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1089 Tama

From Wikipedia, the free encyclopedia
Florian asteroid and synchronous binary system

1089 Tama
Lightcurve-based 3D-model ofTama
Discovery[1]
Discovered byO. Oikawa
Discovery siteTokyo Astronomical Obs.
Discovery date17 November 1927
Designations
(1089) Tama
PronunciationJapanese:[tama]
Named after
Tama River[2]
(Japaneseriver)
1927 WB · 1930 ST
1952 HE4 · A894 VA
A904 VD · A919 HA
main-belt · (inner)
Flora[3] · background[4]
Orbital characteristics[1]
Epoch 4 September 2017 (JD 2458000.5)
Uncertainty parameter 0
Observation arc122.40 yr (44,708 days)
Aphelion2.4951AU
Perihelion1.9327 AU
2.2139 AU
Eccentricity0.1270
3.29yr (1,203 days)
82.843°
0° 17m 57.12s / day
Inclination3.7264°
71.489°
354.29°
Knownsatellites[3][5][6]
Physical characteristics
Dimensions11.33±2.00 km[7]
12.2±1.6 km[8]
12.82 km(derived)[3]
12.92±0.6 km[9]
13.08±0.37 km[10]
13.082±0.373 km[10]
13.32±0.19 km[11]
4(dated)h[12]
16.4±0.1 h[13]
16.44 h[8]
16.444±0.001 h[14]
16.4442±0.0004 h[6][13]
16.445±0.005 h[13]
16.45±0.05 h[13]
16.4530±0.0004 h[13]
16.464±0.004 h[15]
16.4655 h[16]
0.2048(derived)[3]
0.216±0.029[10]
0.2424±0.023[9]
0.243±0.008[11]
0.267±0.083[8]
0.32±0.23[7]
S(assumed)[3]
11.60[9][11] · 11.63±0.0[8] · 11.70[7][10] · 11.8[1][3] · 11.86±0.85[17]

1089 Tama, provisional designation1927 WB, is an elongated Florianasteroid and synchronousbinary system from the inner regions of theasteroid belt, approximately 12 kilometers in diameter.

It was discovered by Japanese astronomerOkuro Oikawa at the old Tokyo Astronomical Observatory (389) on 17 November 1927.[18] The asteroid was named after theTama River in Japan.[2] Itsminor-planet moon was discovered in December 2003 and measures approximately 9 kilometers.[6]

Orbit and classification

[edit]

Tama is a member of theFlora family (402), a giantasteroid family and the largest family of stony asteroids in the main-belt.[3] It is, however, a non-family asteroid from the main belt'sbackground population when applying the Hierarchical Clustering Method to its proper orbital elements.[4]

The asteroid orbits the Sun in theinner main-belt at a distance of 1.9–2.5 AU once every 3 years and 3 months (1,203 days). Its orbit has aneccentricity of 0.13 and aninclination of 4° with respect to theecliptic.[1]Tama was first identified asA894 VA atHeidelberg Observatory in November 1894. The body'sobservation arc begins with its identification asA904 VD at Heidelberg in November 1904, or 23 years prior to its official discovery observation at Tokyo.[18]

Physical characteristics

[edit]

Tama is an assumed stonyS-type asteroid.[3]

Rotation period

[edit]

A large number of rotationallightcurves ofTama were obtained from photometric observations since it has been identified as abinary asteroid(see below). Lightcurve analysis gave arotation period between 16.4 and 16.464 hours with a brightness variation between 0.08 and 0.41magnitude (U=2-/2-3-/3), superseding a period of 4 hours from a fragmentary lightcurve obtained in the 1990s (U=1).[6][8][12][13][15]

Tama appears to be somewhat elongated in shape.[6] LCDB's consolidated result gives a period of 16.44 hours and an amplitude of 0.41 magnitude (U=3).[3]

Diameter and albedo

[edit]

According to the surveys carried out by the Infrared Astronomical SatelliteIRAS, the JapaneseAkari satellite, theSpitzer Space Telescope and theNEOWISE mission of theWide-field Infrared Survey Explorer,Tama measures between 11.33 and 13.32 kilometers in diameter and its surface has analbedo between 0.216 and 0.32.[7][8][9][10][11]

TheCollaborative Asteroid Lightcurve Link derives an albedo of 0.2048 and a diameter of 12.82 kilometers based on anabsolute magnitude of 11.8.[3]

Satellite

[edit]

In 2004, it was announced thatTama has aminor-planet moon. The satellite was identified based on lightcurve observations with mutualoccultation and eclipsing events from 24 December 2003 to 5 January 2004 byRaoul Behrend,René Roy,Claudine Rinner,Pierre Antonini,Petr Pravec,Alan Harris,Stefano Sposetti, Russell Durkee, andAlain Klotz.[6][13] The moon measures approximately 9 kilometers in diameter. It may orbits 20 km away in a period of 16.4442 hours (synchronously).[3][5][6]

Spin axis

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Tamas lightcurve has also been modeled. In 2013, modelling by an international study using photometric data from theUS Naval Observatory, the Uppsala Asteroid Photometric Catalogue (UAPC) and thePalmer Divide Observatory, gave a concurring rotation period of 16.4655 hours.[16] Another modeled lightcurve using data from UAPC, thePalomar Transient Factory survey, and individual observers, gave a period of 16.4461 hours as well as twospin axes of (193.0°, 32.0°) and (9.0°, 28.0°) inecliptic coordinates (λ, β).[19]

Naming

[edit]

Thisminor planet was named afterTama River near the discovering Tokyo Astronomical Observatory (389) in Japan. The official naming citation was mentioned inThe Names of the Minor Planets byPaul Herget in 1955 (H 103).[2]

References

[edit]
  1. ^abcd"JPL Small-Body Database Browser: 1089 Tama (1927 WB)" (2017-03-29 last obs.).Jet Propulsion Laboratory. Archived fromthe original on 19 August 2020. Retrieved26 September 2017.
  2. ^abcSchmadel, Lutz D. (2007). "(1089) Tama".Dictionary of Minor Planet Names – (1089) Tama.Springer Berlin Heidelberg. p. 93.doi:10.1007/978-3-540-29925-7_1090.ISBN 978-3-540-00238-3.
  3. ^abcdefghijk"LCDB Data for (1089) Tama". Asteroid Lightcurve Database (LCDB). Retrieved26 September 2017.
  4. ^ab"Asteroid 1089 Tama – Nesvorny HCM Asteroid Families V3.0".Small Bodies Data Ferret. Retrieved26 October 2019.
  5. ^ab"(1089) Tama".Asteroids with Satellites Database – Johnston's Archive. Retrieved26 September 2017.
  6. ^abcdefgBehrend, R.; Roy, R.; Rinner, C.; Antonini, P.; Pravec, P.; Harris, A. W.; et al. (January 2004)."(1089) Tama".IAU Circ.8265 (8265): 2.Bibcode:2004IAUC.8265....2B. Retrieved26 September 2017.
  7. ^abcdNugent, C. R.; Mainzer, A.; Masiero, J.; Bauer, J.; Cutri, R. M.; Grav, T.; et al. (December 2015)."NEOWISE Reactivation Mission Year One: Preliminary Asteroid Diameters and Albedos".The Astrophysical Journal.814 (2): 13.arXiv:1509.02522.Bibcode:2015ApJ...814..117N.doi:10.1088/0004-637X/814/2/117. Retrieved26 September 2017.
  8. ^abcdefMarchis, F.; Enriquez, J. E.; Emery, J. P.; Mueller, M.; Baek, M.; Pollock, J.; et al. (November 2012)."Multiple asteroid systems: Dimensions and thermal properties from Spitzer Space Telescope and ground-based observations".Icarus.221 (2):1130–1161.arXiv:1604.05384.Bibcode:2012Icar..221.1130M.doi:10.1016/j.icarus.2012.09.013.hdl:2060/20130014861. Retrieved26 September 2017.
  9. ^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.
  10. ^abcdeMasiero, Joseph R.; Mainzer, A. K.; Grav, T.; Bauer, J. M.; Cutri, R. M.; Nugent, C.; et al. (November 2012)."Preliminary Analysis of WISE/NEOWISE 3-Band Cryogenic and Post-cryogenic Observations of Main Belt Asteroids".The Astrophysical Journal Letters.759 (1): 5.arXiv:1209.5794.Bibcode:2012ApJ...759L...8M.doi:10.1088/2041-8205/759/1/L8. Retrieved26 September 2017.
  11. ^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)
  12. ^abSárneczky, K.; Szabó, Gy.; Kiss, L. L. (June 1999)."CCD observations of 11 faint asteroids".Astronomy and Astrophysics Supplement.137 (2):363–368.Bibcode:1999A&AS..137..363S.doi:10.1051/aas:1999251.
  13. ^abcdefgBehrend, Raoul."Asteroids and comets rotation curves – (1089) Tama".Geneva Observatory. Retrieved26 September 2017.
  14. ^Behrend, R.; Bernasconi, L.; Roy, R.; Klotz, A.; Colas, F.; Antonini, P.; et al. (February 2006)."Four new binary minor planets: (854) Frostia, (1089) Tama, (1313) Berna, (4492) Debussy".Astronomy and Astrophysics.446 (3):1177–1184.Bibcode:2006A&A...446.1177B.doi:10.1051/0004-6361:20053709.
  15. ^abPolishook, David (October 2012)."Lightcurves for Shape Modeling: 852 Wladilena, 1089 Tama, and 1180 Rita".The Minor Planet Bulletin.39 (4):242–244.Bibcode:2012MPBu...39..242P.ISSN 1052-8091. Retrieved26 September 2017.
  16. ^abDurech, J.; Kaasalainen, M.; Warner, B. D.; Fauerbach, M.; Marks, S. A.; Fauvaud, S.; et al. (January 2009)."Asteroid models from combined sparse and dense photometric data".Astronomy and Astrophysics.493 (1):291–297.Bibcode:2009A&A...493..291D.doi:10.1051/0004-6361:200810393.
  17. ^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 September 2017.
  18. ^ab"1089 Tama (1927 WB)".Minor Planet Center. Retrieved26 September 2017.
  19. ^Hanus, J.; Durech, J.; Broz, M.; Marciniak, A.; Warner, B. D.; Pilcher, F.; et al. (March 2013). "Asteroids' physical models from combined dense and sparse photometry and scaling of the YORP effect by the observed obliquity distribution".Astronomy and Astrophysics.551: 16.arXiv:1301.6943.Bibcode:2013A&A...551A..67H.doi:10.1051/0004-6361/201220701.

External links

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