Venus

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Venus is the second planet from the Sun.[3] Venus is the only planet in the Solar System that has a day longer than a year. The year length of Venus is 225 Earth days. The day length of Venus is 243 Earth days.[3]

Venus ♀
Venus in approximately true colour, a nearly uniform pale cream, although the image has been processed to bring out details.[1] The planet's disc is about three-quarters illuminated; almost no variation or detail can be seen in the clouds
A real-colour image taken by Mariner 10 processed from two filters, the surface is obscured by thick sulfuric acid clouds
Designations
Pronunciation/ˈvnəs/ ( listen)
AdjectivesVenusian or (rarely) Cytherean, Venerean
Orbital characteristics
Epoch J2000
Aphelion
  • 0.728213 AU
  • 108,939,000 km
Perihelion
  • 0.718440 AU
  • 107,477,000 km
  • 0.723332 AU
  • 108,208,000 km
Eccentricity0.006772
583.92 days
35.02 km/s
50.115°
Inclination
76.680°
54.884°
SatellitesNone
Physical characteristics
Mean radius
  • 6,051.8±1.0 km
  • 0.9499 Earths
Flattening0
  • 4.6023×108 km2
  • 0.902 Earths
Volume
  • 9.2843×1011 km3
  • 0.866 Earths
Mass
  • 4.8675×1024 kg
  • 0.815 Earths
Mean density
5.243 g/cm3
  • 8.87 m/s2
  • 0.904 g
10.36 km/s (6.44 mi/s)[2]
−243.025 d (retrograde)
Equatorial rotation velocity
6.52 km/h (1.81 m/s)
2.64° (for retrograde rotation)
177.36° (to orbit)[note 1]
North pole right ascension
  • 18h 11m 2s
  • 272.76°
North pole declination
67.16°
Albedo
Surface temp. min mean max
Kelvin 737 K
Celsius 462 °C
Fahrenheit 864 °F
−4.92 to −2.98
9.7″–66.0″
Atmosphere
Surface pressure
92 bar (9.2 MPa)
Composition by volume
  1. Defining the rotation as retrograde, as done by NASA space missions and the USGS, puts Ishtar Terra in the northern hemisphere and makes the axial tilt 2.64°. Following the right-hand rule for prograde rotation puts Ishtar Terra in the southern hemisphere and makes the axial tilt 177.36°.

Venus is a terrestrial planet because it has a solid, rocky surface like other planets in the inner Solar System. Astronomers have known Venus for thousands of years. The ancient Romans named it after their goddess Venus, goddess of love and beauty.[3]

Venus is the brightest thing in the night sky except for the Moon. It is sometimes called the morning star or the evening star as at some elongations it is easily seen just before the sun comes up in the morning. At other times, it can be seen just after the sun goes down in the evening. Venus comes closer to the Earth than any other planet does.

Venus is sometimes called the sister planet of Earth as they are quite similar in size and gravity. In other ways the planets are very different. Venus' atmosphere (air) is mostly carbon dioxide with clouds of sulphuric acid.[4] Sulphuric acid is a chemical that is poisonous to life. For this it is sometimes known as the Earth's "evil twin".[5][6]

The thick atmosphere makes it hard to see the surface. Until the late twentieth century many thought there might be life there. The pressure on Venus' surface is 92 times that of Earth. Venus is one of only two planets in the Solar System (the other being Mercury) that has no moons. Venus spins very slowly on its axis and it spins in the opposite direction to the other planets.

Physical properties

 
Radar view of the surface of Venus (Magellan spacecraft)

Venus is a terrestrial planet so, like the Earth, its surface is made of rock. Venus is much hotter than Earth. All the carbon dioxide in the atmosphere acts like a blanket, trapping heat from the Sun. This effect is called the greenhouse effect and it is very strong on Venus. This makes the surface of Venus the hottest of any planet's surface in the Solar System with an estimated average temperature of 480 °C (896.0 °F).[7][8] This is hot enough to melt lead or zinc.

Geography

Venus has no oceans because it is much too hot for water. Venus' surface is a dry desert. Because of the clouds, only radar can map the surface. It is about 80% smooth, rocky plains, made mostly of basalt. Two higher areas called continents make up the north and south of the planet. The north is called Ishtar Terra and the south is called Aphrodite Terra. They are named after the Babylonian and Greek goddesses of love.[9]

The surface of Venus looks like it has been shaped by volcanic activity. Venus has a lots of volcanoes.[10] The surface of Venus is estimated to be 300–600 million years old.[10][11]

Unlike Earth or Mars, Venus does not have defined highlands or lowlands, and it does not have tectonic plates.

Atmosphere

Venus' atmosphere is mostly carbon dioxide and nitrogen gas with clouds of sulphuric acid. Because the atmosphere is so thick or dense the pressure is very high. The pressure is 92 times the pressure on Earth, enough to crush many things.

It is impossible to see the planet's surface from space as the thick cloud layer reflects 60% of the light that hits it. The only way scientists are able to see it is by using infrared and ultraviolet cameras and radar.

Scientists believe that billions of years ago, the atmosphere of Venus could have been like Earth's atmosphere. There may have been lots of water on the surface of Venus. But after 600 million to several billion years, the evaporation of the water put greenhouse gases into its atmosphere.[12]

Magnetic field

In 1967, Venera 4 found that the magnetic field of Venus was much weaker than that of Earth. This magnetic field is induced by an interaction between the ionosphere and the solar wind. Venus' magnetosphere is not strong enough to protect the atmosphere from cosmic rays.[13]

Transit of Venus

Venus can sometimes be seen passing between the Sun and Earth. Venus looks like a black dot when seen through a special telescope. These passages are called "transits". These "transits" happen in pairs eight years apart. Then it is more than a hundred years to the next pair.

Orbit and rotation

 
Orbit of Venus compared to the orbit of the Earth

Venus orbits the Sun at an average distance of about 108 million km (68~ million mi). It completes an orbit every 224.7 days.[14] The rotation of Venus is slow. A Venusian sidereal day is longer than a Venusian year.

List of satellites sent to Venus

Many man-made satellites have been sent to Venus to study it. They are:

Mariner

Template:Transcluded section {{#section-h:List of satellites sent to Venus|Mariner Satellites}}

Venera

Template:Transcluded section {{#section-h:List of satellites sent to Venus|Venera Satellites}}

Venus Media

Related pages

Notes

References

  1. Lakdawalla, Emily better (21 September 2009). "Venus Looks More Boring Than You Think It Does". The Planetary Society. Archived from the original on 6 January 2012. Retrieved 4 December 2011.
  2. "Planets and Pluto: Physical Characteristics". NASA. 5 November 2008. Archived from the original on 7 September 2006. Retrieved 26 August 2015.
  3. 3.0 3.1 3.2 "Venus". NASA Solar System Exploration. Archived from the original on 2021-10-19. Retrieved 2021-10-19.
  4. "The Atmosphere of Venus". Archived from the original on 2009-03-02. Retrieved 2008-08-19.
  5. Hall, Shannon (June 5, 2019). "Venus is Earth's evil twin — and space agencies can no longer resist its pull". Nature. https://www.nature.com/articles/d41586-019-01730-5. Retrieved June 6, 2021. 
  6. Greenfieldboyce, Nell (June 2, 2021). "NASA Picks Twin Missions To Visit Venus, Earth's 'Evil Twin'". NPR. https://www.npr.org/2021/06/02/1002627399/nasa-picks-twin-missions-to-visit-venus-earths-evil-twin. Retrieved June 6, 2021. 
  7. "Venus - an overview". Archived from the original on 2009-09-11. Retrieved 2008-08-20.
  8. "Temperature on the Surface of Venus". Archived from the original on 2008-09-28. Retrieved 2008-08-19.
  9. Batson R.M. & Russell J.F. 1991. Naming the newly found landforms on Venus. Abstracts of the Lunar and Planetary Science Conference, v. 22, p65.
  10. 10.0 10.1 Frankel, Charles. (1996). Volcanoes of the solar system. Cambridge: Cambridge University Press. ISBN 0-521-47201-6. OCLC 32969544. Retrieved 2020-09-14.
  11. Nimmo, F.; Mckenzie, D. (1998). "Volcanism and Tectonics on Venus". Annual Review of Earth and Planetary Sciences. 26: 23–51. Bibcode:1998AREPS..26...23N. doi:10.1146/ANNUREV.EARTH.26.1.23. ISSN 0084-6597. S2CID 862354.
  12. Kasting, James F. (1988). "Runaway and moist greenhouse atmospheres and the evolution of Earth and Venus". Icarus. 74 (3): 472–494. Bibcode:1988Icar...74..472K. doi:10.1016/0019-1035(88)90116-9. PMID 11538226. Archived from the original on 2020-05-31. Retrieved 2020-09-14.
  13. Introduction to space physics. Kivelson, M. G. (Margaret Galland), 1928-, Russell, C. T. (Christopher T.). Cambridge: Cambridge University Press. 1995. ISBN 0-521-45104-3. OCLC 30509600. Retrieved 2020-09-14.{{cite book}}: CS1 maint: others (link)
  14. "Venus Fact Sheet". 2016-03-04. Archived from the original on 2016-03-04. Retrieved 2020-09-14.

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