Magnetospheric Science Sections in Cassini Mission Final Report
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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. -
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. -
“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. -
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. -
PHYS 1401: Descriptive Astronomy Notes: Chapter
PHYS 1401: Descriptive Astronomy Notes: Chapter 07 CHAPTER 07: THE JOVIAN PLANETS NOTES AND SKETCHES 7.1: OBSERVATIONS OF JUPITER AND SATURN The View From Earth ✦ Jupiter and Saturn are naked-eye objects ✦ Uranus and Neptune can be seen using telescopes Spacecraft Exploration Pioneers ✦ Pioneer 10: Launch Mar 72, Jupiter flyby Dec 73 (data relayed through Apr 02) ✦ Pioneer 11: Launch Apr 73, Jupiter Dec 74, Saturn Sep 79 (daily operation stopped Sep 95) Voyager I ✦ Launched Sep 77 ✦ Jupiter flyby Mar 79 ✦ Saturn flyby Nov 80 ✦ Family Portrait Feb 90 ✦ Still transmitting!!! Voyager II ✦ Launched Aug 77 ✦ Jupiter: Jul 79 ✦ Saturn: Aug 81 ✦ Uranus: Jan 86 ✦ Neptune: Aug 89 Galileo ✦ Launched Oct 89 ✦ Reached Jupiter Dec 95 ✦ Orbit until Sep 03 ✦ Decommissioned by sending it crashing into Jupiter Cassini-Huygens ✦ Launched Oct 97 ✦ Jupiter flyby Dec 00 ✦ Arrived at Saturn Jul 04 ✦ Huygens probe separates for Titan: Jan 05 ✦ Still operational New Horizons ✦ Launched Jan 06 ✦ Jupiter flyby Feb 07 ✦ Headed for Pluto then Kuiper belt 7.2: DISCOVERIES OF URANUS AND NEPTUNE ✦ Uranus: 1781, William & Caroline Herschel use telescope ✦ Neptune: 1846, Adams & Leverrier (independently) use gravity 7.3: BULK PROPERTIES OF THE JOVIAN PLANETS Physical Characteristics ✦ All jovians are much less dense than terrestrials ✦ Saturn is least dense; less dense than water ✦ No solid surface; gaseous atmosphere gets hotter & denser deeper below surface until it becomes liquid ✦ Solid core larger than Earth (not Fe-Ni, probably rocky) Rotation Rates ✦ All are spinning -
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. -
Lightning Detection in Planetary Atmospheres
Revised version for Weather Lightning detection in planetary atmospheres Karen L. Aplin1 and Georg Fischer2 1. Department of Physics, University of Oxford, Denys Wilkinson Building, Keble Road, Oxford OX1 3RH UK 2. Space Research Institute, Austrian Academy of Sciences, Schmiedlstr. 6, A- 8042 Graz, Austria Abstract Lightning in planetary atmospheres is now a well-established concept. Here we discuss the available detection techniques for, and observations of, planetary lightning by spacecraft, planetary landers and, increasingly, sophisticated terrestrial radio telescopes. Future space missions carrying lightning-related instrumentation are also summarised, specifically the European ExoMars mission and Japanese Akatsuki mission to Venus, which could both yield lightning observations in 2016. Keywords Atmospheric electricity; instrumentation; space science; measurements 1. Introduction Lightning outside Earth’s atmosphere was first detected at Jupiter by the Voyager 1 spacecraft in March 1979 (Smith et al., 1979; Gurnett et al., 1979). Since then, lightning has been detected on several other planets (e.g. Harrison et al, 2008), and it may even exist outside our solar system (e.g. Aplin, 2013; Hodosán et al., 2016). Beyond simple scientific curiosity, there are several reasons to study planetary lightning. The famous Miller and Urey experiment of the 1950s found that electrical discharges generated in conditions mimicking the early Earth’s atmosphere produced amino acids, the starting point for life (e.g. Parker et al, 2011). More recent work has shown that energetic electrons accelerated in the electric fields in Martian dust storms can affect atmospheric chemistry, which may also be relevant for life (Harrison et al., 2016). The possibility of life elsewhere in the universe, and the conditions needed for it, remains one of the biggest scientific questions facing mankind, and provides a major motivation. -
Overview of Saturn Lightning Observations
OVERVIEW OF SATURN LIGHTNING OBSERVATIONS G. Fischer*, U. A. Dyudina, W. S. Kurth , D. A. Gurnettz, P. Zarka§, T. Barry¶, M. Delcroix, C. Go**, D. Peach, R. Vandebergh , and A. Wesley{ Abstract The lightning activity in Saturn's atmosphere has been monitored by Cassini for more than six years. The continuous observations of the radio signatures called SEDs (Saturn Electrostatic Discharges) combine favorably with imaging observa- tions of related cloud features as well as direct observations of flash–illuminated cloud tops. The Cassini RPWS (Radio and Plasma Wave Science) instrument and ISS (Imaging Science Subsystem) in orbit around Saturn also received ground{based support: The intense SED radio waves were also detected by the giant UTR{2 ra- dio telescope, and committed amateurs observed SED{related white spots with their backyard optical telescopes. Furthermore, the Cassini VIMS (Visual and Infrared Mapping Spectrometer) and CIRS (Composite Infrared Spectrometer) instruments have provided some information on chemical constituents possibly created by the lightning discharges and transported upward to Saturn's upper atmosphere by ver- tical convection. In this paper we summarize the main results on Saturn lightning provided by this multi{instrumental approach and compare Saturn lightning to lightning on Jupiter and Earth. 1 Radio Observations of SEDs by Cassini RPWS Saturn Electrostatic Discharges (SEDs) are short and strong radio bursts that were ini- tially detected by the radio instrument on{board Voyager 1 near Saturn [Warwick et