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Main-belt asteroid From Wikipedia, the free encyclopedia
4432 McGraw-Hill, provisional designation 1981 ER22, is a background asteroid from the inner regions of the asteroid belt, approximately 3 kilometers (2 miles) in diameter. It was discovered on 2 March 1981, by American astronomer Schelte Bus at the Siding Spring Observatory in Australia. The likely S-type asteroid was named for the McGraw-Hill Telescope located at Kitt Peak, Arizona.[1]
Discovery [1] | |
---|---|
Discovered by | S. J. Bus |
Discovery site | Siding Spring Obs. |
Discovery date | 2 March 1981 |
Designations | |
(4432) McGraw-Hill | |
Named after | McGraw-Hill Telescope [1] (at Kitt Peak, Arizona) |
1981 ER22 · 1964 TV | |
main-belt [1][2] · (inner)[3] background [4] | |
Orbital characteristics [2] | |
Epoch 23 March 2018 (JD 2458200.5) | |
Uncertainty parameter 0 | |
Observation arc | 53.54 yr (19,555 d) |
Aphelion | 2.8975 AU |
Perihelion | 1.8747 AU |
2.3861 AU | |
Eccentricity | 0.2143 |
3.69 yr (1,346 d) | |
188.28° | |
0° 16m 2.64s / day | |
Inclination | 0.4616° |
115.15° | |
246.30° | |
Physical characteristics | |
3.042±0.643 km[5][6] 3.43 km (derived)[3] | |
inconclusive [3][7] | |
0.20 (assumed)[3] 0.254±0.224[5][6] | |
S (assumed)[3] | |
14.5[1][2] 14.69[3][6][7] | |
McGraw-Hill is a non-family asteroid from the main belt's background population.[4] It orbits the Sun in the inner asteroid belt at a distance of 1.9–2.9 AU once every 3 years and 8 months (1,346 days; semi-major axis of 2.39 AU). Its orbit has an eccentricity of 0.21 and an inclination of 0° with respect to the ecliptic.[2]
The asteroid was first observed as 1964 TV at Purple Mountain Observatory in October 1964. The body's observation arc begins with a precovery taken at Palomar Observatory in February 1977, or four years prior to its official discovery observation at Siding Spring.[1]
McGraw-Hill is an assumed, stony S-type asteroid,[3] in agreement with the albedo (see below) obtained by the Wide-field Infrared Survey Explorer (WISE).
During the Small Main-Belt Asteroid Lightcurve Survey, McGraw-Hill has been observed photometrically. The observations gave a small brightness variation of 0.06 magnitude but resulted in no useful rotational lightcurve (U=n.a.).[7] As of 2018, the body's rotation period, pole and shape remain unknown.[2]
According to the survey carried out by the NEOWISE mission of NASA's WISE telescope, McGraw-Hill measures 3.042 kilometers in diameter and its surface has an albedo of 0.254,[5][6] while the Collaborative Asteroid Lightcurve Link assumes a standard albedo for a stony asteroid of 0.20 and derives a diameter of 3.43 kilometers based on an absolute magnitude of 14.69.[3]
This minor planet was named after the 1.3-meter McGraw-Hill Telescope located at the MDM Observatory at the Kitt Peak National Observatory site in Arizona, United States.[1] The official naming citation was published by the Minor Planet Center on 18 February 1992 (M.P.C. 19697).[8]
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