Physical Properties of the Small Moon Aegaeon (Saturn LIII)
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Observational Constraints on Surface Characteristics of Comet Nuclei
Observational Constraints on Surface Characteristics of Comet Nuclei Humberto Campins ([email protected] u) Lunar and Planetary Laboratory, University of Arizona Yanga Fernandez University of Hawai'i Abstract. Direct observations of the nuclear surfaces of comets have b een dicult; however a growing number of studies are overcoming observational challenges and yielding new information on cometary surfaces. In this review, we fo cus on recent determi- nations of the alb edos, re ectances, and thermal inertias of comet nuclei. There is not much diversity in the geometric alb edo of the comet nuclei observed so far (a range of 0.025 to 0.06). There is a greater diversity of alb edos among the Centaurs, and the sample of prop erly observed TNOs (2) is still to o small. Based on their alb edos and Tisserand invariants, Fernandez et al. (2001) estimate that ab out 5% of the near-Earth asteroids have a cometary origin, and place an upp er limit of 10%. The agreement between this estimate and two other indep endent metho ds provide the strongest constraint to date on the fraction of ob jects that comets contribute to the p opulation of near-Earth asteroids. There is a diversity of visible colors among comets, extinct comet candidates, Centaurs and TNOs. Comet nuclei are clearly not as red as the reddest Centaurs and TNOs. What Jewitt (2002) calls ultra-red matter seems to be absent from the surfaces of comet nuclei. Rotationally resolved observations of b oth colors and alb edos are needed to disentangle the e ects of rotational variability from other intrinsic qualities. -
Cassini Update
Cassini Update Dr. Linda Spilker Cassini Project Scientist Outer Planets Assessment Group 22 February 2017 Sols%ce Mission Inclina%on Profile equator Saturn wrt Inclination 22 February 2017 LJS-3 Year 3 Key Flybys Since Aug. 2016 OPAG T124 – Titan flyby (1584 km) • November 13, 2016 • LAST Radio Science flyby • One of only two (cf. T106) ideal bistatic observations capturing Titan’s Northern Seas • First and only bistatic observation of Punga Mare • Western Kraken Mare not explored by RSS before T125 – Titan flyby (3158 km) • November 29, 2016 • LAST Optical Remote Sensing targeted flyby • VIMS high-resolution map of the North Pole looking for variations at and around the seas and lakes. • CIRS last opportunity for vertical profile determination of gases (e.g. water, aerosols) • UVIS limb viewing opportunity at the highest spatial resolution available outside of occultations 22 February 2017 4 Interior of Hexagon Turning “Less Blue” • Bluish to golden haze results from increased production of photochemical hazes as north pole approaches summer solstice. • Hexagon acts as a barrier that prevents haze particles outside hexagon from migrating inward. • 5 Refracting Atmosphere Saturn's• 22unlit February rings appear 2017 to bend as they pass behind the planet’s darkened limb due• 6 to refraction by Saturn's upper atmosphere. (Resolution 5 km/pixel) Dione Harbors A Subsurface Ocean Researchers at the Royal Observatory of Belgium reanalyzed Cassini RSS gravity data• 7 of Dione and predict a crust 100 km thick with a global ocean 10’s of km deep. Titan’s Summer Clouds Pose a Mystery Why would clouds on Titan be visible in VIMS images, but not in ISS images? ISS ISS VIMS High, thin cirrus clouds that are optically thicker than Titan’s atmospheric haze at longer VIMS wavelengths,• 22 February but optically 2017 thinner than the haze at shorter ISS wavelengths, could be• 8 detected by VIMS while simultaneously lost in the haze to ISS. -
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 -
Limb Polarization of Uranus and Neptune I
A&A 452, 657–668 (2006) Astronomy DOI: 10.1051/0004-6361:20053273 & c ESO 2006 Astrophysics Limb polarization of Uranus and Neptune I. Imaging polarimetry and comparison with analytic models H. M. Schmid1, F. Joos1, and D. Tschan1,2 1 Institut für Astronomie, ETH Zürich, 8092 Zürich, Switzerland e-mail: [email protected] 2 Alte Kantonsschule Aarau, Bahnhofstrasse 91, 5001 Aarau, Switzerland Received 20 April 2005 / Accepted 10 January 2006 ABSTRACT Imaging polarimetry of Uranus and Neptune in the R, i,andz bands are presented. In all observations a radial limb polarization on the order of 1% was detected with a position angle perpendicular to the limb. The polarization is higher in both planets for the shorter wavelength bands. As a first approximation, the polarization seems to be equally strong along the entire limb. This is unlike Jupiter and Saturn, where significant limb polarization is only observed at the poles. We determined flux-weighted averages of the limb polarization and radial limb polarization profiles, and investigated the degradation and cancellation effects in the polarization signal due to the seeing-limited spatial resolution of our observations. Taking this into account we derived corrected values for the limb polarization in Uranus and Neptune. The results are compared with analytic models for Rayleigh scattering atmospheres for the semi-infinite case and finite layers with ground albedo. The comparison shows that the detected polarization is compatible with expectations. This indicates that limb-polarization measurements offer a powerful diagnostic tool for investigating the properties of scattering particles in the upper atmospheres of Uranus and Neptune, in particular if more sophisticated numerical modeling of the limb polarization becomes available. -
Arxiv:1009.3071V1 [Astro-Ph.EP] 16 Sep 2010 Eovdfo T Aetsa–R Oiae Yrflce Lig Reflected by Dominated AU– Star–Are 1 Parent About Al Its Than the from Larger Stars
ApJ accepted Exoplanet albedo spectra and colors as a function of planet phase, separation, and metallicity Kerri L. Cahoy, Mark S. Marley NASA Ames Research Center, Moffett Field, CA 94035 [email protected] and Jonathan J. Fortney University of California Santa Cruz, Santa Cruz, CA 95064 ABSTRACT First generation space-based optical coronagraphic telescopes will obtain images of cool gas and ice giant exoplanets around nearby stars. The albedo spectra of exoplan- ets lying at planet-star separations larger than about 1 AU–where an exoplanet can be resolved from its parent star–are dominated by reflected light to beyond 1 µm and are punctuated by molecular absorption features. Here we consider how exoplanet albedo spectra and colors vary as a function of planet-star separation, metallicity, mass, and observed phase for Jupiter and Neptune analogs from 0.35 to 1 µm. We model Jupiter analogs with 1 and 3 the solar abundance of heavy elements, and Neptune analogs × × with 10 and 30 solar abundance of heavy elements. Our model planets orbit a solar × × analog parent star at separations of 0.8 AU, 2 AU, 5 AU, and 10 AU. We use a radiative- convective model to compute temperature-pressure profiles. The giant exoplanets are found to be cloud-free at 0.8 AU, possess H2O clouds at 2 AU, and have both NH3 arXiv:1009.3071v1 [astro-ph.EP] 16 Sep 2010 and H2O clouds at 5 AU and 10 AU. For each model planet we compute moderate resolution (R = λ/∆λ 800) albedo spectra as a function of phase. -
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]. -
The Spherical Bolometric Albedo of Planet Mercury
The Spherical Bolometric Albedo of Planet Mercury Anthony Mallama 14012 Lancaster Lane Bowie, MD, 20715, USA [email protected] 2017 March 7 1 Abstract Published reflectance data covering several different wavelength intervals has been combined and analyzed in order to determine the spherical bolometric albedo of Mercury. The resulting value of 0.088 +/- 0.003 spans wavelengths from 0 to 4 μm which includes over 99% of the solar flux. This bolometric result is greater than the value determined between 0.43 and 1.01 μm by Domingue et al. (2011, Planet. Space Sci., 59, 1853-1872). The difference is due to higher reflectivity at wavelengths beyond 1.01 μm. The average effective blackbody temperature of Mercury corresponding to the newly determined albedo is 436.3 K. This temperature takes into account the eccentricity of the planet’s orbit (Méndez and Rivera-Valetín. 2017. ApJL, 837, L1). Key words: Mercury, albedo 2 1. Introduction Reflected sunlight is an important aspect of planetary surface studies and it can be quantified in several ways. Mayorga et al. (2016) give a comprehensive set of definitions which are briefly summarized here. The geometric albedo represents sunlight reflected straight back in the direction from which it came. This geometry is referred to as zero phase angle or opposition. The phase curve is the amount of sunlight reflected as a function of the phase angle. The phase angle is defined as the angle between the Sun and the sensor as measured at the planet. The spherical albedo is the ratio of sunlight reflected in all directions to that which is incident on the body. -
THE SATURNIAN G RING: a SHORT NOTE ABOUT ITS FORMATION Revista Mexicana De Astronomía Y Astrofísica, Vol
Revista Mexicana de Astronomía y Astrofísica ISSN: 0185-1101 [email protected] Instituto de Astronomía México Maravilla, D.; Leal-Herrera, J. L. THE SATURNIAN G RING: A SHORT NOTE ABOUT ITS FORMATION Revista Mexicana de Astronomía y Astrofísica, vol. 50, núm. 2, octubre, 2014, pp. 341- 347 Instituto de Astronomía Distrito Federal, México Available in: http://www.redalyc.org/articulo.oa?id=57148278016 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Revista Mexicana de Astronom´ıa y Astrof´ısica, 50, 341–347 (2014) THE SATURNIAN G RING: A SHORT NOTE ABOUT ITS FORMATION D. Maravilla and J. L. Leal-Herrera Departamento de Ciencias Espaciales, Instituto de Geof´ısica, UNAM, Mexico Received March 21 2014; accepted August 18 2014 RESUMEN En este trabajo se estudia la formaci´on del anillo G de Saturno considerando que el sat´elite Ege´on es la fuente de part´ıculas de polvo. El polvo que forma el anillo se produce por impactos entre los micrometeoroides interplanetarios que ingresan en la magnet´osfera Saturniana y la superficie de Ege´on. Para explicar c´omo se forma el anillo se usa un modelo gravito-electrodin´amico suponiendo que las fuerzas gravitacional y electromagn´etica son las ´unicas fuerzas que modulan el comportamiento din´amico de las part´ıculas de polvo. Las soluciones del modelo muestran que existen reg´ımenes de confinamiento (captura) as´ıcomo reg´ımenes de escape de polvo en la vecindad de Ege´on. -
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.