Near-Infrared Brightness of Saturn Richard W
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(101955) Bennu from OSIRIS-Rex Imaging and Thermal Analysis
ARTICLES https://doi.org/10.1038/s41550-019-0731-1 Properties of rubble-pile asteroid (101955) Bennu from OSIRIS-REx imaging and thermal analysis D. N. DellaGiustina 1,26*, J. P. Emery 2,26*, D. R. Golish1, B. Rozitis3, C. A. Bennett1, K. N. Burke 1, R.-L. Ballouz 1, K. J. Becker 1, P. R. Christensen4, C. Y. Drouet d’Aubigny1, V. E. Hamilton 5, D. C. Reuter6, B. Rizk 1, A. A. Simon6, E. Asphaug1, J. L. Bandfield 7, O. S. Barnouin 8, M. A. Barucci 9, E. B. Bierhaus10, R. P. Binzel11, W. F. Bottke5, N. E. Bowles12, H. Campins13, B. C. Clark7, B. E. Clark14, H. C. Connolly Jr. 15, M. G. Daly 16, J. de Leon 17, M. Delbo’18, J. D. P. Deshapriya9, C. M. Elder19, S. Fornasier9, C. W. Hergenrother1, E. S. Howell1, E. R. Jawin20, H. H. Kaplan5, T. R. Kareta 1, L. Le Corre 21, J.-Y. Li21, J. Licandro17, L. F. Lim6, P. Michel 18, J. Molaro21, M. C. Nolan 1, M. Pajola 22, M. Popescu 17, J. L. Rizos Garcia 17, A. Ryan18, S. R. Schwartz 1, N. Shultz1, M. A. Siegler21, P. H. Smith1, E. Tatsumi23, C. A. Thomas24, K. J. Walsh 5, C. W. V. Wolner1, X.-D. Zou21, D. S. Lauretta 1 and The OSIRIS-REx Team25 Establishing the abundance and physical properties of regolith and boulders on asteroids is crucial for understanding the for- mation and degradation mechanisms at work on their surfaces. Using images and thermal data from NASA’s Origins, Spectral Interpretation, Resource Identification, and Security-Regolith Explorer (OSIRIS-REx) spacecraft, we show that asteroid (101955) Bennu’s surface is globally rough, dense with boulders, and low in albedo. -
(155140) 2005 UD and (3200) Phaethon*
The Planetary Science Journal, 1:15 (15pp), 2020 June https://doi.org/10.3847/PSJ/ab8e45 © 2020. The Author(s). Published by the American Astronomical Society. New Evidence for a Physical Link between Asteroids (155140) 2005 UD and (3200) Phaethon* Maxime Devogèle1 , Eric MacLennan2, Annika Gustafsson3 , Nicholas Moskovitz1 , Joey Chatelain4, Galin Borisov5,6, Shinsuke Abe7, Tomoko Arai8, Grigori Fedorets2,9, Marin Ferrais10,11,12, Mikael Granvik2,13 , Emmanuel Jehin10, Lauri Siltala2,14, Mikko Pöntinen2, Michael Mommert1 , David Polishook15, Brian Skiff1, Paolo Tanga16, and Fumi Yoshida8 1 Lowell Observatory, 1400 W. Mars Hill Rd., Flagstaff, AZ 86001, USA; [email protected] 2 Department of Physics, P.O. Box 64, FI-00014 University of Helsinki, Finland 3 Department of Astronomy & Planetary Science, Northern Arizona University, P.O. Box 6010, Flagstaff, AZ 86011, USA 4 Las Cumbres Observatory, CA, USA 5 Armagh Observatory and Planetarium, College Hill, Armagh BT61 9DG, UK 6 Institute of Astronomy and National Astronomical Observatory, Bulgarian Academy of Sciences, 72, Tsarigradsko Chaussèe Blvd., Sofia BG-1784, Bulgaria 7 Aerospace Engineering, Nihon University, 7-24-1 Narashinodai, Funabashi, Chiba 2748501, Japan 8 Planetary Exploration Research Center, Chiba Institute of Technology, Narashino, Japan 9 Astrophysics Research Centre, School of Mathematics and Physics, Queen’s University Belfast, Belfast BT7 1NN, UK 10 Space sciences, Technologies & Astrophysics Research (STAR) Institute University of Liège Allée du 6 Août 19, B-4000 Liège, Belgium 11 Aix Marseille Université, CNRS, LAM (Laboratoire d’Astrophysique de Marseille) UMR 7326, F-13388, Marseille, France 12 Space sciences, Technologies, France 13 Division of Space Technology, LuleåUniversity of Technology, Box 848, SE-98128 Kiruna, Sweden 14 Nordic Optical Telescope, Apartado 474, E-38700 S/C de La Palma, Santa Cruz de Tenerife, Spain 15 Faculty of Physics, Weizmann Institute of Science, 234 Herzl St. -
The Opposition and Tilt Effects of Saturn's Rings from HST Observations
The opposition and tilt effects of Saturn’s rings from HST observations Heikki Salo, Richard G. French To cite this version: Heikki Salo, Richard G. French. The opposition and tilt effects of Saturn’s rings from HST observa- tions. Icarus, Elsevier, 2010, 210 (2), pp.785. 10.1016/j.icarus.2010.07.002. hal-00693815 HAL Id: hal-00693815 https://hal.archives-ouvertes.fr/hal-00693815 Submitted on 3 May 2012 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. Accepted Manuscript The opposition and tilt effects of Saturn’s rings from HST observations Heikki Salo, Richard G. French PII: S0019-1035(10)00274-5 DOI: 10.1016/j.icarus.2010.07.002 Reference: YICAR 9498 To appear in: Icarus Received Date: 30 March 2009 Revised Date: 2 July 2010 Accepted Date: 2 July 2010 Please cite this article as: Salo, H., French, R.G., The opposition and tilt effects of Saturn’s rings from HST observations, Icarus (2010), doi: 10.1016/j.icarus.2010.07.002 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. -
3.1 Discipline Science Results
CASSINI FINAL MISSION REPORT 2019 1 SATURN Before Cassini, scientists viewed Saturn’s unique features only from Earth and from a few spacecraft flybys. During more than a decade orbiting the gas giant, Cassini studied the composition and temperature of Saturn’s upper atmosphere as the seasons changed there. Cassini also provided up-close observations of Saturn’s exotic storms and jet streams, and heard Saturn’s lightning, which cannot be detected from Earth. The Grand Finale orbits provided valuable data for understanding Saturn’s interior structure and magnetic dynamo, in addition to providing insight into material falling into the atmosphere from parts of the rings. Cassini’s Saturn science objectives were overseen by the Saturn Working Group (SWG). This group consisted of the scientists on the mission interested in studying the planet itself and phenomena which influenced it. The Saturn Atmospheric Modeling Working Group (SAMWG) was formed to specifically characterize Saturn’s uppermost atmosphere (thermosphere) and its variation with time, define the shape of Saturn’s 100 mbar and 1 bar pressure levels, and determine when the Saturn safely eclipsed Cassini from the Sun. Its membership consisted of experts in studying Saturn’s upper atmosphere and members of the engineering team. 2 VOLUME 1: MISSION OVERVIEW & SCIENCE OBJECTIVES AND RESULTS CONTENTS SATURN ........................................................................................................................................................................... 1 Executive -
Extended Mission Orbit #2 (XMO2, ~1500 Km Altitude)
Carol A. Raymond Deputy Principal Investigator SBAG 17 Jet Propulsion Laboratory, Caltech 13 Jun 2017 • Spacecraft and instruments are healthy and data return has been excellent to date • Primary mission ended on June 30 2016. All mission objectives and Level-1 requirements were met. • Extended mission at Ceres ends June 30 2017. All mission objectives and Level-1 requirements were met. • Primary mission data archive complete pending ongoing review; extended mission archive is up to date • NASA is considering options for continued operations beyond June 2017 2 • Loss of third reaction wheel on April 23rd limits Dawn’s lifetime – but otherwise does not affect the mission – dependent on hydrazine jets for attitude control – Lifetime decreases with orbit altitude • Dawn is currently in a ~20000x50000 km eccentric orbit • Recently performed opposition observation • Four special journal issues in work: – Icarus: Geological Mapping (in revision) – Icarus: Mineralogical Mapping (submitted) – MAPS: Composition/Crosscutting (in submission) – Icarus: Occator Crater (in progress) – Interest in a special issue on ground ice: contact Britney Schmidt if you would like to participate 3 Ceres Extended Mission Timeline Start of End of End of Extended Mission Extended Mission Project Operations Operations XM1 Science Plan Extended Mission Orbit #1 (XMO1, ~385 km altitude) • Obtain IR spectra of high-priority targets (VIR) ✓ • Expand high-resolution color imaging (FC) ✓ • Improve elemental mapping (GRaND) ✓ • Expand high-resolution surface coverage for topography -
Instrumental Methods for Professional and Amateur
Instrumental Methods for Professional and Amateur Collaborations in Planetary Astronomy Olivier Mousis, Ricardo Hueso, Jean-Philippe Beaulieu, Sylvain Bouley, Benoît Carry, Francois Colas, Alain Klotz, Christophe Pellier, Jean-Marc Petit, Philippe Rousselot, et al. To cite this version: Olivier Mousis, Ricardo Hueso, Jean-Philippe Beaulieu, Sylvain Bouley, Benoît Carry, et al.. Instru- mental Methods for Professional and Amateur Collaborations in Planetary Astronomy. Experimental Astronomy, Springer Link, 2014, 38 (1-2), pp.91-191. 10.1007/s10686-014-9379-0. hal-00833466 HAL Id: hal-00833466 https://hal.archives-ouvertes.fr/hal-00833466 Submitted on 3 Jun 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. Instrumental Methods for Professional and Amateur Collaborations in Planetary Astronomy O. Mousis, R. Hueso, J.-P. Beaulieu, S. Bouley, B. Carry, F. Colas, A. Klotz, C. Pellier, J.-M. Petit, P. Rousselot, M. Ali-Dib, W. Beisker, M. Birlan, C. Buil, A. Delsanti, E. Frappa, H. B. Hammel, A.-C. Levasseur-Regourd, G. S. Orton, A. Sanchez-Lavega,´ A. Santerne, P. Tanga, J. Vaubaillon, B. Zanda, D. Baratoux, T. Bohm,¨ V. Boudon, A. Bouquet, L. Buzzi, J.-L. Dauvergne, A. -
The Future Exploration of Saturn 417-441, in Saturn in the 21St Century (Eds. KH Baines, FM Flasar, N Krupp, T Stallard)
The Future Exploration of Saturn By Kevin H. Baines, Sushil K. Atreya, Frank Crary, Scott G. Edgington, Thomas K. Greathouse, Henrik Melin, Olivier Mousis, Glenn S. Orton, Thomas R. Spilker, Anthony Wesley (2019). pp 417-441, in Saturn in the 21st Century (eds. KH Baines, FM Flasar, N Krupp, T Stallard), Cambridge University Press. https://doi.org/10.1017/9781316227220.014 14 The Future Exploration of Saturn KEVIN H. BAINES, SUSHIL K. ATREYA, FRANK CRARY, SCOTT G. EDGINGTON, THOMAS K. GREATHOUSE, HENRIK MELIN, OLIVIER MOUSIS, GLENN S. ORTON, THOMAS R. SPILKER AND ANTHONY WESLEY Abstract missions, achieving a remarkable record of discoveries Despite the lack of another Flagship-class mission about the entire Saturn system, including its icy satel- such as Cassini–Huygens, prospects for the future lites, the large atmosphere-enshrouded moon Titan, the ’ exploration of Saturn are nevertheless encoura- planet s surprisingly intricate ring system and the pla- ’ ging. Both NASA and the European Space net s complex magnetosphere, atmosphere and interior. Agency (ESA) are exploring the possibilities of Far from being a small (500 km diameter) geologically focused interplanetary missions (1) to drop one or dead moon, Enceladus proved to be exceptionally more in situ atmospheric entry probes into Saturn active, erupting with numerous geysers that spew – and (2) to explore the satellites Titan and liquid water vapor and ice grains into space some of fi Enceladus, which would provide opportunities for which falls back to form nearly pure white snow elds both in situ investigations of Saturn’s magneto- and some of which escapes to form a distinctive ring sphere and detailed remote-sensing observations around Saturn (e.g. -
A Tale of Two Sides: Pluto's Opposition Surge in 2018 and 2019
EPSC Abstracts Vol. 14, EPSC2020-546, 2020, updated on 27 Sep 2021 https://doi.org/10.5194/epsc2020-546 Europlanet Science Congress 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. A Tale of Two Sides: Pluto's Opposition Surge in 2018 and 2019 Anne Verbiscer1, Paul Helfenstein2, Mark Showalter3, and Marc Buie4 1University of Virginia, Charlottesville, VA, USA ([email protected]) 2Cornell University, Ithaca, NY, USA ([email protected]) 3SETI Institute, Mountain View, CA, USA ([email protected]) 4Southwest Research Institute, Boulder, CO, USA ([email protected]) Near-opposition photometry employs remote sensing observations to reveal the microphysical properties of regolith-covered surfaces over a wide range of solar system bodies. When aligned directly opposite the Sun, objects exhibit an opposition effect, or surge, a dramatic, non-linear increase in reflectance seen with decreasing solar phase angle (the Sun-target-observer angle). This phenomenon is a consequence of both interparticle shadow hiding and a constructive interference phenomenon known as coherent backscatter [1-3]. While the size of the Earth’s orbit restricts observations of Pluto and its moons to solar phase angles no larger than α = 1.9°, the opposition surge, which occurs largely at α < 1°, can discriminate surface properties [4-6]. The smallest solar phase angles are attainable at node crossings when the Earth transits the solar disk as viewed from the object. In this configuration, a solar system body is at “true” opposition. When combined with observations acquired at larger phase angles, the resulting reflectance measurement can be related to the optical, structural, and thermal properties of the regolith and its inferred collisional history. -
Near-Infrared Photometry of Mercury Richard W
Georgia Journal of Science Volume 76 No.2 Scholarly Contributions from the Article 4 Membership and Others 2018 Near-Infrared Photometry of Mercury Richard W. Schmude Jr. Gordon State College, [email protected] Follow this and additional works at: https://digitalcommons.gaacademy.org/gjs Recommended Citation Schmude, Richard W. Jr. (2018) "Near-Infrared Photometry of Mercury," Georgia Journal of Science, Vol. 76, No. 2, Article 4. Available at: https://digitalcommons.gaacademy.org/gjs/vol76/iss2/4 This Research Articles is brought to you for free and open access by Digital Commons @ the Georgia Academy of Science. It has been accepted for inclusion in Georgia Journal of Science by an authorized editor of Digital Commons @ the Georgia Academy of Science. Near-Infrared Photometry of Mercury Acknowledgements I am grateful to Gordon State College for a Faculty Development Grand which was awarded in 2014 and enabled me to purchase the SSP-4 photometer. This research articles is available in Georgia Journal of Science: https://digitalcommons.gaacademy.org/gjs/vol76/iss2/4 Schmude: Near-Infrared Photometry of Mercury NEAR-INFRARED PHOTOMETRY OF MERCURY Richard W. Schmude, Jr. Gordon State College ABSTRACT This report summarizes 100 brightness measurements of Mercury made between May 2014 and September 2017 in the J and H near-infrared filters. Brightness models are reported for the J (solar phase angles between 52.3° and 124.5°) and H (solar phase angles between 38.6° and 133.0°) filters. Additional conclusions are as follows: Mercury’s brightness is within 0.1 magnitudes, at a given phase angle, for waxing and waning phases, and the geometric albedos at a solar phase angle of 0° are estimated to be 0.16 ± 0.03 and 0.24 ± 0.05 for the J and H filters, respectively. -
Icarus 220 (2012) 561–576
Icarus 220 (2012) 561–576 Contents lists available at SciVerse ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Ground-based observations of the long-term evolution and death of Saturn’s 2010 Great White Spot ⇑ Agustín Sánchez-Lavega a, , Teresa del Río-Gaztelurrutia a, Marc Delcroix b, Jon J. Legarreta c, Josep M. Gómez-Forrellad d, Ricardo Hueso a, Enrique García-Melendo d,e, Santiago Pérez-Hoyos a, David Barrado-Navascués f,g, Jorge Lillo f,g, International Outer Planet Watch Team IOPW-PVOL 1 a Departamento de Física Aplicada I, Escuela T. Superior de Ingeniería, Universidad del País Vasco, Bilbao, Spain b Commission des Observations Planétaires, Société Astronomique de France, 2 rue de l’Ardèche, 31170 Tournefeuille, France c Departamento de Ingeniería de Sistemas y Automática, E.U.I.T.I., Universidad del País Vasco, Bilbao, Spain d Esteve Duran Observatory Foundation, Montseny 46, 08553 Seva, Spain e Institut de Ciències de l’Espai (CSIC-IEEC), Campus UAB, Facultat de Ciències, Torre C5, parell, 2a pl., E-08193 Bellaterra, Spain f Observatorio de Calar Alto, Centro Astronómico Hispano Alemán, MPIA-CSIC, Calle Jesús Durbán Remón 2-2, 04004 Almería, Spain g Centro de Astrobiología (INTA-CSIC), Dpto. Astrofísica, ESAC campus, PO BOX 78, 28691 Villanueva de la Cañada, Madrid, Spain article info abstract Article history: We report on the long-term evolution of Saturn’s sixth Great White Spot (GWS) event that initiated at Received 25 January 2012 northern mid-latitudes of the planet on December 5th, 2010 (Fletcher, L. et al. [2011]. Science 332, Revised 30 May 2012 1413–1417; Sánchez-Lavega, A. -
Saturnis the Second of the 4 Gas Giants. Like Jupiter It Gives Off More
Saturn is the second of the 4 gas giants. Like Jupiter it gives off more heat than it gets from the Sun. But unlike Jupiter, it has a magnificent set of rings, and it's so light that it would float in water - if you could find a bath big enough! Saturn is about 120,000 km across. It takes 29.46 years to go around the Sun. Like Jupiter, it spins very rapidly - the day lasts for 10 hours and 39 minutes. It has a similar structure to Jupiter. It has a solid core, which is surrounded by a shell of solid hydrogen, which is in turn surrounded by a shell of liquid hydrogen, and then the giant shell of atmosphere. This atmosphere is made of hydrogen and helium gases, and ammonia, with small amounts of other gases. Like Jupiter, Saturn seems to be a bubbling cauldron of liquid and gas. Like Jupiter, the atmosphere of Saturn is NOT in chemical balance, with some unknown process making trace amounts of various gases. Like Jupiter, Saturn gives out more heat than it gets from the Sun. But the heat is made in a different way. On Saturn, the heat comes from the condensing of helium as it sinks in the atmosphere. In the same way that steam gives off heat as it turns from gas into liquid, so helium gives off heat. This heat is is the power supply for the weather of Saturn. Saturn has fierce winds which travel at some 1,700 km/hr near the equator - 3.5 times faster than the winds on Jupiter. -
Your Guide to the Universe
Contents 1. The Sun 3 11. The Place of our Solar System in the Universe 27 2. Why Do We Study the Sun? 4 12. Space Exploration 28 2.1. Top 10 Facts About the Sun: 4 13. South Africa and Space Exploration 30 2.2. A Closer Look at the Sun 5 14. Famous Astronomers 31 3. The Solar System 6 15. Famous Women Astronomers 32 4. The Planets 7 16. Women Astronomers in South Africa 33 4.1. Mercury 8 17. Astronomers in South African History 33 4.2. Venus 9 18. Astronomy In South Africa 34 4.3. Earth 10 18.1. History 34 4.4. Mars 11 18.2. Modern Times 35 4.5. Jupiter 12 18.3. Radio Astronomy 36 4.6. Saturn 13 18.4. The Square Kilometre Array Radio Telescope 37 4.7. Uranus 14 18.5. Geodesy 38 4.8. Neptune 15 4.9. Pluto and Dwarf planets 16 4.10. Asteroids 17 4.11. Moon 18 4.12. Meteoroids, Meteors and Meteorites 19 4.13. Comets 20 5. Stars 21 6. Exoplanets 22 7. Galaxies 23 8. The Milky Way Galaxy 24 9. The Universe and the Big Bang 25 10. Cosmology 26 The Sun We look at the Sun rising every day. It’s bright, it’s big and it warms us up. Our Sun happens to be the brightest object in our Solar System and naturally we are really curious to know more about it. The Sun’s heat and light provide the energy for life to exist on Earth.