Hiʻiaka (moon)

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Hiʻiaka
2003 EL61 Haumea, with moons.jpg
Hiʻiaka is above Haumea (center) in this Keck telescope image.
Discovery
Discovered by Michael E. Brown,
Chad Trujillo,
David Rabinowitz, et al.
Discovery date 26 January 2005
Designations
MPC designation Haumea I Hiʻiaka
Pronunciation /ˌhʔiˈɑːkə/[1]
(136108) 2003 EL61 I,
S/2005 (2003 EL61) 1
Orbital characteristics[2]
49880±198 km
Eccentricity 0.0513±0.0078
49.12±0.03 d
Inclination 126.356±0.064°
Satellite of Haumea
Physical characteristics
Mean radius
~160 km[2]
Mass (1.79±0.11)×1019 kg[2] (0.45% of Haumea)
Mean density
~1 g/cm3
Temperature 32±K
3.3 difference from primary's 17.3

Hiʻiaka is the larger, outer moon of the dwarf planet Haumea.

Discovery and naming

Hiʻiaka was the first satellite discovered around Haumea. It is named after one of the daughters of Haumea, Hiʻiaka, the patron goddess of the Big Island of Hawaii, though at first it had gone by the nickname "Rudolph" by its discovery team. It orbits once every 49.12±0.03 d at a distance of 49880±198 km, with an eccentricity of 0.0513±0.0078 and an inclination of 126.356±0.064°. Mutual events expected in July 2009 should improve the knowledge of the orbits and masses of the components of the Haumean system.[2]

Physical characteristics

Size and brightness

Its measured brightness is 5.9±0.5%, translating into a diameter of about 22% of its primary, or in the range of 320 km, assuming similar albedo.[2] To put this in perspective, this would make it larger than all but four of the asteroids, after 1 Ceres, 2 Pallas, 4 Vesta, and 10 Hygiea. However, it is not a dwarf-planet candidate because it is a moon.

Mass

The mass of Hiʻiaka is estimated to be (1.79±0.11)×1019 kg using precise relative astrometry from Hubble Telescope and Keck Telescope and applying 3-body, point-mass model to the Haumean system.[2]

Spectrum and composition

The near infrared spectrum of Hiʻiaka is dominated by water-ice absorption bands, which means that its surface is made mainly of water ice. The presence of the band centered at 1.65 µm indicates that the surface water ice is primarily in the crystalline form. Currently it is unclear why water ice on the surface has not turned into amorphous form as would be expected due to its constant irradiation by cosmic rays.[3]

See also

References

  1. The Hawaiian pronunciation is [ˈhiʔiˈjɐkə].
  2. 2.0 2.1 2.2 2.3 2.4 2.5 Lua error in package.lua at line 80: module 'strict' not found.
  3. Lua error in package.lua at line 80: module 'strict' not found.

External links