Prospects for the Detection of Planetary Rings Around Extrasolar 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 ..................................................... -
The Rings and Inner Moons of Uranus and Neptune: Recent Advances and Open Questions
Workshop on the Study of the Ice Giant Planets (2014) 2031.pdf THE RINGS AND INNER MOONS OF URANUS AND NEPTUNE: RECENT ADVANCES AND OPEN QUESTIONS. Mark R. Showalter1, 1SETI Institute (189 Bernardo Avenue, Mountain View, CA 94043, mshowal- [email protected]! ). The legacy of the Voyager mission still dominates patterns or “modes” seem to require ongoing perturba- our knowledge of the Uranus and Neptune ring-moon tions. It has long been hypothesized that numerous systems. That legacy includes the first clear images of small, unseen ring-moons are responsible, just as the nine narrow, dense Uranian rings and of the ring- Ophelia and Cordelia “shepherd” ring ε. However, arcs of Neptune. Voyager’s cameras also first revealed none of the missing moons were seen by Voyager, sug- eleven small, inner moons at Uranus and six at Nep- gesting that they must be quite small. Furthermore, the tune. The interplay between these rings and moons absence of moons in most of the gaps of Saturn’s rings, continues to raise fundamental dynamical questions; after a decade-long search by Cassini’s cameras, sug- each moon and each ring contributes a piece of the gests that confinement mechanisms other than shep- story of how these systems formed and evolved. herding might be viable. However, the details of these Nevertheless, Earth-based observations have pro- processes are unknown. vided and continue to provide invaluable new insights The outermost µ ring of Uranus shares its orbit into the behavior of these systems. Our most detailed with the tiny moon Mab. Keck and Hubble images knowledge of the rings’ geometry has come from spanning the visual and near-infrared reveal that this Earth-based stellar occultations; one fortuitous stellar ring is distinctly blue, unlike any other ring in the solar alignment revealed the moon Larissa well before Voy- system except one—Saturn’s E ring. -
Planetary Rings
CLBE001-ESS2E November 10, 2006 21:56 100-C 25-C 50-C 75-C C+M 50-C+M C+Y 50-C+Y M+Y 50-M+Y 100-M 25-M 50-M 75-M 100-Y 25-Y 50-Y 75-Y 100-K 25-K 25-19-19 50-K 50-40-40 75-K 75-64-64 Planetary Rings Carolyn C. Porco Space Science Institute Boulder, Colorado Douglas P. Hamilton University of Maryland College Park, Maryland CHAPTER 27 1. Introduction 5. Ring Origins 2. Sources of Information 6. Prospects for the Future 3. Overview of Ring Structure Bibliography 4. Ring Processes 1. Introduction houses, from coalescing under their own gravity into larger bodies. Rings are arranged around planets in strikingly dif- Planetary rings are those strikingly flat and circular ap- ferent ways despite the similar underlying physical pro- pendages embracing all the giant planets in the outer Solar cesses that govern them. Gravitational tugs from satellites System: Jupiter, Saturn, Uranus, and Neptune. Like their account for some of the structure of densely-packed mas- cousins, the spiral galaxies, they are formed of many bod- sive rings [see Solar System Dynamics: Regular and ies, independently orbiting in a central gravitational field. Chaotic Motion], while nongravitational effects, includ- Rings also share many characteristics with, and offer in- ing solar radiation pressure and electromagnetic forces, valuable insights into, flattened systems of gas and collid- dominate the dynamics of the fainter and more diffuse dusty ing debris that ultimately form solar systems. Ring systems rings. Spacecraft flybys of all of the giant planets and, more are accessible laboratories capable of providing clues about recently, orbiters at Jupiter and Saturn, have revolutionized processes important in these circumstellar disks, structures our understanding of planetary rings. -
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). -
Astronomy 4 Test #3 Practice 2. How Were the Rings of Uranus Discovered?
Astronomy 4 Test #3 Practice Multiple Choice Choose the ONE best answer for each question. 1. Which of the following things makes Saturn’s moon Titan unique amongst all of the moon in the solar system? a. It has a rocky surface. b. It orbits Saturn in the opposite direction from Saturn’s other moons. c. It has a thick atmosphere. d. It has flows of molten lava on its surface. 2. How were the rings of Uranus discovered? a. Astronomers used radar signals from the Earth and bounced them off of the rings, receiving the reflected waves with radio telescopes. b. Astronomers saw a star appear to momentarily get dimmer as it passed behind each of the rings. c. They were among the first features discovered with the telescope in the 1600s. d. Astronomers could see them silhouetted in front of Uranus when they observed Uranus with large telescopes. 3. Which of the following statements best describes what’s weird about the orbit of Triton, the large moon of Neptune? a. Its orbit is more elliptical than those of most moons. b. It orbits closer to Neptune than any other moon orbits its `parent’ planet. c. It orbit Neptune in the opposite direction that most moons orbit their `parent’ planets. d. Its orbit is not very close to the plane of the ecliptic; it passes over the north and south poles of Neptune. 1 4. What’s the biggest difference -besides overall size and mass - between the Earth and Jupiter? a. The Earth’s solid surface has much more atmosphere on top of it than is the case for Jupiter. -
Moons and Rings
The Rings of Saturn 5.1 Saturn, the most beautiful planet in our solar system, is famous for its dazzling rings. Shown in the figure above, these rings extend far into space and engulf many of Saturn’s moons. The brightest rings, visible from Earth in a small telescope, include the D, C and B rings, Cassini’s Division, and the A ring. Just outside the A ring is the narrow F ring, shepherded by tiny moons, Pandora and Prometheus. Beyond that are two much fainter rings named G and E. Saturn's diffuse E ring is the largest planetary ring in our solar system, extending from Mimas' orbit to Titan's orbit, about 1 million kilometers (621,370 miles). The particles in Saturn's rings are composed primarily of water ice and range in size from microns to tens of meters. The rings show a tremendous amount of structure on all scales. Some of this structure is related to gravitational interactions with Saturn's many moons, but much of it remains unexplained. One moonlet, Pan, actually orbits inside the A ring in a 330-kilometer-wide (200-mile) gap called the Encke Gap. The main rings (A, B and C) are less than 100 meters (300 feet) thick in most places. The main rings are much younger than the age of the solar system, perhaps only a few hundred million years old. They may have formed from the breakup of one of Saturn's moons or from a comet or meteor that was torn apart by Saturn's gravity. -
Comparing the Rings of the Outer Planets 13
Comparing the Rings of the Outer Planets 13 Courtesy of Nick Strobel at www.astronomynotes.com The rings of Uranus (top right) and Neptune (bottom right) are similar to those of Jupiter and consist millions of small rocky and icy objects in separate orbits. The figure shows a comparison of the scales of the planets and their ring systems. Problem 1 – Compare the extent of the ring systems for each planet in terms of their size in units of the radius of the corresponding planet. For example, ‘The rings of Uranus extend from 1.7 to 2.0 times the radius of Uranus’. Problem 2 – An icy body will be destroyed by a planet if it comes within the Tidal Limit of the planet. At this distance, the difference in gravity between the near and the far side of the body exceeds the body’s ability to hold together by its own gravity, and so it is shredded into smaller pieces. For Jupiter (2.7), Saturn (2.2), Uranus (2.7) and Neptune (2.9), the Tidal Limits are located between 2.2 and 2.9 times the radius of each planet from the planet’s center. Describe where the ring systems are located around each planet compared to the planets Tidal Limit. Could the rings be explained by a moon or moon’s getting too close to the planet? Space Math http://spacemath.gsfc.nasa.gov Answer Key 13 Problem 1 – Compare the extent of the ring systems for each planet in terms of their size in units of the radius of the corresponding planet. -
Red Material on the Large Moons of Uranus: Dust from the Irregular Satellites?
Red material on the large moons of Uranus: Dust from the irregular satellites? Richard J. Cartwright1, Joshua P. Emery2, Noemi Pinilla-Alonso3, Michael P. Lucas2, Andy S. Rivkin4, and David E. Trilling5. 1Carl Sagan Center, SETI Institute; 2University of Tennessee; 3University of Central Florida; 4John Hopkins University Applied Physics Laboratory; 5Northern Arizona University. Abstract The large and tidally-locked “classical” moons of Uranus display longitudinal and planetocentric trends in their surface compositions. Spectrally red material has been detected primarily on the leading hemispheres of the outer moons, Titania and Oberon. Furthermore, detected H2O ice bands are stronger on the leading hemispheres of the classical satellites, and the leading/trailing asymmetry in H2O ice band strengths decreases with distance from Uranus. We hypothesize that the observed distribution of red material and trends in H2O ice band strengths results from infalling dust from Uranus’ irregular satellites. These dust particles migrate inward on slowly decaying orbits, eventually reaching the classical satellite zone, where they collide primarily with the outer moons. The latitudinal distribution of dust swept up by these moons should be fairly even across their southern and northern hemispheres. However, red material has only been detected over the southern hemispheres of these moons, during the Voyager 2 flyby of the Uranian system (subsolar latitude ~81ºS). Consequently, to test whether irregular satellite dust impacts drive the observed enhancement in reddening, we have gathered new ground-based data of the now observable northern hemispheres of these moons (sub-observer latitudes ~17 – 35ºN). Our results and analyses indicate that longitudinal and planetocentric trends in reddening and H2O ice band strengths are broadly consistent across both southern and northern latitudes of these moons, thereby supporting our hypothesis. -
Next Stop: Uranus
www.astrosociety.org/uitc No. 4 - Winter 1985-86 © 1986, Astronomical Society of the Pacific, 390 Ashton Avenue, San Francisco, CA 94112 Next Stop: Uranus On January 24, 1986. the aging but still active Voyager 2 spacecraft will become the first mission to fly by the seventh planet in our solar system. a giant, bluish-green, and often puzzling world called Uranus. Mission scientists predict that we will learn more about this distant planet in the six hours of closest encounter than we have in the roughly 200 years since Uranus was discovered. In this issue of The Universe in the Classroom, we summarize our current knowledge of the complex Uranus system and provide some background to help you evaluate and explain the Voyager results to your classes. History Uranus was the first planet to be discovered that was not known to the ancients. It was found on March 13, 1781 by an amateur astronomer (and professional musician) named William Herschel, using a homemade 6.2-inch telescope. At first Herschel thought he had merely discovered a new comet, but it soon became apparent that the new object behaved like a planet. After some debate it was named Uranus, after the god in Greek mythology who most closely personified the heavens. (Uranus was the father of the Titans and thus grandfather of Jupiter.) As a result of his pioneering find, Herschel received a life-long stipend from the king of England and was able to continue building larger and larger telescopes and making a host of important discoveries. Among these was his spotting of two of Uranus's moons, Titania and Oberon, in 1787. -
Lecture 14: the Giant Planets, Their Moons, and Their Rings
Lecture 14: The Giant Planets, their Moons, and their Rings Jupiter’s Great Red Spot! Claire Max May 22, 2014 Astro 18: Planets and Planetary Systems UC Santa Cruz Class Projects • Today: Each group send me your lists of questions • Today: Each person send me a quick email about how things are going in your group Class Projects, continued • What should your reference sources be? • At least the following, for each question: 1." Two authoritative websites to get started, frame the issues for you to work on, help identify other references. Use to get the “big picture”. 2." Two journal articles on your topic. Look over four or five (read abstracts, skim contents, take notes) before choosing the two you are going to use. Search at http://adsabs.harvard.edu/default_service.html 3." One book or monograph (need not be the whole thing, but use the relevant sections). Use Science Library or UCSC Library website to search. The Giant Planets in our own Solar System • Jupiter, Saturn, Uranus, Neptune (and Earth for comparison)! Outline of lecture • Jovian Planets: – Properties – Formation – Interior structure – Atmospheres • Moons of the Giant Planets Jovian (or Giant) Planet Properties • Compared to the terrestrial planets, the Jovians: – are much larger & more massive – are composed mostly of Hydrogen, Helium, & Hydrogen compounds – have no solid surfaces – rotate more quickly – have slightly “squashed” shapes – have ring systems – have many moons Jupiter – 318 x Earth Saturn 95x Earth Uranus 14x Earth Neptune 17x Earth Why are the Jovian Planets so Different? • They formed beyond the frost line to form large, icy planetesimals which were massive enough to… – Capture H/He far from Sun to form gaseous planets. -
Exploring the Origins and Evolution of Ice Giant Planets C
The science case for an orbital mission to Uranus: Exploring the origins and evolution of ice giant planets C. S. Arridge, N. Achilleos, J. Agarwal, C. B. Agnor, R. Ambrosi, N. André, S. V. Badman, K. Baines, D. Banfield, M. Barthélémy, et al. To cite this version: C. S. Arridge, N. Achilleos, J. Agarwal, C. B. Agnor, R. Ambrosi, et al.. The science case for an orbital mission to Uranus: Exploring the origins and evolution of ice giant planets. Planetary and Space Science, Elsevier, 2014, 104, part A, pp.122-140. 10.1016/j.pss.2014.08.009. hal-01059416 HAL Id: hal-01059416 https://hal.archives-ouvertes.fr/hal-01059416 Submitted on 21 Nov 2020 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. Planetary and Space Science ∎ (∎∎∎∎) ∎∎∎–∎∎∎ Contents lists available at ScienceDirect Planetary and Space Science journal homepage: www.elsevier.com/locate/pss The science case for an orbital mission to Uranus: Exploring the origins and evolution of ice giant planets C.S. Arridge a,b,n, N. Achilleos c,b, J. Agarwal d, C.B. Agnor e, R. Ambrosi f, N. André g, S.V. -
Executive Summary: Mission to Uranus Classification: Unclassified Issue: 1 Date: 15/09/2014
Title: Executive Summary: Mission To Uranus Classification: Unclassified Issue: 1 Date: 15/09/2014 Contact: University of Leicester Department of Physics & Astronomy Space Research Centre University Road Leicester LE1 7RH UK Chris Greenaway, Jack Boughton, Prepared by: Date: 15/09/2014 Nils Dittel Reviewed by: N/A Date: N/A Approved by: N/A Date: N/A Executive Summary: Mission to Uranus Page i DOCUMENT CHANGE DETAILS Issue Date Page Description Of Change Comment 1 15/09/2014 N/A – First issue Executive Summary: Mission to Uranus Issue: 1 15/09/2014 Page ii TABLE OF CONTENTS 1.1 Reference Documents ............................................................................................................................ 1 1.2 Work Breakdown ................................................................................................................................... 5 2 The Icy Giant.................................................................................................................................................. 6 2.1 Science Objectives and Justification ........................................................................................................ 6 2.1.1 The atmosphere ............................................................................................................................... 6 2.1.2 The interior of Uranus ...................................................................................................................... 7 2.1.3 The Rings of Uranus .......................................................................................................................