Exploring the Origins and Evolution of Ice Giant Planets
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7 Planetary Rings Matthew S
7 Planetary Rings Matthew S. Tiscareno Center for Radiophysics and Space Research, Cornell University, Ithaca, NY, USA 1Introduction..................................................... 311 1.1 Orbital Elements ..................................................... 312 1.2 Roche Limits, Roche Lobes, and Roche Critical Densities .................... 313 1.3 Optical Depth ....................................................... 316 2 Rings by Planetary System .......................................... 317 2.1 The Rings of Jupiter ................................................... 317 2.2 The Rings of Saturn ................................................... 319 2.3 The Rings of Uranus .................................................. 320 2.4 The Rings of Neptune ................................................. 323 2.5 Unconfirmed Ring Systems ............................................. 324 2.5.1 Mars ............................................................... 324 2.5.2 Pluto ............................................................... 325 2.5.3 Rhea and Other Moons ................................................ 325 2.5.4 Exoplanets ........................................................... 327 3RingsbyType.................................................... 328 3.1 Dense Broad Disks ................................................... 328 3.1.1 Spiral Waves ......................................................... 329 3.1.2 Gap Edges and Moonlet Wakes .......................................... 333 3.1.3 Radial Structure ..................................................... -
Planetary Ring Systems Edited by Matthew S
Cambridge University Press 978-1-107-11382-4 — Planetary Ring Systems Edited by Matthew S. Tiscareno , Carl D. Murray Frontmatter More Information Planetary Ring Systems Properties, Structure, and Evolution Planetary rings are among the most intriguing structures of our solar system and have fas- cinated generations of astronomers. Collating emerging knowledge in the field, this volume reviews our current understanding of ring systems with reference to the rings of Saturn, Uranus, Neptune, and more. Written by leading experts, the history of ring research and the basics of ring-particle orbits is followed by a review of the known planetary ring sys- tems. All aspects of ring system science are described in detail, including specific dynamical processes, types of structures, thermal properties, their origins, and investigations using com- puter simulations and laboratory experiments. The concluding chapters discuss the prospects of future missions to planetary rings, the ways in which ring science informs and is informed by the study of other astrophysical disks, and a perspective on the field’s future. Researchers of all levels benefit from this thorough and engaging presentation. MATTHEW S. TISCARENO is a Senior Research Scientist at the SETI Institute, California. He is a Participating Scientist and an Imaging Team Associate with the Cassini- Huygens mission. His research output includes solar system dynamics and space-based observations of the outer solar system. CARL D. MURRAYis Professor of Mathematics and Astronomy at Queen Mary Univer- sity of London. He has contributed to numerous ring and moon discoveries as an original member of the Imaging Team with the Cassini-Huygens mission and he is co-author of the textbook Solar System Dynamics (1999). -
Neptune and Uranus: Ice Or Rock Giants? Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 378(2187)
Teanby, N. A., Irwin, P. G. J., Moses, J. I., & Helled, R. (2020). Neptune and Uranus: ice or rock giants? Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 378(2187). https://doi.org/10.1098/rsta.2019.0489 Peer reviewed version Link to published version (if available): 10.1098/rsta.2019.0489 Link to publication record in Explore Bristol Research PDF-document This is the author accepted manuscript (AAM). The final published version (version of record) is available online via The Royal Society at https://royalsocietypublishing.org/doi/10.1098/rsta.2019.0489 . Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Submitted to Phil. Trans. R. Soc. A - Issue Page 2 of 19 1 2 3 4 5 Neptune and Uranus: ice or 6 7 rock giants? 8 rsta.royalsocietypublishing.org 1 2 3 9 N. A. Teanby , P. G. J. Irwin , J. I. Moses 10 4 11 and R. Helled 12 1 13 Research School of Earth Sciences, University of Bristol, Wills 14 Memorial Building, Queens Road, Bristol, BS8 1RJ, UK 15 2Atmospheric, Oceanic & Planetary Physics, University Article submitted to journal 16 of Oxford, Clarendon Laboratory, Parks Road, Oxford, 17 18 OX1 3PU. UK. 3 19 Subject Areas: Space Science Institute, 4750 Walnut Street, Suite 20 Solar System, Planetary Interiors,For Review205, Boulder, Only CO 80301, USA. -
Uranus Pathfinder: Exploring the Origins and Evolution of Ice Giant Planets
EPSC Abstracts Vol. 7 EPSC2012-660 2012 European Planetary Science Congress 2012 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2012 Uranus Pathfinder: Exploring the Origins and Evolution of Ice Giant Planets C.S. Arridge (1,2) for the Uranus Pathfinder Consortium (1) Mullard Space Science Laboratory, University College London, UK, (2) The Centre for Planetary Sciences at UCL/Birkbeck, London, UK ([email protected]) Abstract In this paper we discuss this European effort to explore Uranus and outline ongoing developments of The “Ice Giants” Uranus and Neptune are a different the mission concept. class of planet compared to Jupiter and Saturn. Studying these objects is important for furthering our References understanding of the formation and evolution of the planets, and unravelling the fundamental physical [1] Arridge, C.S., et al.: Uranus Pathfinder: Exploring the and chemical processes in the Solar System. The origins and evolution of ice giant planets, Exp. Astron., doi: 10.1007/s10686-011-9251-4, 2012. importance of filling these gaps in our knowledge of the Solar System is particularly acute when trying to apply our understanding to the numerous planetary systems that have been discovered around other stars. The Uranus Pathfinder (UP) mission [1] thus represents the quintessential aspects of the objectives of the European planetary community as expressed in ESA’s Cosmic Vision 2015–2025. UP was proposed to the European Space Agency’s M3 call for medium-class missions in 2010 and proposed to be the first orbiter of an Ice Giant planet. As the most accessible Ice Giant within the M-class mission envelope Uranus was identified as the mission target. -
Weighing Uranus' Moon Cressida with the Η Ring
The Astronomical Journal, 154:153 (8pp), 2017 October https://doi.org/10.3847/1538-3881/aa880e © 2017. The American Astronomical Society. All rights reserved. Weighing Uranus’ Moon Cressida with the η Ring Robert O. Chancia1 , Matthew M. Hedman1 , and Richard G. French2 1 Department of Physics, University of Idaho, Moscow, ID 83844-0903, USA; [email protected] 2 Astronomy Department, Wellesley College, Wellesley, MA 02481, USA Received 2017 June 19; revised 2017 August 9; accepted 2017 August 21; published 2017 September 20 Abstract The η ring is one of the narrow rings of Uranus, consisting of a dense core that is 1–2 km wide and a diffuse outer sheet spanning about 40 km. Its dense core lies just exterior to the 3:2 Inner Lindblad Resonance of the small moon Cressida. We fit the η ring radius residuals and longitudes from a complete set of both ground-based and Voyager stellar and radio occultations of the Uranian rings spanning 1977–2002. We find variations in the radial position of the η ring that are likely generated by this resonance, and take the form of a 3-lobed structure rotating at an angular rate equal to the mean motion of the moon Cressida. The amplitude of these radial oscillations is 0.667±0.113 km, which is consistent with the expected shape due to the perturbations from Cressida. The magnitude of these variations provides the first measurement of the mass and density of the moon Cressida (m =´()2.5 0.4 1017 kg and r =0.86 0.16 gcm−3) or, indeed, any of Uranus’ small inner moons. -
Arxiv:1509.00872V1 [Astro-Ph.EP] 2 Sep 2015 H Bevblt Fipcso in Xpaes H Oe Matc Impact Comet the Exoplanets
Detectability of Planetesimal Impacts on Giant Exoplanets Laura Flagga,b,∗, Alycia J. Weinbergerb, Keith Matthewsc aDepartment of Physics and Astronomy, Northern Arizona University, Flagstaff, AZ 86011-6010, USA bDepartment of Terrestrial Magnetism, Carnegie Institution of Washington, 5241 Broad Branch Road NW, Washington, DC 20015, USA cCaltech Optical Observatories, California Institute of Technology, MC 301-17, Pasadena, CA 91125, USA Abstract The detectability of planetesimal impacts on imaged exoplanets can be measured using Jupiter during the 1994 comet Shoemaker-Levy 9 events as a proxy. By integrating the whole planet flux with and without impact spots, the effect of the impacts at wavelengths from 2 - 4 µm is revealed. Jupiter’s reflected light spectrum in the near-infrared is dominated by its methane opacity including a deep band at 2.3 µm. After the impact, sunlight that would have normally been absorbed by the large amount of methane in Jupiter’s atmosphere was instead reflected by the cometary material from the impacts. As a result, at 2.3 µm, where the planet would normally have low reflectivity, it brightened substantially and stayed brighter for at least a month. Keywords: comets, debris disks, extra-solar planets, Jupiter 1. Introduction The frequencies with which giant planets and cold circumstellar debris disks encircle old (i.e. >1 Gyr) Sun-like stars are both ∼20% (Eiroa et al. 2013; Marshall et al. 2014). The debris disks are generated in the collisions and evaporation of planetesimals, analogous to the comets and asteroids of today’s Solar System. That most debris disks contain cold, ∼50 K, dust indicates that the reservoirs of parent bodies are at ∼100 AU from the parent stars, in a region analogous to our Edgeworth-Kuiper Belt. -
The Mystery and Majesty
The mystery and majesty Nearly 40 years after THE SPACE AGE BLASTED off when the Soviet Union launched the Voyager 2 visited Uranus world’s first artificial satellite in 1957. Since then, humanity has explored our cosmic and Neptune, scientists are backyard with vigor — and yet two planets have fallen to the planetary probe wayside. eager for new expeditions. In the 63 years since Sputnik, humanity has only visited Neptune and Uranus once BY JOEL DAVIS — when Voyager 2 flew past Uranus in January 1986 and Neptune in August 1989 40 ASTRONOMY • DECEMBER 2020 of the ICE GIANTS — and even that wasn’t entirely pre- interstellar mission, more than a dozen pro- In 1781, Uranus became the first planet planned. The unmitigated success of posals have been offered for return missions ever discovered using a telescope. Nearly 200 years later, Voyager 2 Voyager 1 and 2 on their original mission to one or both ice giants. So far, none have became the first spacecraft to visit to explore Jupiter and Saturn earned the made it past the proposal stage due to lack Uranus and Neptune, in 1986 and 1989 respectively. NASA/JPL twin spacecrafts further missions in our of substantial scientific interest. Effectively, solar system and beyond, with Neptune and the planetary research community has been Uranus acting as the last stops on a Grand giving the ice giants the cold shoulder. Tour of the outer solar system. But recently, exoplanet data began In the 31 years since Voyager 2 left the revealing the abundance of icy exoplanets Neptune system in 1989 and began its in our galaxy “and new questions about WWW.ASTRONOMY.COM 41 With a rotation axis tilted more than 90 degrees compared to its orbital plane, Neptune likewise has a highly tilted rotation axis and tilted magnetic axis. -
Uranus, Neptune, Pluto, and the Outer Solar System Linda T
Uranus, Neptune, Pluto, and the Outer Solar System Linda T. Elkins-Tanton Uranus, Neptune, Pluto, and the Outer Solar System Copyright © 2006 by Linda T.Elkins-Tanton All rights reserved. No part of this book may be reproduced or utilized in any form or by any means, electronic or mechani- cal, including photocopying, recording, or by any information storage or retrieval systems, without permission in writing from the publisher. For information contact: Chelsea House An imprint of Infobase Publishing 132 West 31st Street New York NY 10001 Library of Congress Cataloging-in-Publication Data Elkins-Tanton, Linda T. Uranus, Neptune, Pluto, and the outer solar system / Linda T.Elkins-Tanton. p. cm. — (The Solar system) Includes bibliographical references and index. ISBN 0-8160-5197-6 (acid-free paper) 1. Uranus (Planet)—Popular works. 2. Neptune (Planet)—Popular works. 3. Pluto (Planet)—Popular works. 4. Solar system—Popular works. I.Title. QB681.E45 2006 523.47—dc22 2005014801 Chelsea House books are available at special discounts when purchased in bulk quantities for businesses, associations, institu- tions, or sales promotions. Please call our Special Sales Department in New York at (212) 967-8800 or (800) 322-8755. You can find Chelsea House on the World Wide Web at http://www.chelseahouse.com Text and cover design by Dorothy M. Preston Illustrations by Richard Garratt Printed in the United States of America VB Hermitage 10 9 8 7 6 5 4 3 2 1 This book is printed on acid-free paper. In memory of my brother Thomas Turner Elkins, who, when I was 10 years old, taught me about the Oort cloud, and together we named our pet mouse Oort. -
The Comparative Exploration of the Ice Giant Planets with Twin Spacecraft
The Comparative Exploration of the Ice Giant Planets with Twin Spacecraft The Comparative Exploration of the Ice Giant Planets with Twin Spacecraft: Unveiling the History of our Solar System Diego Turrini1*, Romolo Politi1, Roberto Peron1, Davide Grassi1, Christina Plainaki1, Mauro Barbieri2, David M. Lucchesi1, Gianfranco Magni1, Francesca Altieri1, Valeria Cottini3, Nicolas Gorius4, Patrick Gaulme5,6, François-Xavier Schmider7, Alberto Adriani1, Giuseppe Piccioni1 1 Institute for Space Astrophysics and Planetology INAF-IAPS, Italy. 2 Center of Studies and Activities for Space CISAS, University of Padova, Italy. 3 University of Maryland, USA. 4 Catholic University of America, USA 5 Department of Astronomy, New Mexico State University, P.O. Box 30001, MSC 4500, Las Cruces, NM 88003-8001, USA 6 Apache Point Observatory, 2001 Apache Point Road, P.O. Box 59, Sunspot, NM 88349, USA 7 Laboratoire Lagrange, Observatoire de la Côte d'Azur, France Abstract In the course of the selection of the scientific themes for the second and third L-class missions of the Cosmic Vision 2015-2025 program of the European Space Agency, the exploration of the ice giant planets Uranus and Neptune was defined “a timely milestone, fully appropriate for an L class mission”. Among the proposed scientific themes, we presented the scientific case of exploring both planets and their satellites in the framework of a single L-class mission and proposed a mission scenario that could allow to achieve this result. In this work we present an updated and more complete discussion of the scientific rationale and of the mission concept for a comparative exploration of the ice giant planets Uranus and Neptune and of their satellite systems with twin spacecraft. -
Jupiter's Ring-Moon System
11 Jupiter’s Ring-Moon System Joseph A. Burns Cornell University Damon P. Simonelli Jet Propulsion Laboratory Mark R. Showalter Stanford University Douglas P. Hamilton University of Maryland Carolyn C. Porco Southwest Research Institute Larry W. Esposito University of Colorado Henry Throop Southwest Research Institute 11.1 INTRODUCTION skirts within the outer stretches of the main ring, while Metis is located 1000 km closer to Jupiter in a region where the ∼ Ever since Saturn’s rings were sighted in Galileo Galilei’s ring is depleted. Each of the vertically thick gossamer rings early sky searches, they have been emblematic of the ex- is associated with a moon having a somewhat inclined orbit; otic worlds beyond Earth. Now, following discoveries made the innermost gossamer ring extends towards Jupiter from during a seven-year span a quarter-century ago (Elliot and Amalthea, and exterior gossamer ring is connected similarly Kerr 1985), the other giant planets are also recognized to be with Thebe. circumscribed by rings. Small moons are always found in the vicinity of plane- Jupiter’s diaphanous ring system was unequivocally de- tary rings. Cuzzi et al. 1984 refer to them as “ring-moons,” tected in long-exposure images obtained by Voyager 1 (Owen while Burns 1986 calls them “collisional shards.” They may et al. 1979) after charged-particle absorptions measured by act as both sources and sinks for small ring particles (Burns Pioneer 11 five years earlier (Fillius et al. 1975, Acu˜na and et al. 1984, Burns et al. 2001). Ness 1976) had hinted at its presence. The Voyager flybys also discovered three small, irregularly shaped satellites— By definition, tenuous rings are very faint, implying Metis, Adrastea and Thebe in increasing distance from that particles are so widely separated that mutual collisions Jupiter—in the same region; they joined the similar, but play little role in the evolution of such systems. -
Giant Planets
Giant Planets Mark Marley (NASA Ames) for the Planetary Decadal Survey Giant Planets Subpanel Tuesday, December 22, 2009 1 GPP Membership Reta Beebe Brigette Hesman Wayne Richie NMSU NRAO NASA Langley atmos. dynamics atm chemistry engineer John Casani William Hubbard Kunio Sayanagi JPL University of Arizona CalTech engineer, NAE interiors dynamics, theory John Clarke Mark Marley Amy Simon-Miller Boston University NASA Ames NASA Goddard aurorae, magnetos. exoplanets panel vice-chair Heidi Hammel Phil Nicholson Space Science Cornell University Institute rings panel chair Tuesday, December 22, 2009 2 Today • Some highlights of giant planet science in the past decade that impact future exploration goals (personal perspective, neglecting Cassini) • Stressing: Connection to brown dwarfs & 400+ exoplanets • Decadal process • whitepapers • mission studies • key technologies • community input Tuesday, December 22, 2009 3 Solar System Jovian Planets Serve as Waypoints in a Continuum of Objects Tuesday, December 22, 2009 4 TiO FeH K H2O H2O 6 H2O M6.5 V 10 L5 H O T.5 CO 2 Jupiter K M6 4 CIA H2 10 CH4 CH4 CH4 CH4 CH4 L5 CH4 NH3 2 10 T5 CH4 (1.30µm) x Constant ! f NH ! 3 / ! f ! 100 Jupiter CH4 1 2 3 4 5 6 7 8 9 10 Wavelength (µm) Marley & Leggett (2009) Tuesday, December 22, 2009 5 oklo.org Tuesday, December 22, 2009 6 15 ) • Transiting planets 10Earth reveal a continuum of M, R • Microlensing suggests Radius (R Neptunes are 5 common 0.1 1000 Charbonneau et al. (2009) Charbonneau et al. Mass (MEarth) Tuesday, December 22, 2009 7 Some Highlights and Questions Tuesday, December 22, 2009 8 signature of planethood? vary with mass? Owen et al. -
A European Perspective on Uranus Mission Architectures
A European perspective on Uranus mission architectures Chris Arridge1,2 1. Mullard Space Science Laboratory, UCL, UK. 2. The Centre for Planetary Sciences at UCL/Birkbeck, UK. Twitter: @chrisarridge Ice Giants Workshop – JHU Applied Physics Laboratory, MD, USA – 30 July 2014 2/32 Overview of the Cosmic Vision • Originated with Horizon and Horizon+ programmes. – Missions born from that programme include Mars Express, Venus Express, ROSETTA, HERSCHEL, Huygens, HST. • Cosmic Vision driven by scientific themes: 1. What are the conditions for planetary formation and the emergence of life? 2. How does the Solar System work? 3. What are the physical fundamental laws of the Universe? 4. How did the Universe originate and what is it made of? • Part of ESA’s mandatory programme – contributions from member states weighted by GDP, • Operate according to a set of guidelines that broadly-speaking demand a programmatic balance (between scientific domains) and due return. 3/32 Overview of the Cosmic Vision • Originated with Horizon and Horizon+ programmes. – Missions born from that programme include Mars Express, Venus Express, ROSETTA, HERSCHEL, Huygens, HST. • Cosmic Vision driven by scientific themes: 1. What are the conditions for planetary formation and the emergence of life? 2. How does the Solar System work? 3. What are the physical fundamental laws of the Universe? 4. How did the Universe originate and what is it made of? • Part of ESA’s mandatory programme – contributions from member states weighted by GDP, • Operate according to a set of guidelines that broadly-speaking demand a programmatic balance (between scientific domains) and due return. 4/32 Mission classes • Medium “M”-class: 500 M€ - example Solar Orbiter.