Saturn's Exploration Beyond Cassini
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JUICE Red Book
ESA/SRE(2014)1 September 2014 JUICE JUpiter ICy moons Explorer Exploring the emergence of habitable worlds around gas giants Definition Study Report European Space Agency 1 This page left intentionally blank 2 Mission Description Jupiter Icy Moons Explorer Key science goals The emergence of habitable worlds around gas giants Characterise Ganymede, Europa and Callisto as planetary objects and potential habitats Explore the Jupiter system as an archetype for gas giants Payload Ten instruments Laser Altimeter Radio Science Experiment Ice Penetrating Radar Visible-Infrared Hyperspectral Imaging Spectrometer Ultraviolet Imaging Spectrograph Imaging System Magnetometer Particle Package Submillimetre Wave Instrument Radio and Plasma Wave Instrument Overall mission profile 06/2022 - Launch by Ariane-5 ECA + EVEE Cruise 01/2030 - Jupiter orbit insertion Jupiter tour Transfer to Callisto (11 months) Europa phase: 2 Europa and 3 Callisto flybys (1 month) Jupiter High Latitude Phase: 9 Callisto flybys (9 months) Transfer to Ganymede (11 months) 09/2032 – Ganymede orbit insertion Ganymede tour Elliptical and high altitude circular phases (5 months) Low altitude (500 km) circular orbit (4 months) 06/2033 – End of nominal mission Spacecraft 3-axis stabilised Power: solar panels: ~900 W HGA: ~3 m, body fixed X and Ka bands Downlink ≥ 1.4 Gbit/day High Δv capability (2700 m/s) Radiation tolerance: 50 krad at equipment level Dry mass: ~1800 kg Ground TM stations ESTRAC network Key mission drivers Radiation tolerance and technology Power budget and solar arrays challenges Mass budget Responsibilities ESA: manufacturing, launch, operations of the spacecraft and data archiving PI Teams: science payload provision, operations, and data analysis 3 Foreword The JUICE (JUpiter ICy moon Explorer) mission, selected by ESA in May 2012 to be the first large mission within the Cosmic Vision Program 2015–2025, will provide the most comprehensive exploration to date of the Jovian system in all its complexity, with particular emphasis on Ganymede as a planetary body and potential habitat. -
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 -
So, Has Voyager 1 Left the Solar System? Scientists Face Off Cosmic-Ray Fluctuations Could Mean the Craft Has Exited the Sun's Magnetic Field
NATURE | NEWS So, has Voyager 1 left the Solar System? Scientists face off Cosmic-ray fluctuations could mean the craft has exited the Sun's magnetic field. Ron Cowen 21 March 2013 A space physicist this week suggests that NASA’s venerable Voyager 1 spacecraft has become the first vehicle to venture beyond the heliosphere — the magnetic bubble created by the Sun — but other mission scientists disagree. William Webber of New Mexico State University in Las Cruces bases the claim on signals recorded last August by the Voyager 1 cosmic-ray subsystem — a device that he helped to build — along with his late colleague and study co-author Francis McDonald. JPL-Caltech/NASA Voyager 1 recorded a sudden drop in cosmic rays The instrument recorded a dramatic drop in the intensity of the cosmic rays trapped last August, a possible sign that it had left the in the Sun’s magnetic field and a concomitant rise in that of rays generated by more Sun's sphere of influence. distant reaches of the Galaxy. That pattern indicates that Voyager 1 has travelled beyond the Sun’s magnetic influence and is no longer being shielded from galactic cosmic rays, the researchers report in a study published online this week in Geophysical Research Letters1. But if one is to believe a press release issued by NASA on 20 March (the same day the report was published), the two researchers jumped the gun. Other Voyager scientists who analysed the same data last autumn reiterate what they said then: the cosmic-ray data indicate that Voyager 1 is in a transition zone within the outer part of the heliosphere, but until a dramatic change in magnetic-field intensity and direction is detected, the craft remains firmly within the Sun’s magnetic sphere of influence. -
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. -
FROM the SUN to the STARS Narration & Sync Transcript FINAL
FROM THE SUN TO THE STARS narration & sync transcript FINAL page 1 of 35 FROM THE SUN TO THE STARS Transcript including narration (in caps) and sync dialog (lower case.) Existing “open” captions (lower thirds and web icons and language sub-titles noted.) Underwriter announce: “FROM THE SUN TO THE STARS” IS MADE POSSIBLE, IN PART, BY NASA, THE NATIONAL AERONAUTICS AND SPACE ADMINISTRATION. (Sputnik beep) Narration: IN JUST FIFTY YEARS, WE’VE GONE FROM ONE SIMPLE SATELLITE CIRCLING EARTH… …TO MANY THOUSANDS OF OBJECTS ORBITING OUR PLANET. THE FIRST DISCOVERY OF THE SPACE AGE WAS THAT BELTS OF RADIATION SURROUND US. NOW WE KNOW THAT FORCES ORIGINATING AT THE SUN EXTEND OUT ALMOST EIGHT BILLION MILES, TO THE VERY EDGE OF OUR SOLAR SYSTEM. (Music swells) …AND THAT OUR HIGH-TECH CIVILIZATION IS MIGHTILY IMPACTED BY “SPACE WEATHER” NICKY FOX: (no lower third here) We live in the atmosphere of the sun so when the Sun sneezes the Earth catches a cold. IT WAS THE “INTERNATIONAL GEOPHYSICAL YEAR” OF 1957 THAT LAUNCHED THE SPACE AGE. TWO THOUSAND SEVEN AND EIGHT HAVE BEEN WHAT’S KNOWN AS THE “INTERNATIONAL HELIOPHYSICAL YEAR” OR “IHY.” IT’S A TIME TO PLAN NEW SPACECRAFT… …AND TO RECRUIT A NEW GENERATION OF TEACHERS, STUDENTS, AND SCIENTISTS IN NATIONS ACROSS THE GLOBE TO WORK IN SPACE PHYSICS. (Segment titles – text over black – fly in rapidly) FROM THE SUN TO THE STARS narration & sync transcript FINAL page 2 of 35 EACH ACT IN OUR PROGRAM STANDS ALONE… BUT TOGETHER THEY’RE A COMPREHENSIVE OVERVIEW OF IHY… AND WHEN YOU SEE THIS ICON, THAT’S A SIGNAL THERE’S LOTS MORE INFORMATION ONLINE. -
CASSINI Exploration of Saturn
CASSINI Exploration of Saturn Launch Location Cape Canaveral Air Force Station Launch Vehicle Titan IV-B Launch Date October 15, 1997 SATURN What do I see when I picture Saturn? Saturn is the sixth planet from the Sun and has been called “The Jewel of the Solar System.” Scientists be- lieve that Saturn formed more than four billion years ago from the same giant cloud of gas and dust whirling around the very young Sun that formed Earth and the other planets of our solar system. Saturn is much larg- er than Earth. Its mass is 95.18 times Earth’s mass. In other words, it would take over 95 Earths to equal the mass of Saturn. If you could weigh the planets on a giant scale, you would need slightly more than 95 Earths to equal the weight of Saturn. Saturn’s diameter is about 9.5 Earths across. At that ratio, if Saturn were as big as a baseball, Earth would be about half the size of a regular M&M candy. Saturn spins on its axis (rotates) just as our planet Earth spins on its axis. However, its period of rotation, or the time it takes Saturn to spin around one time, is only 10.2 Earth hours. A day on Saturn is just a little more than 10 hours long; so if you lived on Saturn, you would only have to be in school for a couple of hours each day! Because Saturn spins so fast, and its interior is gas, not rock, Saturn is noticeably flattened, top and bottom. -
MOONS of the SOLAR SYSTEM Europa Narrator: Ever Since Man First Looked Into the Heavens, the Most Intriguing Question Has Alway
MOONS OF THE SOLAR SYSTEM Europa Narrator: Ever since man first looked into the heavens, the most intriguing question has always been, "Are we alone?". An icy world, circling Jupiter, could answer that age old question. Professor Michele Dougherty: Moons in our Solar system are very important so that we can understand how they formed and what their interiors are made of, then we'll better understand how our planets formed, and so we'll better understand where we came from. Dr Lewis Dartnell: We now think that beneath the frozen shell of Europa there lies an ocean with more liquid water in it than al the seas and lakes and rivers and oceans for the whole of the Earth put together. And on Earth, where there's water there's life. Narrator: Europa first attracted attention back in the 1970s, when the Voyager spacecraft flew past Jupiter and took the first close up images of its moons. Dr David Rothery: The Voyager fly bys showed that Europa had a young surface and we already knew it was icy and we already knew that the ice couldn't be more than about a 100 kilometres thick. The question was, is it ice all the way the to the rock or is the ice sitting on top of some water? And because it looks like though the surface has moved around a little bit, a lot of people including Arthur C Clarke, the famous science fiction author, were suggesting there is water down there below the ice. Mission Audio: The spacecraft is stable. -
Leonid Gurvits JIVE and TU Delft June 3, 2021 ©Cristian Fattinanzi Piter Y Moons Xplorer
Leonid Gurvits JIVE and TU Delft June 3, 2021 ©Cristian Fattinanzi piter y moons xplorer Why a mission to Jupiter? Bits of history Mission challenges Where radio astronomy comes in • ~2000–2005: success of Cassini and Huygens missions (NASA, ESA, ASI) • 2006: Europlanet meeting in Berlin – “thinking aloud” on a Jovian mission • 2008: ESA-NASA jointly exploring a mission to giant planets’ satellites • ESA "Laplace" mission proposal (Blanc et al. 2009) • ESA Titan and Enceladus Mission (TandEM, Coustenis et al., 2009) • NASA Titan Explorer • 2009: two joint (ESA+NASA) concepts selected for further studies: • Europa Jupiter System Mission (EJSM) • Titan Saturn System Mission (TSSM: Coustenis et al., 2009) • 2010: EJSM-Laplace selected, consisting of two spacecraft: • ESA’s Jupiter Ganymede Orbiter (JGO) • NASA’s Jupiter Europa Orbiter (JEO) • 2012: NASA drops off; EJSM-Laplace/JGO becomes JUICE • 2013: JUICE payload selection completed by ESA; JUICE becomes an L-class mission of ESA’s Vision 2015-2025 • 2015: NASA selects Europa Clipper mission (Pappalardo et al., 2013) Voyager 1, 1979 ©NASA HOW DOES IT SEARCH FOR ORIGINS & WORK? LIFE FORMATION HABITABILITY Introduction Overarching questions JUICE JUICE Science Themes • Emergence of habitable worlds around gas giants • Jupiter system as an archetype for gas giants JUICE concept • European-led mission to the Jovian system • First orbiter of an icy moon • JGO/Laplace scenario with two Europa flybys and moderate-inclination phase at Jupiter • Science payload selected in Feb 2013, fully compatible -
In Situ Exploration of the Giant Planets Olivier Mousis, David H
In situ Exploration of the Giant Planets Olivier Mousis, David H. Atkinson, Richard Ambrosi, Sushil Atreya, Don Banfield, Stas Barabash, Michel Blanc, T. Cavalié, Athena Coustenis, Magali Deleuil, et al. To cite this version: Olivier Mousis, David H. Atkinson, Richard Ambrosi, Sushil Atreya, Don Banfield, et al.. In situ Exploration of the Giant Planets. 2019. hal-02282409 HAL Id: hal-02282409 https://hal.archives-ouvertes.fr/hal-02282409 Submitted on 2 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. In Situ Exploration of the Giant Planets A White Paper Submitted to ESA’s Voyage 2050 Call arXiv:1908.00917v1 [astro-ph.EP] 31 Jul 2019 Olivier Mousis Contact Person: Aix Marseille Université, CNRS, LAM, Marseille, France ([email protected]) July 31, 2019 WHITE PAPER RESPONSE TO ESA CALL FOR VOYAGE 2050 SCIENCE THEME In Situ Exploration of the Giant Planets Abstract Remote sensing observations suffer significant limitations when used to study the bulk atmospheric composition of the giant planets of our solar system. This impacts our knowledge of the formation of these planets and the physics of their atmospheres. A remarkable example of the superiority of in situ probe measurements was illustrated by the exploration of Jupiter, where key measurements such as the determination of the noble gases’ abundances and the precise measurement of the helium mixing ratio were only made available through in situ measurements by the Galileo probe. -
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 -
The Origins of the Discovery Program, 1989-1993
Space Policy 30 (2014) 5e12 Contents lists available at ScienceDirect Space Policy journal homepage: www.elsevier.com/locate/spacepol Transforming solar system exploration: The origins of the Discovery Program, 1989e1993 Michael J. Neufeld National Air and Space Museum, Smithsonian Institution, United States article info abstract Article history: The Discovery Program is a rarity in the history of NASA solar system exploration: a reform program that Received 18 October 2013 has survived and continued to be influential. This article examines its emergence between 1989 and Accepted 18 October 2013 1993, largely as the result of the intervention of two people: Stamatios “Tom” Krimigis of the Johns Available online 19 April 2014 Hopkins University Applied Physics Laboratory (APL), and Wesley Huntress of NASA, who was Division Director of Solar System Exploration 1990e92 and the Associate Administrator for Space Science 1992 Keywords: e98. Krimigis drew on his leadership experience in the space physics community and his knowledge of Space history its Explorer program to propose that it was possible to create new missions to the inner solar system for a NASA Space programme organization fraction of the existing costs. He continued to push that idea for the next two years, but it took the influence of Huntress at NASA Headquarters to push it on to the agenda. Huntress explicitly decided to use APL to force change on the Jet Propulsion Laboratory and the planetary science community. He succeeded in moving the JPL Mars Pathfinder and APL Near Earth Asteroid Rendezvous (NEAR) mission proposals forward as the opening missions for Discovery. But it took Krimigis’s political skill and access to Sen. -
Detection of Chemical Species in Titan's Atmosphere Using High
UNIVERSIDADE DE LISBOA FACULDADE DE CIÊNCIAS DEPARTAMENTO FÍSICA Detection of Chemical Species in Titan’s Atmosphere using High-Resolution Spectroscopy José Luís Fernandes Ribeiro Mestrado em Física Especialização em Astrofísica e Cosmologia Dissertação orientada por: Doutor Pedro Machado 2019 Acknowledgments This master’s thesis would not be possible without the support of my parents, Maria de F´atimaPereira Fernandes Ribeiro and Lu´ısCarlos Pereira Ribeiro, who I would like to thank for believing in me, encouraging me and allowing me to embark on this journey of knowledge and discovery. They made the person that I am today. I would like to thank all my friends and colleagues who accompanied me all these years for the great moments and new experiences that happened trough these years of university. They contributed a lot to my life and for that I am truly grateful. I just hope that I contributed to theirs as well. I also would like to thank John Pritchard from ESO Operations Support for helping me getting the EsoReflex UVES pipeline working on my computer, without him we would probably wouldn’t have the Titan spectra reduced by now. And I also like to thank Doctor Santiago P´erez-Hoyos for his availability to teach our planetary sciences group how to use the NEMESIS Radiative Transfer model and Doctor Th´er`ese Encrenaz for providing the ISO Saturn and Jupiter data. I would like to give a special thank you to Jo˜aoDias and Constan¸caFreire, for their support and help during this work. Lastly, and surely not the least, I would like to thank my supervisor Pedro Machado for showing me how to be a scientist and how to do scientific work.