
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]
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]
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]
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]
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]
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]
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]
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]
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.
| Designation | Perihelion (AU) | Semi-major axis (AU) | Aphelion (AU) | Eccentricity | Inclination (°) | Period (days) | Observation arc (days) | (H) | Diameter(A) (m) | Discoverer | Ref |
|---|---|---|---|---|---|---|---|---|---|---|---|
| Mercury (for comparison) | 0.307 | 0.3871 | 0.467 | 0.2056 | 7.01 | 88 | NA | −0.6 | 4,879,400 | NA | |
| Venus (for comparison) | 0.718 | 0.7233 | 0.728 | 0.0068 | 3.39 | 225 | NA | −4.5 | 12,103,600 | NA | |
| 1998 DK36 | 0.404 | 0.6923 | 0.980 | 0.4160 | 2.02 | 210 | 1 | 25.0 | 35 | David J. Tholen | MPC · JPL |
| 163693 Atira | 0.502 | 0.7410 | 0.980 | 0.3221 | 25.62 | 233 | 7766 | 16.4 | 4800±500(B) | LINEAR | List MPC · JPL |
| (164294) 2004 XZ130 | 0.337 | 0.6176 | 0.898 | 0.4545 | 2.95 | 177 | 3564 | 20.5 | 290 | David J. Tholen | List MPC · JPL |
| (434326) 2004 JG6 | 0.298 | 0.6352 | 0.973 | 0.5311 | 18.94 | 185 | 6227 | 18.5 | 710 | LONEOS | List MPC · JPL |
| (413563) 2005 TG45 | 0.428 | 0.6813 | 0.935 | 0.3723 | 23.33 | 205 | 7031 | 17.6 | 1,100 | Catalina Sky Survey | List MPC · JPL |
| 2013 JX28 (aka2006 KZ39) | 0.262 | 0.6008 | 0.940 | 0.5641 | 10.76 | 170 | 5110 | 20.1 | 340 | Mount Lemmon Survey Pan-STARRS | MPC · JPL |
| (613676) 2006 WE4 | 0.641 | 0.7848 | 0.928 | 0.1829 | 24.77 | 254 | 4995 | 18.9 | 590 | Mount Lemmon Survey | List MPC · JPL |
| (418265) 2008 EA32 | 0.428 | 0.6159 | 0.804 | 0.3050 | 28.26 | 177 | 5816 | 16.5 | 1,800 | Catalina Sky Survey | List MPC · JPL |
| (481817) 2008 UL90 | 0.431 | 0.6950 | 0.959 | 0.3799 | 24.31 | 212 | 5537 | 18.6 | 680 | Mount Lemmon Survey | List MPC · JPL |
| 2010 XB11 | 0.288 | 0.6181 | 0.948 | 0.5338 | 29.88 | 178 | 5183 | 19.7 | 410 | Mount Lemmon Survey | MPC · JPL |
| 2012 VE46 | 0.455 | 0.7131 | 0.971 | 0.3612 | 6.67 | 220 | 2225 | 20.2 | 320 | Pan-STARRS | MPC · JPL |
| 2013 JX28 | 0.262 | 0.6008 | 0.940 | 0.5642 | 10.77 | 170 | 5110 | 20.1 | 340 | Mount Lemmon Survey | MPC · JPL |
| 2013 TQ5 | 0.653 | 0.7737 | 0.894 | 0.1557 | 16.40 | 249 | 4031 | 19.9 | 380 | Mount Lemmon Survey | MPC · JPL |
| 2014 FO47 | 0.548 | 0.7522 | 0.956 | 0.2711 | 19.20 | 238 | 3259 | 20.2 | 320 | Mount Lemmon Survey | MPC · JPL |
| 2015 DR215 | 0.352 | 0.6666 | 0.981 | 0.4715 | 4.06 | 199 | 2602 | 20.5 | 280 | Pan-STARRS | MPC · JPL |
| 2017 XA1 | 0.646 | 0.8094 | 0.973 | 0.2016 | 17.18 | 266 | 1084 | 21.3 | 200 | Pan-STARRS | MPC · JPL |
| (678861) 2017 YH (aka2016 XJ24) | 0.329 | 0.6346 | 0.941 | 0.4823 | 19.85 | 185 | 2980 | 18.1 | 840 | Spacewatch ATLAS | MPC · JPL |
| 2018 JB3 | 0.485 | 0.6832 | 0.882 | 0.2904 | 40.39 | 206 | 3321 | 17.7 | 1,020 | Catalina Sky Survey | MPC · JPL |
| 2019 AQ3 | 0.404 | 0.5886 | 0.774 | 0.3143 | 47.22 | 165 | 2996 | 17.5 | 1,120 | Zwicky Transient Facility | MPC · JPL |
| 2019 LF6 | 0.317 | 0.5554 | 0.794 | 0.4293 | 29.50 | 151 | 1108 | 17.3 | 1,230 | Zwicky Transient Facility | MPC · JPL |
| 594913 ꞌAylóꞌchaxnim | 0.457 | 0.5553 | 0.654 | 0.1772 | 15.87 | 151 | 1827 | 16.2 | 1,700 | Zwicky Transient Facility | MPC · JPL |
| 2020 HA10 | 0.692 | 0.8197 | 0.947 | 0.1553 | 49.65 | 271 | 4043 | 19.0 | 560 | Mount Lemmon Survey | MPC · JPL |
| 2020 OV1 | 0.476 | 0.6376 | 0.800 | 0.2541 | 32.58 | 186 | 1179 | 18.7 | 640 | Zwicky Transient Facility | MPC · JPL |
| 2021 BS1 | 0.396 | 0.5984 | 0.800 | 0.3376 | 31.73 | 169 | 1564 | 18.6 | 670 | Zwicky Transient Facility | MPC · JPL |
| 2021 LJ4 | 0.418 | 0.6764 | 0.935 | 0.3820 | 9.82 | 203 | 2860 | 20.1 | 340 | Scott S. Sheppard | MPC · JPL |
| 2021 PB2 | 0.610 | 0.7174 | 0.825 | 0.1500 | 24.83 | 222 | 4448 | 18.8 | 610 | Zwicky Transient Facility | MPC · JPL |
| 2021 PH27 | 0.133 | 0.4618 | 0.790 | 0.7115 | 31.94 | 115 | 2552 | 17.7 | 1,020 | Scott S. Sheppard | MPC · JPL |
| 2021 VR3 | 0.313 | 0.5339 | 0.755 | 0.4139 | 18.07 | 143 | 1716 | 18.0 | 890 | Zwicky Transient Facility | MPC · JPL |
| 2022 BJ8 | 0.590 | 0.7853 | 0.981 | 0.2487 | 15.83 | 254 | 816 | 19.4 | 470 | Kitt Peak-Bok | MPC · JPL |
| 2023 EL | 0.581 | 0.7714 | 0.961 | 0.2462 | 13.88 | 247 | 2864 | 19.2 | 520 | Scott S. Sheppard | MPC · JPL |
| 2023 EY2 | 0.398 | 0.6036 | 0.809 | 0.3398 | 35.47 | 171 | 325 | 19.8 | 400 | Kitt Peak-Bok | MPC · JPL |
| 2023 KQ5 | 0.805 | 0.8722 | 0.939 | 0.0771 | 67.43 | 298 | 3318 | 18.8 | 630 | Pan-STARRS | MPC · JPL |
| 2023 EY2 | 0.398 | 0.6033 | 0.809 | 0.3978 | 35.55 | 171 | 6 | 19.9 | 370 | Kitt Peak-Bok | MPC · JPL |
| 2023 WK3 | 0.322 | 0.6442 | 0.966 | 0.4998 | 24.47 | 189 | 3606 | 20.5 | 290 | Moonbase South Observatory | MPC · JPL |
| 2024 UM9 | 0.803 | 0.8609 | 0.919 | 0.0672 | 21.17 | 292 | 1753 | 20.6 | 260 | Mount Lemmon Survey | MPC · JPL |
| 2024 WD19 | 0.572 | 0.6795 | 0.787 | 0.1579 | 3.79 | 205 | 32 | 21.3 | 190 | Subaru Telescope, Maunakea | MPC · JPL |
| 2025 GN1 | 0.136 | 0.4620 | 0.788 | 0.7051 | 32.84 | 115 | 88 | 20.1 | 350 | Cerro Tololo-DECam | MPC · JPL |
| 2025 LP | 0.623 | 0.7437 | 0.864 | 0.1624 | 33.34 | 234 | 110 | 19.6 | 430 | Cerro Tololo-DECam | MPC · JPL |
| 2025 SC79 | 0.273 | 0.4958 | 0.719 | 0.4499 | 16.77 | 128 | 10 | 18.8 | 620 | Cerro Tololo-DECam | MPC · JPL |
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.