Csaba Kiss: Collisional History of the Kuiper Belt and Binary Kuiper Belt
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Trans-Neptunian Objects a Brief History, Dynamical Structure, and Characteristics of Its Inhabitants
Trans-Neptunian Objects A Brief history, Dynamical Structure, and Characteristics of its Inhabitants John Stansberry Space Telescope Science Institute IAC Winter School 2016 IAC Winter School 2016 -- Kuiper Belt Overview -- J. Stansberry 1 The Solar System beyond Neptune: History • 1930: Pluto discovered – Photographic survey for Planet X • Directed by Percival Lowell (Lowell Observatory, Flagstaff, Arizona) • Efforts from 1905 – 1929 were fruitless • discovered by Clyde Tombaugh, Feb. 1930 (33 cm refractor) – Survey continued into 1943 • Kuiper, or Edgeworth-Kuiper, Belt? – 1950’s: Pluto represented (K.E.), or had scattered (G.K.) a primordial, population of small bodies – thus KBOs or EKBOs – J. Fernandez (1980, MNRAS 192) did pretty clearly predict something similar to the trans-Neptunian belt of objects – Trans-Neptunian Objects (TNOs), trans-Neptunian region best? – See http://www2.ess.ucla.edu/~jewitt/kb/gerard.html IAC Winter School 2016 -- Kuiper Belt Overview -- J. Stansberry 2 The Solar System beyond Neptune: History • 1978: Pluto’s moon, Charon, discovered – Photographic astrometry survey • 61” (155 cm) reflector • James Christy (Naval Observatory, Flagstaff) – Technologically, discovery was possible decades earlier • Saturation of Pluto images masked the presence of Charon • 1988: Discovery of Pluto’s atmosphere – Stellar occultation • Kuiper airborne observatory (KAO: 90 cm) + 7 sites • Measured atmospheric refractivity vs. height • Spectroscopy suggested N2 would dominate P(z), T(z) • 1992: Pluto’s orbit explained • Outward migration by Neptune results in capture into 3:2 resonance • Pluto’s inclination implies Neptune migrated outward ~5 AU IAC Winter School 2016 -- Kuiper Belt Overview -- J. Stansberry 3 The Solar System beyond Neptune: History • 1992: Discovery of 2nd TNO • 1976 – 92: Multiple dedicated surveys for small (mV > 20) TNOs • Fall 1992: Jewitt and Luu discover 1992 QB1 – Orbit confirmed as ~circular, trans-Neptunian in 1993 • 1993 – 4: 5 more TNOs discovered • c. -
A Dwarf Planet Class Object in the 21:5 Resonance with Neptune
A dwarf planet class object in the 21:5 resonance with Neptune Holman, M. J., Payne, M. J., Fraser, W., Lacerda, P., Bannister, M. T., Lackner, M., Chen, Y. T., Lin, H. W., Smith, K. W., Kokotanekova, R., Young, D., Chambers, K., Chastel, S., Denneau, L., Fitzsimmons, A., Flewelling, H., Grav, T., Huber, M., Induni, N., ... Weryk, R. (2018). A dwarf planet class object in the 21:5 resonance with Neptune. Astrophysical Journal Letters, 855(1), [L6]. https://doi.org/10.3847/2041-8213/aaadb3 Published in: Astrophysical Journal Letters Document Version: Publisher's PDF, also known as Version of record Queen's University Belfast - Research Portal: Link to publication record in Queen's University Belfast Research Portal Publisher rights © 2018 American Astronomical Society. This work is made available online in accordance with the publisher’s policies. Please refer to any applicable terms of use of the publisher. General rights Copyright for the publications made accessible via the Queen's University Belfast Research Portal is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The Research Portal is Queen's institutional repository that provides access to Queen's research output. Every effort has been made to ensure that content in the Research Portal does not infringe any person's rights, or applicable UK laws. If you discover content in the Research Portal that you believe breaches copyright or violates any law, please contact [email protected]. -
Abstracts of the 50Th DDA Meeting (Boulder, CO)
Abstracts of the 50th DDA Meeting (Boulder, CO) American Astronomical Society June, 2019 100 — Dynamics on Asteroids break-up event around a Lagrange point. 100.01 — Simulations of a Synthetic Eurybates 100.02 — High-Fidelity Testing of Binary Asteroid Collisional Family Formation with Applications to 1999 KW4 Timothy Holt1; David Nesvorny2; Jonathan Horner1; Alex B. Davis1; Daniel Scheeres1 Rachel King1; Brad Carter1; Leigh Brookshaw1 1 Aerospace Engineering Sciences, University of Colorado Boulder 1 Centre for Astrophysics, University of Southern Queensland (Boulder, Colorado, United States) (Longmont, Colorado, United States) 2 Southwest Research Institute (Boulder, Connecticut, United The commonly accepted formation process for asym- States) metric binary asteroids is the spin up and eventual fission of rubble pile asteroids as proposed by Walsh, Of the six recognized collisional families in the Jo- Richardson and Michel (Walsh et al., Nature 2008) vian Trojan swarms, the Eurybates family is the and Scheeres (Scheeres, Icarus 2007). In this theory largest, with over 200 recognized members. Located a rubble pile asteroid is spun up by YORP until it around the Jovian L4 Lagrange point, librations of reaches a critical spin rate and experiences a mass the members make this family an interesting study shedding event forming a close, low-eccentricity in orbital dynamics. The Jovian Trojans are thought satellite. Further work by Jacobson and Scheeres to have been captured during an early period of in- used a planar, two-ellipsoid model to analyze the stability in the Solar system. The parent body of the evolutionary pathways of such a formation event family, 3548 Eurybates is one of the targets for the from the moment the bodies initially fission (Jacob- LUCY spacecraft, and our work will provide a dy- son and Scheeres, Icarus 2011). -
The Fate of Debris in the Pluto-Charon System
MNRAS 000,1{13 (2016) Preprint 6 August 2018 Compiled using MNRAS LATEX style file v3.0 The Fate of Debris in the Pluto-Charon System Rachel A. Smullen,1? Kaitlin M. Kratter,1 1Steward Observatory, University of Arizona, Tucson, AZ 85721, USA Accepted XXX. Received YYY; in original form ZZZ ABSTRACT The Pluto-Charon system has come into sharper focus following the fly by of New Horizons. We use N-body simulations to probe the unique dynamical history of this binary dwarf planet system. We follow the evolution of the debris disc that might have formed during the Charon-forming giant impact. First, we note that in-situ formation of the four circumbinary moons is extremely difficult if Charon undergoes eccentric tidal evolution. We track collisions of disc debris with Charon, estimating that hundreds to hundreds of thousands of visible craters might arise from 0.3{5 km radius bodies. New Horizons data suggesting a dearth of these small craters may place constraints on the disc properties. While tidal heating will erase some of the cratering history, both tidal and radiogenic heating may also make it possible to differentiate disc debris craters from Kuiper belt object craters. We also track the debris ejected from the Pluto-Charon system into the Solar System; while most of this debris is ultimately lost from the Solar System, a few tens of 10{30 km radius bodies could survive as a Pluto-Charon collisional family. Most are plutinos in the 3:2 resonance with Neptune, while a small number populate nearby resonances. We show that migration of the giant planets early in the Solar System's history would not destroy this collisional family. -
1 on the Origin of the Pluto System Robin M. Canup Southwest Research Institute Kaitlin M. Kratter University of Arizona Marc Ne
On the Origin of the Pluto System Robin M. Canup Southwest Research Institute Kaitlin M. Kratter University of Arizona Marc Neveu NASA Goddard Space Flight Center / University of Maryland The goal of this chapter is to review hypotheses for the origin of the Pluto system in light of observational constraints that have been considerably refined over the 85-year interval between the discovery of Pluto and its exploration by spacecraft. We focus on the giant impact hypothesis currently understood as the likeliest origin for the Pluto-Charon binary, and devote particular attention to new models of planet formation and migration in the outer Solar System. We discuss the origins conundrum posed by the system’s four small moons. We also elaborate on implications of these scenarios for the dynamical environment of the early transneptunian disk, the likelihood of finding a Pluto collisional family, and the origin of other binary systems in the Kuiper belt. Finally, we highlight outstanding open issues regarding the origin of the Pluto system and suggest areas of future progress. 1. INTRODUCTION For six decades following its discovery, Pluto was the only known Sun-orbiting world in the dynamical vicinity of Neptune. An early origin concept postulated that Neptune originally had two large moons – Pluto and Neptune’s current moon, Triton – and that a dynamical event had both reversed the sense of Triton’s orbit relative to Neptune’s rotation and ejected Pluto onto its current heliocentric orbit (Lyttleton, 1936). This scenario remained in contention following the discovery of Charon, as it was then established that Pluto’s mass was similar to that of a large giant planet moon (Christy and Harrington, 1978). -
Trans-Neptunian Space and the Post-Pluto Paradigm
Trans-Neptunian Space and the Post-Pluto Paradigm Alex H. Parker Department of Space Studies Southwest Research Institute Boulder, CO 80302 The Pluto system is an archetype for the multitude of icy dwarf planets and accompanying satellite systems that populate the vast volume of the solar system beyond Neptune. New Horizons’ exploration of Pluto and its five moons gave us a glimpse into the range of properties that their kin may host. Furthermore, the surfaces of Pluto and Charon record eons of bombardment by small trans-Neptunian objects, and by treating them as witness plates we can infer a few key properties of the trans-Neptunian population at sizes far below current direct-detection limits. This chapter summarizes what we have learned from the Pluto system about the origins and properties of the trans-Neptunian populations, the processes that have acted upon those members over the age of the solar system, and the processes likely to remain active today. Included in this summary is an inference of the properties of the size distribution of small trans-Neptunian objects and estimates on the fraction of binary systems present at small sizes. Further, this chapter compares the extant properties of the satellites of trans-Neptunian dwarf planets and their implications for the processes of satellite formation and the early evolution of planetesimals in the outer solar system. Finally, this chapter concludes with a discussion of near-term theoretical, observational, and laboratory efforts that can further ground our understanding of the Pluto system and how its properties can guide future exploration of trans-Neptunian space. -
ALMA Investigates 'Deedee,' a Distant, Dim Member of Our Solar System 12 April 2017
ALMA investigates 'DeeDee,' a distant, dim member of our solar system 12 April 2017 spherical, the criteria necessary for astronomers to consider it a dwarf planet, though it has yet to receive that official designation. "Far beyond Pluto is a region surprisingly rich with planetary bodies. Some are quite small but others have sizes to rival Pluto, and could possibly be much larger," said David Gerdes, a scientist with the University of Michigan and lead author on a paper appearing in the Astrophysical Journal Letters. "Because these objects are so distant and dim, it's incredibly difficult to even detect them, let Artist concept of the planetary body 2014 UZ224, more alone study them in any detail. ALMA, however, informally known as DeeDee. ALMA was able to observe has unique capabilities that enabled us to learn the faint millimeter-wavelength "glow" emitted by the exciting details about these distant worlds." object, confirming it is roughly 635 kilometers across. At this size, DeeDee should have enough mass to be Currently, DeeDee is about 92 astronomical units spherical, the criteria necessary for astronomers to (AU) from the Sun. An astronomical unit is the consider it a dwarf planet, though it has yet to receive average distance from the Earth to the Sun, or that official designation. Credit: Alexandra Angelich (NRAO/AUI/NSF) about 150 million kilometers. At this tremendous distance, it takes DeeDee more than 1,100 years to complete one orbit. Light from DeeDee takes nearly 13 hours to reach Earth. Using the Atacama Large Millimeter/submillimeter Array (ALMA), astronomers have revealed Gerdes and his team announced the discovery of extraordinary details about a recently discovered DeeDee in the fall of 2016. -
A DEEP SEARCH for ADDITIONAL SATELLITES AROUND the DWARF PLANET HAUMEA Luke D
The Astronomical Journal, 151:162 (10pp), 2016 June doi:10.3847/0004-6256/151/6/162 © 2016. The American Astronomical Society. All rights reserved. A DEEP SEARCH FOR ADDITIONAL SATELLITES AROUND THE DWARF PLANET HAUMEA Luke D. Burkhart1,2, Darin Ragozzine1,3,4, and Michael E. Brown5 1 Harvard-Smithsonian Center for Astrophysics, 60 Garden Street, Cambridge, MA 02138, USA; [email protected] 2 Yale University, Department of Physics, 217 Prospect Street, New Haven, CT 06511, USA 3 University of Florida, 211 Bryant Space Science Center, Gainesville, FL 32611, USA 4 Florida Institute of Technology, Department of Physics and Space Sciences, 150 West University Boulevard, Melbourne, FL 32901, USA 5 California Institute of Technology, Division of Geological and Planetary Sciences, MC 150-21, Pasadena, CA 91125, USA Received 2015 July 10; accepted 2016 March 27; published 2016 May 27 ABSTRACT Haumea is a dwarf planet with two known satellites, an unusually high spin rate, and a large collisional family, making it one of the most interesting objects in the outer solar system. A fully self-consistent formation scenario responsible for the satellite and family formation is still elusive, but some processes predict the initial formation of many small moons, similar to the small moons recently discovered around Pluto. Deep searches for regular satellites around Kuiper belt objects are difficult due to observational limitations, but Haumea is one of the few for which sufficient data exist. We analyze Hubble Space Telescope (HST) observations, focusing on a 10- consecutive-orbit sequence obtained in 2010 July, to search for new very small satellites. -
On a Scattered-Disk Origin for The
ON A SCATTERED-DISK ORIGIN FOR THE 2003 EL61 COLLISIONAL FAMILY - AN EXAMPLE OF THE IMPORTANCE OF COLLISIONS ON THE DYNAMICS OF SMALL BODIES Harold Levison, Morbidelli Alessandro, David Vokrouhlicky, William Bottke To cite this version: Harold Levison, Morbidelli Alessandro, David Vokrouhlicky, William Bottke. ON A SCATTERED- DISK ORIGIN FOR THE 2003 EL61 COLLISIONAL FAMILY - AN EXAMPLE OF THE IM- PORTANCE OF COLLISIONS ON THE DYNAMICS OF SMALL BODIES. Astronomical Journal, American Astronomical Society, 2008, in press. hal-00316161 HAL Id: hal-00316161 https://hal.archives-ouvertes.fr/hal-00316161 Submitted on 2 Sep 2008 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. ON A SCATTERED-DISK ORIGIN FOR THE 2003 EL61 COLLISIONAL FAMILY — AN EXAMPLE OF THE IMPORTANCE OF COLLISIONS ON THE DYNAMICS OF SMALL BODIES Harold F. Levison Southwest Research Institute 1050 Walnut St, Suite 300 Boulder, CO 80302 [email protected] Alessandro Morbidelli Observatoire de la Cˆote d’Azur Boulevard de l’Observatoire B.P. 4229, 06304 Nice Cedex 4, France David Vokrouhlick´y Institute of Astronomy, Charles University V Holeˇsoviˇck´ach 2 18000 Prague 8, Czech Republic and William F. -
The Formation of the Collisional Family Around the Dwarf Planet Haumea
The Astrophysical Journal, 714:1789–1799, 2010 May 10 doi:10.1088/0004-637X/714/2/1789 C 2010. The American Astronomical Society. All rights reserved. Printed in the U.S.A. THE FORMATION OF THE COLLISIONAL FAMILY AROUND THE DWARF PLANET HAUMEA Zoe¨ M. Leinhardt1, Robert A. Marcus2, and Sarah T. Stewart3 1 Department of Applied Mathematics and Theoretical Physics, University of Cambridge, CB3 0WA, UK; [email protected] 2 Astronomy Department, Harvard University, 60 Garden Street, Cambridge, MA 02138, USA 3 Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, MA 02138, USA Received 2009 November 5; accepted 2010 March 23; published 2010 April 22 ABSTRACT Haumea, a rapidly rotating elongated dwarf planet (∼1500 km in diameter), has two satellites and is associated with a “family” of several smaller Kuiper Belt objects (KBOs) in similar orbits. All members of the Haumea system share a water ice spectral feature that is distinct from all other KBOs. The relative velocities between the Haumea family members are too small to have formed by catastrophic disruption of a large precursor body, which is the process that formed families around much smaller asteroids in the main belt. Here, we show that all of the unusual characteristics of the Haumea system are explained by a novel type of giant collision: a graze and merge impact between two comparably sized bodies. The grazing encounter imparted the high angular momentum that spun off fragments from the icy crust of the elongated merged body. The fragments became satellites and family members. -
JWST Planetary Observations Within the Solar System
JWST Planetary Observations within the Solar System Jonathan Lunine Department of Physics The University of Rome, Tor Vergata Heidi Hammel Space Science Institute, Boulder, CO Emily Schaller Lunar and Planetary Laboratory The University of Arizona George Sonneborn NASA Goddard Space Flight Center Glenn Orton NASA Jet Propulsion Laboratory California Institute of Technology George Rieke Steward Observatory, The University of Arizona Marcia Rieke Steward Observatory, The University of Arizona March 9, 2010 1 Abstract JWST provides capabilities unmatched by other telescopic facilities in the near to mid infrared part of the electromagnetic spectrum. Its combination of broad wavelength range, high sensitivity and near diffraction-limited imaging around two microns wavelength make it a high value facility for a variety of Solar System targets. Beyond Neptune, a class of cold, large bodies that include Pluto, Triton and Eris exhibits surface deposits of nitrogen, methane, and other molecules that are poorly observed from the ground, but for which JWST might provide spectral mapping at high sensitivity and spatial resolution difficult to match with the current generation of ground-based observatories. The observatory will also provide unique sensitivity in a variety of near and mid infrared windows for observing relatively deep into the atmospheres of Uranus and Neptune, searching there for minor species. It will examine the Jovian aurora in a wavelength regime where the background atmosphere is dark. Special provision of a sub- array observing strategy may allow observation of Jupiter and Saturn over a larger wavelength range despite their large surface brightnesses, allowing for detailed observation of transient phenomena including large scale storms and impact-generation disturbances. -
On the Origin of the Pluto System
Pluto System After New Horizons 2019 (LPI Contrib. No. 2133) 7027.pdf ON THE ORIGIN OF THE PLUTO SYSTEM. M. Neveu1,2, R. M. Canup3, and K. M. Kratter4, 1U. of Mary- land, College Park, MD, USA. 2NASA Goddard Space Flight Center, Greenbelt, MD, USA ([email protected]). 3Southwest Research Institute, Boulder, CO, USA ([email protected]). 4Astronomy Department / Steward Observatory, U. of Arizona, Tucson, AZ, USA ([email protected]). Introduction: We describe constraints and review Giant impact. The Pluto-Charon binary’s low mass models for the origin of the Pluto-Charon binary and ratio, high angular momentum, and close separation the small moons Styx, Nix, Kerberos and Hydra. We makes an impact on Pluto from a like-sized impactor also highlight open issues and discuss implications. its prime origin scenario [19-21 and references there- Observational Constraints: The heliocentric or- in]. This impact must predate Charon’s ≈4 Gyr old bit of the Pluto system at ≈40 AU is triply resonant surface [22]. At ≈40 AU, binary-forming impacts with Neptune’s orbit, involving mean motions (3:2), could have occurred every 100-300 Myr [23], and arguments of perihelion, and longitudes of ascending likely more often closer in. The mass ratio is repro- node. Therefore, Neptune likely shaped the Pluto sys- duced with an impact velocity only slightly higher tem’s eccentric and inclined heliocentric orbit [1,2]. than proto-Pluto’s escape velocity [20]. Two scenari- System dynamics. The plane of the Pluto system is os yield the observed mass and angular momentum highly oblique to its heliocentric orbit.