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Atira asteroid

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(Redirected fromList of Apohele asteroids)
Group of near-Earth asteroids
Common orbital subgroups ofNear-Earth Objects (NEOs)

Atira asteroids/əˈtɪrə/ orApohele asteroids, also known asinterior-Earth objects (IEOs), areNear-Earth objects whose orbits are entirely confined withinEarth's orbit;[1] that is, their orbit has anaphelion (farthest point from the Sun) smaller than Earth'sperihelion (nearest point to the Sun), which is 0.983astronomical units (AU). Atira asteroids are by far the least numerous group ofnear-Earth objects, compared to the more populousAten,Apollo andAmor asteroids.[2]

History

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Naming

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There is no official name for the class commonly referred as Atira asteroids. The term "Apohele asteroids" was proposed by the discoverers of1998 DK36,[3] after theHawaiian word fororbit, fromapo[ˈɐpo] 'circle' andhele[ˈhɛlɛ] 'to go'.[4] This was suggested partly because of its similarity to the wordsaphelion (apoapsis) andhelios.[a] Other authors adopted the designation "Inner Earth Objects" (IEOs).[5] Following the general practice to name a new class of asteroids for the first recognized member of that class, which in this case was163693 Atira, the designation of "Atira asteroids" was largely adopted by the scientific community, including byNASA.[6][1]

Discovery and observation

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Their location inside the Earth's orbit makes Atiras very difficult to observe, as from Earth's perspective they are close to theSun and therefore 'drowned out' by the Sun's overpowering light.[7] This means that Atiras can usually only be seen duringtwilight.[7] The first documented twilight searches for asteroids inside Earth's orbit were performed by astronomerRobert Trumpler over the early 20th century, but he failed to find any.[7]

The first confirmed Atira asteroid was 163693 Atira in 2003, discovered by the Lincoln Laboratory Near Earth Asteroid Research Team.[8] As of January 2025[update], there are 34 known Atiras, two of which are named, nine of which have received anumbered designation, and seven of which arepotentially hazardous objects.[2][9][10]

Origins

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Most Atira asteroids originated in theasteroid belt and were driven to their current locations as a result ofgravitational perturbation, as well as other causes such as theYarkovsky effect.[7] A number of known Atiras could be fragments or former moons of larger Atiras as they exhibit an unusually high level of orbital correlation.[11]

Orbits

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Atiras do not cross Earth's orbit and are not immediateimpact event threats, but their orbits may beperturbed outward by a close approach to either Mercury or Venus and become Earth-crossing asteroids in the future. The dynamics of many Atira asteroids resemble the one induced by theKozai-Lidov mechanism,[b] which contributes to enhanced long-term orbital stability, since there is nolibration of the perihelion.[12][13]

Exploration

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A 2017 study published in the journalAdvances in Space Research proposed a low-costspace probe be sent to study Atira asteroids, citing the difficulty in observing the group from Earth as a reason to undertake the mission.[14] The study proposed that the mission would be powered byspacecraft electric propulsion and would follow a path designed toflyby as many Atira asteroids as possible. The probe would also attempt to discover new NEO's that may pose a threat to Earth.[14]

Related asteroid groups

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ꞌAylóꞌchaxnim asteroids

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ꞌAylóꞌchaxnim asteroids, which had been provisionally nicknamed "Vatira" asteroids before the first was discovered,[c] are a subclass of Atiras that orbit entirely interior to the orbit ofVenus, aka 0.718 AU.[16] Despite their orbits placing them at a significant distance from Earth, they are still classified as near-Earth objects.[17] Observations suggest that ꞌAylóꞌchaxnim asteroids frequently have their orbits altered into Atira asteroids and vice versa.[18]

First formally theorised to exist by William F. Bottke and Gianluca Masi in 2002 and 2003,[19][20] the first and to date only such asteroid found is594913 ꞌAylóꞌchaxnim,[21][22] which was discovered on 4 January 2020 by theZwicky Transient Facility. As the archetype, it subsequently gave its name to the class.[16] It has an aphelion of only 0.656 AU, the smallest of any known asteroid.[9][12]

Vulcanoids

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Main article:Vulcanoid

No asteroids have yet been discovered to orbit entirely inside the orbit ofMercury (q = 0.307 AU). Such hypothetical asteroids would likely be termedvulcanoids, although the term often refers to asteroids which more specifically have remained in the intra-Mercurian region over the age of theSolar System.[15]

Members

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The following table lists the known and suspected Atiras as of November 2025[update]. 594913 ꞌAylóꞌchaxnim, due to itsunique classification, has been highlighted in pink. Theinterior planets Mercury and Venus have been included for comparison as grey rows.

List of known and suspected Atiras as of October 2025 (Q < 0.983 AU)[9]
DesignationPerihelion
(AU)
Semi-major axis
(AU)
Aphelion
(AU)
EccentricityInclination
(°)
Period
(days)
Observation arc
(days)
(H)Diameter(A)
(m)
DiscovererRef
Mercury
(for comparison)
0.3070.38710.4670.20567.0188NA−0.64,879,400NA
Venus
(for comparison)
0.7180.72330.7280.00683.39225NA−4.512,103,600NA
1998 DK360.4040.69230.9800.41602.02210125.035David J. TholenMPC · JPL
163693 Atira0.5020.74100.9800.322125.62233776616.44800±500(B)LINEARList
MPC · JPL
(164294) 2004 XZ1300.3370.61760.8980.45452.95177356420.5290David J. TholenList
MPC · JPL
(434326) 2004 JG60.2980.63520.9730.531118.94185622718.5710LONEOSList
MPC · JPL
(413563) 2005 TG450.4280.68130.9350.372323.33205703117.61,100Catalina Sky SurveyList
MPC · JPL
2013 JX28
(aka2006 KZ39)
0.2620.60080.9400.564110.76170511020.1340Mount Lemmon Survey
Pan-STARRS
MPC · JPL
(613676) 2006 WE40.6410.78480.9280.182924.77254499518.9590Mount Lemmon SurveyList
MPC · JPL
(418265) 2008 EA320.4280.61590.8040.305028.26177581616.51,800Catalina Sky SurveyList
MPC · JPL
(481817) 2008 UL900.4310.69500.9590.379924.31212553718.6680Mount Lemmon SurveyList
MPC · JPL
2010 XB110.2880.61810.9480.533829.88178518319.7410Mount Lemmon SurveyMPC · JPL
2012 VE460.4550.71310.9710.36126.67220222520.2320Pan-STARRSMPC · JPL
2013 JX280.2620.60080.9400.564210.77170511020.1340Mount Lemmon SurveyMPC · JPL
2013 TQ50.6530.77370.8940.155716.40249403119.9380Mount Lemmon SurveyMPC · JPL
2014 FO470.5480.75220.9560.271119.20238325920.2320Mount Lemmon SurveyMPC · JPL
2015 DR2150.3520.66660.9810.47154.06199260220.5280Pan-STARRSMPC · JPL
2017 XA10.6460.80940.9730.201617.18266108421.3200Pan-STARRSMPC · JPL
(678861) 2017 YH
(aka2016 XJ24)
0.3290.63460.9410.482319.85185298018.1840Spacewatch
ATLAS
MPC · JPL
2018 JB30.4850.68320.8820.290440.39206332117.71,020Catalina Sky SurveyMPC · JPL
2019 AQ30.4040.58860.7740.314347.22165299617.51,120Zwicky Transient FacilityMPC · JPL
2019 LF60.3170.55540.7940.429329.50151110817.31,230Zwicky Transient FacilityMPC · JPL
594913 ꞌAylóꞌchaxnim0.4570.55530.6540.177215.87151182716.21,700Zwicky Transient FacilityMPC · JPL
2020 HA100.6920.81970.9470.155349.65271404319.0560Mount Lemmon SurveyMPC · JPL
2020 OV10.4760.63760.8000.254132.58186117918.7640Zwicky Transient FacilityMPC · JPL
2021 BS10.3960.59840.8000.337631.73169156418.6670Zwicky Transient FacilityMPC · JPL
2021 LJ40.4180.67640.9350.38209.82203286020.1340Scott S. SheppardMPC · JPL
2021 PB20.6100.71740.8250.150024.83222444818.8610Zwicky Transient FacilityMPC · JPL
2021 PH270.1330.46180.7900.711531.94115255217.71,020Scott S. SheppardMPC · JPL
2021 VR30.3130.53390.7550.413918.07143171618.0890Zwicky Transient FacilityMPC · JPL
2022 BJ80.5900.78530.9810.248715.8325481619.4470Kitt Peak-BokMPC · JPL
2023 EL0.5810.77140.9610.246213.88247286419.2520Scott S. SheppardMPC · JPL
2023 EY20.3980.60360.8090.339835.4717132519.8400Kitt Peak-BokMPC · JPL
2023 KQ50.8050.87220.9390.077167.43298331818.8630Pan-STARRSMPC · JPL
2023 EY20.3980.60330.8090.397835.55171619.9370Kitt Peak-BokMPC · JPL
2023 WK30.3220.64420.9660.499824.47189360620.5290Moonbase South ObservatoryMPC · JPL
2024 UM90.8030.86090.9190.067221.17292175320.6260Mount Lemmon SurveyMPC · JPL
2024 WD190.5720.67950.7870.15793.792053221.3190Subaru Telescope, MaunakeaMPC · JPL
2025 GN10.1360.46200.7880.705132.841158820.1350Cerro Tololo-DECamMPC · JPL
2025 LP0.6230.74370.8640.162433.3423411019.6430Cerro Tololo-DECamMPC · JPL
2025 SC790.2730.49580.7190.449916.771281018.8620Cerro Tololo-DECamMPC · JPL
(A) All diameter estimates are based on an assumedalbedo of 0.14 (except 163693 Atira, for which the size has been directly measured; and 594913 ꞌAylóꞌchaxnim, for which an albedo of 0.22 is assumed based on its knownstony composition)
(B) Binary asteroid

See also

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Notes

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  1. ^Cambridge Conference Correspondence, (2):WHAT'S IN A NAME: APOHELE = APOAPSIS & HELIOSfrom Dave Tholen, Cambridge Conference Network (CCNet) DIGEST, 9 July 1998
    Benny,
    Duncan Steel has already brought up the subject of a class name for objects with orbits interior to the Earth's. To be sure, we've already given that subject some thought. I also wanted a word that begins with the letter "A", but there was some desire to work Hawaiian culture into it. I consulted with a friend of mine that has a master's degree in the Hawaiian language, and she recommended "Apohele", the Hawaiian word for "orbit". I found that an interesting suggestion, because of the similarity to fragments of "apoapsis" and "helios", and these objects would have their apoapsis closer to the Sun than the Earth's orbit. By the way, the pronunciation would be like "ah-poe-hey-lay". Rob Whiteley has suggested "Aliʻi", which refers to the Hawaiian elite, which provides a rich bank of names for discoveries in this class, such as Kuhio, Kalakaua, Kamehameha, Liliuokalani, and so on. Unfortunately, I think theokina (the reverse apostrophe) would be badly treated by most people.
    I wasn't planning to bring it up at this stage, but because Duncan has already done so, here's what we've got on the table so far. I'd appreciate some feedback on the suggestions.
    --Dave
  2. ^Namely, they have coupledoscillations in orbitaleccentricity andinclination
  3. ^The nickname "Vatira" combined "Venus" with "Atira".[15]

References

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  1. ^abBaalke, Ron."Near-Earth Object Groups".Jet Propulsion Laboratory.NASA. Archived fromthe original on 2 February 2002. Retrieved11 November 2016.
  2. ^abChodas, Paul; Khudikyan, Shakeh; Chamberlin, Alan (14 May 2019)."Near-Earth Asteroid Discovery Statistics".Jet Propulsion Laboratory.NASA. Retrieved25 May 2019.
  3. ^Tholen, David J.; Whiteley, Robert J. (September 1998). "Results From NEO Searches At Small Solar Elongation".American Astronomical Society.30: 1041.Bibcode:1998DPS....30.1604T.
  4. ^(Ulukau Hawaiian Electronic Library)
  5. ^Michel, Patrick;Zappalà, Vincenzo; Cellino, Alberto; Tanga, Paolo (February 2000). "NOTE: Estimated Abundance of Atens and Asteroids Evolving on Orbits between Earth and Sun".Icarus.143 (2).Harcourt:421–424.Bibcode:2000Icar..143..421M.doi:10.1006/icar.1999.6282.
  6. ^Ribeiro, Anderson O.; et al. (1 June 2016)."Dynamical study of the Atira group of asteroids".Monthly Notices of the Royal Astronomical Society.458 (4):4471–4476.doi:10.1093/mnras/stw642.
  7. ^abcdYe, Quanzhi; et al. (2020)."A Twilight Search for Atiras, Vatiras, and Co-orbital Asteroids: Preliminary Results".The Astronomical Journal.159 (2).IOP Publishing: 70.arXiv:1912.06109.Bibcode:2020AJ....159...70Y.doi:10.3847/1538-3881/ab629c.S2CID 209324310.
  8. ^"Minor Planet Circular 61768"(PDF). Minor Planet Center. Retrieved2024-08-22.
  9. ^abc"JPL Small-Body Database Search Engine: Q < 0.983 (AU)".JPL Solar System Dynamics.NASA. Retrieved30 December 2017.
  10. ^"Small-Body Database Query".Solar System Dynamics – Jet Propulsion Laboratory. NASA – California Institute of Technology. Retrieved2025-01-17.
  11. ^de la Fuente Marcos, Carlos; de la Fuente Marcos, Raúl (20 December 2023)."Baked before Breaking into Bits: Evidence for Atira-type Asteroid Splits".Research Notes of the American Astronomical Society.7 (12): 278 (3 pages).Bibcode:2023RNAAS...7..278D.doi:10.3847/2515-5172/ad16de.
  12. ^abde la Fuente Marcos, Carlos; de la Fuente Marcos, Raúl (11 June 2018)."Kozai--Lidov Resonant Behavior Among Atira-class Asteroids".Research Notes of the AAS.2 (2): 46.arXiv:1806.00442.Bibcode:2018RNAAS...2...46D.doi:10.3847/2515-5172/aac9ce.S2CID 119239031.
  13. ^de la Fuente Marcos, Carlos; de la Fuente Marcos, Raúl (1 August 2019)."Understanding the evolution of Atira-class asteroid 2019 AQ3, a major step towards the future discovery of the Vatira population".Monthly Notices of the Royal Astronomical Society.487 (2):2742–2752.arXiv:1905.08695.Bibcode:2019MNRAS.487.2742D.doi:10.1093/mnras/stz1437.S2CID 160009327.
  14. ^abDi Carlo, Marilena; Martin, Juan Manuel Romero; Gomez, Natalia Ortiz; Vasile, Massimiliano (1 April 2017)."Optimised low-thrust mission to the Atira asteroids".Advances in Space Research.59 (7).Elsevier:1724–1739.Bibcode:2017AdSpR..59.1724D.doi:10.1016/j.asr.2017.01.009.S2CID 116216149. RetrievedFebruary 9, 2023.
  15. ^abGreenstreet, Sarah; Ngo, Henry; Gladman, Brett (January 2012)."The orbital distribution of Near-Earth Objects inside Earth's orbit"(PDF).Icarus.217 (1).Elsevier:355–366.Bibcode:2012Icar..217..355G.doi:10.1016/j.icarus.2011.11.010.hdl:2429/37251.We have provisionally named objects with 0.307 < Q < 0.718 AU Vatiras, because they are Atiras which are decoupled from Venus. Provisional because it will be abandoned once the first discovered member of this class will be named.
  16. ^abBolin, Bryce T.; et al. (November 2022)."The discovery and characterization of (594913) 'Ayló'chaxnim, a kilometre sized asteroid inside the orbit of Venus"(PDF).Monthly Notices of the Royal Astronomical Society: Letters.517 (1):L49 –L54.doi:10.1093/mnrasl/slac089. Retrieved1 October 2022.
  17. ^"JPL Small-Body Database Browser: 2020 AV2".Jet Propulsion Laboratory.NASA.Archived from the original on 11 January 2020. Retrieved9 January 2020.
  18. ^Lai, H.T.; Ip, W.H. (4 December 2022)."The orbital evolution of Atira asteroids".Monthly Notices of the Royal Astronomical Society.517 (4):5921–5929.arXiv:2210.09652.doi:10.1093/mnras/stac2991. RetrievedFebruary 9, 2023.
  19. ^Bottke, William F.; et al. (April 2002)."Debiased Orbital and Absolute Magnitude Distribution of the Near-Earth Objects".Icarus.156 (2):399–433.Bibcode:2002Icar..156..399B.doi:10.1006/icar.2001.6788.
  20. ^Masi, Gianluca (June 2003)."Searching for inner-Earth objects: a possible ground-based approach".Icarus.163 (2):389–397.Bibcode:2003Icar..163..389M.doi:10.1016/S0019-1035(03)00082-4.
  21. ^Masi, Gianluca (9 January 2020)."2020 AV2, the first intervenusian asteroid ever discovered: an image – 08 Jan. 2020". Virtual Telescope Project. Retrieved9 January 2020.
  22. ^Popescu, Marcel M.; et al. (11 August 2020)."Physical characterization of 2020 AV2, the first known asteroid orbiting inside Venus orbit".Monthly Notices of the Royal Astronomical Society.496 (3):3572–3581.arXiv:2006.08304.Bibcode:2020MNRAS.496.3572P.doi:10.1093/mnras/staa1728.S2CID 219687045. Retrieved8 July 2020.

External links

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