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1989 Tatry

Asteroid


Summary

Asteroid

FieldValue
minorplanetyes
name1989 Tatry
background#D6D6D6
discovery_ref
discovered20 March 1955
discovererA. Paroubek
R. Podstanicka
discovery_siteSkalnaté Pleso Obs.
mpc_name(1989) Tatry
alt_names1955 FG1935 UQ
1944 DL1955 DY
1964 WK1968 YC
named_afterHigh Tatra Mountains
(in northern Slovakia)
mp_categorymain-beltVestian
orbit_ref
epoch4 September 2017 (JD 2458000.5)
uncertainty0
observation_arc81.63 yr (29,815 days)
aphelion2.5314 AU
perihelion2.1704 AU
semimajor2.3509 AU
eccentricity0.0768
period3.60 yr (1,317 days)
mean_anomaly166.59°
mean_motion/ day
inclination7.7654°
asc_node25.305°
arg_peri88.343°
dimensionskm
km
km
km
16.81 km (calculated)
rotationh
h
h
albedo0.057 (assumed)
spectral_typeSMASS C
abs_magnitude12.1012.4012.512.6

R. Podstanicka 1944 DL1955 DY 1964 WK1968 YC

(in northern Slovakia) km km km 16.81 km (calculated) h h

1989 Tatry, provisional designation , is a carbonaceous Vestian asteroid and tumbling slow rotator from the inner regions of the asteroid belt, approximately 16 kilometers in diameter.

It was discovered on 20 March 1955, by the Slovakian astronomers Alois Paroubek and Regina Podstanická at Skalnate Pleso Observatory, Slovakia, and named for the High Tatra Mountains. It was their only minor planet discovery.

Orbit and classification

Based on its orbital elements, the asteroid is a member of the Vesta family and classified as a carbonaceous C-type asteroid in the SMASS taxonomy. It orbits the Sun in the inner main-belt at a distance of 2.2–2.5 AU once every 3 years and 7 months (1,317 days). Its orbit has an eccentricity of 0.08 and an inclination of 8° with respect to the ecliptic. It was first identified as at the South African Union Observatory in 1935, extending the asteroid's observation arc by 20 years prior to its official discovery.

Diameter and albedo

According to the surveys carried out by the Japanese Akari satellite, and NASA's Wide-field Infrared Survey Explorer with its subsequent NEOWISE mission, the asteroid measures between 8.99 and 9.87 kilometers in diameter and its surface has an albedo between 0.175 and 0.262. The Collaborative Asteroid Lightcurve Link assumes a standard albedo for carbonaceous asteroids of 0.057 and calculates a much larger diameter of 16.8 kilometers, as the lower the albedo (reflectivity), the higher the diameter at a constant absolute magnitude (brightness).

Lightcurves

Photometric measurements of the asteroid made in January 2005, by astronomer Brian D. Warner at his Palmer Divide Observatory, Colorado, gave a lightcurve with a period of hours and a brightness variation of below in magnitude. However, the data was incomplete, so the period is considered suspect (). Further measurements made in October 2007, by Adrián Galád, Leonard Kornoš and Štefan Gajdoš at Modra Observatory in Slovakia, showed a much longer period of hours with a brightness variation of 0.5 in magnitude (). In March 2009, a fragmentary lightcurve obtained by French amateur astronomer Pierre Antonini gave a period of 24 hours ().

Tumbler

The observers also detected a non-principal axis rotation seen in distinct rotational cycles in successive order. This is commonly known as tumbling. Tatry is one of a group of less than 200 bodies known to be is such a state (also see List of tumblers).

Naming

This minor planet is named after the location of the discovering observatory, High Tatras (), the highest mountain range in northern Slovakia. The approved naming citation was published by the Minor Planet Center on 1 February 1980 (M.P.C. 5183).

References

Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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