469219 Kamoʻoalewa
Orbit of Kamoʻoalewa in the inner Solar System | |
| Discovery | |
|---|---|
| Discovered by | Pan-STARRS |
| Discovery site | Haleakala Observatory |
| Discovery date | 27 April 2016 |
| Designations | |
| (469219) 2016 HO3 | |
| Pronunciation | /kəˌmoʊʔoʊəˈlɛvə/ Hawaiian: [kəˈmoʔowəˈlɛvə] |
Named after | Ka moʻo a lewa ("the oscillating fragment") |
| 2016 HO3 | |
| |
| Orbital characteristics | |
| Epoch 2024-Mar-31 (JD 2460400.5) | |
| Uncertainty parameter 0 | |
| Observation arc | 20.00 yr (7,306 d) |
| Aphelion | 1.10373 AU |
| Perihelion | 0.89816 AU |
| 1.00094 AU | |
| Eccentricity | 0.10269 (964 wrt Earth) |
| 1.0014 yr (365.77 d) | |
| 175.153° | |
| 0° 59m 3.192s / day | |
| Inclination | 7.79605° |
| 65.7907° | |
| 305.0478° | |
| Earth MOID | 0.0311 AU (12.1 LD) |
| Physical characteristics | |
| |
| 0.467±0.008 h | |
| 0.20 (assumed) | |
| S (assumed) | |
| |
469219 Kamoʻoalewa (/kəˌmoʊʔoʊəˈlɛvə/), provisionally designated 2016 HO3, is a very small elongated asteroid, fast rotator and near-Earth object of the Apollo group, approximately 40–100 meters (130–330 feet) in diameter. At present it is a quasi-satellite of Earth, and currently the second-smallest, closest, and most stable known such quasi-satellite (after 2023 FW13).
The asteroid was discovered by Pan-STARRS at Haleakala Observatory on 27 April 2016. Numerous proposed missions have since targeted the object, including a NASA solar-sail mission, a University of Colorado flyby and impact experiment, and was selected as a target for the Chinese ZhengHe project, which has developed into the Tianwen-2 mission. The chondritic simulants QLS-1, 2, and 3 have been developed by the Qian Xuesen Laboratory of Space Technology to better prepare for these missions. In an ambitious proposal, 469219 Kamo'oalewa is even considered for use as a space station for Earth-to-Mars travel.
The object's Earth-like orbit, proximity to the Earth-Moon system, higher spectral reddening to other asteroids, and similarity to space weathered lunar materials indicate that it is likely lunar ejecta. However, it might also be an S-type or L-type asteroid. Despite being most similar to weathered Apollo 14 and Luna 24 Lunar Mare soils, it is suggested to be from the lunar far-side highland crust crater, Giordano Bruno.
Orbital similarities suggest it is likely a co-orbital pair with 2000 WN10 or a broken up set including the other NEOs 2020 KZ2, 2020 PN1, and 2020 PP1.