2099 Öpik
Mars-crossing asteroid
From Wikipedia, the free encyclopedia
2099 Öpik, provisional designation 1977 VB, is a dark and eccentric asteroid and Mars-crosser from the inner regions of the asteroid belt, approximately 5.1 kilometers in diameter.
| Discovery[1] | |
|---|---|
| Discovered by | E. F. Helin |
| Discovery site | Palomar Obs. |
| Discovery date | 8 November 1977 |
| Designations | |
| (2099) Opik | |
Named after | Ernst Öpik (Estonian astronomer)[2] |
| 1977 VB · 1977 UL2 | |
| Mars-crosser[1][3] | |
| Orbital characteristics[1] | |
| Epoch 4 September 2017 (JD 2458000.5) | |
| Uncertainty parameter 0 | |
| Observation arc | 60.26 yr (22,009 days) |
| Aphelion | 3.1370 AU |
| Perihelion | 1.4710 AU |
| 2.3040 AU | |
| Eccentricity | 0.3616 |
| 3.50 yr (1,277 days) | |
| 148.76° | |
| 0° 16m 54.48s / day | |
| Inclination | 26.966° |
| 218.84° | |
| 159.18° | |
| Earth MOID | 0.4926 AU |
| Physical characteristics | |
| Dimensions | 5.12 km (calculated)[4] 5.17±1.35 km[5] |
| 6.4430±0.0002 h[6] 9.3 h[7] | |
| 0.05±0.06[5] 0.057 (assumed)[4] | |
| S (Tholen)[1] Ch (SMASS)[1] C (CALL)[4] B–V = 0.690[1] U–B = 0.350[1] | |
| 15.18[1][4] · 15.22[5] | |
The asteroid was discovered on 8 November 1977, by American astronomer Eleanor Helin at the Palomar Observatory in California, and named after Estonian astronomer Ernst Öpik.[3]
Orbit and classification
Öpik orbits the Sun in the inner main-belt at a distance of 1.5–3.1 AU once every 3 years and 6 months (1,277 days). Its orbit has an eccentricity of 0.36 and an inclination of 27° with respect to the ecliptic.[1] The first used precovery was taken at the discovering observatory in 1970, extending the asteroid's observation arc by 7 years prior to its discovery.[3]
Physical characteristics
Originally, the asteroid's spectral type was that of a bright S-type asteroid in the Tholen classification. More recently, it has been characterized as a dark Ch-type, a hydrated subtype of the carbonaceous C-type asteroids in the SMASS classification, which is in agreement with its low albedo (below).[1]
Diameter and albedo
According to the survey carried out by NASA's Wide-field Infrared Survey Explorer with its subsequent NEOWISE mission, Öpik measures 5.17 kilometers in diameter and its surface has an albedo of 0.05.[5] The Collaborative Asteroid Lightcurve Link assumes a standard albedo for carbonaceous asteroids of 0.057 and calculates a diameter of 5.12 kilometers with an absolute magnitude of 15.18.[4]
Rotation period
In 2005, a photometric lightcurve analysis by several astronomers including Pierre Antonini, rendered a rotation period of 6.4430±0.0002 hours and with a brightness amplitude of 0.21 in magnitude (U=2),[6] superseding the results of an observation from the 1990s that gave a longer period of 9.3 hours (U=2).[7]
Naming
This minor planet was named after Estonian astronomer and astrophysicist, Ernst Öpik (1893–1985), who has influenced many fields of astronomy during his 60-year long career. He is noted for developing the discipline of statistical celestial mechanics and for methods to estimate the lifetimes of planet-crossing asteroids. In the early 1950s, he calculated the impact probability of Mars-crossing asteroids with Mars, and concluded that a search for impact craters on Mars would be a fruitful. Fourteen years later, Martian craters were discovered by Mariner 4.[2] The official naming citation was published by the Minor Planet Center on 1 November 1978 (M.P.C. 4548).[8]