469219 Kamoʻoalewa

469219 Kamoʻoalewa
Orbit of Kamoʻoalewa in the inner Solar System
Discovery
Discovered byPan-STARRS
Discovery siteHaleakala Observatory
Discovery date27 April 2016
Designations
(469219) 2016 HO3
Pronunciation/kəˌmʔəˈlɛvə/
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 arc20.00 yr (7,306 d)
Aphelion1.10373 AU
Perihelion0.89816 AU
1.00094 AU
Eccentricity0.10269
(964 wrt Earth)
1.0014 yr (365.77 d)
175.153°
0° 59m 3.192s / day
Inclination7.79605°
65.7907°
305.0478°
Earth MOID0.0311 AU (12.1 LD)
Physical characteristics
  • 0.041 km (calculated)
  • 0.04–0.10 km
0.467±0.008 h
0.20 (assumed)
S (assumed)
  • 24.33
  • 24.3

    469219 Kamoʻoalewa (/kəˌmʔəˈlɛvə/), 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.