Trans-Neptunian Space and the Post-Pluto Paradigm
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Planetary Geologic Mappers Annual Meeting
Program Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 Planetary Geologic Mappers Annual Meeting June 12–14, 2018 • Knoxville, Tennessee Institutional Support Lunar and Planetary Institute Universities Space Research Association Convener Devon Burr Earth and Planetary Sciences Department, University of Tennessee Knoxville Science Organizing Committee David Williams, Chair Arizona State University Devon Burr Earth and Planetary Sciences Department, University of Tennessee Knoxville Robert Jacobsen Earth and Planetary Sciences Department, University of Tennessee Knoxville Bradley Thomson Earth and Planetary Sciences Department, University of Tennessee Knoxville Abstracts for this meeting are available via the meeting website at https://www.hou.usra.edu/meetings/pgm2018/ Abstracts can be cited as Author A. B. and Author C. D. (2018) Title of abstract. In Planetary Geologic Mappers Annual Meeting, Abstract #XXXX. LPI Contribution No. 2066, Lunar and Planetary Institute, Houston. Guide to Sessions Tuesday, June 12, 2018 9:00 a.m. Strong Hall Meeting Room Introduction and Mercury and Venus Maps 1:00 p.m. Strong Hall Meeting Room Mars Maps 5:30 p.m. Strong Hall Poster Area Poster Session: 2018 Planetary Geologic Mappers Meeting Wednesday, June 13, 2018 8:30 a.m. Strong Hall Meeting Room GIS and Planetary Mapping Techniques and Lunar Maps 1:15 p.m. Strong Hall Meeting Room Asteroid, Dwarf Planet, and Outer Planet Satellite Maps Thursday, June 14, 2018 8:30 a.m. Strong Hall Optional Field Trip to Appalachian Mountains Program Tuesday, June 12, 2018 INTRODUCTION AND MERCURY AND VENUS MAPS 9:00 a.m. Strong Hall Meeting Room Chairs: David Williams Devon Burr 9:00 a.m. -
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]. -
Motivation Sputnik Planitia Flexural Modeling Plans for GEOL
Motivation Sputnik Planitia Flexural modeling Sputnik Planitia Flexure model • Large teardrop-shaped basin The flexure of an elastic plate in two dimensions obeys Equation 1 located on Pluto at 20°N 180°E 푑4푤 퐷 + 푚 − 푐 푔푤 = 푉0 Equation 1. • Size: 1300 km by 900 km 푑푥4 4퐷 1/4 퐸∗ℎ3 • Depth: 3-4 km (basin) where 훼 = is the flexural parameter, 퐷 = is the flexural rigidity, is the 휌 −휌 12(1−푣2) 푚 • 푚 푐 Deposit of nitrogen ice density of the underlying layer of the ice shell, is the density of the ice shell. g is the gravity on • 푐 Water ice basement Pluto, E is the Young’s modulus of water ice, h is the elastic thickness, and 휈 is Poisson’s ratio 푑3푤 1 푑푤 For a single vertical load at 푥 = 0 , the boundary conditions are 퐷 = 푉 and = 0 Formation Hypotheses 푑푥3 2 0 푑푥 • An ancient impact basin created The deflection due to several line loads is found by superposition: 푉 훼3 푥−푥 푥−푥 푥−푥 by an impactor later filled with 푤 = σ 푖 sin 푖 + cos 푖 exp − 푖 Equation 2. 푖 8퐷 훼 훼 훼 N2 ice. The feature would have moved to the current location Where {푉푖} is the magnitude of the loads at position {푥푖} through polar wander. • Runaway deposition of N2 ice Inversion due to albedo feedback at the The load vector 퐕 that produces topography 퐰, is found by least squares optimization: ±30°. The depression is due to 퐕 = 퐌′퐌 + 퐂 −1 퐌′퐰 elastic flexure under the load of 풎 where M is the operator matrix that links a load at position 푥푗 to deflection at a point 푥푖 a thick N2 ice cap. -
Martian Crater Morphology
ANALYSIS OF THE DEPTH-DIAMETER RELATIONSHIP OF MARTIAN CRATERS A Capstone Experience Thesis Presented by Jared Howenstine Completion Date: May 2006 Approved By: Professor M. Darby Dyar, Astronomy Professor Christopher Condit, Geology Professor Judith Young, Astronomy Abstract Title: Analysis of the Depth-Diameter Relationship of Martian Craters Author: Jared Howenstine, Astronomy Approved By: Judith Young, Astronomy Approved By: M. Darby Dyar, Astronomy Approved By: Christopher Condit, Geology CE Type: Departmental Honors Project Using a gridded version of maritan topography with the computer program Gridview, this project studied the depth-diameter relationship of martian impact craters. The work encompasses 361 profiles of impacts with diameters larger than 15 kilometers and is a continuation of work that was started at the Lunar and Planetary Institute in Houston, Texas under the guidance of Dr. Walter S. Keifer. Using the most ‘pristine,’ or deepest craters in the data a depth-diameter relationship was determined: d = 0.610D 0.327 , where d is the depth of the crater and D is the diameter of the crater, both in kilometers. This relationship can then be used to estimate the theoretical depth of any impact radius, and therefore can be used to estimate the pristine shape of the crater. With a depth-diameter ratio for a particular crater, the measured depth can then be compared to this theoretical value and an estimate of the amount of material within the crater, or fill, can then be calculated. The data includes 140 named impact craters, 3 basins, and 218 other impacts. The named data encompasses all named impact structures of greater than 100 kilometers in diameter. -
What Is the Color of Pluto? - Universe Today
What is the Color of Pluto? - Universe Today space and astronomy news Universe Today Home Members Guide to Space Carnival Photos Videos Forum Contact Privacy Login NASA’s New Horizons spacecraft captured this high-resolution enhanced color view of http://www.universetoday.com/13866/color-of-pluto/[29-Mar-17 13:18:37] What is the Color of Pluto? - Universe Today Pluto on July 14, 2015. Credit: NASA/JHUAPL/SwRI WHAT IS THE COLOR OF PLUTO? Article Updated: 28 Mar , 2017 by Matt Williams When Pluto was first discovered by Clybe Tombaugh in 1930, astronomers believed that they had found the ninth and outermost planet of the Solar System. In the decades that followed, what little we were able to learn about this distant world was the product of surveys conducted using Earth-based telescopes. Throughout this period, astronomers believed that Pluto was a dirty brown color. In recent years, thanks to improved observations and the New Horizons mission, we have finally managed to obtain a clear picture of what Pluto looks like. In addition to information about its surface features, composition and tenuous atmosphere, much has been learned about Pluto’s appearance. Because of this, we now know that the one-time “ninth planet” of the Solar System is rich and varied in color. Composition: With a mean density of 1.87 g/cm3, Pluto’s composition is differentiated between an icy mantle and a rocky core. The surface is composed of more than 98% nitrogen ice, with traces of methane and carbon monoxide. Scientists also suspect that Pluto’s internal structure is differentiated, with the rocky material having settled into a dense core surrounded by a mantle of water ice. -
Martian Subsurface Properties and Crater Formation Processes Inferred from Fresh Impact Crater Geometries
Martian Subsurface Properties and Crater Formation Processes Inferred From Fresh Impact Crater Geometries The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Stewart, Sarah T., and Gregory J. Valiant. 2006. Martian subsurface properties and crater formation processes inferred from fresh impact crater geometries. Meteoritics and Planetary Sciences 41: 1509-1537. Published Version http://meteoritics.org/ Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:4727301 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA Meteoritics & Planetary Science 41, Nr 10, 1509–1537 (2006) Abstract available online at http://meteoritics.org Martian subsurface properties and crater formation processes inferred from fresh impact crater geometries Sarah T. STEWART* and Gregory J. VALIANT Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, Massachusetts 02138, USA *Corresponding author. E-mail: [email protected] (Received 22 October 2005; revision accepted 30 June 2006) Abstract–The geometry of simple impact craters reflects the properties of the target materials, and the diverse range of fluidized morphologies observed in Martian ejecta blankets are controlled by the near-surface composition and the climate at the time of impact. Using the Mars Orbiter Laser Altimeter (MOLA) data set, quantitative information about the strength of the upper crust and the dynamics of Martian ejecta blankets may be derived from crater geometry measurements. -
Minor Body Science with the Nancy Grace Roman Space Telescope
! Minor Body Science with the Nancy Grace Roman Space Telescope Bryan J. Holler (STScI)*, Stefanie N. Milam (NASA/GSFC), James M. Bauer (U. Maryland), Jeffrey W. Kruk (NASA/GSFC), Charles Alcock (Harvard/CfA), Michele T. Bannister (U. of Canterbury), Gordon L. Bjoraker (NASA/GSFC), Dennis Bodewits (Auburn), Amanda S. Bosh (MIT), Marc W. Buie (SwRI), Tony L. Farnham (UMD), Nader Haghighipour (Hawaii/IfA), Paul S. Hardersen (Unaffiliated), Alan W. Harris (MoreData! Inc.), Christopher M. Hirata (Ohio State), Henry H. Hsieh (PSI, Academica Sinica), Michael S. P. Kelley (U. Maryland), Matthew M. Knight (USNA/U. Maryland), Emily A. Kramer (Caltech/JPL), Andrea Longobardo (INAF/IAPS), Conor A. Nixon (NASA/GSFC), Ernesto Palomba (INAF/IAPS), Silvia Protopapa (SwRI), Lynnae C. Quick (Smithsonian), Darin Ragozzine (BYU), Jason D. Rhodes (Caltech/JPL), Andy S. Rivkin (JHU/APL), Gal Sarid (SETI, Science Systems and Applications, Inc.), Amanda A. Sickafoose (SAAO, MIT), Cristina A. Thomas (NAU), David E. Trilling (NAU), Robert A. West (Caltech/JPL) *Contact information for primary author: Bryan J. Holler (STScI), [email protected], (667) 218-6404 Thematic areas: Ground- and space-based telescopes, Primitive bodies Solar system science with space telescopes There is a long history of solar system observations with space telescope facilities, from the Infrared Astronomical Satellite (IRAS) in the 1980s to present-day facilities such as the Hubble Space Telescope. Some of these facilities include a prominent solar system component as part of the original mission plan (e.g., WISE, JWST), some included this component late in mission design or even after primary operations begin (e.g., HST), and others never intended to support solar system observations until the proper opportunity arose (e.g., Kepler, Chandra). -
The Impact of Star Cluster Environments on Planet Formation
The Impact of Star Cluster Environments on Planet Formation Rhana Bethany Nicholson A thesis submitted in partial fulfilment of the requirements of Liverpool John Moores University for the degree of Doctor of Philosophy June 2019 i Declaration of Authorship I, Rhana Bethany Nicholson, declare that this thesis titled, “The Impact of Star Cluster Environments on Planet Formation” and the work presented in it are my own. I confirm that: • This work was done wholly or mainly while in candidature for a research degree at this University. • Where any part of this thesis has previously been submitted for a degree or any other qualification at this University or any other institution, this has been clearly stated. • Where I have consulted the published work of others, this is always clearly attributed. • Where I have quoted from the work of others, the source is always given. With the exception of such quotations, this thesis is entirely my own work. • I have acknowledged all main sources of help. • Where the thesis is based on work done by myself jointly with others, I have made clear exactly what was done by others and what I have contributed myself. Signed: Date: ii To Mum and Dad, for making me do Kumon. iii “For all the tenure of humans on Earth, the night sky has been a companion and an inspiration... At the very moment that humans discovered the scale of the Universe and found that their most unconstrained fancies were in fact dwarfed by the true dimensions of even the Milky Way Galaxy, they took steps that ensured that their descendants would be unable to see the stars at all...” - Carl Sagan, Contact iv Acknowledgements Firstly I must begin by thanking my supervisor, Richard Parker, without whom this thesis would most definitely not exist. -
Results from the New Horizons Encounter with Pluto
EPSC Abstracts Vol. 11, EPSC2017-140, 2017 European Planetary Science Congress 2017 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2017 Results from the New Horizons encounter with Pluto C. B. Olkin (1), S. A. Stern (1), J. R. Spencer (1), H. A. Weaver (2), L. A. Young (1), K. Ennico (3) and the New Horizons Team (1) Southwest Research Institute, Colorado, USA, (2) Johns Hopkins University Applied Physics Laboratory, Maryland, USA (3) NASA Ames Research Center, California, USA ([email protected]) Abstract Hydra) and the various processes that would darken those surfaces over time [5]. In July 2015, the New Horizons spacecraft flew through the Pluto system providing high spatial resolution panchromatic and color visible light imaging, near-infrared composition mapping spectroscopy, UV airglow measurements, UV solar and radio uplink occultations for atmospheric sounding, and in situ plasma and dust measurements that have transformed our understanding of Pluto and its moons [1]. Results from the science investigations focusing on geology, surface composition and atmospheric studies of Pluto and its largest satellite Charon will be presented. We also describe the New Horizons extended mission. 1. Geology and Size Highlights from the geology investigation of Pluto Figure 1: The glacial ices of Sputnik Planitia. The include the discovery of a unexpected diversity of cellular pattern is a surface expression of mobile lid geomorpholgies across the surface, the discovery of a convection. The boundaries of the cells are troughs. deep basin (informally known as Sputnik Planitia) Despite it’s size of ~900,000 km2, there are no containing glacial ices undergoing mobile-lid identified craters across Sputnik Planitia. -
Redalyc.Búsqueda General Con La Cámara Mosaico CCD Del
Revista Mexicana de Física ISSN: 0035-001X [email protected] Sociedad Mexicana de Física A.C. México Ferrín, I.; Leal, C.; Hernandez, J. Búsqueda general con la cámara mosaico CCD del telescopio Schmidt de 1m del Observatorio Nacional de Venezuela Revista Mexicana de Física, vol. 52, núm. 3, mayo, 2006, pp. 9-11 Sociedad Mexicana de Física A.C. Distrito Federal, México Disponible en: http://www.redalyc.org/articulo.oa?id=57020393003 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto ASTROFISICA´ REVISTA MEXICANA DE FISICA´ S 52 (3) 9–11 MAYO 2006 Busqueda´ general con la camara´ mosaico CCD del telescopio Schmidt de 1m del Observatorio Nacional de Venezuela I. Ferr´ın y C. Leal Facultad de Ciencias, Departamento de F´ısica, Centro de Astrof´ısica Teorica,´ Universidad de Los Andes Merida,´ Venezuela J. Hernandez Centro de investigaciones de astronom´ıa, CIDA, Merida,´ Venezuela Recibido el 25 de noviembre de 2003; aceptado el 12 de octubre de 2004 En el presente trabajo se muestran los resultados del programa de busqueda´ y seguimiento de diversos objetos astronomicos:´ estrellas variables, supernovas y objetos en movimiento dentro del Sistema Solar. Para ello estamos utilizando el telescopio Schmidt de 1m de diametro´ del Observatorio Nacional de Venezuela, el cual tiene acoplado una camara´ mosaico CCD de 67 Megap´ıxeles, en un arreglo de 4 £ 4 CCDs, cada uno de 2048 £ 2048 p´ıxeles. -
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). -
Artificial Intelligence at the Jet Propulsion Laboratory
AI Magazine Volume 18 Number 1 (1997) (© AAAI) Articles Making an Impact Artificial Intelligence at the Jet Propulsion Laboratory Steve Chien, Dennis DeCoste, Richard Doyle, and Paul Stolorz ■ The National Aeronautics and Space Administra- described here is in the context of the remote- tion (NASA) is being challenged to perform more agent autonomy technology experiment that frequent and intensive space-exploration mis- will fly on the New Millennium Deep Space sions at greatly reduced cost. Nowhere is this One Mission in 1998 (a collaborative effort challenge more acute than among robotic plane- involving JPL and NASA Ames). Many of the tary exploration missions that the Jet Propulsion AI technologists who work at NASA expected Laboratory (JPL) conducts for NASA. This article describes recent and ongoing work on spacecraft to have the opportunity to build an intelli- autonomy and ground systems that builds on a gent spacecraft at some point in their careers; legacy of existing success at JPL applying AI tech- we are surprised and delighted that it has niques to challenging computational problems in come this early. planning and scheduling, real-time monitoring By the year 2000, we expect to demonstrate and control, scientific data analysis, and design NASA spacecraft possessing on-board automat- automation. ed goal-level closed-loop control in the plan- ning and scheduling of activities to achieve mission goals, maneuvering and pointing to execute these activities, and detecting and I research and technology development resolving of faults to continue the mission reached critical mass at the Jet Propul- without requiring ground support. At this Asion Laboratory (JPL) about five years point, mission accomplishment can begin to ago.