Saturn's Magnetosphere Via Reconnection at the Magnetopause Compares To
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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 -
Science Objectives May Be Summarized As Follows
MAGNETOSPHERE IMAGING INSTRUMENT (MIMI) 9 ON THE CASSINI MISSION TO SATURN/TITAN 2. Scientific Objectives MIMI science objectives may be summarized as follows: Saturn • Determine the global configuration and dynamics of hot plasma in the magneto- sphere of Saturn through energetic neutral particle imaging of ring current, radia- tion belts, and neutral clouds. • Study the sources of plasmas and energetic ions through in situ measurements of energetic ion composition, spectra, charge state, and angular distributions. • Search for, monitor, and analyze magnetospheric substorm-like activity at Saturn. • Determine through the imaging and composition studies the magnetosphere– satellite interactions at Saturn and understand the formation of clouds of neutral hydrogen, nitrogen, and water products. •Investigate the modification of satellite surfaces and atmospheres through plasma and radiation bombardment. • Study Titan’s cometary interaction with Saturn’s magnetosphere (and the solar wind) via high-resolution imaging and in situ ion and electron measurements. • Measure the high energy (Ee > 1 MeV, Ep > 15 MeV) particle component in the inner (L < 5 RS) magnetosphere to assess cosmic ray albedo neutron decay (CRAND) source characteristics. •Investigate the absorption of energetic ions and electrons by the satellites and rings in order to determine particle losses and diffusion processes within the mag- netosphere. • Study magnetosphere–ionosphere coupling through remote sensing of aurora and in situ measurements of precipitating energetic ions and electrons. Jupiter • Study ring current(s), plasma sheet, and neutral clouds in the magnetosphere and magnetotail of Jupiter during Cassini flyby, using global imaging and in situ mea- surements. S. M. KRIMIGIS ET AL. 10 Interplanetary • Determine elemental and isotopic composition of local interstellar medium through measurements of interstellar pickup ions. -
Voyager 1 Encounter with the Saturnian System Author(S): E
Voyager 1 Encounter with the Saturnian System Author(s): E. C. Stone and E. D. Miner Source: Science, New Series, Vol. 212, No. 4491 (Apr. 10, 1981), pp. 159-163 Published by: American Association for the Advancement of Science Stable URL: http://www.jstor.org/stable/1685660 . Accessed: 04/02/2014 18:59 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. American Association for the Advancement of Science is collaborating with JSTOR to digitize, preserve and extend access to Science. http://www.jstor.org This content downloaded from 131.215.71.79 on Tue, 4 Feb 2014 18:59:21 PM All use subject to JSTOR Terms and Conditions was complicated by several factors. Sat- urn's greater distance necessitated a fac- tor of 3 reduction in the rate of data transmission (44,800 bits per second at Saturn compared to 115,200 bits per sec- Reports ond at Jupiter). Furthermore, Saturn's satellites and rings provided twice as many objects to be studied at Saturn as at Jupiter, and the close approaches to Voyager 1 Encounter with the Saturnian System these objects all occurred within a 24- hour period, compared to nearly 72 Abstract. -
“Phobos Events”—Signatures of Solar Wind Interaction with a Gas Torus?
Earth Planets Space, 50, 453–462, 1998 “Phobos events”—Signatures of solar wind interaction with a gas torus? K. Baumgärtel1,7, K. Sauer2,7, E. Dubinin2,3,7, V. Tarrasov4,5,7, and M. Dougherty6 1Astrophysikalisches Institut Potsdam, 14482 Potsdam, Germany 2Max-Planck-Institut für Aeronomie, 37191 Katlenburg-Lindau, Germany 3Institute of Space Research, 117810 Moscow, Russia 4Centre d’Etude des Environments Terrestre et Planetaires, 78140 Velizy, France 5Lviv Centre of the Institute of Space Research, 290601 Lviv, Ukraine 6Space and Atmospheric Physics, Imperial College, London SW72AZ, U.K. 7International Space Science Institute (ISSI), 3012 Bern, Switzerland (Received August 28, 1997; Revised January 30, 1998; Accepted February 20, 1998) Following recent simulations of the Phobos dust belt formation (Krivov and Hamilton, 1997), the effective dust- induced charge density as estimated is too small to account for the significant solar wind (sw) plasma and magnetic field perturbations observed by the Phobos-2 spacecraft in 1989 near the crossings of the Phobos orbit. In this paper the sw interaction with the Phobos neutral gas torus is re-investigated in a two-ion plasma model in which the newly created ions are treated as unmagnetized, forming a beam (not a ring beam) in the sw frame. A linear instability analysis based on both a cold fluid and a kinetic approach shows that electromagnetic ion beam waves in the whistler range of frequencies, driven most unstable at oblique propagation and appearing as almost purely growing waves in the beam frame, aquire high growth rates and provide a likely mechanism to cause the observed events. -
Dust Clouds and Plasmoids in Saturn's Magnetosphere
Dust clouds and plasmoids in Saturn’s Magnetosphere as seen with four Cassini instruments Emil Khalisi1 Max-Planck-Institute for Nuclear Physics, Saupfercheckweg 1, D–69117 Heidelberg, Germany Abstract We revisit the evidence for a ”dust cloud” observed by the Cassini space- craft at Saturn in 2006. The data of four instruments are simultaneously compared to interpret the signatures of a coherent swarm of dust that would have remained near the equatorial plane for as long as six weeks. The con- spicuous pattern, as seen in the dust counters of the Cosmic Dust Analyser (CDA), clearly repeats on three consecutive revolutions of the spacecraft. That particular cloud is estimated to about 1.36 Saturnian radii in size, and probably broadening. We also present a reconnection event from the magnetic field data (MAG) that leave behind several plasmoids like those reported from the Voyager flybys in the early 1980s. That magnetic bubbles happened at the dawn side of Saturn’s magnetosphere. At their nascency, the magnetic field showed a switchover of its alignment, disruption of flux tubes and a recovery on a time scale of about 30 days. However, we cannot rule out that different events might have taken place. Empirical evidence is shown at another occasion when a plasmoid was carrying a cloud of tiny dust particles such that a connection between plasmoids and coherent dust clouds is probable. Keywords: Dust clouds, Saturn, Cassini mission, Cosmic Dust Analyser, arXiv:1702.01579v1 [astro-ph.EP] 6 Feb 2017 Magnetosphere URL: DOI: http://dx.doi.org/10.1016/j.asr.2016.12.030 (Emil Khalisi) 1Corresponding author: [email protected] Preprint accepted by Advances in Space Research [JASR13029] 7th February 2017 1. -
The Cassini-Huygens Mission Overview
SpaceOps 2006 Conference AIAA 2006-5502 The Cassini-Huygens Mission Overview N. Vandermey and B. G. Paczkowski Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109 The Cassini-Huygens Program is an international science mission to the Saturnian system. Three space agencies and seventeen nations contributed to building the Cassini spacecraft and Huygens probe. The Cassini orbiter is managed and operated by NASA's Jet Propulsion Laboratory. The Huygens probe was built and operated by the European Space Agency. The mission design for Cassini-Huygens calls for a four-year orbital survey of Saturn, its rings, magnetosphere, and satellites, and the descent into Titan’s atmosphere of the Huygens probe. The Cassini orbiter tour consists of 76 orbits around Saturn with 45 close Titan flybys and 8 targeted icy satellite flybys. The Cassini orbiter spacecraft carries twelve scientific instruments that are performing a wide range of observations on a multitude of designated targets. The Huygens probe carried six additional instruments that provided in-situ sampling of the atmosphere and surface of Titan. The multi-national nature of this mission poses significant challenges in the area of flight operations. This paper will provide an overview of the mission, spacecraft, organization and flight operations environment used for the Cassini-Huygens Mission. It will address the operational complexities of the spacecraft and the science instruments and the approach used by Cassini- Huygens to address these issues. I. The Mission Saturn has fascinated observers for over 300 years. The only planet whose rings were visible from Earth with primitive telescopes, it was not until the age of robotic spacecraft that questions about the Saturnian system’s composition could be answered. -
Cassini-Huygens
High Ambitions for an Outstanding Planetary Mission: Cassini-Huygens Composite image of Titan in ultraviolet and infrared wavelengths taken by Cassini’s imaging science subsystem on 26 October. Red and green colours show areas where atmospheric methane absorbs light and reveal a brighter (redder) northern hemisphere. Blue colours show the high atmosphere and detached hazes (Courtesy of JPL /Univ. of Arizona) Cassini-Huygens Jean-Pierre Lebreton1, Claudio Sollazzo2, Thierry Blancquaert13, Olivier Witasse1 and the Huygens Mission Team 1 ESA Directorate of Scientific Programmes, ESTEC, Noordwijk, The Netherlands 2 ESA Directorate of Operations and Infrastructure, ESOC, Darmstadt, Germany 3 ESA Directorate of Technical and Quality Management, ESTEC, Noordwijk, The Netherlands Earl Maize, Dennis Matson, Robert Mitchell, Linda Spilker Jet Propulsion Laboratory (NASA/JPL), Pasadena, California Enrico Flamini Italian Space Agency (ASI), Rome, Italy Monica Talevi Science Programme Communication Service, ESA Directorate of Scientific Programmes, ESTEC, Noordwijk, The Netherlands assini-Huygens, named after the two celebrated scientists, is the joint NASA/ESA/ASI mission to Saturn Cand its giant moon Titan. It is designed to shed light on many of the unsolved mysteries arising from previous observations and to pursue the detailed exploration of the gas giants after Galileo’s successful mission at Jupiter. The exploration of the Saturnian planetary system, the most complex in our Solar System, will help us to make significant progress in our understanding -
Impact of Io's Volcanic Activity to Environment and Dynamics in the Jovian Magnetosphere : from HISAKI Results
Impact of Io's volcanic activity to environment and dynamics in the Jovian magnetosphere : from HISAKI results F. Tsuchiya(1) , K. Yoshioka(2), T. Kimura(1), G. Murakami(3), A. Yamazaki(3), M. Kagitani(1), C. Tao(4), H. Kita(3), R. Koga(1), F. Suzuki(2), R. Hikida(2), Y. Kasaba(1), H. Misawa(1), and T. Sakanoi(1), I. Yoshikawa(2) (1)Tohoku Univ., (2)Univ. Tokyo, (3)ISAS/JAXA, (4)NICT - Launch : Sep 14, 2013, The Hisaki satellite - Size:1m×1m×4m - Orbit:950km×1150km (LEO) EUV spectrograph (EXCEED): Major specifications - Inclination: 30 deg - Wavelength range: 55-145nm - Orbital period : 106 min - Spectral resolution: 0.4-1.0nm Difficult to observe a moon itself - Spatial coverage ~370 arc-sec But designed to observed plasma - Spatial resolution : 17 arc-sec torus and aurora simultaneously Allowed transition lines of FUV/EUV aurora S,O ions (satellite origin) H2 Lyman & Werner bands Mission periods Aurora & gas torus slit Energy flow from outer to inner part of magnetosphere (Primary) 2013-09 - 2014-11 (Extended 1) 2014-12 - 2017-03 (Extended 2) 2017-04 - 2020-03 Yoshioka et al. 2013, Yoshikawa et al. 2014, Yamazaki et al. 2014 2 Summary of the HISAKI findings • Jupiter 1. Internally driven energy release process & inward transport of the energy Yoshioka et al. 2014, Kimura et al. 2015, Badman et al. 2015, Yoshikawa et al. 2016, 2017, Suzuki et al. 2018 2. Solar wind influence on the magnetosphere (plasma torus, radiation belt, and aurora) Kimura et al. 2016, Tao et al. 2016a, 2016b, Kita et al. -
A Study of the Structure and Dynamics of Saturn's Inner Plasma Disk
Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology 1298 A study of the structure and dynamics of Saturn's inner plasma disk MIKA HOLMBERG ACTA UNIVERSITATIS UPSALIENSIS ISSN 1651-6214 ISBN 978-91-554-9353-0 UPPSALA urn:nbn:se:uu:diva-263278 2015 Dissertation presented at Uppsala University to be publicly examined in Lägerhyddsvägen 1, Uppsala, Thursday, 19 November 2015 at 13:00 for the degree of Doctor of Philosophy. The examination will be conducted in English. Faculty examiner: Professor Thomas Cravens (University of Kansas). Abstract Holmberg, M. 2015. A study of the structure and dynamics of Saturn's inner plasma disk. Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology 1298. 53 pp. Uppsala: Acta Universitatis Upsaliensis. ISBN 978-91-554-9353-0. This thesis presents a study of the inner plasma disk of Saturn. The results are derived from measurements by the instruments on board the Cassini spacecraft, mainly the Cassini Langmuir probe (LP), which has been in orbit around Saturn since 2004. One of the great discoveries of the Cassini spacecraft is that the Saturnian moon Enceladus, located at 3.95 Saturn radii (1 RS = 60,268 km), constantly expels water vapor and condensed water from ridges and troughs located in its south polar region. Impact ionization and photoionization of the water molecules, and subsequent transport, creates a plasma disk around the orbit of Enceladus. The plasma disk ion + + + + + + components are mainly hydrogen ions H and water group ions W (O , OH , H2O , and H3O ). The Cassini LP is used to measure the properties of the plasma. -
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 ............................................................................... -
Low Energy Charged Particles at Saturn
JAMES F. CARBARY and STAMATIOS M. KRIMIGIS LOW ENERGY CHARGED PARTICLES AT SATURN Voyager 1 observations of low energy charged particles (electrons and ions) in the magnetosphere of Saturn are described. The ions consist primarily of protons. Molecular hydrogen and a low con centration of helium are also present. Space scientists had long suspected that Saturn, can provide information about the chemical compo 2 like Earth and Jupiter, had a magnetic field capable sition of the particles. ,3 In addition, the instrument of presenting an obstacle to the supersonic flow of scans through a full 360 0 and is thus the only detector the solar wind. This obstacle - a magnetosphere - on board Voyager (a three-axis stabilized spacecraft) could not be detected remotely from the Earth via capable of determining actual flow anisotropies of Saturnian radio emissions because of the great dis charged particles. tance between Earth and Saturn. However, in Sep The trajectory of Voyager 1 during its encounter tember 1979, the Pioneer 11 spacecraft penetrated with Saturn is shown in Fig. 1. In this three the magnetosphere of Saturn and confirmed the ex dimensional view, the bullet-shaped surface labelled pectations that the planet possessed such an environ "magnetopause" represents the magnetohydrody ment. In November 1980, the Voyager 1 spacecraft namic boundary between Saturn's magnetic field and flew past Saturn and made a full set of magnetic field the solar wind. The magnetosphere exhibits a high and charged particle observations of its magneto degree of symmetry due to the alignment of the sphere. planet's magnetic axis with its spin axis. -
Energetic Particle Injection Events in the Kronian Magnetosphere: Applications and Properties
Energetic particle injection events in the Kronian magnetosphere: applications and properties Inaugural-Dissertation zur Erlangung des Doktorgrades der Mathematisch-Naturwissenschaftlichen Fakultät der Universität zu Köln vorgelegt von Anna Liane Müller aus Aßlar Köln 2011 Bibliografische Information der Deutschen Bibliothek Die Deutsche Nationalbibliothek verzeichnet diese Publikation in der Deutschen Nationalbibliografie; detaillierte bibliografische Daten sind im Internet über http://dnb.ddb.de abrufbar. 1. Referent: Prof. Dr. Joachim Saur 2. Referent: Prof. Dr. Bülent Tezkan 3. Referent: Dr. Norbert Krupp eingereicht am: 10.12.2010 Tag der mündlichen Prüfung (Disputation): 31.01.2011 ISBN 978-3-942171-44-1 uni-edition GmbH 2011 http://www.uni-edition.de c Anna L. Müller x This work is distributed under a x Creative Commons Attribution 3.0 License Printed in Germany At the touch of love everybody becomes a poet. - Plato Abstract The Kronian magnetosphere is highly dynamical. The inner part between 3 Rs and 13 Rs contains numerous injections of hot plasma with energies up to a few hundred keV. This thesis concentrates on electron measurements of the Magnetospheric Imaging Instrument (MIMI) onboard the Cassini spacecraft. The azimuthal plasma velocity as well as the in- jections of charged particles will be characterized. Due to the magnetic drifts, the injected particles at various energies begin to disperse and leave an imprint in the electron as well as in the ion energy spectrograms of the MIMI instrument. The shape of these profiles strongly depends on the azimuthal velocity distribution of the magnetospheric plasma, the age of the injection events as well as the trajectory of Cassini.