface. On other cratered bodies, such as Earth
Earth
and the Moon, craters show a range of states of degradation. On the Moon, degradation is caused by subsequent impacts, whereas on Earth
Earth
it is caused by wind and rain erosion. On Venus, about 85% of the craters are in pristine condition. The number of craters, together with their well-preserved condition, indicates the planet underwent a global resurfacing event about 300–600 million years ago,[29][30] followed by a decay in volcanism.[50] Whereas Earth's crust is in continuous motion, Venus
Venus
is thought to be unable to sustain such a process. Without plate tectonics to dissipate heat from its mantle, Venus instead undergoes a cyclical process in which mantle temperatures rise until they reach a critical level that weakens the crust. Then, over a period of about 100 million years, subduction occurs on an enormous scale, completely recycling the crust.[31] Venusian craters range from 3 to 280 km (2 to 174 mi) in diameter. No craters are smaller than 3 km, because of the effects of the dense atmosphere on incoming objects. Objects with less than a certain kinetic energy are slowed down so much by the atmosphere that they do not create an impact crater.[51] Incoming projectiles less than 50 m (160 ft) in diameter will fragment and burn up in the atmosphere before reaching the ground.[52] Internal structure

The internal structure of Venus
Venus
– the crust (outer layer), the mantle (middle layer) and the core (yellow inner layer)

Without seismic data or knowledge of its moment of inertia, little direct information is available about the internal structure and geochemistry of Venus.[53] The similarity in size and density between Venus
Venus
and Earth
Earth
suggests they share a similar internal structure: a core, mantle, and crust. Like that of Earth, the Venusian core is at least partially liquid because the two planets have been cooling at about the same rate.[54] The slightly smaller size of Venus
Venus
means pressures are 24% lower in its deep interior than Earth's.[55] The principal difference between the two planets is the lack of evidence for plate tectonics on Venus, possibly because its crust is too strong to subduct without water to make it less viscous. This results in reduced heat loss from the planet, preventing it from cooling and providing a likely explanation for its lack of an internally generated magnetic field.[56] Instead, Venus
Venus
may lose its internal heat in periodic major resurfacing events.[29] Atmosphere
Atmosphere
and climate

Cloud structure in the Venusian atmosphere in 1979, revealed by observations in the ultraviolet band by Pioneer Venus
Venus
Orbiter

Global radar view of Venus
Venus
(without the clouds) from Magellan between 1990 and 1994

Main article: Atmosphere
Atmosphere
of Venus Venus
Venus
has an extremely dense atmosphere composed of 96.5% carbon dioxide, 3.5% nitrogen, and traces of other gases, most notably sulfur dioxide.[57] The mass of its atmosphere is 93 times that of Earth's, whereas the pressure at its surface is about 92 times that at Earth's—a pressure equivalent to that at a depth of nearly 1 kilometre (0.62 mi) under Earth's oceans. The density at the surface is 65 kg/m3, 6.5% that of water or 50 times as dense as Earth's atmosphere at 293 K (20 °C; 68 °F) at sea level. The CO 2-rich atmosphere generates the strongest greenhouse effect in the Solar System, creating surface temperatures of at least 735 K (462 °C; 864 °F).[12][58] This makes Venus's surface hotter than Mercury's, which has a minimum surface temperature of 53 K (−220 °C; −364 °F) and maximum surface temperature of 693 K (420 °C; 788 °F),[59] even though Venus
Venus
is nearly twice Mercury's distance from the Sun
Sun
and thus receives only 25% of Mercury's solar irradiance. This temperature is higher than that used for sterilization. The surface of Venus
Venus
is often said to resemble traditional accounts of Hell.[60][61] Studies have suggested that billions of years ago Venus's atmosphere was much more like Earth's than it is now, and that there may have been substantial quantities of liquid water on the surface, but after a period of 600 million to several billion years,[62] a runaway greenhouse effect was caused by the evaporation of that original water, which generated a critical level of greenhouse gases in its atmosphere.[63] Although the surface conditions on Venus
Venus
are no longer hospitable to any Earthlike life that may have formed before this event, there is speculation on the possibility that life exists in the upper cloud layers of Venus, 50 km (31 mi) up from the surface, where the temperature ranges between 303 and 353 K (30 and 80 °C; 86 and 176 °F) but the environment is acidic.[64][65][66] Thermal inertia and the transfer of heat by winds in the lower atmosphere mean that the temperature of Venus's surface does not vary significantly between the night and day sides, despite Venus's extremely slow rotation. Winds at the surface are slow, moving at a few kilometres per hour, but because of the high density of the atmosphere at the surface, they exert a significant amount of force against obstructions, and transport dust and small stones across the surface. This alone would make it difficult for a human to walk through, even if the heat, pressure, and lack of oxygen were not a problem.[67] Above the dense CO 2 layer are thick clouds consisting mainly of sulfuric acid, which is formed by sulfur dioxide and water through a chemical reaction resulting in sulfuric acid hydrate. Additionally, the atmosphere consists of approximately 1% ferric chloride.[68][69] Other possible constituents of the cloud particles are ferric sulfate, aluminium chloride and phosphoric anhydride. Clouds at different levels have different compositions and particle size distributions.[68] These clouds reflect and scatter about 90% of the sunlight that falls on them back into space, and prevent visual observation of Venus's surface. The permanent cloud cover means that although Venus
Venus
is closer than Earth
Earth
to the Sun, it receives less sunlight on the ground. Strong 300 km/h (185 mph) winds at the cloud tops go around Venus about every four to five Earth
Earth
days.[70] Winds on Venus
Venus
move at up to 60 times the speed of its rotation, whereas Earth's fastest winds are only 10–20% rotation speed.[71] The surface of Venus
Venus
is effectively isothermal; it retains a constant temperature not only between day and night sides but between the equator and the poles.[2][72] Venus's minute axial tilt—less than 3°, compared to 23° on Earth—also minimises seasonal temperature variation.[73] The only appreciable variation in temperature occurs with altitude. The highest point on Venus, Maxwell Montes, is therefore the coolest point on Venus, with a temperature of about 655 K (380 °C; 715 °F) and an atmospheric pressure of about 4.5 MPa (45 bar).[74][75] In 1995, the Magellan spacecraft imaged a highly reflective substance at the tops of the highest mountain peaks that bore a strong resemblance to terrestrial snow. This substance likely formed from a similar process to snow, albeit at a far higher temperature. Too volatile to condense on the surface, it rose in gaseous form to higher elevations, where it is cooler and could precipitate. The identity of this substance is not known with certainty, but speculation has ranged from elemental tellurium to lead sulfide (galena).[76] The clouds of Venus
Venus
may be capable of producing lightning.[77] The existence of lightning in the atmosphere of Venus
Venus
has been controversial since the first suspected bursts were detected by the Soviet Venera
Venera
probes. In 2006–07, Venus Express
Venus Express
clearly detected whistler mode waves, the signatures of lightning. Their intermittent appearance indicates a pattern associated with weather activity. According to these measurements, the lightning rate is at least half of that on Earth.[41] In 2007, Venus Express
Venus Express
discovered that a huge double atmospheric vortex exists at the south pole.[78][79] Venus Express
Venus Express
also discovered, in 2011, that an ozone layer exists high in the atmosphere of Venus.[80] On 29 January 2013, ESA scientists reported that the ionosphere of Venus
Venus
streams outwards in a manner similar to "the ion tail seen streaming from a comet under similar conditions."[81][82] In December 2015 and to a lesser extent in April and May 2016, researchers working on Japan's Akatsuki mission observed bow shapes in the atmosphere of Venus. This was considered direct evidence of the existence of perhaps the largest stationary gravity waves in the solar system.[83][84][85]

Atmospheric composition

Absorption spectrum of a simple gas mixture corresponding to Earth's atmosphere

The composition of the atmosphere of Venus
Venus
based on HITRAN data[86] created using HITRAN on the Web system.[87]

Green colour – water vapour, red – carbon dioxide, WN – wavenumber (other colours have different meanings, lower wavelengths on the right, higher on the left).

Magnetic field
Magnetic field
and core In 1967, Venera
Venera
4 found Venus's magnetic field to be much weaker than that of Earth. This magnetic field is induced by an interaction between the ionosphere and the solar wind,[88][89] rather than by an internal dynamo as in the Earth's core. Venus's small induced magnetosphere provides negligible protection to the atmosphere against cosmic radiation. The lack of an intrinsic magnetic field at Venus
Venus
was surprising, given that it is similar to Earth
Earth
in size, and was expected also to contain a dynamo at its core. A dynamo requires three things: a conducting liquid, rotation, and convection. The core is thought to be electrically conductive and, although its rotation is often thought to be too slow, simulations show it is adequate to produce a dynamo.[90][91] This implies that the dynamo is missing because of a lack of convection in Venus's core. On Earth, convection occurs in the liquid outer layer of the core because the bottom of the liquid layer is much hotter than the top. On Venus, a global resurfacing event may have shut down plate tectonics and led to a reduced heat flux through the crust. This caused the mantle temperature to increase, thereby reducing the heat flux out of the core. As a result, no internal geodynamo is available to drive a magnetic field. Instead, the heat from the core is being used to reheat the crust.[92] One possibility is that Venus
Venus
has no solid inner core,[93] or that its core is not cooling, so that the entire liquid part of the core is at approximately the same temperature. Another possibility is that its core has already completely solidified. The state of the core is highly dependent on the concentration of sulfur, which is unknown at present.[92] The weak magnetosphere around Venus
Venus
means that the solar wind is interacting directly with its outer atmosphere. Here, ions of hydrogen and oxygen are being created by the dissociation of neutral molecules from ultraviolet radiation. The solar wind then supplies energy that gives some of these ions sufficient velocity to escape Venus's gravity field. This erosion process results in a steady loss of low-mass hydrogen, helium, and oxygen ions, whereas higher-mass molecules, such as carbon dioxide, are more likely to be retained. Atmospheric erosion by the solar wind probably led to the loss of most of Venus's water during the first billion years after it formed.[94] The erosion has increased the ratio of higher-mass deuterium to lower-mass hydrogen in the atmosphere 100 times compared to the rest of the solar system.[95] Orbit and rotation Main article: Orbit of Venus

Venus
Venus
orbits the Sun
Sun
at an average distance of about 108 million kilometres (about 0.7 AU) and completes an orbit every 224.7 days. Venus
Venus
is the second planet from the Sun and orbits the Sun
Sun
approximately 1.6 times (yellow trail) in Earth's 365 days (blue trail)

Venus
Venus
orbits the Sun
Sun
at an average distance of about 0.72 AU (108 million km; 67 million mi), and completes an orbit every 224.7 days. Although all planetary orbits are elliptical, Venus's orbit is the closest to circular, with an eccentricity of less than 0.01.[2] When Venus
Venus
lies between Earth
Earth
and the Sun
Sun
in inferior conjunction, it makes the closest approach to Earth
Earth
of any planet at an average distance of 41 million km (25 million mi).[2] The planet reaches inferior conjunction every 584 days, on average.[2] Because of the decreasing eccentricity of Earth's orbit, the minimum distances will become greater over tens of thousands of years. From the year 1 to 5383, there are 526 approaches less than 40 million km; then there are none for about 60,158 years.[96] All the planets in the Solar System
Solar System
orbit the Sun
Sun
in a counterclockwise direction as viewed from above Earth's north pole. Most planets also rotate on their axes in an anti-clockwise direction, but Venus
Venus
rotates clockwise in retrograde rotation once every 243 Earth days—the slowest rotation of any planet. Because its rotation is so slow, Venus
Venus
is very close to spherical.[97] A Venusian sidereal day thus lasts longer than a Venusian year (243 versus 224.7 Earth
Earth
days). Venus's equator rotates at 6.52 km/h (4.05 mph), whereas Earth's rotates at 1,669.8 km/h (1,037.6 mph).[98] Venus's rotation has slowed down in the 16 years between the Magellan spacecraft and Venus
Venus
Express visits; each Venusian sidereal day has increased by 6.5 minutes in that time span.[99] Because of the retrograde rotation, the length of a solar day on Venus
Venus
is significantly shorter than the sidereal day, at 116.75 Earth days (making the Venusian solar day shorter than Mercury's 176 Earth days).[100] One Venusian year is about 1.92 Venusian solar days.[101] To an observer on the surface of Venus, the Sun
Sun
would rise in the west and set in the east,[101] although Venus's opaque clouds prevent observing the Sun from the planet's surface.[102] Venus
Venus
may have formed from the solar nebula with a different rotation period and obliquity, reaching its current state because of chaotic spin changes caused by planetary perturbations and tidal effects on its dense atmosphere, a change that would have occurred over the course of billions of years. The rotation period of Venus
Venus
may represent an equilibrium state between tidal locking to the Sun's gravitation, which tends to slow rotation, and an atmospheric tide created by solar heating of the thick Venusian atmosphere.[103][104] The 584-day average interval between successive close approaches to Earth
Earth
is almost exactly equal to 5 Venusian solar days,[105] but the hypothesis of a spin–orbit resonance with Earth
Earth
has been discounted.[106] Venus
Venus
has no natural satellites.[107] It has several trojan asteroids: the quasi-satellite 2002 VE68[108][109] and two other temporary trojans, 2001 CK32 and 2012 XE133.[110] In the 17th century, Giovanni Cassini
Giovanni Cassini
reported a moon orbiting Venus, which was named Neith and numerous sightings were reported over the following 7009631152000000000♠200 years, but most were determined to be stars in the vicinity. Alex Alemi's and David Stevenson's 2006 study of models of the early Solar System
Solar System
at the California Institute of Technology shows Venus
Venus
likely had at least one moon created by a huge impact event billions of years ago.[111] About 10 million years later, according to the study, another impact reversed the planet's spin direction and caused the Venusian moon gradually to spiral inward until it collided with Venus.[112] If later impacts created moons, these were removed in the same way. An alternative explanation for the lack of satellites is the effect of strong solar tides, which can destabilize large satellites orbiting the inner terrestrial planets.[107] Observation

Venus
Venus
is always brighter than all other planets or stars as seen from Earth. The second brightest object on the image is Jupiter.

To the naked eye, Venus
Venus
appears as a white point of light brighter than any other planet or star (apart from the Sun).[113] Its brightest apparent magnitude, −4.9,[10] occurs during crescent phase, only 36 days before or after inferior conjunction.[114] Venus
Venus
was brightest on 30 April 2017, then grew dimmer for nearly a year. Venus
Venus
fades to about magnitude −3 when it is backlit by the Sun.[9] The planet is bright enough to be seen in a clear midday sky[115] and is more easily visible when the Sun
Sun
is low on the horizon or setting. As an inferior planet, it always lies within about 47° of the Sun.[11] Venus
Venus
"overtakes" Earth
Earth
every 584 days as it orbits the Sun.[2] As it does so, it changes from the "Evening Star", visible after sunset, to the "Morning Star", visible before sunrise. Although Mercury, the other inferior planet, reaches a maximum elongation of only 28° and is often difficult to discern in twilight, Venus
Venus
is hard to miss when it is at its brightest. Its greater maximum elongation means it is visible in dark skies long after sunset. As the brightest point-like object in the sky, Venus
Venus
is a commonly misreported "unidentified flying object". Phases Main article: Phases of Venus

The phases of Venus
Venus
and evolution of its apparent diameter

As it orbits the Sun, Venus
Venus
displays phases like those of the Moon
Moon
in a telescopic view. The planet appears as a small and "full" disc when it is on the opposite side of the Sun
Sun
(at superior conjunction). Venus shows a larger disc and "quarter phase" at its maximum elongations from the Sun, and appears its brightest in the night sky. The planet presents a much larger thin "crescent" in telescopic views as it passes along the near side between Earth
Earth
and the Sun. Venus
Venus
displays its largest size and "new phase" when it is between Earth
Earth
and the Sun (at inferior conjunction). Its atmosphere is visible through telescopes by the halo of sunlight refracted around it.[11] Transits Main articles: Transit of Venus
Transit of Venus
and Transit of Venus, 2012

2004 transit of Venus

The Venusian orbit is slightly inclined relative to Earth's orbit; thus, when the planet passes between Earth
Earth
and the Sun, it usually does not cross the face of the Sun. Transits of Venus
Transits of Venus
occur when the planet's inferior conjunction coincides with its presence in the plane of Earth's orbit. Transits of Venus
Transits of Venus
occur in cycles of 7009766849680000000♠243 years with the current pattern of transits being pairs of transits separated by eight years, at intervals of about 7009332932680000000♠105.5 years or 7009383424840000000♠121.5 years—a pattern first discovered in 1639 by the English astronomer Jeremiah Horrocks.[116] The latest pair was June 8, 2004 and June 5–6, 2012. The transit could be watched live from many online outlets or observed locally with the right equipment and conditions.[117] The preceding pair of transits occurred in December 1874 and December 1882; the following pair will occur in December 2117 and December 2125.[118] The oldest film known is the 1874 Passage de Venus, showing the 1874 Venus
Venus
transit of the sun. Historically, transits of Venus were important, because they allowed astronomers to determine the size of the astronomical unit, and hence the size of the Solar System
Solar System
as shown by Horrocks in 1639.[119] Captain Cook's exploration of the east coast of Australia came after he had sailed to Tahiti
Tahiti
in 1768 to observe a transit of Venus.[120][121] Pentagram of Venus

The pentagram of Venus. Earth
Earth
is positioned at the centre of the diagram, and the curve represents the direction and distance of Venus as a function of time.

The pentagram of Venus
Venus
is the path that Venus
Venus
makes as observed from Earth. Successive inferior conjunctions of Venus
Venus
repeat very near a 13:8 orbital resonance ( Earth
Earth
orbits 8 times for every 13 orbits of Venus), shifting 144° upon sequential inferior conjunctions. The resonance 13:8 ratio is approximate. 8/13 is approximately 0.615385 while Venus
Venus
orbits the Sun
Sun
in 0.615187 years.[122] Daylight apparitions Naked eye
Naked eye
observations of Venus
Venus
during daylight hours exist in several anecdotes and records. Astronomer Edmund Halley
Edmund Halley
calculated its maximum naked eye brightness in 1716, when many Londoners were alarmed by its appearance in the daytime. French emperor Napoleon Bonaparte
Napoleon Bonaparte
once witnessed a daytime apparition of the planet while at a reception in Luxembourg.[123] Another historical daytime observation of the planet took place during the inauguration of the American president Abraham Lincoln in Washington, D.C., on 4 March 1865.[124] Although naked eye visibility of Venus's phases is disputed, records exist of observations of its crescent.[125] Ashen light A long-standing mystery of Venus
Venus
observations is the so-called ashen light—an apparent weak illumination of its dark side, seen when the planet is in the crescent phase. The first claimed observation of ashen light was made in 1643, but the existence of the illumination has never been reliably confirmed. Observers have speculated it may result from electrical activity in the Venusian atmosphere, but it could be illusory, resulting from the physiological effect of observing a bright, crescent-shaped object.[126][39] Studies Early studies

The "black drop effect" as recorded during the 1769 transit

Venus
Venus
was known to ancient civilizations both as the "morning star" and as the "evening star", names that reflect the early assumption that these were two separate objects. The ancient Sumerians, who recognized Venus
Venus
as a single object,[127] believed that it was their goddess Inanna.[127][128][129] Inanna's movements in several of her myths, including Inanna
Inanna
and Shukaletuda and Inanna's Descent into the Underworld appear to parallel the motion of the planet Venus.[127] The Venus
Venus
tablet of Ammisaduqa, believed to have been compiled around the mid-seventeenth century BCE,[130] shows the Babylonians understood the two were a single object, referred to in the tablet as the "bright queen of the sky", and could support this view with detailed observations.[131] The ancient Greeks thought that Venus
Venus
was two separate stars: Phosphorus and Hesperus. Pliny the Elder
Pliny the Elder
credited the realization that they were a single object to Pythagoras
Pythagoras
in the sixth century BCE,[132] while Diogenes Laertius
Diogenes Laertius
argued that Parmenides
Parmenides
was probably responsible.[133] The ancient Chinese referred to the morning Venus
Venus
as "the Great White" (Tai-bai 太白) or "the Opener (Starter) of Brightness" (Qi-ming 啟明), and the evening Venus
Venus
as "the Excellent West One" (Chang-geng 長庚). The Romans designated the morning aspect of Venus
Venus
as Lucifer, literally "Light-Bringer", and the evening aspect as Vesper, both literal translations of the respective Greek names. In the second century, in his astronomical treatise Almagest, Ptolemy theorized that both Mercury and Venus
Venus
are located between the Sun
Sun
and the Earth. The 11th century Persian astronomer Avicenna
Avicenna
claimed to have observed the transit of Venus,[134] which later astronomers took as confirmation of Ptolemy's theory.[135] In the 12th century, the Andalusian astronomer Ibn Bajjah observed "two planets as black spots on the face of the Sun", which were later identified as the transits of Venus
Venus
and Mercury by the Maragha astronomer Qotb al-Din Shirazi
Qotb al-Din Shirazi
in the 13th century.[136][n 2]

Galileo's discovery that Venus
Venus
showed phases (although remaining near the Sun
Sun
in Earth's sky) proved that it orbits the Sun
Sun
and not Earth

When the Italian physicist Galileo
Galileo
Galilei first observed the planet in the early 17th century, he found it showed phases like the Moon, varying from crescent to gibbous to full and vice versa. When Venus
Venus
is furthest from the Sun
Sun
in the sky, it shows a half-lit phase, and when it is closest to the Sun
Sun
in the sky, it shows as a crescent or full phase. This could be possible only if Venus
Venus
orbited the Sun, and this was among the first observations to clearly contradict the Ptolemaic geocentric model that the Solar System
Solar System
was concentric and centred on Earth.[139][140] The 1639 transit of Venus
Venus
was accurately predicted by Jeremiah Horrocks and observed by him and his friend, William Crabtree, at each of their respective homes, on 4 December 1639 (24 November under the Julian calendar
Julian calendar
in use at that time).[141] The atmosphere of Venus
Venus
was discovered in 1761 by Russian polymath Mikhail Lomonosov.[142][143] Venus's atmosphere was observed in 1790 by German astronomer Johann Schröter. Schröter found when the planet was a thin crescent, the cusps extended through more than 180°. He correctly surmised this was due to scattering of sunlight in a dense atmosphere. Later, American astronomer Chester Smith Lyman
Chester Smith Lyman
observed a complete ring around the dark side of the planet when it was at inferior conjunction, providing further evidence for an atmosphere.[144] The atmosphere complicated efforts to determine a rotation period for the planet, and observers such as Italian-born astronomer Giovanni Cassini
Giovanni Cassini
and Schröter incorrectly estimated periods of about 7004864000000000000♠24 h from the motions of markings on the planet's apparent surface.[145] Ground-based research

Modern telescopic view of Venus
Venus
from Earth's surface

Little more was discovered about Venus
Venus
until the 20th century. Its almost featureless disc gave no hint what its surface might be like, and it was only with the development of spectroscopic, radar and ultraviolet observations that more of its secrets were revealed. The first ultraviolet observations were carried out in the 1920s, when Frank E. Ross found that ultraviolet photographs revealed considerable detail that was absent in visible and infrared radiation. He suggested this was due to a dense, yellow lower atmosphere with high cirrus clouds above it.[146] Spectroscopic observations in the 1900s gave the first clues about the Venusian rotation. Vesto Slipher
Vesto Slipher
tried to measure the Doppler shift
Doppler shift
of light from Venus, but found he could not detect any rotation. He surmised the planet must have a much longer rotation period than had previously been thought.[147] Later work in the 1950s showed the rotation was retrograde. Radar
Radar
observations of Venus
Venus
were first carried out in the 1960s, and provided the first measurements of the rotation period, which were close to the modern value.[148] Radar
Radar
observations in the 1970s revealed details of the Venusian surface for the first time. Pulses of radio waves were beamed at the planet using the 300 m (980 ft) radio telescope at Arecibo Observatory, and the echoes revealed two highly reflective regions, designated the Alpha and Beta regions. The observations also revealed a bright region attributed to mountains, which was called Maxwell Montes.[149] These three features are now the only ones on Venus
Venus
that do not have female names.[33] Exploration Main article: Observations and explorations of Venus

Artist's impression of Mariner 2, launched in 1962, a skeletal, bottle-shaped spacecraft with a large radio dish on top

The first robotic space probe mission to Venus, and the first to any planet, began with the Soviet Venera
Venera
program in 1961.[150] The United States' exploration of Venus
Venus
had its first success with the Mariner 2 mission on 14 December 1962, becoming the world's first successful interplanetary mission, passing 34,833 km (21,644 mi) above the surface of Venus, and gathering data on the planet's atmosphere.[151][152]

180-degree panorama of Venus's surface from the Soviet Venera 9 lander, 1975. Black-and-white image of barren, black, slate-like rocks against a flat sky. The ground and the probe are the focus. Several lines are missing due to a simultaneous transmission of the scientific data

On 18 October 1967, the Soviet Venera
Venera
4 successfully entered the atmosphere and deployed science experiments. Venera
Venera
4 showed the surface temperature was hotter than Mariner 2
Mariner 2
had calculated, at almost 500 °C, determined that the atmosphere is 95% carbon dioxide (CO 2), and discovered that Venus's atmosphere was considerably denser than Venera
Venera
4's designers had anticipated.[153] The joint Venera 4– Mariner 5
Mariner 5
data were analysed by a combined Soviet–American science team in a series of colloquia over the following year,[154] in an early example of space cooperation.[155] In 1974, Mariner 10
Mariner 10
swung by Venus
Venus
on its way to Mercury and took ultraviolet photographs of the clouds, revealing the extraordinarily high wind speeds in the Venusian atmosphere.

Global view of Venus
Venus
in ultraviolet light done by Mariner 10.

In 1975, the Soviet Venera
Venera
9 and 10 landers transmitted the first images from the surface of Venus, which were in black and white. In 1982 the first colour images of the surface were obtained with the Soviet Venera
Venera
13 and 14 landers. NASA
NASA
obtained additional data in 1978 with the Pioneer Venus
Venus
project that consisted of two separate missions:[156] Pioneer Venus
Venus
Orbiter and Pioneer Venus
Venus
Multiprobe.[157] The successful Soviet Venera program came to a close in October 1983, when Venera
Venera
15 and 16 were placed in orbit to conduct detailed mapping of 25% of Venus's terrain (from the north pole to 30°N latitude)[158] Several other Venus
Venus
flybys took place in the 1980s and 1990s that increased the understanding of Venus, including Vega 1
Vega 1
(1985), Vega 2 (1985), Galileo
Galileo
(1990), Magellan (1994), Cassini–Huygens
Cassini–Huygens
(1998), and MESSENGER (2006). Then, Venus Express
Venus Express
by the European Space Agency (ESA) entered orbit around Venus
Venus
in April 2006. Equipped with seven scientific instruments, Venus Express
Venus Express
provided unprecedented long-term observation of Venus's atmosphere. ESA
ESA
concluded that mission in December 2014. As of 2016, Japan's Akatsuki is in a highly elliptical orbit around Venus
Venus
since 7 December 2015, and there are several probing proposals under study by Roscosmos, NASA, and India's ISRO. In 2016, NASA
NASA
announced that it was planning a rover, the Automaton Rover for Extreme Environments, designed to survive for an extended time in Venus's environmental conditions. It would be controlled by a mechanical computer and driven by wind power.[159] In culture See also: Venus in fiction
Venus in fiction
and Observations and explorations of Venus § Historical observations and impact Venus
Venus
is a primary feature of the night sky, and so has been of remarkable importance in mythology, astrology and fiction throughout history and in different cultures. Classical poets such as Homer, Sappho, Ovid
Ovid
and Virgil
Virgil
spoke of the star and its light.[160] Romantic poets such as William Blake, Robert Frost, Alfred Lord Tennyson
Alfred Lord Tennyson
and William Wordsworth
William Wordsworth
wrote odes to it.[161] With the invention of the telescope, the idea that Venus
Venus
was a physical world and possible destination began to take form. The impenetrable Venusian cloud cover gave science fiction writers free rein to speculate on conditions at its surface; all the more so when early observations showed that not only was it similar in size to Earth, it possessed a substantial atmosphere. Closer to the Sun
Sun
than Earth, the planet was frequently depicted as warmer, but still habitable by humans.[162] The genre reached its peak between the 1930s and 1950s, at a time when science had revealed some aspects of Venus, but not yet the harsh reality of its surface conditions. Findings from the first missions to Venus
Venus
showed the reality to be quite different, and brought this particular genre to an end.[163] As scientific knowledge of Venus
Venus
advanced, so science fiction authors tried to keep pace, particularly by conjecturing human attempts to terraform Venus.[164] Symbol Main article: Venus
Venus
symbol The astronomical symbol for Venus
Venus
is the same as that used in biology for the female sex: a circle with a small cross beneath.[165] The Venus symbol
Venus symbol
also represents femininity, and in Western alchemy stood for the metal copper.[165] Polished copper has been used for mirrors from antiquity, and the symbol for Venus
Venus
has sometimes been understood to stand for the mirror of the goddess.[165] Habitability Main article: Life
Life
on Venus See also: Colonization of Venus The speculation of the existence of life on Venus
Venus
decreased significantly since the early 1960s, when spacecraft began studying Venus
Venus
and it became clear that the conditions on Venus
Venus
are extreme compared to those on Earth. The fact that Venus
Venus
is located closer to the Sun
Sun
than Earth, raising temperatures on the surface to nearly 735 K (462 °C; 863 °F), the atmospheric pressure is ninety times that of Earth, and the extreme impact of the greenhouse effect, make water-based life as we know it unlikely. A few scientists have speculated that thermoacidophilic extremophile microorganisms might exist in the lower-temperature, acidic upper layers of the Venusian atmosphere.[166][167][168] The atmospheric pressure and temperature fifty kilometres above the surface are similar to those at Earth's surface. This has led to proposals to use aerostats (lighter-than-air balloons) for initial exploration and ultimately for permanent "floating cities" in the Venusian atmosphere.[169] Among the many engineering challenges are the dangerous amounts of sulfuric acid at these heights.[169] See also

Solar System
Solar System
portal

Book: Venus Book: Solar System

Aspects of Venus Geodynamics of Venus Outline of Venus Venus
Venus
zone

Notes

^ Misstated as "Ganiki Chasma" in the press release and scientific publication.[47] ^ Several claims of transit observations made by medieval Islamic astronomers have been shown to be sunspots.[137] Avicenna
Avicenna
did not record the date of his observation. There was a transit of Venus within his lifetime, on 24 May 1032, although it is questionable whether it would have been visible from his location.[138]

References

^ a b 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
Moon
and planets". Astronomy
Astronomy
and Astrophysics. 282 (2): 663–683. Bibcode:1994A&A...282..663S.  ^ a b c d e f g h i j k l m n Williams, David R. (15 April 2005). " Venus
Venus
Fact Sheet". NASA. Retrieved 12 October 2007.  ^ "The MeanPlane (Invariable plane) of the Solar System
Solar System
passing through the barycenter". 3 April 2009. Archived from the original on 17 April 2012. Retrieved 10 April 2009.  (produced with Solex 10 (Archived 29 April 2009 at WebCite) written by Aldo Vitagliano; see also Invariable plane) ^ Yeomans, Donald K. "HORIZONS Web-Interface for Venus
Venus
(Major Body=2)". JPL Horizons On-Line Ephemeris System. —Select "Ephemeris Type: Orbital Elements", "Time Span: 2000-01-01 12:00 to 2000-01-02". ("Target Body: Venus" and "Center: Sun" should be defaulted to.) Results are instantaneous osculating values at the precise J2000 epoch. ^ a b Seidelmann, P. Kenneth; Archinal, Brent A.; A'Hearn, Michael F.; et al. (2007). "Report of the IAU/IAG Working Group on cartographic coordinates and rotational elements: 2006". Celestial Mechanics and Dynamical Astronomy. 98 (3): 155–180. Bibcode:2007CeMDA..98..155S. doi:10.1007/s10569-007-9072-y.  ^ Konopliv, A. S.; Banerdt, W. B.; Sjogren, W. L. (May 1999). "Venus Gravity: 180th Degree and Order Model" (PDF). Icarus. 139 (1): 3–18. Bibcode:1999Icar..139....3K. doi:10.1006/icar.1999.6086. Archived from the original (PDF) on 26 May 2010.  ^ "Planets and Pluto: Physical Characteristics". NASA. 5 November 2008. Retrieved 26 August 2015.  ^ "Report on the IAU/IAG Working Group on cartographic coordinates and rotational elements of the planets and satellites". International Astronomical Union. 2000. Retrieved 12 April 2007.  ^ a b Mallama, A. (2011). "Planetary magnitudes". Sky & Telescope. 121 (1): 51–56.  ^ a b "HORIZONS Web-Interface for Venus
Venus
(Major Body=299)". JPL Horizons On-Line Ephemeris System (Geophysical data). 27 February 2006. Retrieved 28 November 2010.  (Using JPL Horizons you can see that on 2013-Dec-08 Venus
Venus
will have an apmag of −4.89) ^ a b c Espenak, Fred (1996). "Venus: Twelve year planetary ephemeris, 1995–2006". NASA
NASA
Reference Publication 1349. NASA/Goddard Space Flight Center. Archived from the original on 17 August 2000. Retrieved 20 June 2006.  ^ a b "Venus: Facts & Figures". NASA. Archived from the original on 29 September 2006. Retrieved 12 April 2007.  ^ Castro, Joseph (3 February 2015). "What Would It Be Like to Live on Venus?". Space.com. Retrieved 15 March 2018.  ^ Lawrence, Pete (2005). "In Search of the Venusian Shadow". Digitalsky.org.uk. Archived from the original on 11 June 2012. Retrieved 13 June 2012.  ^ Walker, John. "Viewing Venus
Venus
in Broad Daylight". Fourmilab Switzerland. Retrieved 19 April 2017.  ^ Hashimoto, G. L.; Roos-Serote, M.; Sugita, S.; Gilmore, M. S.; Kamp, L. W.; Carlson, R. W.; Baines, K. H. (2008). "Felsic highland crust on Venus
Venus
suggested by Galileo
Galileo
Near- Infrared
Infrared
Mapping Spectrometer data". Journal of Geophysical Research: Planets. 113: E00B24. Bibcode:2008JGRE..11300B24H. doi:10.1029/2008JE003134.  ^ David Shiga (10 October 2007). "Did Venus's ancient oceans incubate life?". New Scientist.  ^ Jakosky, Bruce M. (1999). "Atmospheres of the Terrestrial Planets". In Beatty, J. Kelly; Petersen, Carolyn Collins; Chaikin, Andrew. The New Solar System
Solar System
(4th ed.). Boston: Sky Publishing. pp. 175–200. ISBN 978-0-933346-86-4. OCLC 39464951.  ^ "Caught in the wind from the Sun". European Space Agency. 28 November 2007. Retrieved 12 July 2008.  ^ Evans, James (1998). The History and Practice of Ancient Astronomy. Oxford University Press. pp. 296–7. ISBN 978-0-19-509539-5. Retrieved 4 February 2008.  ^ Lopes, Rosaly M. C.; Gregg, Tracy K. P. (2004). Volcanic worlds: exploring the Solar System's volcanoes. Springer Publishing. p. 61. ISBN 978-3-540-00431-8.  ^ " Atmosphere
Atmosphere
of Venus". The Encyclopedia of Astrobiology, Astronomy, and Spaceflght. Retrieved 29 April 2007.  ^ Mueller, Nils (2014). " Venus
Venus
Surface and Interior". In Tilman, Spohn; Breuer, Doris; Johnson, T. V. Encyclopedia of the Solar System (3rd ed.). Oxford: Elsevier
Elsevier
Science & Technology. ISBN 978-0-12-415845-0. Retrieved 12 January 2016.  ^ Esposito, Larry W. (9 March 1984). " Sulfur
Sulfur
Dioxide: Episodic Injection Shows Evidence for Active Venus
Venus
Volcanism". Science. 223 (4640): 1072–1074. Bibcode:1984Sci...223.1072E. doi:10.1126/science.223.4640.1072. PMID 17830154. Retrieved 29 April 2009.  ^ Bullock, Mark A.; Grinspoon, David H. (March 2001). "The Recent Evolution of Climate on Venus" (PDF). Icarus. 150 (1): 19–37. Bibcode:2001Icar..150...19B. doi:10.1006/icar.2000.6570. Archived from the original (PDF) on 23 October 2003.  ^ Basilevsky, Alexander T.; Head, James W., III (1995). "Global stratigraphy of Venus: Analysis of a random sample of thirty-six test areas". Earth, Moon, and Planets. 66 (3): 285–336. Bibcode:1995EM&P...66..285B. doi:10.1007/BF00579467. CS1 maint: Multiple names: authors list (link) ^ Jones, Tom; Stofan, Ellen (2008). Planetology: Unlocking the Secrets of the Solar System. National Geographic Society. p. 74. ISBN 978-1-4262-0121-9.  ^ Kaufmann, W. J. (1994). Universe. New York: W. H. Freeman. p. 204. ISBN 978-0-7167-2379-0.  ^ a b c d Nimmo, F.; McKenzie, D. (1998). "Volcanism and Tectonics on Venus". Annual Review of Earth
Earth
and Planetary Sciences. 26 (1): 23–53. Bibcode:1998AREPS..26...23N. doi:10.1146/annurev.earth.26.1.23.  ^ a b Strom, Robert G.; Schaber, Gerald G.; Dawson, Douglas D. (25 May 1994). "The global resurfacing of Venus". Journal of Geophysical Research. 99 (E5): 10899–10926. Bibcode:1994JGR....9910899S. doi:10.1029/94JE00388.  ^ a b c d Frankel, Charles (1996). Volcanoes of the Solar System. Cambridge University Press. ISBN 978-0-521-47770-3.  ^ Batson, R.M.; Russell J. F. (18–22 March 1991). "Naming the Newly Found Landforms on Venus" (PDF). Proceedings of the Lunar and Planetary Science Conference XXII. Houston, Texas. p. 65. Retrieved 12 July 2009.  ^ a b Carolynn Young, ed. (1 August 1990). The Magellan Venus Explorer's Guide. California: Jet Propulsion Laboratory. p. 93. Retrieved 13 January 2016.  ^ Davies, M. E.; Abalakin, V. K.; Bursa, M.; Lieske, J. H.; Morando, B.; Morrison, D.; Seidelmann, P. K.; Sinclair, A. T.; Yallop, B.; Tjuflin, Y. S. (1994). "Report of the IAU Working Group on Cartographic Coordinates and Rotational Elements of the Planets and Satellites". Celestial Mechanics and Dynamical Astronomy. 63 (2): 127–148. Bibcode:1996CeMDA..63..127D. doi:10.1007/BF00693410.  ^ "USGS Astrogeology: Rotation and pole position for the Sun
Sun
and planets (IAU WGCCRE)". United States Geological Survey. JPL Publication 90-24. Retrieved 22 October 2009.  ^ Carolynn Young, ed. (1 August 1990). The Magellan Venus
Venus
Explorer's Guide. California: Jet Propulsion Laboratory. pp. 99–100. Retrieved 13 January 2016.  ^ Karttunen, Hannu; Kroger, P.; Oja, H.; Poutanen, M.; Donner, K. J. (2007). Fundamental Astronomy. Springer. p. 162. ISBN 978-3-540-34143-7.  ^ Kranopol'skii, V. A. (1980). " Lightning
Lightning
on Venus
Venus
according to Information Obtained by the Satellites Venera
Venera
9 and 10". Cosmic Research. 18 (3): 325–330. Bibcode:1980CosRe..18..325K.  ^ a b Russell, C. T.; Phillips, J. L. (1990). "The Ashen Light". Advances in Space Research. 10 (5): 137–141. Bibcode:1990AdSpR..10..137R. doi:10.1016/0273-1177(90)90174-X.  ^ " Venera
Venera
12 Descent Craft". National Space Science Data Center. NASA. Retrieved 10 September 2015.  ^ a b Russell, C. T.; Zhang, T. L.; Delva, M.; Magnes, W.; Strangeway, R. J.; Wei, H. Y. (November 2007). " Lightning
Lightning
on Venus
Venus
inferred from whistler-mode waves in the ionosphere" (PDF). Nature. 450 (7170): 661–662. Bibcode:2007Natur.450..661R. doi:10.1038/nature05930. PMID 18046401.  ^ " Venus
Venus
also zapped by lightning". CNN.com. 29 November 2007. Archived from the original on 30 November 2007. Retrieved 29 November 2007.  ^ Bauer, Markus (3 December 2012). "Have Venusian volcanoes been caught in the act?". European Space Agency. Archived from the original on 3 November 2013. Retrieved 20 June 2015.  ^ Glaze, Lori S. (August 1999). "Transport of SO 2 by explosive volcanism on Venus". Journal of Geophysical Research. 104 (E8): 18899–18906. Bibcode:1999JGR...10418899G. doi:10.1029/1998JE000619.  ^ Marcq, Emmanuel; Bertaux, Jean-Loup; Montmessin, Franck; Belyaev, Denis (January 2013). "Variations of sulphur dioxide at the cloud top of Venus's dynamic atmosphere". Nature Geoscience. 6 (1): 25–28. Bibcode:2013NatGe...6...25M. doi:10.1038/ngeo1650.  ^ "Ganis Chasma". Gazetteer of Planetary Nomenclature. USGS Astrogeology Science Center. Retrieved 19 June 2015.  ^ a b Lakdawalla, Emily (18 June 2015). "Transient hot spots on Venus: Best evidence yet for active volcanism". The Planetary Society. Retrieved 20 June 2015.  ^ "Hot lava flows discovered on Venus". European Space Agency. 18 June 2015. Archived from the original on 19 June 2015. Retrieved 20 June 2015.  ^ Shalygin, E. V.; Markiewicz, W. J.; Basilevsky, A. T.; Titov, D. V.; Ignatiev, N. I.; Head, J. W. (17 June 2015). "Active volcanism on Venus
Venus
in the Ganiki Chasma
Ganiki Chasma
rift zone". Geophysical Research Letters. 42: 4762–4769. Bibcode:2015GeoRL..42.4762S. doi:10.1002/2015GL064088.  ^ Romeo, I.; Turcotte, D. L. (2009). "The frequency-area distribution of volcanic units on Venus: Implications for planetary resurfacing". Icarus. 203 (1): 13–19. Bibcode:2009Icar..203...13R. doi:10.1016/j.icarus.2009.03.036.  ^ Herrick, R. R.; Phillips, R. J. (1993). "Effects of the Venusian atmosphere on incoming meteoroids and the impact crater population". Icarus. 112 (1): 253–281. Bibcode:1994Icar..112..253H. doi:10.1006/icar.1994.1180.  ^ Morrison, David; Owens, Tobias C. (2003). The Planetary System (3rd ed.). San Francisco: Benjamin Cummings. ISBN 978-0-8053-8734-6.  ^ Goettel, K. A.; Shields, J. A.; Decker, D. A. (16–20 March 1981). " Density
Density
constraints on the composition of Venus". Proceedings of the Lunar and Planetary Science Conference. Houston, TX: Pergamon Press. pp. 1507–1516. Bibcode:1982LPSC...12.1507G. Retrieved 12 July 2009.  ^ Faure, Gunter; Mensing, Teresa M. (2007). Introduction to planetary science: the geological perspective. Springer e Book
Book
collection. Springer. p. 201. ISBN 978-1-4020-5233-0.  ^ Aitta, A. (April 2012), "Venus' internal structure, temperature and core composition" (PDF), Icarus, 218 (2): 967–974, Bibcode:2012Icar..218..967A, doi:10.1016/j.icarus.2012.01.007, retrieved 17 January 2016.  ^ Nimmo, F. (2002). "Crustal analysis of Venus
Venus
from Magellan satellite observations at Atalanta Planitia, Beta Regio, and Thetis Regio". Geology. 30 (11): 987–990. Bibcode:2002Geo....30..987N. doi:10.1130/0091-7613(2002)030<0987:WDVLAM>2.0.CO;2. ISSN 0091-7613.  ^ Taylor, Fredric W. (2014). "Venus: Atmosphere". In Tilman, Spohn; Breuer, Doris; Johnson, T. V. Encyclopedia of the Solar System. Oxford: Elsevier
Elsevier
Science & Technology. ISBN 978-0-12-415845-0. Retrieved 12 January 2016.  ^ "Venus". Case Western Reserve University. 13 September 2006. Archived from the original on 26 April 2012. Retrieved 21 December 2011.  ^ Lewis, John S. (2004). Physics and Chemistry of the Solar System (2nd ed.). Academic Press. p. 463. ISBN 978-0-12-446744-6.  ^ Henry Bortman (2004). "Was Venus
Venus
Alive? 'The Signs are Probably There'". Space.com. Retrieved 31 July 2010.  ^ Hammonds, Markus (16 May 2013). "Does Alien Life
Life
Thrive in Venus's Mysterious Clouds?". Discovery News. Retrieved 11 August 2015.  ^ Grinspoon, David H.; Bullock, M. A. (October 2007). "Searching for Evidence of Past Oceans on Venus". Bulletin of the American Astronomical Society. 39: 540. Bibcode:2007DPS....39.6109G.  ^ Kasting, J. F. (1988). "Runaway and moist greenhouse atmospheres and the evolution of Earth
Earth
and Venus". Icarus. 74 (3): 472–494. Bibcode:1988Icar...74..472K. doi:10.1016/0019-1035(88)90116-9. PMID 11538226.  ^ Mullen, Leslie (13 November 2002). "Venusian Cloud Colonies". Astrobiology Magazine. Archived from the original on 16 August 2014.  ^ Landis, Geoffrey A. (July 2003). "Astrobiology: The Case for Venus" (PDF). Journal of the British Interplanetary Society. 56 (7–8): 250–254. Bibcode:2003JBIS...56..250L. NASA/TM—2003-212310. Archived from the original (PDF) on 7 August 2011.  ^ Cockell, Charles S. (December 1999). " Life
Life
on Venus". Planetary and Space Science. 47 (12): 1487–1501. Bibcode:1999P&SS...47.1487C. doi:10.1016/S0032-0633(99)00036-7.  ^ Moshkin, B. E.; Ekonomov, A. P.; Golovin Iu. M. (1979). "Dust on the surface of Venus". Kosmicheskie Issledovaniia (Cosmic Research). 17: 280–285. Bibcode:1979CoRe...17..232M.  ^ a b Krasnopolsky, V. A.; Parshev, V. A. (1981). "Chemical composition of the atmosphere of Venus". Nature. 292 (5824): 610–613. Bibcode:1981Natur.292..610K. doi:10.1038/292610a0.  ^ Krasnopolsky, Vladimir A. (2006). "Chemical composition of Venus atmosphere and clouds: Some unsolved problems". Planetary and Space Science. 54 (13–14): 1352–1359. Bibcode:2006P&SS...54.1352K. doi:10.1016/j.pss.2006.04.019.  ^ W. B. Rossow; A. D. del Genio; T. Eichler (1990). "Cloud-tracked winds from Pioneer Venus
Venus
OCPP images" (PDF). Journal of the Atmospheric Sciences. 47 (17): 2053–2084. Bibcode:1990JAtS...47.2053R. doi:10.1175/1520-0469(1990)047<2053:CTWFVO>2.0.CO;2. ISSN 1520-0469.  ^ Normile, Dennis (7 May 2010). "Mission to probe Venus's curious winds and test solar sail for propulsion". Science. 328 (5979): 677. Bibcode:2010Sci...328..677N. doi:10.1126/science.328.5979.677-a. PMID 20448159.  ^ Lorenz, Ralph D.; Lunine, Jonathan I.; Withers, Paul G.; McKay, Christopher P. (2001). "Titan, Mars
Mars
and Earth: Entropy Production by Latitudinal Heat Transport" (PDF). Ames Research Center, University of Arizona Lunar and Planetary Laboratory. Retrieved 21 August 2007.  ^ "Interplanetary Seasons". NASA. Archived from the original on 16 October 2007. Retrieved 21 August 2007.  ^ Basilevsky A. T.; Head J. W. (2003). "The surface of Venus". Reports on Progress in Physics. 66 (10): 1699–1734. Bibcode:2003RPPh...66.1699B. doi:10.1088/0034-4885/66/10/R04.  ^ McGill, G. E.; Stofan, E. R.; Smrekar, S. E. (2010). "Venus tectonics". In T. R. Watters; R. A. Schultz. Planetary Tectonics. Cambridge University Press. pp. 81–120. ISBN 978-0-521-76573-2.  ^ Otten, Carolyn Jones (2004). ""Heavy metal" snow on Venus
Venus
is lead sulfide". Washington University in St Louis. Retrieved 21 August 2007.  ^ Upadhyay, H. O.; Singh, R. N. (April 1995). "Cosmic ray Ionization of Lower Venus
Venus
Atmosphere". Advances in Space Research. 15 (4): 99–108. Bibcode:1995AdSpR..15...99U. doi:10.1016/0273-1177(94)00070-H.  ^ Hand, Eric (November 2007). "European mission reports from Venus". Nature (450): 633–660. doi:10.1038/news.2007.297.  ^ Staff (28 November 2007). " Venus
Venus
offers Earth
Earth
climate clues". BBC News. Retrieved 29 November 2007.  ^ " ESA
ESA
finds that Venus
Venus
has an ozone layer too". European Space Agency. 6 October 2011. Retrieved 25 December 2011.  ^ "When A Planet
Planet
Behaves Like A Comet". European Space Agency. 29 January 2013. Retrieved 31 January 2013.  ^ Kramer, Miriam (30 January 2013). " Venus
Venus
Can Have 'Comet-Like' Atmosphere". Space.com. Retrieved 31 January 2013.  ^ Fukuhara, Tetsuya; Futaguchi, Masahiko; Hashimoto, George L.; et al. (16 January 2017). "Large stationary gravity wave in the atmosphere of Venus". Nature Geoscience. 10: 85–88. Bibcode:2017NatGe..10...85F. doi:10.1038/ngeo2873. Retrieved 17 January 2017.  ^ Rincon, Paul (16 January 2017). " Venus
Venus
wave may be Solar System's biggest". BBC News. Retrieved 17 January 2017.  ^ Chang, Kenneth (16 January 2017). " Venus
Venus
Smiled, With a Mysterious Wave Across Its Atmosphere". The New York Times. Retrieved 17 January 2017.  ^ "The HITRAN Database". Atomic and Molecular Physics Division, Harvard-Smithsonian Center for Astrophysics. Retrieved 8 August 2012. HITRAN is a compilation of spectroscopic parameters that a variety of computer codes use to predict and simulate the transmission and emission of light in the atmosphere.  ^ " HITRAN on the Web Information System". V.E. Zuev Institute of Atmospheric Optics. Retrieved 11 August 2012.  ^ Dolginov, Sh.; Eroshenko, E. G.; Lewis, L. (September 1969). "Nature of the Magnetic Field in the Neighborhood of Venus". Cosmic Research. 7: 675. Bibcode:1969CosRe...7..675D.  ^ Kivelson G. M.; Russell, C. T. (1995). "Introduction to Space Physics". Cambridge University Press. ISBN 978-0-521-45714-9.  ^ Luhmann, J. G.; Russell, C. T. (1997). "Venus: Magnetic Field and Magnetosphere". In Shirley, J. H.; Fainbridge, R. W. Encyclopedia of Planetary Sciences. New York: Chapman and Hall. pp. 905–907. ISBN 978-1-4020-4520-2.  ^ Stevenson, D. J. (15 March 2003). "Planetary magnetic fields". Earth and Planetary Science Letters. 208 (1–2): 1–11. Bibcode:2003E&PSL.208....1S. doi:10.1016/S0012-821X(02)01126-3.  ^ a b Nimmo, Francis (November 2002). "Why does Venus
Venus
lack a magnetic field?" (PDF). Geology. 30 (11): 987–990. Bibcode:2002Geo....30..987N. doi:10.1130/0091-7613(2002)030<0987:WDVLAM>2.0.CO;2. ISSN 0091-7613. Retrieved 28 June 2009.  ^ Konopliv, A. S.; Yoder, C. F. (1996). "Venusian k2 tidal Love number from Magellan and PVO tracking data". Geophysical Research Letters. 23 (14): 1857–1860. Bibcode:1996GeoRL..23.1857K. doi:10.1029/96GL01589. Archived from the original on 12 May 2011. Retrieved 12 July 2009.  ^ Svedhem, Håkan; Titov, Dmitry V.; Taylor, Fredric W.; Witasse, Olivier (November 2007). " Venus
Venus
as a more Earth-like planet". Nature. 450 (7170): 629–632. Bibcode:2007Natur.450..629S. doi:10.1038/nature06432. PMID 18046393.  ^ Donahue, T. M.; Hoffman, J. H.; Hodges, R. R.; Watson, A. J. (1982). " Venus
Venus
Was Wet: A Measurement of the Ratio of Deuterium
Deuterium
to Hydrogen". Science. 216 (4546): 630–633. Bibcode:1982Sci...216..630D. doi:10.1126/science.216.4546.630. ISSN 0036-8075. PMID 17783310.  ^ " Venus
Venus
Close Approaches to Earth
Earth
as predicted by Solex 11". Archived from the original on 9 August 2012. Retrieved 19 March 2009.  Numbers generated by Solex ^ Squyres, Steven W. (2016). "Venus". Encyclopædia Britannica Online. Retrieved 7 January 2016.  ^ Bakich, Michael E. (2000). "Rotational velocity (equatorial)". The Cambridge Planetary Handbook. Cambridge University Press. p. 50. ISBN 978-0-521-63280-5.  ^ "Could Venus
Venus
Be Shifting Gear?". Venus
Venus
Express. European Space Agency. 10 February 2012. Retrieved 7 January 2016.  ^ "Planetary Facts". The Planetary Society. Archived from the original on 11 May 2012. Retrieved 20 January 2016.  ^ a b "Space Topics: Compare the Planets". The Planetary Society. Archived from the original on 18 February 2006. Retrieved 12 January 2016.  ^ Serge Brunier
Serge Brunier
(2002). Solar System
Solar System
Voyage. Translated by Dunlop, Storm. Cambridge University Press. p. 40. ISBN 978-0-521-80724-1.  ^ Correia, Alexandre C. M.; Laskar, Jacques; De Surgy, Olivier Néron (May 2003). "Long-Term Evolution of the Spin of Venus, Part I: Theory" (PDF). Icarus. 163 (1): 1–23. Bibcode:2003Icar..163....1C. doi:10.1016/S0019-1035(03)00042-3.  ^ Laskar, Jacques; De Surgy, Olivier Néron. "Long-Term Evolution of the Spin of Venus, Part II: Numerical Simulations" (PDF). Icarus. 163 (1): 24–45. Bibcode:2003Icar..163...24C. doi:10.1016/S0019-1035(03)00043-5.  ^ Gold, T.; Soter, S. (1969). "Atmospheric Tides and the Resonant Rotation of Venus". Icarus. 11 (3): 356–66. Bibcode:1969Icar...11..356G. doi:10.1016/0019-1035(69)90068-2.  ^ Shapiro, I. I.; Campbell, D. B.; De Campli, W. M. (June 1979). "Nonresonance Rotation of Venus". Astrophysical Journal. 230: L123–L126. Bibcode:1979ApJ...230L.123S. doi:10.1086/182975.  ^ a b Sheppard, Scott S.; Trujillo, Chadwick A. (July 2009). "A Survey for Satellites of Venus". Icarus. 202 (1): 12–16. arXiv:0906.2781 . Bibcode:2009Icar..202...12S. doi:10.1016/j.icarus.2009.02.008.  ^ Mikkola, S.; Brasser, R.; Wiegert, P.; Innanen, K. (July 2004). " Asteroid
Asteroid
2002 VE68: A Quasi-Satellite of Venus". Monthly Notices of the Royal Astronomical Society. 351 (3): L63. Bibcode:2004MNRAS.351L..63M. doi:10.1111/j.1365-2966.2004.07994.x.  ^ De la Fuente Marcos, Carlos; De la Fuente Marcos, Raúl (November 2012). "On the Dynamical Evolution of 2002 VE68". Monthly Notices of the Royal Astronomical Society. 427 (1): 728–39. arXiv:1208.4444 . Bibcode:2012MNRAS.427..728D. doi:10.1111/j.1365-2966.2012.21936.x.  ^ De la Fuente Marcos, Carlos; De la Fuente Marcos, Raúl. "Asteroid 2012 XE133: A Transient Companion to Venus". Monthly Notices of the Royal Astronomical Society. 432 (2): 886–93. arXiv:1303.3705 . Bibcode:2013MNRAS.432..886D. doi:10.1093/mnras/stt454.  ^ Musser, George (10 October 2006). "Double Impact May Explain Why Venus
Venus
Has No Moon". Scientific American. Retrieved 7 January 2016.  ^ Tytell, David (10 October 2006). "Why Doesn't Venus
Venus
Have a Moon?". Sky & Telescope. Retrieved 7 January 2016.  ^ Dickinson, Terrence (1998). NightWatch: A Practical Guide to Viewing the Universe. Buffalo, NY: Firefly Books. p. 134. ISBN 978-1-55209-302-3. Retrieved 12 January 2016.  ^ Bower, Gordon. "When is Venus
Venus
brightest?". Excelsior Statistics and Optimization. Retrieved 2 April 2017.  ^ Tony Flanders (25 February 2011). "See Venus
Venus
in Broad Daylight!". Sky & Telescope. Retrieved 11 January 2016.  ^ Anon. "Transit of Venus". History. University of Central Lancashire. Archived from the original on 30 July 2012. Retrieved 14 May 2012.  ^ Boyle, Alan (5 June 2012). " Venus
Venus
transit: A last-minute guide". NBC News. Archived from the original on 18 June 2013. Retrieved 11 January 2016.  ^ Espenak, Fred (2004). "Transits of Venus, Six Millennium Catalog: 2000 BCE to 4000 CE". Transits of the Sun. NASA. Retrieved 14 May 2009.  ^ Kollerstrom, Nicholas (1998). "Horrocks and the Dawn of British Astronomy". University College London. Retrieved 11 May 2012.  ^ Hornsby, T. (1771). "The quantity of the Sun's parallax, as deduced from the observations of the transit of Venus
Venus
on June 3, 1769". Philosophical Transactions of the Royal Society. 61 (0): 574–579. doi:10.1098/rstl.1771.0054.  ^ Woolley, Richard (1969). " Captain Cook
Captain Cook
and the Transit of Venus
Transit of Venus
of 1769". Notes and Records of the Royal Society of London. 24 (1): 19–32. doi:10.1098/rsnr.1969.0004. ISSN 0035-9149. JSTOR 530738.  ^ Baez, John (4 January 2014). "The Pentagram of Venus". Azimuth. Archived from the original on 14 December 2015. Retrieved 7 January 2016.  ^ Chatfield, Chris (2010). "The Solar System
Solar System
with the naked eye". The Gallery of Natural Phenomena. Retrieved 19 April 2017.  ^ Gaherty, Geoff (26 March 2012). " Planet
Planet
Venus
Venus
Visible in Daytime Sky Today: How to See It". Space.com. Retrieved 19 April 2017.  ^ Goines, David Lance (18 October 1995). "Inferential Evidence for the Pre-telescopic Sighting of the Crescent Venus". Goines.net. Retrieved 19 April 2017.  ^ Baum, R. M. (2000). "The enigmatic ashen light of Venus: an overview". Journal of the British Astronomical Association. 110: 325. Bibcode:2000JBAA..110..325B.  ^ a b c Cooley, Jeffrey L. (2008). "Inana and Šukaletuda: A Sumerian Astral Myth". KASKAL. 5: 161–172. ISSN 1971-8608.  ^ Black, Jeremy; Green, Anthony (1992). Gods, Demons and Symbols of Ancient Mesopotamia: An Illustrated Dictionary. The British Museum Press. pp. 108–109. ISBN 0-7141-1705-6.  ^ Nemet-Nejat, Karen Rhea (1998), Daily Life
Life
in Ancient Mesopotamia, Daily Life, Greenwood, p. 203, ISBN 978-0313294976  ^ Hobson, Russell (2009). The Exact Transmission of Texts in the First Millennium B.C.E. (PDF) (Ph.D.). University of Sydney, Department of Hebrew, Biblical and Jewish Studies.  ^ Waerden, Bartel (1974). Science awakening II: the birth of astronomy. Springer. p. 56. ISBN 978-90-01-93103-2. Retrieved 10 January 2011.  ^ Pliny the Elder
Pliny the Elder
(1991). Natural History II:36–37. translated by John F. Healy. Harmondsworth, Middlesex, UK: Penguin. pp. 15–16.  ^ Burkert, Walter (1972). Lore and Science in Ancient Pythagoreanism. Harvard University Press. p. 307. ISBN 978-0-674-53918-1.  ^ Goldstein, Bernard R. (March 1972). "Theory and Observation in Medieval Astronomy". Isis. University of Chicago Press. 63 (1): 39–47 [44]. doi:10.1086/350839.  ^ "AVICENNA viii. Mathematics and Physical Sciences". Encyclopedia Iranica.  ^ S. M. Razaullah Ansari (2002). History of Oriental Astronomy: Proceedings of the Joint Discussion-17 at the 23rd General Assembly of the International Astronomical Union, Organised by the Commission 41 (History of Astronomy), Held in Kyoto, August 25–26, 1997. Springer Science+Business Media. p. 137. ISBN 978-1-4020-0657-9.  ^ J.M. Vaquero; M. Vázquez (2009). The Sun
Sun
Recorded Through History. Springer Science & Business Media. p. 75. ISBN 978-0-387-92790-9.  ^ Fredrick Kennard. Thought Experiments: Popular Thought Experiments in Philosophy, Physics, Ethics, Computer Science & Mathematics. p. 113. ISBN 978-1-329-00342-2.  ^ Palmieri, Paolo (2001). " Galileo
Galileo
and the discovery of the phases of Venus". Journal for the History of Astronomy. 21 (2): 109–129. Bibcode:2001JHA....32..109P.  ^ Fegley Jr, B (2003). Heinrich D. Holland; Karl K. Turekian, eds. Venus. Treatise on Geochemistry. Elsevier. pp. 487–507. ISBN 978-0-08-043751-4.  ^ Kollerstrom, Nicholas (2004). "William Crabtree's Venus
Venus
transit observation" (PDF). Proceedings IAU Colloquium No. 196, 2004. International Astronomical Union. Retrieved 10 May 2012.  ^ Marov, Mikhail Ya. (2004). D.W. Kurtz, ed. Mikhail Lomonosov
Mikhail Lomonosov
and the discovery of the atmosphere of Venus
Venus
during the 1761 transit. Proceedings of IAU Colloquium No. 196. Preston, U.K.: Cambridge University Press. pp. 209–219. Bibcode:2005tvnv.conf..209M. doi:10.1017/S1743921305001390.  ^ "Mikhail Vasilyevich Lomonosov". Encyclopædia Britannica Online. Retrieved 12 July 2009.  ^ Russell, H. N. (1899). "The Atmosphere
Atmosphere
of Venus". Astrophysical Journal. 9: 284–299. Bibcode:1899ApJ.....9..284R. doi:10.1086/140593.  ^ Hussey, T. (1832). "On the Rotation of Venus". Monthly Notices of the Royal Astronomical Society. 2: 78–126. Bibcode:1832MNRAS...2...78H. doi:10.1093/mnras/2.11.78d.  ^ Ross, F. E. (1928). "Photographs of Venus". Astrophysical Journal. 68–92: 57. Bibcode:1928ApJ....68...57R. doi:10.1086/143130.  ^ Slipher, V. M. (1903). "A Spectrographic Investigation of the Rotation Velocity of Venus". Astronomische Nachrichten. 163 (3–4): 35–52. Bibcode:1903AN....163...35S. doi:10.1002/asna.19031630303.  ^ Goldstein, R. M.; Carpenter, R. L. (1963). "Rotation of Venus: Period Estimated from Radar
Radar
Measurements". Science. 139 (3558): 910–911. Bibcode:1963Sci...139..910G. doi:10.1126/science.139.3558.910. PMID 17743054.  ^ Campbell, D. B.; Dyce, R. B.; Pettengill G. H. (1976). "New radar image of Venus". Science. 193 (4258): 1123–1124. Bibcode:1976Sci...193.1123C. doi:10.1126/science.193.4258.1123. PMID 17792750.  ^ Mitchell, Don (2003). "Inventing The Interplanetary Probe". The Soviet Exploration of Venus. Retrieved 27 December 2007.  ^ Mayer; McCullough & Sloanaker (January 1958). "Observations of Venus
Venus
at 3.15-cm Wave Length". The Astrophysical Journal. 127: 1. Bibcode:1958ApJ...127....1M. doi:10.1086/146433.  ^ Jet Propulsion Laboratory (1962). "Mariner- Venus
Venus
1962 Final Project Report" (PDF). SP-59. NASA.  ^ Mitchell, Don (2003). "Plumbing the Atmosphere
Atmosphere
of Venus". The Soviet Exploration of Venus. Retrieved 27 December 2007.  ^ "Report on the Activities of the COSPAR Working Group VII". Preliminary Report, COSPAR Twelfth Plenary Meeting and Tenth International Space Science Symposium. Prague, Czechoslovakia: National Academy of Sciences. 11–24 May 1969. p. 94.  ^ Sagdeev, Roald; Eisenhower, Susan (28 May 2008). "United States-Soviet Space Cooperation during the Cold War". Retrieved 19 July 2009.  ^ Colin, L.; Hall, C. (1977). "The Pioneer Venus
Venus
Program". Space Science Reviews. 20 (3): 283–306. Bibcode:1977SSRv...20..283C. doi:10.1007/BF02186467.  ^ Williams, David R. (6 January 2005). "Pioneer Venus
Venus
Project Information". NASA/Goddard Space Flight Center. Retrieved 19 July 2009.  ^ Greeley, Ronald; Batson, Raymond M. (2007). Planetary Mapping. Cambridge University Press. p. 47. ISBN 978-0-521-03373-2. Retrieved 19 July 2009.  ^ Hall, Loura (1 April 2016). "Automaton Rover for Extreme Environments (AREE)". NASA. Retrieved 29 August 2017.  ^ Aaron J. Atsma. "Eospheros & Hespheros". Theoi.com. Retrieved 15 January 2016.  ^ Dava Sobel
Dava Sobel
(2005). The Planets. Harper Publishing. pp. 53–70. ISBN 978-0-14-200116-5.  ^ Miller, Ron (2003). Venus. Twenty-First Century Books. p. 12. ISBN 978-0-7613-2359-4.  ^ Dick, Steven (2001). Life
Life
on Other Worlds: The 20th-Century Extraterrestrial Life
Life
Debate. Cambridge University Press. p. 43. ISBN 978-0-521-79912-6.  ^ Seed, David (2005). A Companion to Science Fiction. Blackwell Publishing. pp. 134–135. ISBN 978-1-4051-1218-5.  ^ a b c Stearn, William (May 1968). "The Origin of the Male and Female Symbols of Biology". Taxon. 11 (4): 109–113. doi:10.2307/1217734. JSTOR 1217734.  ^ Clark, Stuart (26 September 2003). "Acidic clouds of Venus
Venus
could harbour life". New Scientist. Retrieved 30 December 2015.  ^ Redfern, Martin (25 May 2004). " Venus
Venus
clouds 'might harbour life'". BBC News. Retrieved 30 December 2015. ^ Dartnell, Lewis R.; Nordheim, Tom Andre; Patel, Manish R.; Mason, Jonathon P.; et al. (September 2015). "Constraints on a potential aerial biosphere on Venus: I. Cosmic rays". Icarus. 257: 396–405. Bibcode:2015Icar..257..396D. doi:10.1016/j.icarus.2015.05.006. Retrieved 20 August 2015.  ^ a b Landis, Geoffrey A. (2003). "Colonization of Venus". AIP Conference Proceedings. 654. pp. 1193–1198. doi:10.1063/1.1541418. Archived from the original on 11 July 2012. 

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WorldCat Identities VIAF: 316741882 LCCN: sh85142768 GND: 40625

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