A Comparison of Centering Algorithms in the Astrometry of Cassini Imaging Science Subsystem Images and Anthe’S Astrometric Reduction
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Dynamics of Saturn's Small Moons in Coupled First Order Planar Resonances
Dynamics of Saturn's small moons in coupled first order planar resonances Maryame El Moutamid Bruno Sicardy and St´efanRenner LESIA/IMCCE | Paris Observatory 26 juin 2012 Maryame El Moutamid ESLAB-2012 | ESA/ESTEC Noordwijk Saturn system Maryame El Moutamid ESLAB-2012 | ESA/ESTEC Noordwijk Very small moons Maryame El Moutamid ESLAB-2012 | ESA/ESTEC Noordwijk New satellites : Anthe, Methone and Aegaeon (Cooper et al., 2008 ; Hedman et al., 2009, 2010 ; Porco et al., 2005) Very small (0.5 km to 2 km) Vicinity of the Mimas orbit (outside and inside) The aims of the work A better understanding : - of the dynamics of this population of news satellites - of the scenario of capture into mean motion resonances Maryame El Moutamid ESLAB-2012 | ESA/ESTEC Noordwijk Dynamical structure of the system µ µ´ Mp We consider only : - The resonant terms - The secular terms causing the precessions of the orbit When µ ! 0 ) The symmetry is broken ) different kinds of resonances : - Lindblad Resonance - Corotation Resonance D'Alembert rules : 0 0 c = (m + 1)λ − mλ − $ 0 L = (m + 1)λ − mλ − $ Maryame El Moutamid ESLAB-2012 | ESA/ESTEC Noordwijk Corotation Resonance - Aegaeon (7/6) : c = 7λMimas − 6λAegaeon − $Mimas - Methone (14/15) : c = 15λMethone − 14λMimas − $Mimas - Anthe (10/11) : c = 11λAnthe − 10λMimas − $Mimas Maryame El Moutamid ESLAB-2012 | ESA/ESTEC Noordwijk Corotation resonances Mean motion resonance : n1 = m+q n2 m Particular case : Lagrangian Equilibrium Points Maryame El Moutamid ESLAB-2012 | ESA/ESTEC Noordwijk Adam's ring and Galatea Maryame -
Observing the Universe
ObservingObserving thethe UniverseUniverse :: aa TravelTravel ThroughThrough SpaceSpace andand TimeTime Enrico Flamini Agenzia Spaziale Italiana Tokyo 2009 When you rise your head to the night sky, what your eyes are observing may be astonishing. However it is only a small portion of the electromagnetic spectrum of the Universe: the visible . But any electromagnetic signal, indipendently from its frequency, travels at the speed of light. When we observe a star or a galaxy we see the photons produced at the moment of their production, their travel could have been incredibly long: it may be lasted millions or billions of years. Looking at the sky at frequencies much higher then visible, like in the X-ray or gamma-ray energy range, we can observe the so called “violent sky” where extremely energetic fenoena occurs.like Pulsar, quasars, AGN, Supernova CosmicCosmic RaysRays:: messengersmessengers fromfrom thethe extremeextreme universeuniverse We cannot see the deep universe at E > few TeV, since photons are attenuated through →e± on the CMB + IR backgrounds. But using cosmic rays we should be able to ‘see’ up to ~ 6 x 1010 GeV before they get attenuated by other interaction. Sources Sources → Primordial origin Primordial 7 Redshift z = 0 (t = 13.7 Gyr = now ! ) Going to a frequency lower then the visible light, and cooling down the instrument nearby absolute zero, it’s possible to observe signals produced millions or billions of years ago: we may travel near the instant of the formation of our universe: 13.7 By. Redshift z = 1.4 (t = 4.7 Gyr) Credits A. Cimatti Univ. Bologna Redshift z = 5.7 (t = 1 Gyr) Credits A. -
Long-Term Evolution and Stability of Saturnian Small Satellites
MNRAS 000, 1–17 (2016) Preprint 30 August 2021 Compiled using MNRAS LATEX style file v3.0 Long-term Evolution and Stability of Saturnian Small Satellites: Aegaeon, Methone, Anthe, and Pallene. M. A. Mun˜oz-Guti´errez,1⋆ and S. Giuliatti Winter1 1Universidade Estadual Paulista - UNESP, Grupo de Dinˆamica Orbital e Planetologia, Av. Ariberto Pereira da Cunha, 333, Guaratinguet´a-SP, 12516-410, Brazil Accepted XXX. Received YYY; in original form ZZZ ABSTRACT Aegaeon, Methone, Anthe, and Pallene are four Saturnian small moons, discovered by the Cassini spacecraft. Although their orbital characterization has been carried on by a number of authors, their long-term evolution has not been studied in detail so far. In this work, we numerically explore the long-term evolution, up to 105 yr, of the small moons in a system formed by an oblate Saturn and the five largest moons close to the region: Janus, Epimetheus, Mimas, Enceladus, and Tethys. By using frequency analysis we determined the stability of the small moons and characterize, through diffusion maps, the dynamical behavior of a wide region of geometric phase space, a vs e, surrounding them. Those maps could shed light on the possible initial number of small bodies close to Mimas, and help to better understand the dynamical origin of the small satellites. We found that the four small moons are long-term stable and no mark of chaos is found for them. Aegaeon, Methone, and Anthe could remain unaltered for at least ∼ 0.5Myr, given the current configuration of the system. They remain well- trapped in the corotation eccentricity resonances with Mimas in which they currently librate. -
An Analytical Model for the Dust Environment Around Saturn's
EPSC Abstracts Vol. 9, EPSC2014-310, 2014 European Planetary Science Congress 2014 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2014 An Analytical Model for the Dust Environment around Saturn’s Moons Pallene, Methone and Anthe Michael Seiler, Martin Seiß, Kai-Lung Sun and Frank Spahn Institute of Physics and Astronomy, University of Potsdam, Germany ([email protected]) Abstract Acknowledgements Since its arrival at Saturn in 2004 the observations This work was supported by the Deutsche Forschungs- by the spacecraft Cassini have revolutionised the gemeinschaft (Sp 384/28-1, Sp 384/21-2) and the understanding of the dynamics in planetary rings. Deutsches Zentrum für Luft- und Raumfahrt (OH By analysing Cassini images, Hedman et al. [1] 0003). detected faint dust along the orbits of Saturn’s tiny moons Methone, Anthe and Pallene. While the ring material around Methone and Anthe appears to be References longitudinally confined to arcs, a continuous ring of material has been observed around the orbit of Pallene [1] Hedman, M. M. et al., "Three tenuous rings/arcs for three tiny moons", Icarus, 199, pp. 378-386, 2009 by the Cassini dust analyzer. The data show, that at least part of the torus lies exterior Pallene’s orbit. [2] Cooper, N. J. et al. "Astrometry and dynamics of Anthe (S/2007 S 4), a new satellite of Saturn", Icarus, 195, pp. Many tiny moons are located between Mimas and 765-777, 2008 Enceladus and are known to be resonantly perturbed [3] Spitale, J. N. et al. "The Orbits of Saturn’s Small Satel- by these [2, 3]. -
Resonant Moons of Neptune
EPSC Abstracts Vol. 13, EPSC-DPS2019-901-1, 2019 EPSC-DPS Joint Meeting 2019 c Author(s) 2019. CC Attribution 4.0 license. Resonant moons of Neptune Marina Brozović (1), Mark R. Showalter (2), Robert A. Jacobson (1), Robert S. French (2), Jack L. Lissauer (3), Imke de Pater (4) (1) Jet Propulsion Laboratory, California Institute of Technology, California, USA, (2) SETI Institute, California, USA, (3) NASA Ames Research Center, California, USA, (4) University of California Berkeley, California, USA Abstract We used integrated orbits to fit astrometric data of the 2. Methods regular moons of Neptune. We found a 73:69 inclination resonance between Naiad and Thalassa, the 2.1 Observations two innermost moons. Their resonant argument librates around 180° with an average amplitude of The astrometric data cover the period from 1981-2016, ~66° and a period of ~1.9 years. This is the first fourth- with the most significant amount of data originating order resonance discovered between the moons of the from the Voyager 2 spacecraft and HST. Voyager 2 outer planets. The resonance enabled an estimate of imaged all regular satellites except Hippocamp the GMs for Naiad and Thalassa, GMN= between 1989 June 7 and 1989 August 24. The follow- 3 -2 3 0.0080±0.0043 km s and GMT=0.0236±0.0064 km up observations originated from several Earth-based s-2. More high-precision astrometry of Naiad and telescopes, but the majority were still obtained by HST. Thalassa will help better constrain their masses. The [4] published the latest set of the HST astrometry GMs of Despina, Galatea, and Larissa are more including the discovery and follow up observations of difficult to measure because they are not in any direct Hippocamp. -
Moons of Saturn
National Aeronautics and Space Administration 0 300,000,000 900,000,000 1,500,000,000 2,100,000,000 2,700,000,000 3,300,000,000 3,900,000,000 4,500,000,000 5,100,000,000 5,700,000,000 kilometers Moons of Saturn www.nasa.gov Saturn, the sixth planet from the Sun, is home to a vast array • Phoebe orbits the planet in a direction opposite that of Saturn’s • Fastest Orbit Pan of intriguing and unique satellites — 53 plus 9 awaiting official larger moons, as do several of the recently discovered moons. Pan’s Orbit Around Saturn 13.8 hours confirmation. Christiaan Huygens discovered the first known • Mimas has an enormous crater on one side, the result of an • Number of Moons Discovered by Voyager 3 moon of Saturn. The year was 1655 and the moon is Titan. impact that nearly split the moon apart. (Atlas, Prometheus, and Pandora) Jean-Dominique Cassini made the next four discoveries: Iapetus (1671), Rhea (1672), Dione (1684), and Tethys (1684). Mimas and • Enceladus displays evidence of active ice volcanism: Cassini • Number of Moons Discovered by Cassini 6 Enceladus were both discovered by William Herschel in 1789. observed warm fractures where evaporating ice evidently es- (Methone, Pallene, Polydeuces, Daphnis, Anthe, and Aegaeon) The next two discoveries came at intervals of 50 or more years capes and forms a huge cloud of water vapor over the south — Hyperion (1848) and Phoebe (1898). pole. ABOUT THE IMAGES As telescopic resolving power improved, Saturn’s family of • Hyperion has an odd flattened shape and rotates chaotically, 1 2 3 1 Cassini’s visual known moons grew. -
PDS4 Context List
Target Context List Name Type LID 136108 HAUMEA Planet urn:nasa:pds:context:target:planet.136108_haumea 136472 MAKEMAKE Planet urn:nasa:pds:context:target:planet.136472_makemake 1989N1 Satellite urn:nasa:pds:context:target:satellite.1989n1 1989N2 Satellite urn:nasa:pds:context:target:satellite.1989n2 ADRASTEA Satellite urn:nasa:pds:context:target:satellite.adrastea AEGAEON Satellite urn:nasa:pds:context:target:satellite.aegaeon AEGIR Satellite urn:nasa:pds:context:target:satellite.aegir ALBIORIX Satellite urn:nasa:pds:context:target:satellite.albiorix AMALTHEA Satellite urn:nasa:pds:context:target:satellite.amalthea ANTHE Satellite urn:nasa:pds:context:target:satellite.anthe APXSSITE Equipment urn:nasa:pds:context:target:equipment.apxssite ARIEL Satellite urn:nasa:pds:context:target:satellite.ariel ATLAS Satellite urn:nasa:pds:context:target:satellite.atlas BEBHIONN Satellite urn:nasa:pds:context:target:satellite.bebhionn BERGELMIR Satellite urn:nasa:pds:context:target:satellite.bergelmir BESTIA Satellite urn:nasa:pds:context:target:satellite.bestia BESTLA Satellite urn:nasa:pds:context:target:satellite.bestla BIAS Calibrator urn:nasa:pds:context:target:calibrator.bias BLACK SKY Calibration Field urn:nasa:pds:context:target:calibration_field.black_sky CAL Calibrator urn:nasa:pds:context:target:calibrator.cal CALIBRATION Calibrator urn:nasa:pds:context:target:calibrator.calibration CALIMG Calibrator urn:nasa:pds:context:target:calibrator.calimg CAL LAMPS Calibrator urn:nasa:pds:context:target:calibrator.cal_lamps CALLISTO Satellite urn:nasa:pds:context:target:satellite.callisto -
Dust Phenomena Relating to Airless Bodies
Space Sci Rev (2018) 214:98 https://doi.org/10.1007/s11214-018-0527-0 Dust Phenomena Relating to Airless Bodies J.R. Szalay1 · A.R. Poppe2 · J. Agarwal3 · D. Britt4 · I. Belskaya5 · M. Horányi6 · T. Nakamura7 · M. Sachse8 · F. Spahn 8 Received: 8 August 2017 / Accepted: 10 July 2018 © Springer Nature B.V. 2018 Abstract Airless bodies are directly exposed to ambient plasma and meteoroid fluxes, mak- ing them characteristically different from bodies whose dense atmospheres protect their surfaces from such fluxes. Direct exposure to plasma and meteoroids has important con- sequences for the formation and evolution of planetary surfaces, including altering chemical makeup and optical properties, generating neutral gas and/or dust exospheres, and leading to the generation of circumplanetary and interplanetary dust grain populations. In the past two decades, there have been many advancements in our understanding of airless bodies and their interaction with various dust populations. In this paper, we describe relevant dust phenomena on the surface and in the vicinity of airless bodies over a broad range of scale sizes from ∼ 10−3 km to ∼ 103 km, with a focus on recent developments in this field. Keywords Dust · Airless bodies · Interplanetary dust Cosmic Dust from the Laboratory to the Stars Edited by Rafael Rodrigo, Jürgen Blum, Hsiang-Wen Hsu, Detlef Koschny, Anny-Chantal Levasseur-Regourd, Jesús Martín-Pintado, Veerle Sterken and Andrew Westphal B J.R. Szalay [email protected] A.R. Poppe [email protected] 1 Department of Astrophysical Sciences, Princeton University, Princeton, NJ 08540, USA 2 Space Sciences Laboratory, U.C. Berkeley, Berkeley, CA, USA 3 Max Planck Institute for Solar System Research, Göttingen, Germany 4 University of Central Florida, Orlando, FL 32816, USA 5 Institute of Astronomy, V.N. -
Mission Science Highlights and Science Objectives Assessment
CASSINI FINAL MISSION REPORT 2019 1 MISSION SCIENCE HIGHLIGHTS AND SCIENCE OBJECTIVES ASSESSMENT Cassini-Huygens, humanity’s most distant planetary orbiter and probe to date, provided the first in- depth, close up study of Saturn, its magnificent rings and unique moons, including Titan and Enceladus, and its giant magnetosphere. Discoveries from the Cassini-Huygens mission revolutionized our understanding of the Saturn system and fundamentally altered many of our concepts of where life might be found in our solar system and beyond. Cassini-Huygens arrived at Saturn in 2004, dropped the parachuted probe named Huygens to study the atmosphere and surface of Saturn’s planet-sized moon Titan, and orbited Saturn for the next 13 years making remarkable discoveries. When it was running low on fuel, the Cassini orbiter was programmed to vaporize in Saturn’s atmosphere in 2017 to protect the ocean worlds, Enceladus and Titan, where it discovered potential habitats for life. CASSINI FINAL MISSION REPORT 2019 2 CONTENTS MISSION SCIENCE HIGHLIGHTS AND SCIENCE OBJECTIVES ASSESSMENT ........................................................ 1 Executive Summary................................................................................................................................................ 5 Origin of the Cassini Mission ....................................................................................................................... 5 Instrument Teams and Interdisciplinary Investigations ............................................................................... -
Perfect Little Planet Educator's Guide
Educator’s Guide Perfect Little Planet Educator’s Guide Table of Contents Vocabulary List 3 Activities for the Imagination 4 Word Search 5 Two Astronomy Games 7 A Toilet Paper Solar System Scale Model 11 The Scale of the Solar System 13 Solar System Models in Dough 15 Solar System Fact Sheet 17 2 “Perfect Little Planet” Vocabulary List Solar System Planet Asteroid Moon Comet Dwarf Planet Gas Giant "Rocky Midgets" (Terrestrial Planets) Sun Star Impact Orbit Planetary Rings Atmosphere Volcano Great Red Spot Olympus Mons Mariner Valley Acid Solar Prominence Solar Flare Ocean Earthquake Continent Plants and Animals Humans 3 Activities for the Imagination The objectives of these activities are: to learn about Earth and other planets, use language and art skills, en- courage use of libraries, and help develop creativity. The scientific accuracy of the creations may not be as im- portant as the learning, reasoning, and imagination used to construct each invention. Invent a Planet: Students may create (draw, paint, montage, build from household or classroom items, what- ever!) a planet. Does it have air? What color is its sky? Does it have ground? What is its ground made of? What is it like on this world? Invent an Alien: Students may create (draw, paint, montage, build from household items, etc.) an alien. To be fair to the alien, they should be sure to provide a way for the alien to get food (what is that food?), a way to breathe (if it needs to), ways to sense the environment, and perhaps a way to move around its planet. -
Dust in the Arcs of Methone and Anthe
Dust in the arcs of Methone and Anthe Kai-Lung Sun, Martin Seiß, Frank Spahn Karl-Liebknecht-Str. 24/25, 14476 Potsdam Golm Abstract Methone and Anthe are two tiny moons (with diameter < 3 km) in the in- ner part of Saturn's E ring. Both moons are embedded in an arc of dust particles. To understand the amount of micron-sized dust and their spatial distribution in these arcs, we model the source, dynamical evolution, and sinks of these dust in the arc. We assume hypervelocity impacts of microm- eteoroids on the moons as source of these dust (Hedman et al., 2009), the so called impact-ejecta process (Krivov et al., 2003; Spahn et al., 2006). After ejecting and escaping from the moons, these micron-sized particles are sub- ject to several perturbing forces, including gravitational perturbation from Mimas, oblateness of Saturn, Lorentz force, solar radiation pressure, and plasma drag. Particles can be either confined in the arcs due to corota- tional resonance with Mimas, as their source moons (Spitale et al., 2006; Cooper et al., 2008; Hedman et al., 2009), or pushed outward by plasma drag. Particle sinks are recollisions with the source moon, collision with other moons, or migrate out of the radial zone of interest. In addition to that, the upper limit of the particle lifetimes are controlled by plasma sput- tering, which decreases the particle size in a rate of order 1 µm radius every 100 years (Johnson et al., 2008). Our simulation results show that ejecta from both moons can form the arcs of maximal optical depths τ in the order of 10−8 − 10−6, although the absolute amount of dust have uncertainties. -
Aegaeon (Saturn LIII), a G-Ring Object 1
Aegaeon (Saturn LIII), a G-ring object 1 M.M. Hedmana, N.J. Cooperb, C.D.Murrayb, K. Beurleb, M.W. Evansb;a, M.S. Tiscarenoa, J. A. Burnsa;c a Department of Astronomy, Cornell University, Ithaca NY 14853 USA b Queen Mary University of London, Astronomy Unit, School of Mathematical Sciences, Mile End Road, London E1 4NS, UK c Department of Theoretical and Applied Mechanics, Cornell University, Ithaca NY 14853 USA Proposed Running Head: Aegaeon (Saturn LIII), a G-ring object Keywords: Saturn, Satellites; Saturn, rings; Satellites, dynamics; Resonances, orbital 1This paper is dedicated to the memory of Kevin Beurle. arXiv:0911.0171v2 [astro-ph.EP] 1 Dec 2009 { 2 { Abstract: Aegaeon (Saturn LIII, S/2008 S1) is a small satellite of Saturn that orbits within a bright arc of material near the inner edge of Saturn's G ring. This object was observed in 21 images with Cassini's Narrow-Angle Camera between June 15 (DOY 166), 2007 and February 20 (DOY 51), 2009. If Aegaeon has similar surface scattering properties as other nearby small Saturnian satellites (Pallene, Methone and Anthe), then its diameter is approximately 500 m. Orbit models based on numerical integrations of the full equations of motion show that Aegaeon's orbital motion is strongly influenced by multiple resonances with Mimas. In particular, like the G-ring arc it inhabits, Aegaeon is trapped in the 7:6 corotation eccentricity resonance with Mimas. Aegaeon, Anthe and Methone therefore form a distinctive class of objects in the Saturn system: small moons in co-rotation eccentricity resonances with Mimas associated with arcs of debris.