Larissa (moon)

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Larissa
Larissa.jpg
Two views of Larissa by Voyager 2
Discovery
Discovered by Harold J. Reitsema, William B. Hubbard, Larry A. Lebofsky, and David J. Tholen
Discovery date May 24, 1981
Orbital characteristics[1]
Epoch 18 August 1989
Semi-major axis 73 548 ± 1 km
Eccentricity 0.001393 ± 0.00008
Orbital period 0.55465332 ± 0.00000001 d
Inclination
  • 0.251 ± 0.009° (to Neptune equator)
  • 0.205° (to local Laplace plane)
Satellite of Neptune
Physical characteristics
Dimensions 216×204×168 km (± ~10 km)[2][3]
Mean radius 97 ± 3 km[4]
Volume ~3.5×106km³
Mass ~4.2×1018 kg (estimate)[a]
Mean density ~1.2 g/cm³ (estimate)[4]
Equatorial surface gravity ~0.03 m/s2[b]
Escape velocity ~0.076 km/s[c]
Rotation period synchronous
Axial tilt zero
Albedo 0.09[2][4]
Temperature ~51 K mean (estimate)
Apparent magnitude 21.5[4]

Larissa (/ləˈrɪsə/ lə-RISS; Greek: Λάρισα), also known as Neptune VII, is the fifth-closest inner satellite of Neptune. It is named after Larissa, a lover of Poseidon (Neptune) in Greek mythology and eponymous nymph of the city in Thessaly, Greece.

Discovery[edit]

It was first discovered by Harold J. Reitsema, William B. Hubbard, Larry A. Lebofsky and David J. Tholen, based on fortuitous ground-based stellar occultation observations[6] on May 24, 1981, given the temporary designation S/1981 N 1 and announced on May 29, 1981.[7] The moon was recovered and confirmed to be the only object in its orbit during the Voyager 2 flyby in 1989[8] after which it received the additional designation S/1989 N 2 on August 2, 1989.[9] The announcement by Stephen P. Synnott spoke of “10 frames taken over 5 days”, which gives a recovery date sometime before July 28. The name was given on September 16, 1991.[10]

Characteristics[edit]

Map of Larissa
A simulated view of Larissa orbiting Neptune. The surface details are fictional.

The fourth-largest satellite of Neptune, Larissa is irregular (non-spherical) in shape and appears to be heavily cratered, with no sign of any geological modification. Little else is known about it. It is likely that Larissa, like the other satellites inward of Triton, is a rubble pile re-accreted from fragments of Neptune's original satellites, which were smashed up by perturbations from Triton soon after that moon's capture into a very eccentric initial orbit.[11]

Larissa's orbit is circular but not perfect and lies below Neptune's synchronous orbit radius, so it is slowly spiralling inward due to tidal deceleration and may eventually impact Neptune's atmosphere, or break up into a planetary ring upon passing its Roche limit due to tidal stretching, similar to how Triton will crash into Neptune or break into a planetary ring.

Exploration[edit]

Larissa has only been visited by Voyager 2, and the probe was able to get photographs of Larissa.

Notes[edit]

  1. ^ The mass estimate is based on the assumed density of 1.2 g/cm³, and a volume of 3.5 ×106 km³ obtained from a detailed shape model in Stooke (1994).[5]
  2. ^ Surface gravity derived from the mass m, the gravitational constant G and the radius r: Gm/r2.
  3. ^ Escape velocity derived from the mass m, the gravitational constant G and the radius r: 2Gm/r.

References[edit]

  1. ^ Jacobson, R. A.; Owen, W. M., Jr. (2004). "The orbits of the inner Neptunian satellites from Voyager, Earthbased, and Hubble Space Telescope observations". Astronomical Journal 128 (3): 1412–1417. Bibcode:2004AJ....128.1412J. doi:10.1086/423037.  edit
  2. ^ a b Karkoschka, Erich (2003). "Sizes, shapes, and albedos of the inner satellites of Neptune". Icarus 162 (2): 400–407. Bibcode:2003Icar..162..400K. doi:10.1016/S0019-1035(03)00002-2.  edit
  3. ^ Williams, Dr. David R. (2008-01-22). "Neptunian Satellite Fact Sheet". NASA (National Space Science Data Center). Retrieved 2008-12-13. 
  4. ^ a b c d "Planetary Satellite Physical Parameters". JPL (Solar System Dynamics). 2010-10-18. Retrieved 2011-10-11. 
  5. ^ Stooke, Philip J. (1994). "The surfaces of Larissa and Proteus". Earth, Moon, and Planets 65 (1): 31–54. Bibcode:1994EM&P...65...31S. doi:10.1007/BF00572198.  edit
  6. ^ Reitsema, H. J.; Hubbard, W. B.; Lebofsky, L. A.; Tholen, D. J. (1982). "Occultation by a Possible Third Satellite of Neptune". Science 215 (4530): 289–291. Bibcode:1982Sci...215..289R. doi:10.1126/science.215.4530.289. PMID 17784355.  edit
  7. ^ Marsden, Brian G. (May 29, 1981). "S/1981 N 1". IAU Circular 3608. Retrieved 2011-10-26. 
  8. ^ Smith, B. A.; Soderblom, L. A.; Banfield, D.; Barnet, C.; Basilevsky, A. T.; Beebe, R. F.; Bollinger, K.; Boyce, J. M.; Brahic, A. (1989). "Voyager 2 at Neptune: Imaging Science Results". Science 246 (4936): 1422–1449. Bibcode:1989Sci...246.1422S. doi:10.1126/science.246.4936.1422. PMID 17755997.  edit [on page 1435]
  9. ^ Marsden, Brian G. (August 2, 1989). "Satellites of Neptune". IAU Circular 4824. Retrieved 2011-10-26. 
  10. ^ Marsden, Brian G. (September 16, 1991). "Satellites of Saturn and Neptune". IAU Circular 5347. Retrieved 2011-10-26. 
  11. ^ Banfield, Don; Murray, Norm (October 1992). "A dynamical history of the inner Neptunian satellites". Icarus 99 (2): 390–401. Bibcode:1992Icar...99..390B. doi:10.1016/0019-1035(92)90155-Z.  edit

External links[edit]