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1140 Crimea

From Wikipedia, the free encyclopedia
Stony asteroid

1140 Crimea
Lightcurve-based 3D-model ofCrimea
Discovery[1]
Discovered byG. Neujmin
Discovery siteSimeiz Obs.
Discovery date30 December 1929
Designations
(1140) Crimea
Named after
Crimea
(Black Sea peninsula)[2]
1929 YC · A922 HA
main-belt · (middle)
Orbital characteristics[1]
Epoch 4 September 2017 (JD 2458000.5)
Uncertainty parameter 0
Observation arc82.04 yr (29,966 days)
Aphelion3.0846AU
Perihelion2.4579 AU
2.7712 AU
Eccentricity0.1131
4.61yr (1,685 days)
64.258°
0° 12m 48.96s / day
Inclination14.136°
72.139°
310.16°
Physical characteristics
Dimensions27.75±1.1 km(IRAS:13)[3]
28.87±0.36 km[4]
29.179±0.155 km[5]
29.554±0.205 km[6]
9.77±0.01h[7]
9.784±0.001 h[8]
9.7869±0.0005 h[9]
0.160±0.023[5]
0.1615±0.0193[6]
0.167±0.005[4]
0.1772±0.014(IRAS:13)[3]
S(Tholen)[1] · S(SMASS)[1]
S[10] · B–V = 0.916[1]
9.58±0.55[11] · 10.28[1][3][4][6][10]

1140 Crimea, provisional designation1929 YC, is a stonyasteroid from the middle region of theasteroid belt, approximately 28 kilometers in diameter. It was discovered on 30 December 1929, by Soviet astronomerGrigory Neujmin atSimeiz Observatory on theCrimean peninsula, after which it was named.[2][12]

Orbit and classification

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Crimea is aS-type asteroid in both theTholen andSMASS taxonomic scheme. It orbits the Sun in thecentral main-belt at a distance of 2.5–3.1 AU once every 4 years and 7 months (1,685 days). Its orbit has aneccentricity of 0.11 and aninclination of 14° with respect to theecliptic.[1] First identified asA922 HA at Simeiz in 1922, the body'sobservation arc begins atUccle in 1935, or 16 years after its official discovery observation at Simeiz.[12]

Lightcurves

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In April 2005, a rotationallightcurve ofCrimea was obtained by American astronomerRobert Stephens at Santana Observatory in California. Lightcurve analysis gave a well-definedrotation period of 9.77 hours with a brightness variation of 0.30magnitude (U=3).[7] Photometric observations by amateur astronomers Federico Manzini andPierre Antonini in March 2014, gave a concurring period of 9.784 hours with an amplitude of 0.23 magnitude (U=2).[8] In addition, a modeled lightcurve using data from the Uppsala Asteroid Photometric Catalogue and other sources gave a period 9.7869 hours, as well as a spin axis of (12.0°, -73.0°) inecliptic coordinates (U=n.a.).[9]

Diameter and albedo

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According to the surveys carried out by the Infrared Astronomical SatelliteIRAS, the JapaneseAkari satellite, and NASA'sWide-field Infrared Survey Explorer with its subsequentNEOWISE mission,Crimea measures between 27.75 and 29.18 kilometers in diameter, and its surface has analbedo between 0.160 and 0.177 (without preliminary results).[3][4][5] TheCollaborative Asteroid Lightcurve Link adopts the results obtained by IRAS, that is, an albedo of 0.1772 and a diameter of 27.75 kilometers with anabsolute magnitude of 10.28.[10]

Naming

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Thisminor planet was named for theCrimean Peninsula on the northern coast of theBlack Sea, where the discovering Simeiz Observatory is located.[2] Naming citation was first mentioned inThe Names of the Minor Planets byPaul Herget in 1955 (H 106).[2]

References

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  1. ^abcdefg"JPL Small-Body Database Browser: 1140 Crimea (1929 YC)" (2017-02-24 last obs.).Jet Propulsion Laboratory. Retrieved25 July 2017.
  2. ^abcdSchmadel, Lutz D. (2007). "(1140) Crimea".Dictionary of Minor Planet Names – (1140) Crimea.Springer Berlin Heidelberg. p. 96.doi:10.1007/978-3-540-29925-7_1141.ISBN 978-3-540-00238-3.
  3. ^abcdTedesco, E. F.; Noah, P. V.; Noah, M.; Price, S. D. (October 2004)."IRAS Minor Planet Survey V6.0".NASA Planetary Data System.12: IRAS-A-FPA-3-RDR-IMPS-V6.0.Bibcode:2004PDSS...12.....T. Retrieved22 October 2019.
  4. ^abcdUsui, Fumihiko; Kuroda, Daisuke; Müller, Thomas G.; Hasegawa, Sunao; Ishiguro, Masateru; Ootsubo, Takafumi; et al. (October 2011). "Asteroid Catalog Using Akari: AKARI/IRC Mid-Infrared Asteroid Survey".Publications of the Astronomical Society of Japan.63 (5):1117–1138.Bibcode:2011PASJ...63.1117U.doi:10.1093/pasj/63.5.1117. (online,AcuA catalog p. 153)
  5. ^abcMasiero, Joseph R.; Grav, T.; Mainzer, A. K.; Nugent, C. R.; Bauer, J. M.; Stevenson, R.; et al. (August 2014)."Main-belt Asteroids with WISE/NEOWISE: Near-infrared Albedos".The Astrophysical Journal.791 (2): 11.arXiv:1406.6645.Bibcode:2014ApJ...791..121M.doi:10.1088/0004-637X/791/2/121. Retrieved26 January 2017.
  6. ^abcMainzer, A.; Grav, T.; Masiero, J.; Hand, E.; Bauer, J.; Tholen, D.; et al. (November 2011). "NEOWISE Studies of Spectrophotometrically Classified Asteroids: Preliminary Results".The Astrophysical Journal.741 (2): 25.arXiv:1109.6407.Bibcode:2011ApJ...741...90M.doi:10.1088/0004-637X/741/2/90.
  7. ^abStephens, Robert D. (December 2005)."Asteroid lightcurve photometry from Santana Observatory - spring 2005".The Minor Planet Bulletin.32 (4):82–83.Bibcode:2005MPBu...32...82S.ISSN 1052-8091. Retrieved26 January 2017.
  8. ^abBehrend, Raoul."Asteroids and comets rotation curves – (1140) Crimea".Geneva Observatory. Retrieved26 January 2017.
  9. ^abHanus, J.; Durech, J.; Broz, M.; Warner, B. D.; Pilcher, F.; Stephens, R.; et al. (June 2011)."A study of asteroid pole-latitude distribution based on an extended set of shape models derived by the lightcurve inversion method".Astronomy & Astrophysics.530: 16.arXiv:1104.4114.Bibcode:2011A&A...530A.134H.doi:10.1051/0004-6361/201116738. Retrieved26 January 2017.
  10. ^abc"LCDB Data for (1140) Crimea". Asteroid Lightcurve Database (LCDB). Retrieved26 January 2017.
  11. ^Veres, Peter; Jedicke, Robert; Fitzsimmons, Alan; Denneau, Larry; Granvik, Mikael; Bolin, Bryce; et al. (November 2015)."Absolute magnitudes and slope parameters for 250,000 asteroids observed by Pan-STARRS PS1 - Preliminary results".Icarus.261:34–47.arXiv:1506.00762.Bibcode:2015Icar..261...34V.doi:10.1016/j.icarus.2015.08.007. Retrieved26 January 2017.
  12. ^ab"1140 Crimea (1929 YC)".Minor Planet Center. Retrieved26 January 2017.

External links

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