47171 Lempo
editLead content
History ✓
editDiscovery ✓
editThe Lempo system was discovered on 1 October 1999 by American astronomers Eric Rubenstein and Louis-Gregory Strolger during an observing run for their Nearby Galaxies Supernova Search (NGSS) project at the Kitt Peak National Observatory in Arizona. Initiated in 1998, the NGSS project was a three-year-long CCD-based survey of galaxies along the celestial equator to search for nearby, low-redshift supernovae. The Kitt Peak Observatory's WIYN 0.9-meter telescope was used for wide-field imaging of this region, which coincided with the ecliptic plane where Kuiper belt objects (KBOs) including Lempo were likely to occur. Lempo was identified by Rubenstein as a relatively bright, slow-moving object in the constellation Cetus on images taken by Strolger on 1 October 1999. At an apparent magnitude of 20, its exceptional brightness for a suspected KBO warranted follow-up observations to confirm the object.
Lempo was observed by Rubenstein and Strolger for three consecutive days after its discovery. The object was also found in images taken by Strolger on 30 September 1999, one day prior to its discovery. The discovery was then announced by the Minor Planet Center on 21 December 1999 and the object was given the provisional designation 1999 TC36. The provisional designation indicates that Lempo was the 903rd minor planet discovered in the first half of October 1999. By 2002, additional observations have extended Lempo's observation arc to over two years, sufficient to determine an accurate orbit. Lempo was consequently given the permanent minor planet number 47171 by the Minor Planet Center on 21 September 2002. As of 2020[update], over 500 total observations of Lempo have been obtained within an observation arc of over 45 years. The earliest known observations of Lempo have been identified in precovery images dating back to 18 June 1974, as photographic plates of the Siding Spring Observatory's Digitized Sky Survey from June 1974 and May and September 1976.
Name ✓
editName origin, meaning, and date (MPC 2017)
Trinary system
editLempo is a hierarchical triple (or trinary) system consisting of a central primary, which is itself a binary system of two similarly-sized components (Lempo and Hiisi), and a small satellite on a wide and eccentric circumbinary orbit (Paha). The structure of the hierarchy is discerned by denoting the apparent Lempo–Hiisi primary with the letter A and the smaller, outer companion Paha with the letter B; the individual primary components Lempo and Hiisi are distinguished as A1 and A2, respectively.[1] The three components ordered from largest to smallest are Lempo, Hiisi, and Paha.[2]
Assuming spherical shapes with a uniform bulk density for all components, the system mass estimated based on the motion of Paha is (12.75±0.06)×1018 kg.[1][3] The orbital motion of the Lempo–Hiisi components gives somewhat a higher estimated mass of (14.20±0.05)×1018 kg. This discrepancy is probably related to unaccounted gravitational interactions of the components in a complex triple system.[1]
Lempo is one of the only three trans-Neptunian multiple systems with more than two components; the other two are the dwarf planets Pluto and Haumea.[1] The binary Kuiper belt object 385446 Manwë is suspected to have once been a hierarchical triple system similar to Lempo, but the orbit of its inner binary evolved by tides and became a contact binary.[4]
Paha
editDiscovery[5] | |
---|---|
Discovered by | Chadwick A. Trujillo Michael E. Brown |
Discovery date | 8 December 2001 |
Designations | |
(47171) Lempo I [6] | |
Pronunciation | /ˈpɑːhɑː/ |
S/2001 (1999 TC36) 1 [7] S/2001 (47171) 1 | |
Orbital characteristics[8] | |
Epoch 24 May 2006 12:00 UT (JD 2453880.0) | |
7411±12 km | |
Eccentricity | 0.2949±0.0009 |
50.302±0.001 d | |
Inclination | 79.3°±0.2°[a] |
325.2°±0.1° | |
292.1°±0.2° | |
Satellite of | 47171 Lempo |
Physical characteristics | |
132+8 −9 km[9] | |
Mass | 7.67×1017 kg[3] |
Mean density | 0.64 g/cm3 (system)[9] |
0.079+0.013 −0.011 (system)[9] | |
V−I=1.120±0.050[10] | |
22.6[11] (Δmag 2.24±0.03)[1] | |
Paha, officially designated (47171) Lempo I Paha,[6] is the smaller, outer component of the Lempo triple system. It was discovered on 8 December 2001 by astronomers Chadwick Trujillo and Michael Brown using the Hubble Space Telescope's Space Telescope Imaging Spectrograph to survey for binary trans-Neptunian objects.[12] The discovery was reported in an IAU Circular notice published by the International Astronomical Union 10 January 2002.[5]
The discovery observations of the apparent Lempo–Paha binary were taken on 8 and 9 December, which had measured apparent separations of 0.365″±0.001″ and 0.370″±0.001″, respectively. The pair exhibited a large flux difference of 2.21±0.01 magnitudes in the unfiltered images.[5] Following the discovery announcement, Franck Marchis and colleagues reanalyzed archival 4 October 2001 observations of Lempo from the Lick Observatory's Shane telescope adaptive optics system and identified a clear detection of Paha.[13] They reported an apparent separation of 0.246″±0.017″ and flux difference of 1.89±0.14 magnitudes in a follow-up IAU Circular published on 24 January 2002.[14]
Paha previously had the temporary provisional designation S/2001 (1999 TC36) 1 before it was changed to S/2001 (47171) 1 after Lempo was numbered.[7] Being the smaller, outer component on a circumbinary orbit around the central Lempo–Hiisi binary, it was sometimes designated "component B" in scientific literature.[1] It received its permanent satellite designation and name alongside Lempo and Hiisi on 5 October 2017.[15]
Characteristics
editSize, density, mass, etc.
In unfiltered visual wavelengths, Paha appears 2.2 magnitudes dimmer than the primary on average, corresponding to an individual apparent magnitude of 22.6.[11]
Circumbinary orbit, chaos, etc.
Keplerian orbit fit suggests mutual events occuring between Paha and Lempo–Hiisi around 2069, but mutual perturbations may shift the timing on the order of a decade.
Hiisi
editDiscovery[16][1] | |
---|---|
Discovered by | Seth Jacobson Jean-Luc Margot Susan D. Benecchi et al. |
Discovery date | October 2007 |
Designations | |
(47171) Lempo II [6] | |
Pronunciation | /ˈpɑːhɑː/ |
Orbital characteristics[8] | |
Epoch 24 May 2006 12:00 UT (JD 2453880.0) | |
867±11 km | |
Eccentricity | 0.101±0.006 |
1.9068±0.0001 d | |
Inclination | 88.9°±0.6°[a] |
330.0°±1.0° | |
47.7°±6.3° | |
Satellite of | 47171 Lempo |
Physical characteristics | |
251+16 −17 km[9] | |
Mass | 5.273×1018 kg[3] |
Mean density | 0.64 g/cm3 (system)[9] |
45.763±0.002 h (assumed)[1] | |
0.079+0.013 −0.011 (system)[9] | |
V−I=1.19±0.01[1] | |
20.2[11] (Δmag 0.17)[1] | |
Hiisi, officially designated (47171) Lempo II Hiisi,[17] is the inner, second-largest component of the Lempo triple system. Together with the primary component Lempo, it forms the central binary Lempo–Hiisi which the outer component Paha revolves around. The existence of a third, inner component (or second companion) in the Lempo system was first hypothesized in 2006 by John Stansberry and collaborators, who noted that the primary seemed to have an unusually low density.[18] Further evidence to the existence of an inner component was posited by Seth Jacobson and Jean-Luc Margot in October 2007, who noticed a distinct elongation of the primary in Hubble images.[16] The binarity of the Lempo primary was eventually confirmed in a more extensive analysis of Hubble images by Susan Benecchi and collaborators in 2009.[1][6]
Due to complex discovery circumstances involving different independent groups of researchers,[19] Hiisi did not have a formal provisional designation signifying the year of its first observation or discovery.[17] Instead, it was unofficially designated "component A2" in scientific literature for being the smaller component of the central Lempo–Hiisi binary.[1] It eventually received its permanent satellite designation and name while the larger, first component A1 maintained the name Lempo on 5 October 2017.[15]
Characteristics
editThe separation between the two components is only about half the diffraction limit of Hubble, making it impossible to fully resolve the system. Instead, it appears elongated in Hubble images, revealing its binary nature.
The separation between the two components is only about half the diffraction limit of Hubble, making it impossible to fully resolve the system. Instead, it appears elongated in Hubble images, revealing its binary nature.[1] This central pair has a semi-major axis of around 867 km and a period of about 1.9 days.[1] Assuming equal albedos of about 0.079, Lempo and Hiisi are approximately 272+17
−19 km and 251+16
−17 km in diameter, respectively.[9] The earlier discovered satellite Paha orbits the barycenter of the Lempo–Hiisi system.
Keplerian orbit fit suggests mutual events around 2075, but mutual perturbations may shift the timing on the order of a decade.
System dynamics
editThe orbital dynamics of the Lempo system are highly complex and could not be modelled with solely Keplerian dynamics.[1][3] Many crucial parameters such as initial spin states and shapes of the individual components are unknown and thus could not adequately model the dynamics of the Lempo system as a three-body problem without leading to significantly chaotic behavior. In a 2018 dynamical study, Alexandre Correia found that simulated models using realistically assumed spin states and shapes failed to explain the presently eccentric mutual orbit of the inner Lempo–Hiisi binary, even with the inclusion of eccentricity-damping tidal forces. Correia concluded that the present orbits, spin states and shapes of all components of the Lempo system needed to be remeasured to a greater precision before a more sophisticated model could be developed.[3]
Origin
editFormation hypotheses
Physical characteristics
editIntroduce the system absolute magnitude and (erroneous) dwarf planet candidate prior to discovery of its components. Mention effective diameter as a single object. (single paragraph)
Spectra and surface
editSurface composition, albedo, color, and spectroscopy/photometry studies
Internal structure
editDensity, mass, and internal structure of the components.
Orbit
editHeliocentric orbit from JPL-SSD and Buie
Exploration
editMention New Horizons 2 and other exploration proposals from Zangari et al. (2018)
References
editReferences
External links
editExternal links
Lempo resources
edit- http://iota-es.de/JOA/JOA2020_4.pdf (2020) General summary of Lempo - 2020JOA....10a..24K
Discovery
edit- MPEC 1999-Y19 : 1999 RV214, 1999 TC36, 1999 XX143, 1999 XY143 (Discovery announcement of Lempo; Dec 1999)
- Lou Strolger's Page – An Old Discovery Gets a New Name
- The Nearby Galaxies Supernova Search project: The rate of supernovae in the local universe, Strolger (2003)
- MPEC 2000-O37 : 1999 TC36 (Follow-up observations of Lempo; July 2000)
- (47171) 1999 TC36 Precovery Images (2007)
Trinary system
edit- IAUC 7787: 1999 TC_36; 2001is, 2001it (Hubble discovery of outer companion Paha; Jan 2002)
- IAUC 7807: (26308) 1998 SM_165; 1999 TC_36; C/1996 Y2 (Paha confirmation with Lick Shane 3-m telescope; Jan 2002)
- The Albedo, Size, and Density of Binary Kuiper Belt Object (47171) 1999 TC36, Stansberry et al. (2006)
- Stansberry et al. (2006) independently hypothesized the trinary nature of Lempo due to its unexpectedly low density and negligible light curve.
- Colors of TNO Binaries and Evidence for a Triple System from HST Observations, Jacobson et al. (2007)
- Discovery and confirmation of third, inner component Hiisi by Hubble. Preliminary results announced at the 39th DPS meeting in October 2007.
- (47171) 1999 TC36, A transneptunian triple, Benecchi et al. (2010)
- Lempo–Hiisi color index: V–I=1.19±0.01 and Paha color index: V–I=1.12±0.03
System dynamics
edit- Chaotic dynamics in the (47171) Lempo triple system, Correia (2018)
- Mass estimates and dynamical constraints on rotation and orbits
Formation
edit- Formation of Kuiper Belt Binaries by Gravitational Collapse, Nesvorný et al. (2010)
- The origin of (47171) Lempo-like Kuiper belt triple systems during binary-binary interactions, Brunini & López (2020)
- Binary Planetesimal Formation from Gravitationally Collapsing Pebble Clouds, Nesvorný et al. (2021)
- "About 10% of collapse simulations produce hierarchical systems with two or more large moons."
Photometry and size/density
edit- Size estimates of some optically bright KBOs, Altenhoff et al. (2004)
- Derived effective diameter of 609+93
−47 km (566 and 225 km for components) from absolute magnitude of 4.9 and geometric albedo of 0.05±0.01.
- Derived effective diameter of 609+93
- The Albedo, Size, and Density of Binary Kuiper Belt Object (47171) 1999 TC36
- Anomalously low density of 0.3–0.8 g/cm3 if assuming a single primary body 350–470 km. (corresponds to porosity of 65% or 45%–80%)
- Accounting for the system's multiplicity, the density range is higher at 0.4–1.1 g/cm3, with a mean density of 0.7 g/cm3 for all three components. Porosity range is decreased to 15%–70%.
- If the components do have such low densities and high porosities, they are most likely spherically-shaped rubble piles with possible rocky cores less than 50% of their radii.
- Effective geometric albedo of 0.079, from the range 0.055–0.110.
- Physical Properties of Transneptunian Objects, Cruikshank et al. (2007)
- Lempo is classified under the RR color group (very red and rich with tholins).
- Physical Properties of Kuiper Belt and Centaur Objects: Constraints from the Spitzer Space Telescope, Stansberry et al. (2008)
- Adopted solution gives a geometric albedo of 0.0718+0.0153
−0.0117 and a derived effective diameter 414.6+38.8
−38.2, based on a two-band model. - Two-band thermal model gives a geometric albedo of 0.0718+0.0153
−0.0117 and a derived effective diameter 414.6+38.8
−38.2.
- Adopted solution gives a geometric albedo of 0.0718+0.0153
- TNOs are cool: A survey of the trans-Neptunian region. V. Physical characterization of 18 Plutinos using Herschel-PACS observations, Mommert et al. (2012)
- Absolute magnitude 5.41±0.10 and geometric albedo 0.079+0.013
−0.011 corresponds to effective diameter of 393.1+25.2
−26.8 km. - Light curve amplitude of 0.2±0.04.
- Color indices: B–V=1.00±0.13, V–R=0.70±0.03, V–I=1.30±0.13
- Confirmation of water ice on Lempo.
- Individual sizes for each component and revised bulk density of 0.64+0.15
−0.11 g/cm3 (porosity 36%–68%) for all components.
- Absolute magnitude 5.41±0.10 and geometric albedo 0.079+0.013
Rotation(?)
edit- Visible-IR colors and lightcurve analysis of two bright TNOs: 1999 TC36 and 1998 SN165, Peixinho et al. (2002)
- No detection of variability, though an observed slight decrease in brightness (0.1 mag) implies a longer rotational period.
- A study of short term rotational variability in TNOs and Centaurs from Sierra Nevada Observatory, Ortiz et al. (2003)
- Tentative low-amplitude (0.06 mag) period of 6.21±0.02 detected in September 2001, but further observations in August 2001 yielded no conclusive results.
Spectra and surface
edit- Searching for water ice on 47171 1999 TC36, 1998 SG35, and 2000 QC243: ESO large program on TNOs and centaurs, Dotto et al. (2003)
- The reflectance spectrum of Lempo (between 1.12–2.26 μm) is best modeled with 57% Titan tholin, 25% ice tholin, 10% amorphous carbon, and 8% water ice with an albedo of 0.13.
- Strong red spectral slope from 0.4–1.2 µm.
- Color indices: B–V=1.09±0.04, V–R=0.73±0.04, V–I=1.33±0.04
Results from the Eso Large Program on Transneptunian Objects and Centaurs, Boehnhardt et al. (2003)Detection of water ice; results consistent with Dotto et al. (2003).
- Search for surface variations on TNO 47171 and Centaur 32532, Merlin et al. (2005)
- The best-fit surface composition model for the Lempo's reflectance spectrum (between 0.4–2.3 μm) matches that by Dotto et al. (2003).
- Results consistent with Dotto et al. (2003).
- ESO large program about transneptunian objects: surface variations on (47171) 1999 TC36, Protopapa et al. (2009)
- The reflectance spectrum of Lempo (between 0.37–2.33 μm) can be best explained with two models:
- An intimate mixture of 1% of Triton tholin, 1% of Titan tholin, 97% of serpentine, and 1% of Triton tholin diluted (45% concentration) in crystalline water ice.
- An intimate mixture of 30% of Titan tholin, 44% of amorphous carbon, and 26% of Triton tholin diluted (49% concentration) in crystalline water ice.
- Apparent surface hetrogeneity in different spectra from 2001-2003, maybe due to partial resurfacing by non-disruptive collisions and/or cometary activity.
- The preferred surface composition model for the 2001-2006 spectra is 10% Titan tholin, 85% serpentine, and 5% Triton tholin diluted (39% concentration) in crystalline water ice. All of these materials are in the form of micrometer-sized grains.
- The reflectance spectrum of Lempo (between 0.37–2.33 μm) can be best explained with two models:
- Compositional study of trans-Neptunian objects at λ > 2.2 µm, Boehnhardt et al. (2003)
- Predicted presence of methanol on Lempo.
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