50000 Quaoar (//[a]), provisional designation 2002 LM60, is a non-resonant trans-Neptunian object (cubewano) and a possible dwarf planet in the Kuiper belt, located in the outermost region of the Solar System. It measures approximately 1,100 km (680 mi) in diameter, which is about half the diameter of Pluto. The object was discovered by American astronomers Chad Trujillo and Michael Brown at the Palomar Observatory on 6 June 2002. Signs of water ice on the surface of Quaoar have been found, which suggests that cryovolcanism may be occurring on Quaoar. A small amount of methane is present on its surface, which can only be retained by the largest Kuiper belt objects. In February 2007, Weywot, a synchronous minor-planet moon in orbit around Quaoar, was discovered by Brown. Weywot is measured to be 80 km (50 mi) across. Both objects were named after mythological figures from the Native American Tongva people in Southern California. Quaoar is the Tongva creator deity and Weywot is his son.
Quaoar imaged by the Hubble Space Telescope in 2002
|Discovered by||C. Trujillo|
M. E. Brown
|Discovery site||Palomar Obs.|
|Discovery date||6 June 2002|
|MPC designation||(50000) Quaoar|
(deity of the Tongva people)
|TNO  · cubewano |
|Orbital characteristics |
|Epoch 27 April 2019 (JD 2458600.5)|
|Uncertainty parameter 3|
|Observation arc||64.044 yr (23,376 days)|
|Earliest precovery date||25 May 1954|
|288.81 yr (105,416 d)|
|0° 0m 12.287s / day|
|Known satellites||1 (Weywot; D: ±11 km) 81|
|±5 km (occultation) 1110|
0.12 Eris masses
V−R = ±0.010.64
Quaoar was discovered by astronomer Chad Trujillo on 5 June 2002, when he identified it in images acquired by the Samuel Oschin Telescope at Palomar Observatory the night before. The discovery was submitted to the Minor Planet Center on 6 June, with Trujillo and his colleague Michael Brown credited for the discovery. At the time of discovery, Quaoar was located in the constellation Ophiuchus, at an apparent magnitude of 18.5. Its discovery was formally announced at a meeting of the American Astronomical Society on 7 October 2002. The earliest prediscovery image of Quaoar was found on a photographic plate imaged on 25 May 1954 from the Palomar Observatory Sky Survey. Quaoar's discovery has been cited as Brown as having contributed to the reclassification of Pluto as a dwarf planet.
Quaoar is named for the Tongva creator god, following the International Astronomical Union (IAU) naming convention for non-resonant Kuiper belt objects after creator deities. The Tongva people are native to area around Los Angeles, the city where Quaoar was discovered. Michael Brown and his team had picked the name with the more intuitive spelling Kwawar, but the preferred spelling among the Tongva was Qua-o-ar. Upon the discovery of Quaoar, prior to IAU approval of its name, Quaoar was temporarily referred as "Object X", after Planet X. At that time, Quaoar was thought to be a possible tenth planet, with a size comparable to that of Pluto. After the announcement of its discovery, Quaoar was provisionally designated 2002 LM60, as it was discovered in the year 2002. The minor planet number 50000 for Quaoar was not a coincidence, but chosen to commemorate a particularly large object found in the search for a Pluto-sized object in the Kuiper belt, parallel to the similarly numbered 20000 Varuna. However, subsequent even larger discoveries such as 136199 Eris were simply numbered according to the order in which their orbits were confirmed.
Quaoar's albedo or reflectivity could be as low as 0.1, which would still be much higher than the lower estimate of 0.04 for 20000 Varuna. This may indicate that fresh ice has disappeared from Quaoar's surface. The surface is moderately red, meaning that Quaoar is relatively more reflective in the red and near-infrared spectrum than in the blue. The Kuiper belt objects Varuna and Ixion are also moderately red in the spectral class. Larger Kuiper belt objects are often much brighter because they are covered in more fresh ice and have a higher albedo, and thus they present a neutral color. A 2006 model of internal heating via radioactive decay suggested that, unlike 90482 Orcus, Quaoar may not be capable of sustaining an internal ocean of liquid water at the mantle–core boundary.
The presence of methane and other volatiles on Quaoar's surface suggest that it may support a tenuous atmosphere produced from the sublimation of volatiles. With a measured mean temperature of ~ 44 K (−229.2 °C), the upper limit of Quaoar's atmospheric pressure is expected to be in the range of a few microbars. Due to Quaoar's small size and mass, the possibility of Quaoar having an atmosphere of nitrogen and carbon monoxide has been ruled out, since the gases would escape from Quaoar. The possibility of a methane atmosphere still remains, with the upper limit being less than 1 microbar. In 2013, Quaoar occulted a 15.8 magnitude star and revealed no sign of a substantial atmosphere, placing an upper limit to at least 20 nanobars, under the assumption that Quaoar's mean temperature is 42 K (−231.2 °C) and that its atmosphere consists of mostly methane.
Mass and densityEdit
Because Quaoar is a binary object, the mass of the system can be calculated from the orbit of the secondary. Quaoar's estimated density of around and estimated size of 1,100 km (680 mi) suggests that it is a 2.2 g/cm3dwarf planet. American astronomer Michael Brown estimates that rocky bodies around 900 km (560 mi) in diameter relax into hydrostatic equilibrium, and that icy bodies relax into hydrostatic equilibrium somewhere between 200 km (120 mi) and 400 km (250 mi). With an estimated mass greater than ×1021 kg, Quaoar has the mass and diameter "usually" required for being in hydrostatic equilibrium according to the 1.62006 IAU draft definition of a planet (5×1020 kg, 800 km), and Brown states that Quaoar "must be" a dwarf planet. Light-curve-amplitude analysis shows only small deviations, suggesting that Quaoar is indeed a spheroid with small albedo spots and hence a dwarf planet.
Planetary scientist Erik Asphaug has suggested that Quaoar may have collided with a much larger body, stripping the lower-density mantle from Quaoar, and leaving behind the denser core. He envisions that Quaoar was originally covered by a mantle of ice that made it 300 km (190 mi) to 500 km (310 mi) bigger than its present size, and that it collided with another Kuiper-belt body about twice its size—an object roughly the diameter of Pluto (or even approaching the size of Mars), possibly Pluto itself. This model was made assuming Quaoar actually had a density of 4.2 g/cm3, but more recent estimates have given it a more Pluto-like density of only 2 g/cm3, with no more need for the collision theory.
Quaoar is thought to be an oblate spheroid around 1,100 km (680 mi) in diameter, being slightly flattened in shape. The estimates come from observations of Quaoar as it occulted a 15.8 magnitude star in 2013. Given that Quaoar has an estimated oblateness value of ±0.006 and a measured equatorial diameter of 0.0897+48
−34 km, Quaoar is believed to be in hydrostatic equilibrium, being described as a 1138Maclaurin spheroid. Quaoar is about as large and massive as (if somewhat smaller than) Pluto's moon Charon.[b] Quaoar is roughly half the size of Pluto.
Quaoar was the first trans-Neptunian object to be measured directly from Hubble Space Telescope images, using a method comparing images with the Hubble point spread function (PSF). In 2004, Quaoar was estimated to have a diameter of 1,260 km (780 mi) with an uncertainty of 190 km (120 mi), using Hubble's measurements. Given its distance Quaoar is on the limit of Hubble's resolution of 40 milliarcseconds and its image is consequently "smeared" on a few adjacent pixels. By comparing carefully this image with the images of stars in the background and using a sophisticated model of Hubble optics (PSF), Brown and Trujillo were able to find the best-fit disk size that would give a similar blurred image. This method was recently applied by the same authors to measure the size of the dwarf planet Eris.
At the time of its discovery in 2002, Quaoar was the largest object found in the Solar System since the discovery of Pluto. Quaoar's size was subsequently revised downward and was later superseded in size as larger objects (Eris, Haumea, and Makemake) were discovered. The uncorrected 2004 Hubble estimates only marginally agree with the 2007 infrared measurements by the Spitzer Space Telescope that suggest a higher albedo (0.19) and consequently a smaller diameter (+206.7
−189.6 km). 844.4 Adopting a Uranian satellite limb darkening profile suggests that the 2004 Hubble size estimate for Quaoar was approximately 40 percent too large, and that a more proper estimate would be about 900 km. In 2010, Quaoar was estimated to be about in diameter, using a weighted average of Spitzer and corrected Hubble estimates. 890 km In observations of the object's shadow as it occulted an unnamed 16th-magnitude star on 4 May 2011, Quaoar was estimated to be 1,170 km (730 mi) in diameter. Measurements from the Herschel Space Observatory in 2013 suggested that Quaoar has a diameter of 1,070 km (660 mi). Quaoar's diameter was later revised to ±5 km after it occulted a 15.8 magnitude star in that same year. 1100
In 2004, signs of crystalline ice were found on Quaoar, indicating that the temperature rose to at least 110 K (−163 °C) sometime in the last ten million years. Speculation began as to what could have caused Quaoar to heat up from its natural temperature of 55 K (−218.2 °C). Some have theorized that a barrage of mini-meteors may have raised the temperature, but the most discussed theory speculates that cryovolcanism may be occurring, spurred by the decay of radioactive elements within Quaoar's core. Since then (2006), crystalline water ice was also found on Haumea, but present in larger quantities and thought to be responsible for the very high albedo of that object (0.7). More precise observations of Quaoar's near infrared spectrum in 2007 indicated the presence of small quantities (5%) of solid methane and ethane. Given its boiling point of 112 K (−161 °C), methane is a volatile ice at average surface temperatures of Quaoar, unlike water ice or ethane. Both models and observations suggest that only a few larger bodies (Pluto, Eris, and Makemake) can retain the volatile ices whereas the dominant population of small TNOs lost them. Quaoar, with only small amounts of methane, appears to be in an intermediary category.
Orbit and rotationEdit
Quaoar orbits at about 43.7 astronomical units (6.54×109 km; 4.06×109 mi) from the Sun with an orbital period of 288.8 years. Quaoar has a low orbital eccentricity of 0.0396, meaning its orbit is nearly circular. Its orbit is moderately inclined to the ecliptic at approximately 8 degrees, typical for the population of small classical Kuiper belt objects (KBOs) but exceptional among large KBOs. Quaoar is not significantly perturbed by Neptune unlike Pluto, which is in 2:3 orbital resonance with Neptune (Pluto orbits the Sun twice for every three orbits completed by Neptune). Quaoar is the largest body that is classified as a cubewano, or classical Kuiper belt object, by both the Minor Planet Center and the Deep Ecliptic Survey (although the dwarf planet Makemake, which is larger, is also classified as a cubewano). Quaoar occasionally moves closer to the Sun than Pluto, as Pluto's aphelion (farthest distance to the Sun) is beyond and below Quaoar's orbit. In 2008, Quaoar was only 14 AU from Pluto, which made it the closest large body to Pluto as of 2019. Quaoar's rotation period is uncertain, and two possible rotation periods of Quaoar are given (8.64 hours or 17.68 hours). Derived from the rotational light curves of Quaoar observed on March through June 2003, its rotation period is measured to be 17.6788 hours.
|Discovered by||Michael E. Brown|
|Discovery date||February 22, 2007|
|MPC designation||(50000) Quaoar I|
|S/2006 (50000) 1|
Quaoar has one known moon, Weywot (full designation (50000) Quaoar I Weywot). Discovered by Michael Brown and T.A. Suer using images acquired by the Hubble Space Telescope on 14 February 2006, its existence was announced in an IAU Circular notice published on 27 February 2007. The satellite was found at 0.35 arcseconds from Quaoar with an apparent magnitude difference of 5.6. Upon discovery, Weywot was issued a provisional designation, S/2006 (50000) 1. Brown left the choice of a name up to the Tongva (whose creator god Quaoar had been named after), who chose the sky god Weywot, son of Quaoar. The naming of Weywot was officially announced in a Minor Planet Circular notice published on 4 October 2009. It was thought that Weywot may have originated from a collision with Quaoar and another large Kuiper belt object.
Two possible orbits for Weywot have been determined from the observations: the first is a prograde orbit with an orbital inclination of 14 degrees, the second a retrograde orbit with an orbital inclination of 30 degrees (150 degrees); the other parameters are very similar between the two orbits. Weywot orbits at a distance of 14,500 km (9,000 mi) from Quaoar and has an orbital eccentricity of about 0.14, it completes one orbit in about 12.5 days. Weywot is estimated to be 81 km (50 mi) in diameter, based on observations with the Herschel Space Observatory in 2013. Prior to the Herschel Space Observatory measurements, Weywot was measured be about 74 km (1⁄12 of Quaoar) according to its apparent magnitude, under the assumption that Weywot has an equal albedo and density to Quaoar. Weywot is estimated to only have 1⁄2000 the mass of Quaoar.
It was calculated that a flyby mission to Quaoar could take 13.57 years using a Jupiter gravity assist, based on launch dates of 25 December 2016, 22 November 2027, 22 December 2028, 22 January 2030 or 20 December 2040. Quaoar would be 41 to 43 AU from the Sun when the spacecraft arrives. In July 2016, the Long Range Reconnaissance Imager (LORRI) aboard the New Horizons spacecraft took a sequence of four images of Quaoar from a distance of about 14 AU. Pontus C. Brandt at Johns Hopkins Applied Physics Laboratory and his colleagues have studied an interstellar probe that would potentially fly by Quaoar in the 2030s before continuing to the interstellar medium. Quaoar has been chosen as a flyby target for such a mission particularly for its escaping methane atmosphere and possible cryovolcanism, as well as its close proximity to the heliospheric nose.
- Brown's website gives a three-syllable pronunciation, //, as an approximation of the Tongva pronunciation [ˈkʷaʔuwar]. However, his students pronounce it with two syllables, //, reflecting the usual English spelling and pronunciation of the deity, Kwawar.
- Charon's mass is ±0.015)×1021 kg(1.586 while Quaoar's mass is ±0.1)×1021 kg. (1.4 Both values are approximately similar, though Charon is slightly more massive. In a similar case, Charon's diameter is ±1 km while Quaoar's diameter is 1212±5 km, being slightly smaller than Charon. 1110
- "50000 Quaoar (2002 LM60)". Minor Planet Center. Retrieved 30 November 2017.
- Schmadel, Lutz D. (2007). "(50000) Quaoar". Dictionary of Minor Planet Names – (50000) Quaoar. Springer Berlin Heidelberg. p. 895. doi:10.1007/978-3-540-29925-7_10041. ISBN 978-3-540-00238-3.
- "JPL Small-Body Database Browser: 50000 Quaoar (2002 LM60)" (2018-05-25 last obs.). Jet Propulsion Laboratory. Retrieved 27 February 2018.
- Buie, Marc W. (2006-05-17). "Orbit Fit and Astrometric record for 50000". SwRI (Space Science Department). Retrieved 27 February 2018.
- "MPEC 2008-O05 : Distant Minor Planets (2008 Aug. 2.0 TT)". IAU Minor Planet Center. Harvard-Smithsonian Center for Astrophysics. 17 July 2008. Retrieved 27 February 2018.
- Daniel W. E. Green (2007-02-22). "IAUC 8812: Sats of 2003 AZ84, (50000), (55637), (90482)". International Astronomical Union Circular. Retrieved 2011-07-05.
- Braga-Ribas, F.; Sicardy, B.; Ortiz, J. L.; Lellouch, E.; Tancredi, G.; Lecacheux, J.; et al. (August 2013). "The Size, Shape, Albedo, Density, and Atmospheric Limit of Transneptunian Object (50000) Quaoar from Multi-chord Stellar Occultations". The Astrophysical Journal. 773 (1): 13. Bibcode:2013ApJ...773...26B. doi:10.1088/0004-637X/773/1/26. Retrieved 27 February 2018.
- Fornasier, S.; Lellouch, E.; Müller, T.; Santos-Sanz, P.; Panuzzo, P.; Kiss, C.; et al. (July 2013). "TNOs are Cool: A survey of the trans-Neptunian region. VIII. Combined Herschel PACS and SPIRE observations of nine bright targets at 70-500 µm". Astronomy and Astrophysics. 555: 22. arXiv:1305.0449v2. Bibcode:2013A&A...555A..15F. doi:10.1051/0004-6361/201321329. Retrieved 27 February 2018.
- Fraser, Wesley C.; Batygin, Konstantin; Brown, Michael E.; Bouchez, Antonin (January 2013). "The mass, orbit, and tidal evolution of the Quaoar-Weywot system". Icarus. 222 (1): 357–363. arXiv:1211.1016. Bibcode:2013Icar..222..357F. doi:10.1016/j.icarus.2012.11.004.
- Fraser, Wesley C.; Brown, Michael E. (May 2010). "Quaoar: A Rock in the Kuiper Belt". The Astrophysical Journal. 714 (2): 1547–1550. arXiv:1003.5911. Bibcode:2010ApJ...714.1547F. doi:10.1088/0004-637X/714/2/1547.
- "LCDB Data for (50000) Quaoar". Asteroid Lightcurve Database (LCDB). Retrieved 30 November 2017.
- Tegler, Stephen C. (1 February 2007). "Kuiper Belt Object Magnitudes and Surface Colors". Archived from the original on 2006-09-01. Retrieved 27 February 2018.
- "AstDys (50000) Quaoar Ephemerides". Department of Mathematics, University of Pisa, Italy. Retrieved 2009-03-16.
- Crystalline Ice on Kuiper Belt Object (50000) Quaoar – article about crystalline ice on Quaoar
- Schaller, E. L.; Brown, M. E. (November 2007). "Detection of Methane on Kuiper Belt Object (50000) Quaoar". The Astrophysical Journal. 670 (1): L49–L51. arXiv:0710.3591. Bibcode:2007ApJ...670L..49S. doi:10.1086/524140.
- Chad Trujillo. "Frequently Asked Questions About Quaoar". Retrieved 30 November 2017.
- Brown, Michael E. (7 December 2010). "Chapter Five: An Icy Nail". How I Killed Pluto and Why It Had It Coming. Spiegel & Grau. pp. 63–85. ISBN 0-385-53108-7.
- Foust, Jeff (7 October 2002). "Giant Kuiper Belt object discovered". spaceflightnow.com. Retrieved 26 March 2019.
- Howell, Elizabeth (9 May 2014). "Quaoar: Planetoid Beyond Pluto". space.com. Retrieved 14 March 2019.
- "MPC 41805" (PDF). The Minor Planet Circulars/Minor Planets and Comets. 9 January 2001. Retrieved 15 March 2019.
- "How Minor Planets are Named". IAU – International Astronomical Union. 2005. Archived from the original on 16 February 2006. Retrieved 5 January 2017.
- Jewitt, D.C.; J. Luu (2004). "Crystalline water ice on the Kuiper belt object (50000) Quaoar". Nature. 432 (7018): 731–3. Bibcode:2004Natur.432..731J. doi:10.1038/nature03111. PMID 15592406.. Reprint on Jewitt's site (pdf)
- Brown, Michael E. "The Largest Kuiper Belt Objects" (PDF). Retrieved 14 March 2019.
- Hussmann, Hauke; Sohl, Frank; Spohn, Tilman (November 2006). "Subsurface oceans and deep interiors of medium-sized outer planet satellites and large trans-neptunian objects". Icarus. 185 (1): 258–273. Bibcode:2006Icar..185..258H. doi:10.1016/j.icarus.2006.06.005.
- Fraser, Wesley C.; Trujillo, Chad; Stephens, Andrew W.; Gimeno, German; Brown, Michael E.; Gwyn, Stephen; Kavelaars, J. J. (August 2013). "Limits on Quaoar's Atmosphere". The Astrophysical Journal Letters. 774 (2). arXiv:1308.2230. doi:10.1088/2041-8205/774/2/L18. Retrieved 26 March 2019.
- Brown, Michael E. "The-Dwarf-Planets". California Institute of Technology. Retrieved 27 February 2018.
- "The IAU draft definition of "planet" and "plutons"". IAU. August 2006. Retrieved 27 February 2018.
- Brown, Michael E. "How many dwarf planets are there in the outer solar system?". California Institute of Technology. Retrieved 27 February 2018.
- Tancredi, Gonzalo; Favre, Sofía (June 2008). "Which are the dwarfs in the Solar System?" (PDF). Icarus. 195 (2): 851–862. Bibcode:2008Icar..195..851T. doi:10.1016/j.icarus.2007.12.020. Retrieved 27 February 2018.
- George Musser (2009-10-13). "What do we really know about the Kuiper Belt? Fifth dispatch from the annual planets meeting". Scientific American blog. Archived from the original on 14 October 2009. Retrieved 2009-10-13.
- Ron Cowen (2009-01-04). "On the Fringe". ScienceNews. Archived from the original on 7 January 2010. Retrieved 2010-01-04.
- Brown, Michael E.; Trujillo, Chadwick A. (April 2004). "Direct Measurement of the Size of the Large Kuiper Belt Object (50000) Quaoar" (PDF). The Astronomical Journal. 127 (4): 2413–2417. Bibcode:2004AJ....127.2413B. doi:10.1086/382513. Retrieved 27 February 2018.
- Stansberry, J.; Grundy, W.; Brown, M.; Cruikshank, D.; Spencer, J.; Trilling, D.; et al. (December 2007). "Physical Properties of Kuiper Belt and Centaur Objects: Constraints from the Spitzer Space Telescope". The Solar System Beyond Neptune: 161–179. arXiv:astro-ph/0702538. Bibcode:2008ssbn.book..161S.
- Stern, S. A.; Grundy, W.; McKinnon, W. B.; Weaver, H. A.; Young, L. A. (15 December 2017). "The Pluto System After New Horizons". arXiv:1712.05669 [astro-ph.EP].
- Braga-Ribas et al. 2011, "Stellar Occultations by TNOs: the January 08, 2011 by (208996) 2003 AZ84 and the May 04, 2011 by (50000) Quaoar", EPSC Abstracts, vol. 6
- Trujillo; Brown; Barkume; Schaller; Rabinowitz (2007). "The Surface of 2003EL61 in the Near Infrared". The Astrophysical Journal. 655 (2): 1172–1178. arXiv:astro-ph/0601618. Bibcode:2007ApJ...655.1172T. doi:10.1086/509861.
- "50000 Quaoar distance (AU) from Pluto". Archived from the original on 25 February 2012. Retrieved 21 November 2008.
- Ortiz, J. L.; Gutiérrez, P. J.; Sota, Alfredo; Casanova, Casa (2003). "Rotational brightness variations in Trans-Neptunian Object 50000 Quaoar". ResearchGate. doi:10.1051/0004-6361:20031253. Retrieved 15 March 2019.
- Wm. Robert Johnston (21 September 2014). "(50000) Quaoar". Johnston's Archive. Retrieved 26 May 2009.
- Distant EKO The Kuiper Belt Electronic newsletter, March 2007
- "Heavenly Bodies and the People of the Earth", Nick Street, Search Magazine, July/August 2008
- Minor Planet Circular 67220 naming of Weywot
- McGranaghan, R.; Sagan, B.; Dove, G.; Tullos, A.; Lyne, J. E.; Emery, J. P. (2011). "A Survey of Mission Opportunities to Trans-Neptunian Objects". Journal of the British Interplanetary Society. 64: 296–303. Bibcode:2011JBIS...64..296M.
- "New Horizons Spies a Kuiper Belt Companion". The Johns Hopkins University Applied Physics Laboratory LLC. 31 August 2016. Retrieved 7 September 2016.
- "Triennial Earth Sun-Summit". Retrieved 24 July 2018.
- TVIW (4 November 2017), 22. Humanity's First Explicit Step in Reaching Another Star: The Interstellar Probe Mission, retrieved 24 July 2018
- Runyon, Kirby Daniel; Mandt, Kathleen; Stern, S. Alan; Brandt, Pontus C.; McNutt, Ralph L. (12 December 2018). "SH32C-10: Kuiper Belt Planet Geoscience from Interstellar Probe". Retrieved 30 March 2019.
- Frequently Asked Questions About Quaoar
- E. L. Schaller, M. E. Brown, "Detection of Additional Members of the Haumea Collisional Family via Infrared Spectroscopy". AAS DPS conference, 13 Oct. 2008; also podcast: Dwarf Planet Haumea (Darin Ragozzine) at 3′18″
|Wikimedia Commons has media related to Quaoar.|
- Quaoar discoverers' webpage
- Quaoar could have hit a bigger Pluto-sized body at high speeds (Video Credit: Craig Agnor, E. Asphaug)
- Data at Johnston's Archive
- Chilly Quaoar had a warmer past – Nature.com article
- Cryovolcanism on Charon and other Kuiper Belt Objects
- AstorbDB, Lowell Observatory
- 50000 Quaoar at the JPL Small-Body Database