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1. Lunar Solar Occultation Explorer (LunaSOX)

Author: John F. Cooper, Shadia R. Habbal, Benjamin Boe, Vassilis Angelopoulos, David G. Sibeck, Nikolaos Paschalidis, Edward C. Sittler, Lan K. Jian, and Rosemary M. Killen
Subjects: heliophysics, solar corona, Moon, solar eclipse, solar wind, Astronomy, QB1-991, Geophysics. Cosmic physics, QC801-809
Abstract: In the present decade and beyond, now 51 years after the last Apollo landing, the NASA Artemis human exploration program will offer abundant opportunities for heliophysics investigations from, by, and of the Moon from the vantage points of the lunar orbit and the surface. The Lunar Solar Occultation Explorer (LunaSOX) concept uses the lunar limb to occult the solar disk for high-resolution coronal observations at hourly, daily, to biweekly cadences from spacecraft either in the lunar orbit or at the surface. A 0.2 m diameter solar telescope in orbit with white light and narrow-band visible filters would provide arcsecond spectroscopic imaging of the low-to-high corona (1–10 R☉) with an upper limit of 10–12 B☉ on the local scattered light background from lunar atmospheric dust, as compared to 10–9 B☉ for Earth ground-based solar eclipse observations looking up through the atmosphere at totality. For eclipse observations from and by the Moon, there would be no significant atmospheric disturbances that otherwise limit seeing to arcsec resolution from Earth’s surface. The present eccentric orbits of the ARTEMIS P1 and P2 spacecraft are used as models for a 1 × 10 Rm orbit of LunaSOX to compute the times of solar eclipse intervals, up to 2 hours in duration between the east and west solar hemispheres at a daily cadence for coronal observations at 1–16 R☉ when the orbital aposelene is in anti-sunward directions. In a low-altitude circular orbit and from the surface, the observational cadences would, respectively, be hourly and biweekly. LunaSOX satellites also carrying in situ space environment instruments could integrate into a network of orbital platforms for space weather monitoring and communications relay to far-side surface lander and permanent base sites, e.g., for low-frequency radio cosmology and detection of exoplanet magnetospheres.
Published: 2023
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2. Titan's Ionospheric Chemistry, Fullerenes, Oxygen, Galactic Cosmic Rays and the Formation of Exobiological Molecules on and Within Its Surfaces and Lakes

Author: Edward C. Sittler Jr, John F. Cooper, Steven J Sturner, and Ashraf Ali
Subjects: Lunar And Planetary Science And Exploration
Abstract: We discuss the formation of aerosols within Titan's thermosphere-ionosphere and the different chemical pathways. Negative ion measurements by the Cassini Plasma Spectrometer (CAPS) Electron Spectrometer (ELS) give evidence for formation of unsaturated anion carbon chains, while positive ion measurements of the Cassini Ion Neutral Mass Spectrometer (INMS) indicate formation of more aromatic cation hydrocarbons. There is presently no direct observational evidence for large neutral molecule growth in Titan's thermosphere-ionosphere. The hydrocarbon cations are expected to form Polycyclic Aromatic Hydrocarbons (PAHs), those with the addition of nitrogen being called PAHNs. We theorize anion carbon chains can eventually become long enough to fold into fullerene C60,70 carbon shells, of various charge states. Based on laboratory data the fullerenes can trap incoming O+ magnetospheric ions that have relatively high energy collisions with the fullerenes and, once trapped, protect the oxygen atom from Titan's reducing thermosphere-ionosphere. The fullerenes can form into larger onion fullerenes and condense into larger embryo aerosols (i.e., m/q (mass-to-charge ratio) greater than 10,000 amu/q (atomic mass unit-to-charge ratio) anions as observed by CAPS/ELS) eventually falling onto Titan's surface and precipitating to the bottom of its hydrocarbon lakes. Molecule production composed of H, C, N is known to occur in Titan's atmosphere with energy input from the magnetosphere, solar UV (ultraviolet), and deep-penetrating irradiation from galactic cosmic rays (GCR). Space radiation effects by GCR irradiation of Titan's surface and lakes can lead to the manufacture of exobiological molecules with oxygen as the new ingredient. We have developed a model of galactic cosmic ray irradiation of Titan's atmosphere, surface, subsurface and bottoms of Titan lakes. GCR would provide further energy for processing of the aerosols into more complex organic forms such as tholins and precursor molecules for amino acids. A second process called hydrolysis then converts the precursor molecules into amino acids. Hydrolysis is provided via meteor impacts with size greater than 10 kilometers and cryovolcanism both which can produce liquid water on Titan's surface for episodic periods more than several 100 to 1000 years. Our model shows that GCR secondary particles can penetrate ~100 meters below the ice surface (including the bottom of Titan's less dense hydrocarbon lakes ~150-meter depths) and produce chemically significant dosages over very long timescales ~450 million years. The GCR model is combined with laboratory data from experiments in which dry methyl ices were irradiated to doses producing prebiotic amino acids such as glycine. The model calculations show glycine can form to ~2.5 parts-per-billion levels near the surface after ~450 million years of GCR proton irradiation and potentially to 5 parts-per-billion if heavy-ion GCRs up through Fe are included. If such molecules were detected, this would not only confirm this model but indicate that life forms different from ours may not be required.
Published: 2020
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3. Titan's Ionospheric Chemistry, Fullerenes, Oxygen, Galactic Cosmic Rays and the Formation of Exobiological Molecules on and within its Surfaces and Lakes

Author: Edward C. Sittler Jr, John F. Cooper, Steven J. Sturner, and Ashraf Ali
Subjects: Exobiology, Meteorology And Climatology
Abstract: We discuss the formation of aerosols within Titan's thermosphere-ionosphere and the different chemical pathways. Negative ion measurements by the Cassini Plasma Spectrometer (CAPS) Electron Spectrometer (ELS) give evidence for formation of unsaturated anion carbon chains, while positive ion measurements of the Cassini Ion Neutral Mass Spectrometer (INMS) indicate formation of more aromatic cation hydrocarbons. There is presently no direct observational evidence for large neutral molecule growth in Titan's thermosphere-ionosphere. The hydrocarbon cations are expected to form Polycyclic Aromatic Hydrocarbons (PAH), those with the addition of nitrogen being called PAHNs. We theorize anion carbon chains can eventually become long enough to fold into fullerene C(60,70) carbon shells, of various charge states. Based on laboratory data the fullerenes can trap incoming O(sup +) magnetospheric ions that have relatively high energy collisions with the fullerenes and, once trapped, protect the oxygen atom from Titan's reducing thermosphere-ionosphere. The fullerenes can form into larger onion fullerenes and condense into larger embryo aerosols (i.e., m/q > 10,000 amu/q anions as observed by CAPS/ELS) eventually falling onto Titan's surface and precipitating to the bottom of its hydrocarbon lakes. Molecule production composed of H, C, N is known to occur in Titan's atmosphere with energy input from the magnetosphere, solar UV, and deeppenetrating irradiation from galactic cosmic rays (GCR). Space radiation effects by GCR irradiation of Titan's surface and lakes can lead to the manufacture of exobiological molecules with oxygen as the new ingredient. We have developed a model of galactic cosmic ray irradiation of Titan's atmosphere, surface, subsurface and bottoms of Titan lakes. GCR would provide further energy for processing of the aerosols into more complex organic forms such as tholins and precursor molecules for amino acids. A second process called hydrolysis then converts the precursor molecules into amino acids. Hydrolysis is provided via meteor impacts with size > 10 km and cryovolcanism both which can produce liquid water on Titan's surface for episodic periods > several 100 to 1000 years. Our model shows that GCR secondary particles can penetrate ~ 100 m below the ice surface (including the bottom of Titan's less dense hydrocarbon lakes ~ 150 m depths) and produce chemically significant dosages over very long timescales ~ 450 Myrs. The GCR model is combined with laboratory data from experiments in which dry methyl ices were irradiated to doses producing prebiotic amino acids such as glycine. The model calculations show glycine can form to ~ 2.5 ppb levels near the surface after ~450 Myrs of GCR proton irradiation and potentially to 5 ppb if heavy-ion GCRs up through Fe are included. If such molecules were detected, this would not only confirm this model but indicate that life forms different from ours may not be required.
Published: 2019
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4. On a radiolytic origin of red organics at the surface of the Arrokoth Trans-Neptunian Object

Author: Eric Quirico, Aurore Bacmann, Cédric Wolters, Basile Augé, Laurène Flandinet, Thibault Launois, John F. Cooper, Véronique Vuitton, Thomas Gautier, Lora Jovanovic, Philippe Boduch, Hermann Rothard, Léopold Desage, Alexandre Faure, Bernard Schmitt, Olivier Poch, William M. Grundy, Silvia Protopapa, Sonia Fornasier, Dale P. Cruikshank, S. Alan Stern, Institut de Planétologie et d'Astrophysique de Grenoble (IPAG), Centre National d'Études Spatiales [Toulouse] (CNES)-Observatoire des Sciences de l'Univers de Grenoble (OSUG ), Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Météo-France -Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Météo-France, NASA Goddard Space Flight Center (GSFC), PLANETO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Laboratoire d'études spatiales et d'instrumentation en astrophysique = Laboratory of Space Studies and Instrumentation in Astrophysics (LESIA), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Centre de recherche sur les Ions, les MAtériaux et la Photonique (CIMAP - UMR 6252), Université de Caen Normandie (UNICAEN), Normandie Université (NU)-Normandie Université (NU)-École Nationale Supérieure d'Ingénieurs de Caen (ENSICAEN), Normandie Université (NU)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche sur les Matériaux Avancés (IRMA), Normandie Université (NU)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Rouen Normandie (UNIROUEN), Normandie Université (NU)-Institut national des sciences appliquées Rouen Normandie (INSA Rouen Normandie), Institut National des Sciences Appliquées (INSA)-Normandie Université (NU)-Institut National des Sciences Appliquées (INSA)-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Rouen Normandie (UNIROUEN), Institut National des Sciences Appliquées (INSA)-Normandie Université (NU)-Institut National des Sciences Appliquées (INSA)-Centre National de la Recherche Scientifique (CNRS), Lowell Observatory [Flagstaff], Southwest Research Institute [Boulder] (SwRI), Institut Universitaire de France (IUF), Ministère de l'Education nationale, de l’Enseignement supérieur et de la Recherche (M.E.N.E.S.R.), and University of Central Florida [Orlando] (UCF)
Subjects: [SDU]Sciences of the Universe [physics], Space and Planetary Science, Astronomy and Astrophysics
Abstract: International audience; The classical Kuiper Belt Object (KBO) Arrokoth was surveyed by the New Horizons spacecraft on 1st January 2019, revealing a small bilobed object with a red surface, whose spectral slope lies in the average of the whole KBOs population. This red color has been assigned to reddish organic materials, either inherited from the protosolar disk during accretion, or formed through radiolytic processes in the surface due to exposure to solar or interstellar photons, Solar Wind, Solar Energetic Particles or Galactic Cosmic Rays. We report here a study investigating the radiolytic scenario, based on numerical calculations and experimental simulations run with swift heavy ions (74.8 MeV136Xe19+ and 33.06 MeV58Ni9+), and low-energy 105 keV18O6+ions on CH3OH ice, the only molecule identified at Arrokoth’s surface.
Published: 2023

5. Spectra of Saturn’s proton belts revealed

Author: Peter Kollmann, Elias Roussos, George Clark, John F. Cooper, Steven J. Sturner, Anna Kotova, Leonardo Regoli, Yuri Y. Shprits, Nikita Aseev, Norbert Krupp, Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), and Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)
Subjects: Saturn, Space and Planetary Science, [SDU]Sciences of the Universe [physics], Physics::Space Physics, Astronomy and Astrophysics, Proton, Astrophysics::Earth and Planetary Astrophysics, CRAND, Radiation belts
Abstract: International audience; Saturn is permanently surrounded by 6 discrete proton radiation belts that are rigidly separated by the orbits of its inner moons and dense rings. These radiation belts are ideal environments to study the details of radial diffusion and the CRAND source process, yet progress has been hindered by the fact that the energy spectra are not known with certainty: Reanalysis of the response functions of the LEMMS instrument on-board the Cassini orbiter has shown that measurements of ≲ 10 MeV protons may be easily contaminated by ≳ 10 MeV protons and that many available measurements characterize a very broad energy range, so that the calculation of an energy-resolved spectrum is not as straightforward as previously assumed. Here we use forward modeling of the measurements based on the instrument response and combine this technique where useful with numerical modeling of the proton belt physics in order to determine Saturn's spectra with higher certainty. We find significant proton intensities up to ≈ 1 GeV. While earlier studies reported on proton spectra roughly following a power law with exponent ≈ - 2 , our more advanced analysis shows harder spectra with exponent ≈ - 1 . The observed spectra provide independent confirmation that Saturn's proton belts are sourced by CRAND and are consistent with the provided protons being subsequently cooled in the tenuous gas originating from Saturn or Enceladus. The intensities at Saturn are found to be lower than at Jupiter and Earth, which is also consistent with the source of Saturn being exclusively CRAND, while the other planets can draw from additional processes. Our new spectra can be used in the future to further our understanding of Saturn's proton belts and the respective physical processes that occur at other magnetized planets in general. Also, the spectra have applications for several topics of planetary science, such as space weathering of Saturn's moons and rings, and can be useful to constrain properties of the main rings through their production of secondary particles.
Published: 2022

6. Sources, Sinks, and Transport of Energetic Electrons Near Saturn's Main Rings

Author: Stamatios M. Krimigis, Geraint H. Jones, Elias Roussos, Donald G. Mitchell, Chris Paranicas, John F. Cooper, Peter Kollmann, K. Dialynas, and Norbert Krupp
Subjects: Convection, Physics, 010504 meteorology & atmospheric sciences, Magnetosphere, Resonance, Cosmic ray, Electron, 010502 geochemistry & geophysics, 01 natural sciences, Secondary electrons, symbols.namesake, Geophysics, Saturn, Van Allen radiation belt, Physics::Space Physics, symbols, General Earth and Planetary Sciences, Astrophysics::Earth and Planetary Astrophysics, Atomic physics, 0105 earth and related environmental sciences
Abstract: The inner boundary of Saturn's electron radiation belts, near the planet's A‐ring (∼2.27 Rs), is studied using Cassini's Proximal orbit measurements. We find that variable convective flows transport energetic electrons to the A‐ring, which absorbs them instantaneously, forming the inner belt boundary. These flows are also responsible for a variable and longitudinally asymmetric boundary configuration. Pre‐noon, the boundary oscillates towards and away from the A‐ring with a two‐week period. Post‐noon, it maps persistently near the F‐ring (∼2.32 Rs) and coexists with localized MeV electron intensity enhancements (microbelts). We propose that the microbelts contain electrons in drift resonance with corotation, trapped in local‐time confined trajectories which result from the aforementioned convective flows. The microbelts' collocation with the F‐ring implies either a local, secondary electron production due to Galactic Cosmic Ray collisions with F‐ring dust, or an enhanced resonant electron trapping due to an electrodynamic interaction between the F‐ring and Saturn's magnetosphere.
Published: 2019

7. Ocean Worlds: Science Goals for the Next Decade

Author: Tori M. Hoehler, Wes Patterson, Geoffrey C. Collins, Alyssa Rhoden, Christian Lindensmith, Jason M. Soderblom, Rosaly M. C. Lopes, Laura M. Barge, Kelsi N. Singer, Joseph Westlake, Alexander G. Hayes, Alfred S. McEwen, Morgan L. Cable, Bonnie J. Buratti, Cynthia B. Phillips, Marc Neveu, Terry Hurford, Jeff S. Bowman, Britney E. Schmidt, Chris German, Tom Nordheim, Amanda R. Hendrix, Michael T. Bland, Sona Hosseini, Catherine D. Neish, Steve Vance, Jennifer E.C. Scully, Paul K. Byrne, John F. Cooper, Alex Patthoff, Carly Howett, Serina Diniega, William B. Brinckerhoff, Julie Castillo-Rogez, and Nathalie A. Cabrol
Subjects: Engineering, business.industry, business
Published: 2021

8. Comparative Planetology of Kuiper Belt Dwarf Planets Enabled by the Near-Term Interstellar Probe

Author: A. M. Annex, J. T. Keane, Abigail Rymer, Edwin S. Kite, Michele T. Bannister, Bryan J. Holler, Chester \\'Sonny\\' Harman, Richard Cartwright, Kelsi N. Singer, Chloe B. Beddingfield, Kirby Runyon, Joshua T.S. Cahill, Caitlin Ahrens, Noam R. Izenberg, Ian J. Cohen, Peter Kollmann, Alan Stern, John F. Cooper, and T. Stryk
Subjects: Physics, Planetary science, Dwarf planet, Interstellar probe, Astrobiology, Term (time)
Published: 2021

9. Ocean Worlds: A Roadmap for Science and Exploration

Author: Joseph Westlake, Shannon MacKenzie, Terry Hurford, Michael T. Bland, Rosaly M. C. Lopes, Laura M. Barge, Pamela Such, Amanda R. Hendrix, Wes Patterson, Chris German, Steve Vance, Jeff S. Bowman, Alfred S. McEwen, Tom Nordheim, Morgan L. Cable, Cynthia B. Phillips, Marc Neveu, Kelsi N. Singer, Tori M. Hoehler, John F. Cooper, William B. Brinckerhoff, Alex Patthoff, Carly Howett, Serina Diniega, Jennifer E.C. Scully, Julie Castillo-Rogez, Sona Hosseini, Catherine D. Neish, Jason M. Soderblom, Nathalie A. Cabrol, Paul K. Byrne, Christian Lindensmith, Britney E. Schmidt, Alexander G. Hayes, Bonnie J. Buratti, Geoffrey C. Collins, and Alyssa Rhoden
Published: 2021

10. Update on Space Physics Data Facility (SPDF) Data Archives and Services

Author: Dieter Bilitza, B. T. Harris, H. A. Leckner, Michael Liu, Uthra Rao, Lan Jian, Leonard N. Garcia, T. J. Kovalick, R. C. Johnson, Robert E. McGuire, Robert M. Candey, Sonya Lyatsky, Ronald Yurow, John F. Cooper, D. Aaron Roberts, Nand Lal, Natalia E. Papitashvili, and R. Chimiak
Subjects: Heliophysics, Computer science, Systems engineering, ComputerApplications_COMPUTERSINOTHERSYSTEMS, Space physics
Abstract: The Space Physics Data Facility (SPDF https://spdf.gsfc.nasa.gov), as the non-solar NASA Heliophysics active final archive, works with current operating missions and the heliophysics community to i...
Published: 2020

11. Joint Europa Mission (JEM) a multi-scale study of Europa to characterize its habitability and search for extant life

Author: David Gaudin, Federico Tosi, David Mimoun, Luisa Lara, Joachim Saur, Ralph D. Lorenz, Krishan K. Khurana, Veerle Sterken, Hauke Hussmann, Norbert Krupp, Sascha Kempf, William Desprats, Philippe Garnier, Ralf Srama, Geoffrey Colins, Jérémie Lasue, Jan-Erik Wahlund, Aljona Blöcker, Katrin Stephan, Antonio Genova, Marcello Coradini, Dominique Fontaine, Andrea Longobardo, Luciano Iess, Peter Wurz, Jean-Pierre Lebreton, Dominic Dirkx, Frances Westall, Steve Vance, Michel Blanc, Leonid I. Gurvits, Cyril Cavel, Adam Masters, Gaël Choblet, Roland Wagner, Adrian Jäggi, Károly Szegő, O. Prieto-Ballesteros, Zita Martins, Jean-Charles Marty, Victor Parro, Pascal Regnier, Edward C. Sittler, Tilman Spohn, Renaud Broquet, Javier Gómez-Elvira, Georges Balmino, François Leblanc, Nicolas André, Martin Volwerk, Paul Hartogh, Philippe Martins, Adriaan Schutte, Geraint H. Jones, John F. Cooper, Ernesto Palumba, Tim Van Hoolst, Emma J. Bunce, Valery Lainey, The Royal Society, Centre National de la Recherche Scientifique (France), Ministerio de Economía y Competitividad (España), European Commission, Tosi, F. [0000-0003-4002-2434], Prieto Ballesteros, O. [0000-0002-2278-1210], Longobardo, A. [0000-0002-1797-2741], Van Hoolst, T. [0000-0002-9820-8584], Ministerio de Economía y Competitividad (MINECO), Unidad de Excelencia María de Maeztu Centro de Astrobiología del Instituto Nacional de Técnica Aeroespacial y CSIC, Institut de recherche en astrophysique et planétologie (IRAP), Institut national des sciences de l'Univers (INSU - CNRS)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS), Centro de Astrobiologia [Madrid] (CAB), Instituto Nacional de Técnica Aeroespacial (INTA)-Consejo Superior de Investigaciones Científicas [Madrid] (CSIC), Mullard Space Science Laboratory (MSSL), University College of London [London] (UCL), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich), Astronomical Institute [Bern], University of Bern, Institut Supérieur de l'Aéronautique et de l'Espace (ISAE-SUPAERO), Joint Institute for VLBI in Europe (JIVE ERIC), Technische Universiteit Delft (TU Delft), CSIRO Astronomy and Space Science, Commonwealth Scientific and Industrial Research Organisation [Canberra] (CSIRO), Institute of Geophysics and Planetary Physics [Los Angeles] (IGPP), University of California [Los Angeles] (UCLA), University of California-University of California, Royal Institute of Technology [Stockholm] (KTH ), Airbus Defence and Space, Airbus Group, University of Leicester, Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Wheaton College [Norton], Cyprus Space Exploration Organisation (CSEO), NASA Goddard Space Flight Center (GSFC), Delft University of Technology (TU Delft), Laboratoire de Physique des Plasmas (LPP), Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École polytechnique (X)-Sorbonne Université (SU)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Max-Planck-Institut für Sonnensystemforschung (MPS), Max-Planck-Gesellschaft, Università degli Studi di Roma 'La Sapienza' = Sapienza University [Rome], Laboratory for Atmospheric and Space Physics [Boulder] (LASP), University of Colorado [Boulder], Instituto de Astrofísica de Andalucía (IAA), Consejo Superior de Investigaciones Científicas [Madrid] (CSIC), Institut de Mécanique Céleste et de Calcul des Ephémérides (IMCCE), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Lille-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), HELIOS - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS), Laboratoire de Physique et Chimie de l'Environnement et de l'Espace (LPC2E), Observatoire des Sciences de l'Univers en région Centre (OSUC), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Centre National d’Études Spatiales [Paris] (CNES), Istituto di Astrofisica e Planetologia Spaziali - INAF (IAPS), Istituto Nazionale di Astrofisica (INAF), Johns Hopkins University Applied Physics Laboratory [Laurel, MD] (APL), Télécom ParisTech, Universidade de Lisboa (ULISBOA), Imperial College London, Universität zu Köln, Square Kilometre Array Organisation (SKA), Deutsches Zentrum für Luft- und Raumfahrt (DLR), Wigner Research Centre for Physics [Budapest], Hungarian Academy of Sciences (MTA), Jet Propulsion Laboratory (JPL), NASA-California Institute of Technology (CALTECH), Royal Observatory of Belgium [Brussels] (ROB), Space Research Institute of Austrian Academy of Sciences (IWF), Austrian Academy of Sciences (OeAW), Centre de biophysique moléculaire (CBM), Université d'Orléans (UO)-Institut National de la Santé et de la Recherche Médicale (INSERM)-Centre National de la Recherche Scientifique (CNRS)-Institut de Chimie du CNRS (INC), Unidad de Excelencia Científica María de Maeztu Centro de Astrobiología del Instituto Nacional de Técnica Aeroespacial y CSIC, MDM-2017-0737, Agencia Estatal de Investigación (AEI), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), University of California (UC)-University of California (UC), Airbus Defence and Space [Les Mureaux], ASTRIUM, Max-Planck-Institut für Sonnensystemforschung = Max Planck Institute for Solar System Research (MPS), Università degli Studi di Roma 'La Sapienza' = Sapienza University [Rome] (UNIROMA), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Universidade de Lisboa = University of Lisbon (ULISBOA), Universität zu Köln = University of Cologne, Université d'Orléans (UO)-Institut National de la Santé et de la Recherche Médicale (INSERM)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS), Institut Supérieur de l'Aéronautique et de l'Espace - ISAE-SUPAERO (FRANCE), Cardon, Catherine, Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), and Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)
Subjects: Solar System, 010504 meteorology & atmospheric sciences, Outer planets exploration, Habitability, HUYGENS PROBE, Europa mission, Mission, 01 natural sciences, 7. Clean energy, Astrobiology, law.invention, Extant taxon, SULFURIC-ACID, law, Galileo (satellite navigation), 010303 astronomy & astrophysics, Europa Orbiter, INSTRUMENT, SECONDARY, PLUME, HYDRATED SALT MINERALS, Physical Sciences, symbols, Europa, Jupiter system, SURFACE, Astronomy & Astrophysics, [SDU] Sciences of the Universe [physics], symbols.namesake, Orbiter, Search for life, 0103 physical sciences, Ocean moon, 0201 Astronomical and Space Sciences, Astrophysique, 0105 earth and related environmental sciences, Science & Technology, Galilean Satellites, Scale (chemistry), Astronomy and Astrophysics, ATMOSPHERE, EVOLUTION, 13. Climate action, Space and Planetary Science, [SDU]Sciences of the Universe [physics], Environmental science, Joint (building), habitability, jupiter system, ocean moon, outer planets exploration, search for life, SATELLITES
Abstract: Full list of authors: Blanc, Michel; Prieto-Ballesteros, Olga; André, Nicolas; Gomez-Elvira, Javier; Jones, Geraint; Sterken, Veerle; Desprats, William; Gurvits, Leonid I.; Khurana, Krishan; Balmino, Georges; Blöcker, Aljona; Broquet, Renaud; Bunce, Emma; Cavel, Cyril; Choblet, Gaël; Colins, Geoffrey; Coradini, Marcello; Cooper, John; Dirkx, Dominic; Fontaine, Dominique; Garnier, Philippe; Gaudin, David; Hartogh, Paul; Hussmann, Hauke; Genova, Antonio; Iess, Luciano; Jäggi, Adrian; Kempf, Sascha; Krupp, Norbert; Lara, Luisa; Lasue, Jérémie; Lainey, Valéry; Leblanc, François; Lebreton, Jean-Pierre; Longobardo, Andrea; Lorenz, Ralph; Martins, Philippe; Martins, Zita; Marty, Jean-Charles; Masters, Adam; Mimoun, David; Palumba, Ernesto; Parro, Victor; Regnier, Pascal; Saur, Joachim; Schutte, Adriaan; Sittler, Edward C.; Spohn, Tilman; Srama, Ralf; Stephan, Katrin; Szegő, Károly; Tosi, Federico; Vance, Steve; Wagner, Roland; Van Hoolst, Tim; Volwerk, Martin; Wahlund, Jan-Erik; Westall, Frances; Wurz, Peter, Europa is the closest and probably the most promising target to search for extant life in the Solar System, based on complementary evidence that it may fulfil the key criteria for habitability: the Galileo discovery of a sub-surface ocean; the many indications that the ice shell is active and may be partly permeable to transfer of chemical species, biomolecules and elementary forms of life; the identification of candidate thermal and chemical energy sources necessary to drive a metabolic activity near the ocean floor. In this article we are proposing that ESA collaborates with NASA to design and fly jointly an ambitious and exciting planetary mission, which we call the Joint Europa Mission (JEM), to reach two objectives: perform a full characterization of Europa's habitability with the capabilities of a Europa orbiter, and search for bio-signatures in the environment of Europa (surface, subsurface and exosphere) by the combination of an orbiter and a lander. JEM can build on the advanced understanding of this system which the missions preceding JEM will provide: Juno, JUICE and Europa Clipper, and on the Europa lander concept currently designed by NASA (Maize, report to OPAG, 2019). We propose the following overarching goals for our Joint Europa Mission (JEM): Understand Europa as a complex system responding to Jupiter system forcing, characterize the habitability of its potential biosphere, and search for life at its surface and in its sub-surface and exosphere. We address these goals by a combination of five Priority Scientific Objectives, each with focused measurement objectives providing detailed constraints on the science payloads and on the platforms used by the mission. The JEM observation strategy will combine three types of scientific measurement sequences: measurements on a high-latitude, low-altitude Europan orbit; in-situ measurements to be performed at the surface, using a soft lander; and measurements during the final descent to Europa's surface. The implementation of these three observation sequences will rest on the combination of two science platforms: a soft lander to perform all scientific measurements at the surface and sub-surface at a selected landing site, and an orbiter to perform the orbital survey and descent sequences. We describe a science payload for the lander and orbiter that will meet our science objectives. We propose an innovative distribution of roles for NASA and ESA; while NASA would provide an SLS launcher, the lander stack and most of the mission operations, ESA would provide the carrier-orbiter-relay platform and a stand-alone astrobiology module for the characterization of life at Europa's surface: the Astrobiology Wet Laboratory (AWL). Following this approach, JEM will be a major exciting joint venture to the outer Solar System of NASA and ESA, working together toward one of the most exciting scientific endeavours of the 21st century: to search for life beyond our own planet. © 2020, The authors received support from the sponsors of their home institutions during the development of their projects, particularly at the two institutes leading this effort: at IRAP, Toulouse, MB and NA acknowledge the support of CNRS, University Toulouse III - Paul Sabatier and CNES. At CAB, Madrid, OPB and JGE acknowledge the support of INTA and Spanish MINECO project ESP2014-55811-C2-1-P and ESP2017-89053-C2-1-P and the AEI project MDM-2017-0737 Unidad de Excelencia "Maria de Maeztu". We would also like to extend special thanks to the PASO of CNES for its precious assistance and expertise in the design of the mission scenario.
Published: 2020

12. Parker Solar Probe In-Situ Data at the SPDF Archives

Author: Robert M. Candey, Michael Liu, Nand Lal, T. J. Kovalick, R. Chimiak, Dieter Bilitza, Uthra Rao, B. T. Harris, H. A. Leckner, Codie Gladney, Leonard N. Garcia, Natalia E. Papitashvili, Robert E. McGuire, Lan Jian, John F. Cooper, Ronald Yurow, R. C. Johnson, and D. Aaron Roberts
Subjects: Physics, Heliophysics, Astronomy, Space physics, Solar physics, Solar data, Analysis center
Abstract: The Space Physics Data Facility (SPDF https://spdf.gsfc.nasa.gov) and Solar Data Analysis Center (SDAC https://umbra.nascom.nasa.gov/), as the NASA Heliophysics active final archives, will be prese...
Published: 2020

13. Effects of multiscale phase-mixing and interior conductance in the lunar-like pickup ion plasma wake. First results from 3-D hybrid kinetic modeling

Author: John F. Cooper, Menelaos Sarantos, A.S. Lipatov, and William M. Farrell
Subjects: Physics, 010504 meteorology & atmospheric sciences, Gyroradius, Astronomy and Astrophysics, Photoionization, Plasma, Electron, 01 natural sciences, Ion, Pickup Ion, Physics::Plasma Physics, Space and Planetary Science, Ionization, Physics::Space Physics, 0103 physical sciences, Atomic physics, 010303 astronomy & astrophysics, 0105 earth and related environmental sciences, Exosphere
Abstract: The study of multiscale pickup ion phase-mixing in the lunar plasma wake with a hybrid model is the main subject of our investigation in this paper. Photoionization and charge exchange of protons with the lunar exosphere are the ionization processes included in our model. The computational model includes the self-consistent dynamics of the light ( H + or H 2 + and He + ), and heavy ( Na + ) pickup ions. The electrons are considered as a fluid. The lunar interior is considered as a weakly conducting body. In this paper we considered for the first time the cumulative effect of heavy neutrals in the lunar exosphere (e.g., Al, Ar), an effect which was simulated with one species of Na + but with a tenfold increase in total production rates. We find that various species produce various types of plasma tail in the lunar plasma wake. Specifically, Na + and He + pickup ions form a cycloid-like tail, whereas the H + or H 2 + pickup ions form a tail with a high density core and saw-like periodic structures in the flank region. The length of these structures varies from 1.5 R M to 3.3 R M depending on the value of gyroradius for H + or H 2 + pickup ions. The light pickup ions produce more symmetrical jump in the density and magnetic field at the Mach cone which is mainly controlled by the conductivity of the interior, an effect previously unappreciated. Although other pickup ion species had little effect on the nature of the interaction of the Moon with the solar wind, the global structure of the lunar tail in these simulations appeared quite different when the H 2 + production rate was high.
Published: 2018

14. Particle Radiation Sources, Propagation and Interactions in Deep Space, at Earth, the Moon, Mars, and Beyond: Examples of Radiation Interactions and Effects

Author: Cary Zeitlin, John F. Cooper, Harlan E. Spence, C. Joyce, M. I. Desai, Jon A. Linker, Andrew P. Jordan, Lawrence W. Townsend, Kamen Kozarev, Tibor Torok, Pete Riley, Nathan A. Schwadron, Matt Gorby, Cooper Downs, Jody K. Wilson, and Zoran Mikic
Subjects: Physics, Solar System, 010504 meteorology & atmospheric sciences, Astronomy, Astronomy and Astrophysics, Mars Exploration Program, 01 natural sciences, Regolith, Physics::Geophysics, Astrobiology, Planetary science, Space and Planetary Science, Planet, Health threat from cosmic rays, Physics::Space Physics, 0103 physical sciences, Astrophysics::Solar and Stellar Astrophysics, Astrophysics::Earth and Planetary Astrophysics, Particle radiation, Interplanetary spaceflight, 010303 astronomy & astrophysics, 0105 earth and related environmental sciences
Abstract: Particle radiation has significant effects for astronauts, satellites and planetary bodies throughout the Solar System. Acute space radiation hazards pose risks to human and robotic exploration. This radiation also naturally weathers the exposed surface regolith of the Moon, the two moons of Mars, and other airless bodies, and contributes to chemical evolution of planetary atmospheres at Earth, Mars, Venus, Titan, and Pluto. We provide a select review of recent areas of research covering the origin of SEPs from coronal mass ejections low in the corona, propagation of events through the solar system during the anomalously weak solar cycle 24 and important examples of radiation interactions for Earth, other planets and airless bodies such as the Moon.
Published: 2017

15. Energetic Radiation From Galactic Cosmic Ray Interactions With Saturn's Main Rings

Author: John F. Cooper and Steven J. Sturner
Subjects: Photon, 010504 meteorology & atmospheric sciences, Astrophysics::High Energy Astrophysical Phenomena, Rings of Saturn, Gamma ray, Cosmic ray, Radiation, 01 natural sciences, Charged particle, Article, Nuclear physics, Geophysics, Space and Planetary Science, Saturn, 0103 physical sciences, Physics::Space Physics, Astrophysics::Earth and Planetary Astrophysics, 010303 astronomy & astrophysics, 0105 earth and related environmental sciences, Fermi Gamma-ray Space Telescope
Abstract: Saturn’s main rings have an energetic particle and gamma ray photon radiation environment produced by ring interactions of galactic cosmic ray (GCR) protons and heavier ions penetrating the planetary dipolar magnetic field. Accurate models of this radiation environment are important for interpretation of Pioneer 11 and Cassini in situ measurements near the rings and for constraints on radiolytic contributions to neutral gas production and ice chemistry. A GEANT (GEometry ANd Tracking) based simulation is used to model flux spectra of protons, electrons, positrons, charged pions, neutrons, and gamma ray photons emitted from GCR interactions with H(2)O ice spheres approximating the ring material. Dependent on location in the A to D rings within the planetary magnetic field of Saturn, only GCR protons above respective energies of 20 to 72 GeV can reach the rings without being deflected away by the magnetic field. Calculated differential and integral fluxes from our simulations have good agreement with in situ Pioneer-11 measurements in selected energy channels. The charged particle and neutral radiation measurements are sensitive, respectively, to the sizes and areal mass densities of ring bodies. Computed gamma ray emission fluxes are 8% of our calculated limit for detection from the Earth by the Fermi Large Area Telescope. Addition of charged particle sensors and neutron-photon imaging spectrometers to a future Saturn Ring Observer mission would provide valuable information on the ring mass structure. The present paper provides a foundation for modeling of Pioneer 11 and Cassini radiation measurements across the main rings and future measurements of radiation from the rings.
Published: 2019

16. The Contribution of Electrons to the Sputter-produced O2 Exosphere on Europa

Author: Mark J. Loeffler, R. M. Meier, John F. Cooper, and M. R. Davis
Subjects: Physics, Astrochemistry, Jovian satellites, Astronomy, Astronomy and Astrophysics, Cosmic ray, Electron, Galilean moons, symbols.namesake, Space and Planetary Science, Sputtering, symbols, Spectroscopy, Exosphere
Abstract: Electrons contribute a strong radiation component to the surface bombardment of Europa. However, they are not typically considered to contribute to erosion of the surface H2O-ice or produce exospheres of radiolytic O2, as laboratory studies on sputtering induced by electrons are sparse. Here we have measured the sputtering yield of H2O-ice induced by 0.5 keV electrons between 14 and 125 K, estimating the composition of the stable products ejected during irradiation. Combining these measurements with updated electron flux measurements, we estimate for the first time that the global surface production rate of O2 from electron-induced sputtering is larger than the production rate previously estimated for all of the ionic components combined. Our results emphasize the importance of electrons in producing exospheres on icy satellites and suggest that these exospheres need not be tied to environments where the surface is being bombarded with heavy ions.
Published: 2021

17. Direct Carbon Fuel Cells – Wetting behavior of graphitic carbon in molten carbonate

Author: Yue Li, John F. Cooper, Feng Peng, Philip Nash, J. Robert Selman, and Satish J. Parulekar
Subjects: Materials science, Renewable Energy, Sustainability and the Environment, Inorganic chemistry, Energy Engineering and Power Technology, chemistry.chemical_element, 02 engineering and technology, Partial pressure, 010402 general chemistry, 021001 nanoscience & nanotechnology, Condensed Matter Physics, 01 natural sciences, 0104 chemical sciences, Boudouard reaction, Fuel Technology, Adsorption, chemistry, Chemical engineering, Meniscus, Graphite, Wetting, 0210 nano-technology, Carbon, Eutectic system
Abstract: The wetting behavior of graphitic carbon in a eutectic melt of Li K molten carbonate was investigated at two different temperatures (650 and 750 °C) under two different CO2 partial pressures. The development of the meniscus and the formation of a super-meniscus film were followed optically over a period of 24 h after partial immersion of the graphite rods. Post-test EDX analyses of the graphite surfaces exposed to the melt, above and below the meniscus, were compared to those of surfaces not exposed to the melt. The most important feature found in the EDX analyses is the non-uniform atomic distribution of oxygen both along the length of the immersed surface and in the radial cross-section of the rods exposed to the melt. In addition, the effect of pre-test exposure to gas atmospheres at various temperatures and CO2 partial pressures was investigated. The wetting behavior is found to be influenced strongly by reactions occurring at the carbon surface before and after the start of wetting. In particular, CO produced by the reverse Boudouard reaction, which appears to be physisorbed, and chemically adsorbed oxide ion, O2−, are inferred to play a dominant role in the development of the meniscus leading to a super-meniscus film on the graphitic surface. Several reaction mechanisms are examined to explain the results observed in this work, which agree with results of earlier work from this laboratory, in terms of CO and oxide ion formation.
Published: 2016

18. A possible explanation for the presence of crystalline H2O-ice on Kuiper Belt Objects

Author: Mark J. Loeffler, John F. Cooper, Steven J. Sturner, and Patrick D. Tribbett
Subjects: Solar System, Materials science, Astrochemistry, 010504 meteorology & atmospheric sciences, Astronomy and Astrophysics, Cosmic ray, Electron, Astrophysics, 01 natural sciences, Space and Planetary Science, 0103 physical sciences, Spectroscopy, 010303 astronomy & astrophysics, Event (particle physics), 0105 earth and related environmental sciences
Abstract: The detection of crystalline H2O-ice on multiple surfaces of Kuiper Belt Objects (KBOs) seems to contrast with what scientists understand about the surface environment of these objects, as previous estimates suggest that radiolysis should have easily amorphized these objects' surface over their lifetimes. Here, we use a detailed laboratory approach to show that crystalline H2O-ice can be amorphized by energetic electrons at temperatures as high as 70 K. However, the estimated time needed to completely amorphize the H2O-ice present on the surface of a KBO to the depth probed by near-infrared spectroscopy is only slightly less than the age of the solar system. Given the uncertainties involved in these types of extrapolations and the possibility of a resurfacing event occurring in these objects lifetime, the detection of crystalline or at least partially crystalline H2O-ice on KBOs should be expected.
Published: 2020

19. Titan's ionospheric chemistry, fullerenes, oxygen, galactic cosmic rays and the formation of exobiological molecules on and within its surfaces and lakes

Author: Ashraf Ali, Edward C. Sittler, John F. Cooper, and Steven J. Sturner
Subjects: chemistry.chemical_classification, Fullerene, 010504 meteorology & atmospheric sciences, Chemistry, chemistry.chemical_element, Astronomy and Astrophysics, Tholin, Cosmic ray, Photochemistry, Mass spectrometry, 01 natural sciences, Nitrogen, Ion, symbols.namesake, Hydrocarbon, Space and Planetary Science, 0103 physical sciences, symbols, Titan (rocket family), 010303 astronomy & astrophysics, 0105 earth and related environmental sciences
Abstract: We discuss the formation of aerosols within Titan's thermosphere-ionosphere and the different chemical pathways. Negative ion measurements by the Cassini Plasma Spectrometer (CAPS) Electron Spectrometer (ELS) give evidence for formation of unsaturated anion carbon chains, while positive ion measurements of the Cassini Ion Neutral Mass Spectrometer (INMS) indicate formation of more aromatic cation hydrocarbons. There is presently no direct observational evidence for large neutral molecule growth in Titan's thermosphere-ionosphere. The hydrocarbon cations are expected to form Polycyclic Aromatic Hydrocarbons (PAH), those with the addition of nitrogen being called PAHNs. We theorize anion carbon chains can eventually become long enough to fold into fullerene C60,70 carbon shells, of various charge states. Based on laboratory data the fullerenes can trap incoming O+ magnetospheric ions that have relatively high energy collisions with the fullerenes and, once trapped, protect the oxygen atom from Titan's reducing thermosphere-ionosphere. The fullerenes can form into larger onion fullerenes and condense into larger embryo aerosols (i.e., m/q > 10,000 amu/q anions as observed by CAPS/ELS) eventually falling onto Titan's surface and precipitating to the bottom of its hydrocarbon lakes. Molecule production composed of H, C, N is known to occur in Titan's atmosphere with energy input from the magnetosphere, solar UV, and deep-penetrating irradiation from galactic cosmic rays (GCR). Space radiation effects by GCR irradiation of Titan's surface and lakes can lead to the manufacture of exobiological molecules with oxygen as the new ingredient. We have developed a model of galactic cosmic ray irradiation of Titan's atmosphere, surface, subsurface and bottoms of Titan lakes. GCR would provide further energy for processing of the aerosols into more complex organic forms such as tholins and precursor molecules for amino acids. A second process called hydrolysis then converts the precursor molecules into amino acids. Hydrolysis is provided via meteor impacts with size >10 km and cryovolcanism both which can produce liquid water on Titan's surface for episodic periods > several 100 to 1000 years. Our model shows that GCR secondary particles can penetrate ~ 100 m below the ice surface (including the bottom of Titan's less dense hydrocarbon lakes ~ 150 m depths) and produce chemically significant dosages over very long timescales ~ 450 Myrs. The GCR model is combined with laboratory data from experiments in which dry methyl ices were irradiated to doses producing prebiotic amino acids such as glycine. The model calculations show glycine can form to ~ 2.5 ppb levels near the surface after ~ 450 Myrs of GCR proton irradiation and potentially to 5 ppb if heavy-ion GCRs up through Fe are included. If such molecules were detected, this would not only confirm this model but indicate that life forms different from ours may not be required.
Published: 2020

20. Plasma, Neutral Atmosphere, and Energetic Radiation Environments of Planetary Rings

Author: Elias Roussos, Robert E. Johnson, John F. Cooper, E. C. Sittler, and Peter Kollmann
Subjects: Materials science, Neutral atmosphere, Plasma, Radiation, Planetary ring, Astrobiology
Published: 2018

21. MeV proton flux predictions near Saturn's D ring

Author: Elias Roussos, Peter Kollmann, D. G. Mitchell, Chris Paranicas, John F. Cooper, Anna Kotova, and Norbert Krupp
Subjects: Physics, Rings of Saturn, Astronomy, Atmosphere, symbols.namesake, Geophysics, Space and Planetary Science, Planet, Saturn, Magnetosphere of Saturn, Van Allen radiation belt, Physics::Space Physics, symbols, Astrophysics::Earth and Planetary Astrophysics, Absorption (electromagnetic radiation), Saturn's hexagon
Abstract: Radiation belts of MeV protons have been observed just outward of Saturn's main rings. During the final stages of the mission, the Cassini spacecraft will pass through the gap between the main rings and the planet. Based on how the known radiation belts of Saturn are formed, it is expected that MeV protons will be present in this gap and also bounce through the tenuous D ring right outside the gap. At least one model has suggested that the intensity of MeV protons near the planet could be much larger than in the known belts. We model this inner radiation belt using a technique developed earlier to understand Saturn's known radiation belts. We find that the inner belt is very different from the outer belts in the sense that its intensity is limited by the densities of the D ring and Saturn's upper atmosphere, not by radial diffusion and satellite absorption. The atmospheric density is relatively well constrained by EUV occultations. Based on that we predict an intensity in the gap region that is well below that of the known belts. It is more difficult to do the same for the region magnetically connected to the D ring since its density is poorly constrained. We find that the intensity in this region can be comparable to the known belts. Such intensities pose no hazard to the mission since Cassini would only experience these fluxes on timescales of minutes but might affect scientific measurements by decreasing the signal-to-contamination ratio of instruments.
Published: 2015

22. Particle Radiation Sources, Propagation and Interactions in Deep Space, at Earth, the Moon, Mars, and Beyond: Examples of Radiation Interactions and Effects

Author: Nathan A. Schwadron, John F. Cooper, Mihir Desai, Cooper Downs, Matt Gorby, Andrew P. Jordan, Colin J. Joyce, Kamen Kozarev, Jon A. Linker, Zoran Mikíc, Pete Riley, Harlan E. Spence, Tibor Török, Lawrence W. Townsend, Jody K. Wilson, and Cary Zeitlin
Published: 2017

23. Analysis of the carbon anode in carbon conversion cells

Author: J. Robert Selman and John F. Cooper
Subjects: Renewable Energy, Sustainability and the Environment, Direct carbon fuel cell, Chemistry, Open-circuit voltage, Inorganic chemistry, Analytical chemistry, Energy Engineering and Power Technology, Overpotential, Condensed Matter Physics, Electrochemistry, Anode, Electrochemical cell, Fuel Technology, Graphite, Current density
Abstract: We examine further the electrochemical oxidation of carbon in molten carbonate, based on analysis of published research. Ascending and descending branches of voltage hysteresis found in current sweeps of atomically-ordered graphite and of disordered carbon (coal char) are separated by about 0.20–0.25 V and by 0.10–0.15 V for ordered and disordered forms, respectively, over a wide band of current density, 0.03–0.10 A/cm2. The higher voltage of the descending branch is in rough agreement with prediction of the Y. Li model for the carbon/carbonate electrode in the same current range, for ordered graphite (La = 70–100 nm) and for disordered structures (La = 3–5 nm), respectively. We suggest that the amplitude of the hysteresis represents the difference between the overvoltage requirements for 2- and 4 electron net transfer processes, respectively. The 2 e− reaction (C + CO32− = CO + CO2 + 2e−) dominates the low current segment (LCS) of our previous analysis, and the more hindered 4e− transfer reaction (C + 2CO32− = 3CO2 + 4e−) dominates the high current segment (HCS). The voltage increase separating LCS from HCS is effected by accumulation of CO2 within small, melt-filled pores to form highly supersaturated solutions of CO2, which enhance anode voltage by a concentration overpotential of 0.10–0.25 V. Overpotential increases with reaction extent until (1) overall polarization inhibits the interior reaction and shifts CO2 production to the more accessible exterior surface, or, (2) at a critical concentration (dependent on surface tension and pore diameter) bubbles nucleate and block current flow in the pores. Further support for this picture comes from the often-reported deviation of the gas composition from the CO/CO2 ratio of the Boudouard equilibrium at atmospheric pressure, as open circuit conditions are approached in an electrochemical cell. Our interpretation accounts for the mole fraction of CO2 at open circuit being greater than predicted from the Boudouard equilibrium.
Published: 2014

24. Titan׳s plasma environment: 3D hybrid kinetic modeling of the TA flyby and comparison with CAPS-ELS and RPWS LP observations

Author: A.S. Lipatov, David G. Simpson, John F. Cooper, E. C. Sittler, and R. E. Hartle
Subjects: Physics, Astronomy and Astrophysics, Photoionization, Electron, Plasma, Kinetic energy, Ion, Pickup Ion, symbols.namesake, Physics::Plasma Physics, Space and Planetary Science, Ionization, Physics::Space Physics, symbols, Atomic physics, Titan (rocket family)
Abstract: In this report we discuss the global plasma environment of the TA flyby from the perspective of 3D hybrid modeling. In our model the background, pickup, and ionospheric ions are considered as particles, whereas the electrons are described as a fluid. Inhomogeneous photoionization, electron-impact ionization and charge exchange are included in our model. We also take into account the collisions between the ions and neutrals. Our modeling shows that mass loading of the background plasma ( H + , O + ) by pickup ions H 2 + , CH 4 + and N 2 + differs from the T9 encounter simulations when O + ions are not introduced into the background plasma. In our hybrid modeling we use Chamberlain profiles for the atmospheric components. We also include a simple ionosphere model with average mass M =28 amu ions that were generated inside the ionosphere. Titan׳s interior is considered as a weakly conducting body. Special attention has been paid to comparing the simulated pickup ion density distribution with CAPS-ELS and with RPWS LP observations by the Cassini–Huygens spacecraft along the TA trajectory. Our modeling shows an asymmetry of the ion density distribution and the magnetic field, including the formation of Alfven wing-like structures.
Published: 2014

25. Steady-state spin synchronization through the collective motion of trapped ions

Author: Justin G. Bohnet, John J. Bollinger, John F. Cooper, Athreya Shankar, and Murray Holland
Subjects: Condensed Matter::Quantum Gases, Physics, Mesoscopic physics, Sympathetic cooling, Quantum Physics, Atomic Physics (physics.atom-ph), Phonon, FOS: Physical sciences, Superradiance, Penning trap, 01 natural sciences, 3. Good health, Physics - Atomic Physics, 010309 optics, Quantum Gases (cond-mat.quant-gas), Physics::Plasma Physics, Normal mode, 0103 physical sciences, Synchronization (computer science), Physics::Atomic Physics, Atomic physics, Quantum Physics (quant-ph), 010306 general physics, Condensed Matter - Quantum Gases, Spin-½
Abstract: Ultranarrow-linewidth atoms coupled to a lossy optical cavity mode synchronize, i.e. develop correlations, and exhibit steady-state superradiance when continuously repumped. This type of system displays rich collective physics and promises metrological applications. These features inspire us to investigate if analogous spin synchronization is possible in a different platform that is one of the most robust and controllable experimental testbeds currently available: ion-trap systems. We design a system with a primary and secondary species of ions that share a common set of normal modes of vibration. In analogy to the lossy optical mode, we propose to use a lossy normal mode, obtained by sympathetic cooling with the secondary species of ions, to mediate spin synchronization in the primary species of ions. Our numerical study shows that spin-spin correlations develop, leading to a macroscopic collective spin in steady-state. We propose an experimental method based on Ramsey interferometry to detect signatures of this collective spin; we predict that correlations prolong the visibility of Ramsey fringes, and that population statistics at the end of the Ramsey sequence can be used to directly infer spin-spin correlations., 19 pages, 10 figures, includes appendices
Published: 2016

26. Biosignature hide and seek

Author: John F. Cooper
Subjects: 010504 meteorology & atmospheric sciences, Hide and seek, Astronomy and Astrophysics, 01 natural sciences, Article, Physics::Geophysics, Astrobiology, Jupiter, Physics::Space Physics, 0103 physical sciences, Biosignature, Astrophysics::Earth and Planetary Astrophysics, 010303 astronomy & astrophysics, Physics::Atmospheric and Oceanic Physics, Geology, 0105 earth and related environmental sciences
Abstract: A new model predicts locations on the surface of radiation-blasted Europa, the ocean moon of Jupiter, where biochemical signatures of life emergent from the subsurface ocean might survive long enough for detection on the moon's changing surface.
Published: 2018

27. The light (H+,H2+,He+) and heavy (Na+) pickup ion dynamics in the lunar-like plasma environment: 3D hybrid kinetic modeling

Author: Edward C. Sittler, John F. Cooper, R. E. Hartle, and A.S. Lipatov
Subjects: Physics, Atmospheric Science, Aerospace Engineering, Astronomy and Astrophysics, Photoionization, Plasma, Plasma modeling, Ion, Pickup Ion, Solar wind, Geophysics, Space and Planetary Science, Ionization, Physics::Space Physics, General Earth and Planetary Sciences, Pickup, Astrophysics::Earth and Planetary Astrophysics, Atomic physics
Abstract: In this report we discuss the self-consistent dynamics of pickup ions in the solar wind flow around the lunar-like object. In our model the solar wind and pickup ions are considered as a particles, whereas the electrons are described as a fluid. Inhomogeneous photoionization, electron-impact ionization and charge exchange are included in our model. The Moon will be chosen as a basic object for our modeling. The current modeling shows that mass loading by pickup ions H + , H 2 + , He + , and Na + may be very important in the global dynamics of the solar wind around the Moon. In our hybrid modeling we use exponential profiles for the exospheric components. The Moon is considered as a weakly conducting body. Special attention will be paid to comparing the modeling pickup ion velocity distribution with ARTEMIS observations. Our modeling shows an asymmetry of the Mach cone due to mass loading, the upstream flow density distribution and the magnetic field. The pickup ions form an asymmetrical plasma tails that may disturb the lunar plasma wake.
Published: 2013

28. The Uniqueα4(+)/(−)α4 Agonist Binding Site in (α4)3(β2)2Subtype Nicotinic Acetylcholine Receptors Permits Differential Agonist Desensitization Pharmacology versus the (α4)2(β2)3Subtype

Author: J. Brek Eaton, Jon Lindstrom, Paul Whiteaker, Linda Lucero, Harrison Stratton, Yongchang Chang, John F. Cooper, and Ronald J. Lukas
Subjects: Pharmacology, Gene isoform, Agonist, biology, medicine.drug_class, Mutant, Xenopus, biology.organism_classification, Nicotinic agonist, medicine, Molecular Medicine, Binding site, Receptor, Acetylcholine receptor
Abstract: Selected nicotinic agonists were used to activate and desensitize high-sensitivity (HS; (α4)2(β2)3) or low-sensitivity (LS; (α4)3(β2)2) isoforms of human α4β2-nicotinic acetylcholine receptors (nAChR). Function was assessed using 86Rb+ efflux in a stably-transfected SH-EP1-hα4β2 human epithelial cell line, and two-electrode voltage-clamp electrophysiology in Xenopus oocytes expressing concatenated pentameric HS or LS α4β2-nAChR constructs (HSP and LSP). Unlike previously-studied agonists, desensitization bythe highly-selective agonists A-85380 and sazetidine-A (Saz-A) preferentially reduced α4β2-nAChR HS-phase vs. LS-phase responses. The concatenated-nAChR experiments confirmed that ≈20% of LS-isoform ACh-induced function occurs in an HS-like phase, which is abolished by Saz-A preincubation. Six mutant LSP were generated, each targeting a conserved agonist-binding residue within the LS-isoform-only α4(+)/(-)α4 interface agonist binding site. Every mutation reduced the percentage of LS-phase function, demonstrating that this site underpins LS-phase function. Oocyte-surface expression of the HSP and each of the LSP constructs was statistically indistinguishable, as measured using β2-subunit-specific [125I]mAb295 labeling. However, maximum function is approximately 5x greater on a "per receptor" basis for unmodified-LSP vs. HSP α4β2-nAChR. Thus, recruitment of the α4(+)/(-)α4 site at higher agonist concentrations appears to augment otherwise-similar function mediated by the pair of α4(+)/(-)β2 sites shared by both isoforms. These studies elucidate the receptor-level differences underlying the differential pharmacology of the two α4β2-nAChR isoforms, and demonstrate that HS vs. LS α4β2-nAChR activity can be selectively manipulated using pharmacological approaches. Since α4β2 nAChR are the predominant neuronal subtype these discoveries likely have significant functional implications, and may provide important insights for drug discovery and development.
Published: 2013

29. Effects of and pickup ions on the lunar-like plasma environment: 3D hybrid modeling

Author: R. E. Hartle, John F. Cooper, Edward C. Sittler, and A.S. Lipatov
Subjects: Physics, Atmospheric Science, Aerospace Engineering, Astronomy and Astrophysics, Plasma, Electron, Plasma modeling, Ion, Solar wind, Pickup Ion, Geophysics, Physics::Plasma Physics, Space and Planetary Science, Ionization, Physics::Space Physics, General Earth and Planetary Sciences, Pickup, Astrophysics::Earth and Planetary Astrophysics, Atomic physics
Abstract: In this report we discuss the self-consistent dynamics of pickup ions in the solar wind flow around the lunar-like object. In our model the solar wind and pickup ions are considered as a particles, whereas the electrons are described as a fluid. Inhomogeneous photoionization, electron-impact ionization and charge exchange are included in our model. The Moon will be chosen as a basic object for our modeling. The current modeling shows that mass loading by pickup ions Na + and He + may be very important in the global dynamics of the solar wind around the Moon. In our hybrid modeling we use exponential profiles for the exospheric components. The Moon is considered as a weakly conducting body. Special attention will be paid to comparing the modeling pickup ion velocity distribution with ARTEMIS observations. Our modeling shows an asymmetry of the Mach cone due to mass loading, the upstream flow density distribution and the magnetic field. The pickup ions form an asymmetrical plasma tails that may disturb the lunar plasma wake.
Published: 2012

30. Analysis of the carbon anode in direct carbon conversion fuel cells

Author: John F. Cooper and J. Robert Selman
Subjects: Materials science, Renewable Energy, Sustainability and the Environment, Carbonization, Direct carbon fuel cell, Inorganic chemistry, Energy Engineering and Power Technology, Electrolyte, Condensed Matter Physics, Electrochemistry, Anode, Fuel Technology, Chemical engineering, Polarization (electrochemistry), Porosity, Faraday efficiency
Abstract: The total electrochemical efficiency of a direct carbon fuel cell with molten carbonate electrolyte is dominated by the product of coulombic efficiency (electron yield ( n ) per carbon atom, divided by 4) and voltaic efficiency (ratio of cell voltage to theoretical voltage). The voltaic efficiency is acceptably high (70–80%) for many atomically-disordered carbon materials. High coulombic efficiency is more difficult to achieve but ranges from below 50% at low current densities in porous material to 100% in certain monolithic and particulate carbon anodes at high current densities where substantially pure CO 2 is the product gas. We find evidence for two competing anode reactions associated with distinct low- and high polarization segments, respectively: (1) a charge-transfer controlled, linear–polarization reaction occurring predominately within pores, proportional to specific area, and tending toward low efficiency by co-production of CO and CO 2 ; and (2) a flow-dependent reaction occurring on the exterior surface of the anode, requiring > 100 mV polarization and tending to produce CO 2 . Based on this interpretation, high electrochemical efficiency of a carbon fuel cell is expected with anodes made of atomically disordered ("turbostratic") carbon that have negligible porosity, or with anodes of disordered carbon for which interior pores are intentionally blocked with an impervious solid material, such as an inert salt or readily carbonized pitch.
Published: 2012

31. Probing the Fundamental Physics of the Solar Corona with Lunar Solar Occultation Observations

Author: S. Rifai Habbal, Huw Morgan, Edward C. Sittler, Adrian N. Daw, A. Ding, Miloslav Druckmüller, and John F. Cooper
Subjects: Physics, Sunspot, Astronomy, Astronomy and Astrophysics, Coronal loop, Solar irradiance, Corona, Lunar limb, Solar cycle, Solar wind, Space and Planetary Science, Physics::Space Physics, Coronal mass ejection, Astrophysics::Solar and Stellar Astrophysics, Astrophysics::Earth and Planetary Astrophysics
Abstract: Imaging and spectroscopy of the solar corona, coupled with polarimetry, are the only tools available at present to capture signatures of physical processes responsible for coronal heating and solar wind acceleration within the first few solar radii above the solar limb. With the recent advent of improved detector technology and image processing techniques, broad-band white light and narrow-band multi-wavelength observations of coronal forbidden lines, made during total solar eclipses, have started to yield new views about the thermodynamic and magnetic properties of coronal structures. This paper outlines these unique capabilities, which until present, have been feasible primarily with observations during natural total solar eclipses. This work also draws attention to the exciting possibility of greatly increasing the frequency and duration of solar eclipse observations with Moon orbiting observatories utilizing lunar limb occultation of the solar disk for coronal measurements.
Published: 2012

32. (Invited) Determination of Efficiency in Direct Carbon Fuel Cells

Author: John F. Cooper and J. R. Selman
Subjects: Materials science, chemistry, Chemical engineering, Fuel cells, chemistry.chemical_element, Carbon
Abstract: Expressions for total efficiency of a carbon fuel cell reduce to a simple product of voltage efficiency (V(i)/V°) and carbon efficiency (defined as n/4, where n is the number of equivalents of charge associated with reaction of one mole of carbon). Examination of steady state polarization curves led us to propose that separate reactions predominate in two distinct regions of the curve: there is a low potential segment in which rate is proportional to total pore area, and a high potential segment where rate is a function of external flow conditions but not internal area. We make use of the Yongdan Li model for 4-electron net anodic oxidation of carbon to interpret the shift between the two segments as accompanied by shift in location of the reaction from the interior pores to the external surface of the anode, where n = 4. Total efficiency may be maximized using anodes fabricated from atomically disordered carbon by confining current to the exterior surface by means of filling the pores with inert material.
Published: 2012

33. Short wavelength electromagnetic perturbations excited near the Solar Probe Plus spacecraft in the inner heliosphere: 2.5D hybrid modeling

Author: A.S. Lipatov, Edward C. Sittler, John F. Cooper, and Richard E. Hartle
Subjects: Electromagnetic field, Physics, Whistler, Waves in plasmas, Astronomy, Astronomy and Astrophysics, Plasma, Computational physics, Solar wind, Wavelength, Physics::Plasma Physics, Space and Planetary Science, Physics::Space Physics, Ionosphere, Heliosphere
Abstract: A 2.5D numerical plasma model of the interaction of the solar wind (SW) with the Solar Probe Plus spacecraft (SPPSC) is presented. These results should be interpreted as a basic plasma model derived from the SW-interaction with the spacecraft (SC), which could have consequences for both plasma wave and electron plasma measurements on board the SC in the inner heliosphere. Compression waves and electric field jumps with amplitudes of about 1.5 V/m and (12-18) V/m were also observed. A strong polarization electric field was also observed in the wing of the plasma wake. However, 2.5D hybrid modeling did not show excitation of whistler/Alfven waves in the upstream connected with the bidirectional current closure that was observed in short-time 3D modeling SPPSC and near a tether in the ionosphere. The observed strong electromagnetic perturbations may be a crucial point in the electromagnetic measurements planned for the future Solar Probe Plus (SPP) mission. The results of modeling electromagnetic field perturbations in the SW due to shot noise in absence of SPPSC are also discussed.
Published: 2012

34. Saturn's magnetosphere interaction with Titan for T9 encounter: 3D hybrid modeling and comparison with CAPS observations

Author: David G. Simpson, Edward C. Sittler, A.S. Lipatov, R. E. Hartle, and John F. Cooper
Subjects: Physics, Magnetosphere, Astronomy and Astrophysics, Photoionization, Ion, Atmosphere, symbols.namesake, Pickup Ion, Space and Planetary Science, Ionization, symbols, Ionosphere, Atomic physics, Titan (rocket family)
Abstract: Global dynamics of ionized and neutral gases in the environment of Titan plays an important role in the interaction of Saturn s magnetosphere with Titan. Several hybrid simulations of this problem have already been done (Brecht et al., 2000; Kallio et al., 2004; Modolo et al., 2007a; Simon et al., 2007a, 2007b; Modolo and Chanteur, 2008). Observational data from CAPS for the T9 encounter (Sittler et al., 2009) indicates an absence of O(+) heavy ions in the upstream that change the models of interaction which were discussed in current publications (Kallio et al., 2004; Modolo et al., 2007a; Simon et al., 2007a, 2007b; Ma et al., 2007; Szego et al., 2007). Further analysis of the CAPS data shows very low density or even an absence of H(+) ions in upstream. In this paper we discuss two models of the interaction of Saturn s magnetosphere with Titan: (A) high density of H(+) ions in the upstream flow (0.1/cu cm), and (B) low density of H(+) ions in the upstream flow (0.02/cu cm). The hybrid model employs a fluid description for electrons and neutrals, whereas a particle approach is used for ions. We also take into account charge-exchange and photoionization processes and solve self-consistently for electric and magnetic fields. The model atmosphere includes exospheric H(+), H(2+), N(2+)and CH(4+) pickup ion production as well as an immobile background ionosphere and a shell distribution for active ionospheric ions (M(sub i)=28 amu). The hybrid model allows us to account for the realistic anisotropic ion velocity distribution that cannot be done in fluid simulations with isotropic temperatures. Our simulation shows an asymmetry of the ion density distribution and the magnetic field, including the formation of Alfven wing-like structures. The results of the ion dynamics in Titan s environment are compared with Cassini T9 encounter data (CAPS).
Published: 2012

35. Background and pickup ion velocity distribution dynamics in Titan’s plasma environment: 3D hybrid simulation and comparison with CAPS T9 observations

Author: A.S. Lipatov, Edward C. Sittler, John F. Cooper, R. E. Hartle, and David G. Simpson
Subjects: Physics, Atmospheric Science, Aerospace Engineering, Astronomy and Astrophysics, Electron, Photoionization, Plasma, Ion, Magnetic field, Pickup Ion, Geophysics, Physics::Plasma Physics, Space and Planetary Science, Ionization, Physics::Space Physics, General Earth and Planetary Sciences, Atomic physics, Electron ionization
Abstract: In this report we discuss the ion velocity distribution dynamics from the 3D hybrid simulation. In our model the background, pickup, and ionospheric ions are considered as a particles, whereas the electrons are described as a fluid. Inhomogeneous photoionization, electron-impact ionization and charge exchange are included in our model. We also take into account the collisions between the ions and neutrals. The current simulation shows that mass loading by pickup ions H(+); H2(+), CH4(+) and N2(+) is stronger than in the previous simulations when O+ ions are introduced into the background plasma. In our hybrid simulations we use Chamberlain profiles for the atmospheric components. We also include a simple ionosphere model with average mass M = 28 amu ions that were generated inside the ionosphere. The moon is considered as a weakly conducting body. Special attention will be paid to comparing the simulated pickup ion velocity distribution with CAPS T9 observations. Our simulation shows an asymmetry of the ion density distribution and the magnetic field, including the formation of the Alfve n wing-like structures. The simulation also shows that the ring-like velocity distribution for pickup ions relaxes to a Maxwellian core and a shell-like halo.
Published: 2011

36. Jovian plasma torus interaction with Europa: 3D hybrid kinetic simulation. First results

Author: Edward C. Sittler, A.S. Lipatov, R. E. Hartle, John F. Cooper, William R. Paterson, and David G. Simpson
Subjects: Physics, education.field_of_study, Energetic neutral atom, Population, Astronomy and Astrophysics, Photoionization, Plasma, Magnetic field, Physics::Plasma Physics, Space and Planetary Science, Ionization, Physics::Space Physics, Astrophysics::Earth and Planetary Astrophysics, Atomic physics, Magnetohydrodynamics, education, Magnetic dipole
Abstract: The hybrid kinetic model supports comprehensive simulation of the interaction between different spatial and energetic elements of the Europa-moon-magnetosphere system with respect to variable upstream magnetic field and flux or density distributions of plasma and energetic ions, electrons, and neutral atoms. This capability is critical for improving the interpretation of the existing Europa flyby measurements from the Galileo orbiter mission, and for planning flyby and orbital measurements, (including the surface and atmospheric compositions) for future missions. The simulations are based on recent models of the atmosphere of Europa (Cassidy etal.,2007;Shematovichetal.,2005). In contrast to previous approaches with MHD simulations, the hybrid model allows us to fully take into account the finite gyro radius effect and electron pressure, and to correctly estimate the ion velocity distribution and the fluxes along the magnetic field (assuming an initial Maxwellian velocity distribution for upstream background ions).Non-thermal distributions of upstream plasma will be addressed in future work. Photoionization,electron-impact ionization, charge exchange and collisions between the ions and neutrals are also included in our model. We consider two models for background plasma:(a) with O(++) ions; (b) with O(++) and S(++) ions. The majority of O2 atmosphere is thermal with an extended cold population (Cassidyetal.,2007). A few first simulations already include an induced magnetic dipole; however, several important effects of induced magnetic fields arising from oceanic shell conductivity will be addressed in later work.
Published: 2010

37. Saturn's magnetospheric interaction with Titan as defined by Cassini encounters T9 and T18: New results

Author: E. C. Sittler, Andrew J. Coates, John F. Cooper, Karoly Szego, Cesar Bertucci, A. S. Lipatov, Jan-Erik Wahlund, Richard E. Hartle, M. Shappirio, David G. Simpson, and Robert E. Johnson
Subjects: Physics, Field line, Ciencias Físicas, Magnetosphere, Astronomy and Astrophysics, Geophysics, Astrophysics, Astronomía, symbols.namesake, Space and Planetary Science, Magnetic fields, Ionization, Physics::Space Physics, symbols, Magnetodisc Plasma, Magnetopause, Astrophysics::Earth and Planetary Astrophysics, Ionosphere, Atmosphere of Titan, Titan, Titan (rocket family), Saturns magnetosphere, CIENCIAS NATURALES Y EXACTAS, Exosphere
Abstract: We present new results of Cassini’s T9 flyby with complementary observations from T18. Based on Cassini plasma spectrometer (CAPS) and Cassini magnetometer (MAG), compositional evidence shows the upstream flow for both T9 and T18 appears composed of light ions (H+ and H2 +), with external pressures 30 times lower than that for the earlier TA flyby where heavy ions dominated the magnetospheric plasma. When describing the plasma heating and sputtering of Titan’s atmosphere, T9 and T18 can be considered interactions of low magnetospheric energy input. On the other hand, T5, when heavy ion fluxes are observed to be higher than typical (i.e., TA), represents the limiting case of high magnetospheric energy input to Titan’s upper atmosphere. Anisotropy estimates of the upstream flow are 1oT?/T:o3 and the flow is perpendicular to B, indicative of local picked up ions from Titan’s H and H2 coronae extending to Titan’s Hill sphere radius. Beyond this distance the corona forms a neutral torus that surrounds Saturn. The T9 flyby unexpectedly resulted in observation of two ‘‘wake’’ crossings referred to as Events 1 and 2. Event 2 was evidently caused by draped magnetosphere field lines, which are scavenging pickup ions from Titan’s induced magnetopause boundary with outward flux 2 106 ions/cm2 /s. The composition of this out flow is dominated by H2 + and H+ ions. Ionospheric flow away from Titan with ion flux 7 106 ion/cm2 /s is observed for Event 1. In between Events 1 and 2 are high energy field aligned flows of magnetosphere protons that may have been accelerated by the convective electric field across Titan’s topside ionosphere. T18 observations are much closer to Titan than T9, allowing one to probe this type of interaction down to altitudes 950 km. Comparisons with previously reported hybrid simulations are made. Fil: Sittler Jr., E. C.. National Aeronautics And Space Administration. Goddart Institute For Space Studies; Estados Unidos Fil: Hartle, R. E.. National Aeronautics And Space Administration. Goddart Institute For Space Studies; Estados Unidos Fil: Johnson, R. E.. University of Virginia; Estados Unidos Fil: Cooper, J. F.. National Aeronautics And Space Administration. Goddart Institute For Space Studies; Estados Unidos Fil: Lipatov, A. S.. National Aeronautics And Space Administration. Goddart Institute For Space Studies; Estados Unidos. University of Maryland; Estados Unidos Fil: Bertucci, Cesar. Consejo Nacional de Investigaciónes Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Astronomía y Física del Espacio. - Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Astronomía y Física del Espacio; Argentina Fil: Coates, A. J.. University College London; Estados Unidos Fil: Szego, K.. Research Institute for Particle and Nuclear Physics; Hungría Fil: Shappirio, M.. National Aeronautics And Space Administration. Goddart Institute For Space Studies; Estados Unidos Fil: Simpson, D. G.. National Aeronautics And Space Administration. Goddart Institute For Space Studies; Estados Unidos Fil: Wahlund, J. E.. Swedish Institute of Space Physic; Suecia
Published: 2010

38. Old Faithful model for radiolytic gas-driven cryovolcanism at Enceladus

Author: Steven J. Sturner, John F. Cooper, Edward C. Sittler, Paul D. Cooper, and Abigail Rymer
Subjects: Jupiter, Outgassing, Space and Planetary Science, Environmental science, Astronomy and Astrophysics, Blanketing, Ejecta, Icy moon, Enceladus, Regolith, Plume, Astrobiology
Abstract: A new model is presented on how chemically driven cryovolcanism might contribute to episodic outgassing at the icy moon Enceladus and potentially elsewhere including Europa and Kuiper Belt Objects. Exposed water ices can become oxidized from radiolytic chemical alteration of near-surface water ice by space environment irradiation. In contact with primordially abundant reductants such as NH3, CH4, and other hydrocarbons, the product oxidants can react exothermically to produce volatile gases driving cryovolcanism via gas-piston forces on any subsurface liquid reservoirs. Radiolytic oxidants such as H2O2 and O2 can continuously accumulate deep in icy regoliths and be conveyed by rheological flows to subsurface chemical reaction zones over million-year time scales indicated by cratering ages for active regions of Enceladus and Europa. Surface blanketing with cryovolcanic plume ejecta would further accelerate regolith burial of radiolytic oxidants. Episodic heating from transient gravitational tides, radioisotope decay, impacts, or other geologic events might occasionally accelerate chemical reaction rates and ignite the exothermic release of cumulative radiolytic oxidant energy. The time history for the suggested "Old Faithful" model of radiolytic gas-driven cryovolcanism at Enceladus and elsewhere therefore consists of long periods of chemical energy accumulation punctuated by much briefer episodes of cryovolcanic activity. The most probable sequence for detection of activity in the current epoch is a long evolutionary phase of slow but continuous oxidant accumulation over billions of years followed by continuous but variable high activity over the past 10(exp 7)-10(exp 8) years. Detectable cryovolcanic activity could then later decline due to near-total oxidation of the rheologically accessible ice crust and depletion the accessible reductant abundances, as may have already occurred for Europa in the more intense radiation environment of Jupiter's magnetosphere. Astrobiological potential of Enceladus could correspondingly be higher than at Europa due to a less extreme state of oxidation and greater residual abundance of organics.
Published: 2009

39. Heavy ion formation in Titan's ionosphere: Magnetospheric introduction of free oxygen and a source of Titan's aerosols?

Author: John F. Cooper, Richard E. Hartle, D. T. Young, Robert E. Johnson, Andrew J. Coates, Edward C. Sittler, and Ashraf Ali
Subjects: Materials science, Astronomy and Astrophysics, Cosmic ray, Methane, Ion, Astrobiology, symbols.namesake, chemistry.chemical_compound, Solar wind, chemistry, Space and Planetary Science, Physics::Space Physics, symbols, Astrophysics::Earth and Planetary Astrophysics, Atmosphere of Titan, Titan (rocket family), Energy source, Enceladus, Physics::Atmospheric and Oceanic Physics
Abstract: Discovery by Cassini's plasma instrument of heavy positive and negative ions within Titan's upper atmosphere and ionosphere has advanced our understanding of ion neutral chemistry within Titan's upper atmosphere, primarily composed of molecular nitrogen, with approx.2.5% methane. The external energy flux transforms Titan's upper atmosphere and ionosphere into a medium rich in complex hydrocarbons, nitriles and haze particles extending from the surface to 1200 km altitudes. The energy sources are solar UV, solar X-rays, Saturn's magnetospheric ions and electrons, solar wind and shocked magnetosheath ions and electrons, galactic cosmic rays (CCR) and the ablation of incident meteoritic dust from Enceladus' E-ring and interplanetary medium. Here it is proposed that the heavy atmospheric ions detected in situ by Cassini for heights >950 km, are the likely seed particles for aerosols detected by the Huygens probe for altitudes
Published: 2009

40. Electrochemical Oxidation of Carbon for Electric Power Generation: A Review

Author: John F. Cooper and Robert Selman
Subjects: Boudouard reaction, Materials science, Electricity generation, Chemical engineering, Standard electrode potential, Molten carbonate fuel cell, Forensic engineering, Electrolyte, Electrochemistry, Polarization (electrochemistry), Anode
Abstract: Published research is reviewed for purposes of establishing baseline performance expectations for the direct conversion of carbon in a molten carbonate fuel cell. Examination of data from several sources supports the possibility of direct carbon conversion at a total efficiency of 80% (HHV) and peak power of at least 0.11 W/cm2 using atomically disordered carbon materials derived from fossil or biological sources The net anode reaction results in CO2 product at 0.1-0.2 V polarization, while parasitic corrosion of carbon by the reverse Boudouard reaction may be significant in parts of the carbon bed remote from the current collector. Also important are an understanding of the mechanism and extent of carbon wetting by the electrolyte. A cell configuration allowing simultaneous measurement of electrode potentials and off-gas composition is suggested for use in producing the data necessary for scale-up
Published: 2009

41. TandEM: Titan and Enceladus mission

Author: J. E. Blamont, Tobias Owen, Michael Küppers, Xenophon Moussas, Robert H. Brown, Nicole Schmitz, Sascha Kempf, C. Menor Salvan, T. W. Haltigin, Olivier Grasset, Roger V. Yelle, Wayne H. Pollard, Daniel Gautier, Paul R. Mahaffy, Joe Pitman, Iannis Dandouras, Daphne Stam, John C. Zarnecki, Bruno Sicardy, Georges Durry, Jesús Martínez-Frías, Norbert Krupp, S. Le Mouélic, Matthias Grott, Sébastien Lebonnois, T. Krimigis, Elizabeth P. Turtle, Alain Herique, Linda Spilker, Ralph D. Lorenz, Maria Teresa Capria, M. Combes, John F. Cooper, O. Mousis, Joachim Saur, Wlodek Kofman, J. Bouman, M. Paetzold, Hojatollah Vali, C. Dunford, Sushil K. Atreya, Eric Chassefière, I. de Pater, T. B. McCord, Bruno Bézard, Gabriel Tobie, Catherine D. Neish, M. Ruiz Bermejo, Sergei Pogrebenko, Kim Reh, Athena Coustenis, Ralf Jaumann, Angioletta Coradini, Leonid I. Gurvits, Andrew J. Coates, Tibor S. Balint, H. Hussmann, E. Choi, Ioannis A. Daglis, Edward C. Sittler, Emmanuel Lellouch, Robert A. West, L. Boireau, E.F. Young, Timothy A. Livengood, Cesar Bertucci, Martin G. Tomasko, M. Fujimoto, Ingo Müller-Wodarg, Yves Bénilan, Wing-Huen Ip, Marina Galand, Darrell F. Strobel, Cyril Szopa, Pascal Rannou, D. G. Mitchell, Mark Leese, Véronique Vuitton, P. Annan, Tetsuya Tokano, Caitlin A. Griffith, Conor A. Nixon, Stephen A. Ledvina, Karoly Szego, Andrew Morse, Panayotis Lavvas, Luisa Lara, C. de Bergh, Jonathan I. Lunine, R. A. Gowen, Katrin Stephan, Jianping Li, Glenn S. Orton, Michel Blanc, Esa Kallio, Ronan Modolo, M. Hirtzig, Helmut Lammer, Nicholas Achilleos, D. Nna Mvondo, Frank Sohl, M. Nakamura, Andrew Steele, C. C. Porco, Marcello Fulchignoni, Gordon L. Bjoraker, Olga Prieto-Ballesteros, J. J. López-Moreno, Andrew Dominic Fortes, Rafael Rodrigo, Patrice Coll, Francesca Ferri, François Raulin, Tom Spilker, F. J. Crary, J. H. Waite, Dirk Schulze-Makuch, Thomas E. Cravens, Kevin H. Baines, C. P. McKay, L. Richter, D. Luz, David H. Atkinson, Martin Knapmeyer, Robert E. Johnson, D. Fairbrother, F. M. Flasar, Roland Thissen, Paul N. Romani, Sebastien Rodriguez, Urs Mall, Paul M. Schenk, Franck Hersant, R. Koop, Odile Dutuit, I. Vardavas, T. Kostiuk, Ricardo Amils, Konrad Schwingenschuh, Robert V. Frampton, Fritz M. Neubauer, Jan-Erik Wahlund, L. A. Soderblom, Michele K. Dougherty, Anna Milillo, Frank T. Robb, Bernard Schmitt, Christophe Sotin, Michel Cabane, A. Selig, Bernard Marty, Yves Langevin, Rosaly M. C. Lopes, Emmanuel T. Sarris, E. De Angelis, D. Toublanc, Laboratoire d'études spatiales et d'instrumentation en astrophysique (LESIA), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS), Department of Atmospheric, Oceanic, and Space Sciences [Ann Arbor] (AOSS), University of Michigan [Ann Arbor], University of Michigan System-University of Michigan System, Jet Propulsion Laboratory (JPL), NASA-California Institute of Technology (CALTECH), Lunar and Planetary Laboratory [Tucson] (LPL), University of Arizona, Space and Atmospheric Physics Group [London], Blackett Laboratory, Imperial College London-Imperial College London, Centro di Ateneo di Studi e Attività Spaziali 'Giuseppe Colombo' (CISAS), Università degli Studi di Padova = University of Padua (Unipd), Mullard Space Science Laboratory (MSSL), University College of London [London] (UCL), Joint Institute for VLBI in Europe (JIVE ERIC), Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institut d'astrophysique spatiale (IAS), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), The Open University [Milton Keynes] (OU), NASA Ames Research Center (ARC), Department of Physics [Athens], National and Kapodistrian University of Athens (NKUA), University of Cologne, Institute for Astronomy [Honolulu], University of Hawai‘i [Mānoa] (UHM), Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA (UMR_7583)), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS), NASA Goddard Space Flight Center (GSFC), Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Johns Hopkins University Applied Physics Laboratory [Laurel, MD] (APL), Swedish Institute of Space Physics [Uppsala] (IRF), Space Science Division [San Antonio], Southwest Research Institute [San Antonio] (SwRI), Centre National d'Études Spatiales [Toulouse] (CNES), Centre d'étude spatiale des rayonnements (CESR), Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Academy of Athens, Observatoire de Paris - Site de Paris (OP), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS), Space Science Institute [Boulder] (SSI), Bombardier Aerospace, Centro de Astrobiologia [Madrid] (CAB), Instituto Nacional de Técnica Aeroespacial (INTA)-Consejo Superior de Investigaciones Científicas [Madrid] (CSIC), Sensors and Software, University of Idaho [Moscow, USA], SRON Netherlands Institute for Space Research (SRON), PLANETO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Istituto Nazionale di Astrofisica (INAF), University of Kansas [Lawrence] (KU), National Observatory of Athens (NOA), Department of Astronomy [Berkeley], University of California [Berkeley] (UC Berkeley), University of California (UC)-University of California (UC), Service d'aéronomie (SA), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Planétologie de Grenoble (LPG), Université Joseph Fourier - Grenoble 1 (UJF)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Institute of Space and Astronautical Science (ISAS), Japan Aerospace Exploration Agency [Sagamihara] (JAXA), McGill University = Université McGill [Montréal, Canada], FORMATION STELLAIRE 2009, Laboratoire d'astrodynamique, d'astrophysique et d'aéronomie de bordeaux (L3AB), Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Observatoire aquitain des sciences de l'univers (OASU), Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)-Laboratoire d'Astrophysique de Bordeaux [Pessac] (LAB), Université de Bordeaux (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Bordeaux (UB), Institute of Astronomy [Taiwan] (IANCU), National Central University [Taiwan] (NCU), University of Virginia [Charlottesville], Finnish Meteorological Institute (FMI), Max-Planck-Institut für Sonnensystemforschung (MPS), Max-Planck-Gesellschaft, DLR Institut für Planetenforschung, Deutsches Zentrum für Luft- und Raumfahrt [Berlin] (DLR), Space Research Institute of Austrian Academy of Sciences (IWF), Austrian Academy of Sciences (OeAW), Instituto de Astrofísica de Andalucía (IAA), Consejo Superior de Investigaciones Científicas [Madrid] (CSIC), Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL), Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics [Beijing] (IAP), Chinese Academy of Sciences [Beijing] (CAS)-Chinese Academy of Sciences [Beijing] (CAS), National Center for Earth and Space Science Education (NCESSE), Observatório Astronómico de Lisboa, Centre de Recherches Pétrographiques et Géochimiques (CRPG), Institut national des sciences de l'Univers (INSU - CNRS)-Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS), Bear Fight Center, Univers, Transport, Interfaces, Nanostructures, Atmosphère et environnement, Molécules (UMR 6213) (UTINAM), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC), Université Bourgogne Franche-Comté [COMUE] (UBFC)-Université Bourgogne Franche-Comté [COMUE] (UBFC), Lockheed Martin Space, Groupe de spectrométrie moléculaire et atmosphérique (GSMA), Université de Reims Champagne-Ardenne (URCA)-Centre National de la Recherche Scientifique (CNRS), University of Maryland Biotechnology Institute Baltimore, University of Maryland [Baltimore], Astrophysique Interprétation Modélisation (AIM (UMR_7158 / UMR_E_9005 / UM_112)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Democritus University of Thrace (DUTH), Lunar and Planetary Institute [Houston] (LPI), School of Earth and Environmental Sciences [Pullman], Washington State University (WSU), Centre National de la Recherche Scientifique (CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Observatoire de Paris, PSL Research University (PSL)-PSL Research University (PSL)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC), Universita degli Studi di Padova, National and Kapodistrian University of Athens = University of Athens (NKUA | UoA), Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Planétologie et Géodynamique UMR6112 (LPG), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Nantes - Faculté des Sciences et des Techniques, Université de Nantes (UN)-Université de Nantes (UN)-Université d'Angers (UA), Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS), Centre National de la Recherche Scientifique (CNRS)-Observatoire de Paris, PSL Research University (PSL)-PSL Research University (PSL)-Institut national des sciences de l'Univers (INSU - CNRS), Instituto Nacional de Técnica Aeroespacial (INTA)-Consejo Superior de Investigaciones Científicas [Spain] (CSIC), IMPEC - LATMOS, University of California [Berkeley], University of California-University of California, Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), McGill University, École normale supérieure - Paris (ENS Paris)-École normale supérieure - Paris (ENS Paris), Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS), Université de Franche-Comté (UFC)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National d’Études Spatiales [Paris] (CNES), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Observatoire aquitain des sciences de l'univers (OASU), Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)-Laboratoire d'Astrophysique de Bordeaux [Pessac] (LAB), University of Virginia, Max-Planck-Institut für Sonnensystemforschung = Max Planck Institute for Solar System Research (MPS), Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Institut national des sciences de l'Univers (INSU - CNRS), Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École des Ponts ParisTech (ENPC)-École polytechnique (X)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC), Université de Franche-Comté (UFC), Université Bourgogne Franche-Comté [COMUE] (UBFC)-Université Bourgogne Franche-Comté [COMUE] (UBFC)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS), and Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Paris (UP)
Subjects: Exploration of Saturn, Solar System, Cosmic Vision, 010504 meteorology & atmospheric sciences, [PHYS.ASTR.EP]Physics [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP], Computer science, [SDU.ASTR.EP]Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP], TandEM, 01 natural sciences, law.invention, Astrobiology, Enceladus, Orbiter, symbols.namesake, law, Saturnian system, 0103 physical sciences, 010303 astronomy & astrophysics, 0105 earth and related environmental sciences, Spacecraft, Tandem, business.industry, Astronomy and Astrophysics, Landing probes, Space and Planetary Science, symbols, Titan, business, Titan (rocket family)
Abstract: 著者人数：156名, Accepted: 2008-05-27, 資料番号: SA1000998000
Published: 2009

42. Sources and losses of energetic protons in Saturn's magnetosphere

Author: Elias Roussos, Chris Paranicas, D. G. Mitchell, Thomas P. Armstrong, Robert E. Johnson, Norbert Krupp, Stamatios M. Krimigis, John F. Cooper, Geraint H. Jones, and D. C. Hamilton
Subjects: Physics, Range (particle radiation), Proton, Solar energetic particles, Energetic neutral atom, Astrophysics::High Energy Astrophysical Phenomena, Magnetosphere, Astronomy and Astrophysics, Cosmic ray, Ion, Nuclear physics, Space and Planetary Science, Saturn, Astrophysics::Earth and Planetary Astrophysics, Atomic physics, Nuclear Experiment
Abstract: We present Cassini data revealing that protons between a few keV and about 100 keV energy are not stably trapped in Saturn's inner magnetosphere. Instead these ions are present only for relatively short times following injections. Injected protons are lost principally because the neutral gas cloud converts these particles to energetic neutral atoms via charge exchange. At higher energies, in the MeV to GeV range, protons are stably trapped between the orbits of the principal moons because the proton cross-section for charge exchange is very small at such energies. These protons likely result from cosmic ray albedo neutron decay (CRAND) and are lost principally to interactions with satellite surfaces and ring particles during magnetospheric radial diffusion. A main result of this work is to show that the dominant energetic proton loss and source processes are a function of proton energy. Surface sputtering by keV ions is revisited based on the reduced ion intensities observed. Relatively speaking, MeV ion and electron weathering is most important closer to Saturn, e.g. at Janus and Mimas, whereas keV ion weathering is most important farther out, at Dione and Rhea.
Published: 2008

43. The spatial morphology of Europa's near-surface O2 atmosphere

Author: T. A. Cassidy, M. C. Wong, Melissa A. McGrath, Robert E. Johnson, and John F. Cooper
Subjects: Surface (mathematics), Solar System, Airglow, Astronomy, Astronomy and Astrophysics, Astrophysics::Cosmology and Extragalactic Astrophysics, medicine.disease_cause, Regolith, Physics::Geophysics, Atmosphere, Space and Planetary Science, Electron excitation, Physics::Space Physics, medicine, Astrophysics::Solar and Stellar Astrophysics, Astrophysics::Earth and Planetary Astrophysics, Geology, Ultraviolet, Excitation
Abstract: Results from a three-dimensional ballistic model of Europa’s O2 atmosphere are presented. Hubble Space Telescope (HST) ultraviolet observations show spatially non-uniform O2 airglow from Europa. One explanation for this is that the O2 atmosphere is spatially non-uniform. We show that non-uniform ejection of O2 alone cannot reproduce the required morphology, but that a non-uniform distribution of reactive species in Europa’s porous regolith can result in a non-uniform O2 atmosphere. By allowing O2 molecules to react with Europa’s visibly dark surface material, we produced a spatially non-uniform atmosphere which, assuming uniform electron excitation of O2 over the trailing hemisphere, compares favorably with the morphology suggested by the HST observations. This model, which requires a larger source of O2 than has previously been estimated, can in principal be tested by the New Horizons observations of Europa’s O2 atmosphere.
Published: 2007

44. Clathrate Hydrates of Oxidants in the Ice Shell of Europa

Author: Christopher F. Chyba, Kevin P. Hand, Robert W. Carlson, and John F. Cooper
Subjects: Carbon dioxide clathrate, Impact gardening, Ice, Clathrate hydrate, Water, Oxidants, medicine.disease_cause, Agricultural and Biological Sciences (miscellaneous), Ion, Astrobiology, chemistry.chemical_compound, chemistry, Space and Planetary Science, Jupiter, Carbon dioxide, medicine, Ultraviolet, Sulfur dioxide, Hydrosphere
Abstract: Europa's icy surface is radiolytically modified by high-energy electrons and ions, and photolytically modified by solar ultraviolet photons. Observations from the Galileo Near Infrared Mapping Spectrometer, ground-based telescopes, the International Ultraviolet Explorer, and the Hubble Space Telescope, along with laboratory experiment results, indicate that the production of oxidants, such as H2O2, O2, CO2, and SO2, is a consequence of the surface radiolytic chemistry. Once created, some of the products may be entrained deeper into the ice shell through impact gardening or other resurfacing processes. The temperature and pressure environments of regions within the europan hydrosphere are expected to permit the formation of mixed clathrate compounds. The formation of carbon dioxide and sulfur dioxide clathrates has been examined in some detail. Here we add to this analysis by considering oxidants produced radiolytically on the surface of Europa. Our results indicate that the bulk ice shell could have a approximately 1.7-7.6% by number contamination of oxidants resulting from radiolysis at the surface. Oxidant-hosting clathrates would consequently make up approximately 12-53% of the ice shell by number relative to ice, if oxidants were entrained throughout. We examine, in brief, the consequences of such contamination on bulk ice shell thickness and find that clathrate formation could lead to substantially thinner ice shells on Europa than otherwise expected. Finally, we propose that double occupancy of clathrate cages by O2 molecules could serve as an explanation for the observation of condensed-phase O2 on Europa. Clathrate-sealed, gas-filled bubbles in the near surface ice could also provide an effective trapping mechanism, though they cannot explain the 5771 A (O2)2 absorption.
Published: 2006

45. Production, ionization and redistribution of O2 in Saturn's ring atmosphere

Author: D. T. Young, John F. Cooper, Edward C. Sittler, F. J. Crary, T. W. Hill, M. Bouhram, Janet G. Luhmann, Robert E. Johnson, J. J. Berthelier, Howard Smith, R. L. Tokar, M. Liu, and M. Michael
Subjects: Materials science, Mathematics::Commutative Algebra, Hydrogen, Scattering, chemistry.chemical_element, Magnetosphere, Astronomy and Astrophysics, Scale height, Oxygen, Toroidal ring model, Ion, chemistry, Space and Planetary Science, Ionization, Atomic physics
Abstract: Molecular oxygen produced by the decomposition of icy surfaces is ubiquitous in Saturn's magnetosphere. A model is described for the toroidal O2 atmosphere indicated by the detection of O 2 + and O+ over the main rings. The O2 ring atmosphere is produced primarily by UV photon-induced decomposition of ice on the sunlit side of the ring. Because O2 has a long lifetime and interacts frequently with the ring particles, equivalent columns of O2 exist above and below the ring plane with the scale height determined by the local ring temperature. Energetic particles also decompose ice, but estimates of their contribution over the main rings appear to be very low. In steady state, the O2 column density over the rings also depends on the relative efficiency of hydrogen to oxygen loss from the ring/atmosphere system with oxygen being recycled on the grain surfaces. Unlike the neutral density, the ion densities can differ on the sunlit and shaded sides due to differences in the ionization rate, the quenching of ions by the interaction with the ring particles, and the northward shift of the magnetic equator relative to the ring plane. Although O+ is produced with a significant excess energy, O 2 + is not. Therefore, O 2 + should mirror well below those altitudes at which ions were detected. However, scattering by ion–molecule collisions results in much larger mirror altitudes, in ion temperatures that go through a minimum over the B-ring, and in the redistribution of both molecular hydrogen and oxygen throughout the magnetosphere. The proposed model is used to describe the measured oxygen ion densities in Saturn's toroidal ring atmosphere and its hydrogen content. The oxygen ion densities over the B-ring appear to require either significant levels of UV light scattering or ion transmission through the ring plane.
Published: 2006

46. Immunolabeling demonstrates the interdependence of mouse brain α4 and β2 nicotinic acetylcholine receptor subunit expression

Author: Robert Brown, Allan C. Collins, Jon Lindstrom, Tristan D. McClure-Begley, Paul Whiteaker, Outi Salminen, Michael J. Marks, and John F. Cooper
Subjects: Male, Interpeduncular nucleus, Protein subunit, Mutant, In situ hybridization, Receptors, Nicotinic, Biology, Synaptic Transmission, Iodine Radioisotopes, Mice, Radioligand Assay, Immunolabeling, Antibody Specificity, Animals, Receptor, Brain Chemistry, Mice, Knockout, Messenger RNA, General Neuroscience, Antibodies, Monoclonal, Brain, Immunohistochemistry, Molecular biology, Acetylcholine, Mice, Inbred C57BL, Protein Subunits, Nicotinic acetylcholine receptor, Mutation, Autoradiography, Female, sense organs
Abstract: Immunolabeling of beta2 and alpha4 subunits was quantitated in brain sections (14 mum) using [(125)I]mAb 270 and [(125)I]mAb 299, respectively. Specificity was demonstrated by signal loss in beta2(-/-) and alpha4(-/-) brain sections, respectively. Even mild paraformaldehyde fixation severely affected immunolabeling, so this study used unfixed sections. Immunolabeling autoradiography was used to map and quantitate the effects of beta2 and alpha4 subunit-null mutations on their putative partner subunits' protein expression. [(125)I]mAb 299 labeling was nearly eliminated in beta2(-/-) sections, although dorsal interpeduncular nucleus (IPN) retained a faint signal. Therefore, alpha4 subunit expression is almost universally beta2-dependent. In contrast, alpha4-null mutation effects on [(125)I]mAb 270 immunolabeling varied widely among brain regions. In corticothalamic regions, [(125)I]mAb 270 labeling was eliminated. However, in habenulopeduncular regions, alpha4 genotype had no effect. Other (predominantly dopaminergic and optic tract) nuclei also retained reduced [(125)I]mAb 270 labeling in alpha4(-/-) sections. Thus, although most beta2 subunit protein expression is alpha4-dependent, this dependence is not universal. Presumably, residual beta2 subunits are found in non-alpha4* subtypes. Together, these results show that immunolabeling is applicable to reliable, quantitative investigations of neuronal nAChRs, and that subunit-null mutants can be appropriate controls for such experiments. In situ mRNA hybridization was also performed to determine if altered mRNA transcription mediated the interdependence of alpha4 and beta2 subunit expression. alpha4-Null mutation did not affect beta2 mRNA expression, nor did beta2 genotype affect alpha4 mRNA expression. Consequently, it seems that the two subunits' effects on each other's expression are mediated at the protein, rather than gene expression level.
Published: 2006

47. X-ray probes of magnetospheric interactions with Jupiter's auroral zones, the Galilean satellites, and the Io plasma torus

Author: Douglas A. Swartz, Robert E. Johnson, J. H. Waite, John F. Cooper, Brian D. Ramsey, Pavel Rehak, and R. F. Elsner
Subjects: Physics, Solar System, Astrophysics::High Energy Astrophysical Phenomena, Astronomy, Astronomy and Astrophysics, Astrophysics, Icy moon, Jovian, Galilean moons, symbols.namesake, Gas torus, Exploration of Jupiter, Space and Planetary Science, Planet, Physics::Space Physics, symbols, Astrophysics::Earth and Planetary Astrophysics, Emission spectrum
Abstract: Remote observations with the Chandra X-ray Observatory and the XMM-Newton Observatory have shown that the Jovian system is a source of x-rays with a rich and complicated structure. The planet's polar auroral zones and its disk are powerful sources of x-ray emission. Chandra observations revealed x-ray emission from the Io Plasma Torus and from the Galilean moons Io, Europa, and possibly Ganymede. The emission from these moons is certainly due to bombardment of their surfaces of highly energetic protons, oxygen and sulfur ions from the region near the Torus exciting atoms in their surfaces and leading to fluorescent x-ray emission lines. Although the x-ray emission from the Galilean moons is faint when observed fiom Earth orbit, an imaging x-ray spectrometer in orbit around these moons, operating at 200 eV and above with 150 eV energy resolution, would provide a detailed mapping (down to 40 m spatial resolution) of the elemental composition in their surfaces. Here we describe the physical processes leading to x-ray emission fiom the surfaces of Jupiter's moons and the instrumental properties, as well as energetic ion flux models or measurements, required to map the elemental composition of their surfaces. We discuss the proposed scenarios leading to possible surface compositions. For Europa, the two most extreme are (1) a patina produced by exogenic processes such as meteoroid bombardment and ion implantation, and (2) upwelling of material fiom the subsurface ocean. We also describe the characteristics of X - m , an imaging x-ray spectrometer under going a feasibility study for the JIM0 mission, with the ultimate goal of providing unprecedented x-ray studies of the elemental composition of the surfaces of Jupiter's icy moons and Io, as well as of Jupiter's auroral x-ray emission.
Published: 2005

48. Surface-bounded atmosphere of Europa

Author: Valery I. Shematovich, John F. Cooper, M. C. Wong, and Robert E. Johnson
Subjects: Materials science, Hydrogen, chemistry.chemical_element, Astronomy and Astrophysics, Plasma, Oxygen, Charged particle, Dissociation (chemistry), chemistry, Space and Planetary Science, Sputtering, Ionization, Physics::Space Physics, Astrophysics::Earth and Planetary Astrophysics, Physics::Chemical Physics, Atomic physics, Physics::Atmospheric and Oceanic Physics, Electron ionization
Abstract: A 1-D collisional Monte Carlo model of Europa’s atmosphere is described in which the sublimation and sputtering sources of H2O molecules and their molecular fragments are accounted for as well as the radiolytically produced O2. Dissociation and ionization of H2 Oa nd O2 by magnetospheric electron, solar UV-photon and photo-electron impact, and collisional ejection from the atmosphere by the low-energy plasma are taken into account. Reactions with the surface are discussed, but only adsorption and atomic oxygen recombination are included in this model. The size of the surface-bounded oxygen atmosphere of Europa is primarily determined by a balance between atmospheric sources from irradiation of the satellite’s icy surface by the high-energy magnetospheric charged particles and atmospheric losses from collisional ejection by the low-energy plasma, photo- and electron-impact dissociation, and ionization and pick-up from the surface-bounded atmosphere. A range of sources rates for O2 to H2O are used with a larger oxygen-to-water ratio than suggested by laboratory measurements in order to account for differences in adsorption onto grains in the regolith. These calculations show that the atmospheric composition is determined by both the water and oxygen photochemistry in the near-surface region, escape of suprathermal oxygen and water into the jovian system, and the exchange of radiolytic water products with the porous regolith. For the electron impact ionization rates used, pick-up ionization is the dominant oxygen loss process, whereas photo-dissociation and atmospheric sputtering are the dominant sources of neutral oxygen for Europa’s neutral torus. Including desorption and loss of water enhances the supply of oxygen species to the neutral torus, but hydrogen produced by radiolysis is the dominant source of neutrals for Europa’s torus in these models.
Published: 2005

49. Ion irradiation of TNOs: from the fluxes measured in space to the laboratory experiments

Author: Robert E. Johnson, Giovanni Strazzulla, E. R. Christian, and John F. Cooper
Subjects: Planetesimal, Solar System, COSMIC cancer database, Materials science, business.industry, General Engineering, Energy Engineering and Power Technology, Astrophysics, Radiation, Ion, Optics, Irradiation, Trans-Neptunian object, business, Refractory (planetary science)
Abstract: Cosmic ion irradiation is believed to be one of the processes driving the evolution of the surface materials on TNOs. We review the laboratory simulations of radiation effects induced in likely TNO materials. In particular the production of new molecular species, the formation of refractory organics, and the spectral changes induced in icy targets and in natural bitumens are described. In order to establish if the effects seen in the laboratory are in fact responsible for the surface properties of the TNOs, the present knowledge of the ion fluxes is reviewed. For objects at selected solar distances, dosage time is given versus depth into the material. As suggested by recent experiments, the contribution of the electronic energy loss and that due to knock-on collisions are given separately. The relevance of ion-irradiation for the physico-chemical properties of TNOs is demonstrated, and the need for future investigations is outlined. To cite this article: G. Strazzulla et al., C. R. Physique 4 (2003).
Published: 2003

50. The science case for an orbital mission to Uranus: Exploring the origins and evolution of ice giant planets

Author: Roberto Peron, Jonathan J. Fortney, Denis Grodent, Ralf Srama, L. Lamy, Robert Ebert, S. Hsu, Ioannis A. Daglis, Edward C. Sittler, K. Konstantinidis, Matthew S. Tiscareno, O. Karatekin, M. H. Hofstadter, Nicolas Rambaux, Matthew M. Hedman, Richard Holme, Andrew J. Coates, Tom Stallard, Pierre Henri, Sarah V. Badman, Bruno Christophe, Jessica Agarwal, M. I. Desai, Diego Turrini, Fritz M. Neubauer, Andrew Smith, Agustín Sánchez-Lavega, Julianne I. Moses, Davide Grassi, G. S. Orton, O. Mousis, N. André, C. Labrianidis, Mihaly Horanyi, Federico Tosi, Henrik Melin, P. Zarka, Mathew J. Owens, S. M. P. McKenna-Lawlor, Elizabeth P. Turtle, Benoît Noyelles, Shawn M. Brooks, Matthieu Laneuville, Richard M. Ambrosi, John F. Cooper, Dominic Dirkx, Caitriona M. Jackman, Mario M. Bisi, C. Bracken, Kevin H. Baines, Harald Krüger, Mathieu Barthelemy, E. Khalisi, Kunio M. Sayanagi, Pontus Brandt, Tom Nordheim, J. L. MacArthur, Ondrej Santolik, Glyn Collinson, Sascha Kempf, Jürgen Blum, Robert W. Wilson, I. de Pater, Veerle Sterken, William S. Kurth, Patrick G. J. Irwin, Craig B. Agnor, Frank Postberg, T. M. Bocanegra-Bahamón, Jon K. Hillier, Julie Castillo-Rogez, Eberhard Grün, Georg Moragas-Klostermeyer, Michele K. Dougherty, Christelle Briois, Christopher T. Russell, Nicholas Achilleos, Bertrand Bonfond, Mario Trieloff, Kurt D. Retherford, Abigail Rymer, Renaud Sallantin, Christina Plainaki, Frank Spahn, N. Nettelmann, Achim Morschhauser, S. Vinatier, Gabriel Tobie, Serge Reynaud, Elias Roussos, I. Gerth, A. Luntzer, Joachim Saur, M. Costa-Sitja, Paul M. Schenk, Ravit Helled, David M. Lucchesi, C. Briand, J. Schubert, Régis Courtin, George Hospodarsky, Thibault Cavalié, Sebastien Hess, Chris S. Arridge, V. Lainey, Adam Masters, Anna Milillo, Gianrico Filacchione, Andrea Maier, Jacques Gustin, Nick Sergis, Zoltan Sternovsky, Don Banfield, Leigh N. Fletcher, Mullard Space Science Laboratory (MSSL), University College of London [London] (UCL), Centre for Planetary Sciences [UCL/Birkbeck] (CPS), Department of Physics and Astronomy [UCL London], European Space Research and Technology Centre (ESTEC), European Space Agency (ESA), Queen Mary University of London (QMUL), Space Research Centre [Leicester], University of Leicester, Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS), Institute of Space and Astronautical Science (ISAS), Department of Physics [Lancaster], Lancaster University, Jet Propulsion Laboratory (JPL), California Institute of Technology (CALTECH)-NASA, University of Wisconsin-Madison, Cornell University, Institut de Planétologie et d'Astrophysique de Grenoble (IPAG), Centre National d'Études Spatiales [Toulouse] (CNES)-Université Grenoble Alpes (UGA)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Joseph Fourier - Grenoble 1 (UJF)-Centre National de la Recherche Scientifique (CNRS), STFC Rutherford Appleton Laboratory (RAL), Science and Technology Facilities Council (STFC), Technische Universität Braunschweig [Braunschweig], Delft University of Technology (TU Delft), Laboratoire de Physique Atmosphérique et Planétaire (LPAP), Université de Liège, National University of Ireland Maynooth (NUIM), Johns Hopkins University Applied Physics Laboratory [Laurel, MD] (APL), Laboratoire d'études spatiales et d'instrumentation en astrophysique (LESIA), Centre National de la Recherche Scientifique (CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Observatoire de Paris, PSL Research University (PSL)-PSL Research University (PSL)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC), Laboratoire de physique et chimie de l'environnement (LPCE), Université d'Orléans (UO)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Max-Planck-Institut für Sonnensystemforschung (MPS), Max-Planck-Gesellschaft, DPHY, ONERA, Université Paris Saclay [Châtillon], ONERA-Université Paris-Saclay, NASA Goddard Space Flight Center (GSFC), European Space Astronomy Centre (ESAC), Department of Physics [Athens], National and Kapodistrian University of Athens = University of Athens (NKUA | UoA), Lawrence Berkeley National Laboratory [Berkeley] (LBNL), Southwest Research Institute [San Antonio] (SwRI), Istituto di Astrofisica e Planetologia Spaziali - INAF (IAPS), Istituto Nazionale di Astrofisica (INAF), Space and Atmospheric Physics Group [London], Blackett Laboratory, Imperial College London-Imperial College London, Department of Atmospheric, Oceanic and Planetary Physics [Oxford] (AOPP), University of Oxford [Oxford], University of California [Santa Cruz] (UCSC), University of California, Max-Planck-Institut für Kernphysik (MPIK), Laboratory for Atmospheric and Space Physics [Boulder] (LASP), University of Colorado [Boulder], University of Idaho [Moscow, USA], Tel Aviv University [Tel Aviv], HEPPI - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Institut de Mécanique Céleste et de Calcul des Ephémérides (IMCCE), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, PSL Research University (PSL)-PSL Research University (PSL)-Université de Lille-Centre National de la Recherche Scientifique (CNRS), Universität Heidelberg [Heidelberg], School of Environmental Sciences [Liverpool], University of Liverpool, University of Iowa [Iowa City], Department of Physics [Oxford], School of Physics and Astronomy [Southampton], University of Southampton, Royal Observatory of Belgium [Brussels], University of Stuttgart, Universität der Bundeswehr München [Neubiberg], Department of Physics and Astronomy [Iowa City], UTesat-Spacecom, Institut de Physique du Globe de Paris (IPGP), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-IPG PARIS-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Centre National de la Recherche Scientifique (CNRS), University of Vienna [Vienna], Space Research Institute of Austrian Academy of Sciences (IWF), Austrian Academy of Sciences (OeAW), Space Technology Ireland Limited, Institut für Raumfahrtsysteme (IRS), Universität Stuttgart [Stuttgart], Deutsches Zentrum für Luft- und Raumfahrt (DLR), Space Science Institute [Boulder] (SSI), Univers, Transport, Interfaces, Nanostructures, Atmosphère et environnement, Molécules (UMR 6213) (UTINAM), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC), Institute for Geophysics and Meteorology [Köln] (IGM), University of Cologne, Université de Namur [Namur], University of Reading (UOR), Université Pierre et Marie Curie - Paris 6 - UFR de Médecine Pierre et Marie Curie (UPMC), Université Pierre et Marie Curie - Paris 6 (UPMC), Laboratoire Kastler Brossel (LKB (Jussieu)), Fédération de recherche du Département de physique de l'Ecole Normale Supérieure - ENS Paris (FRDPENS), Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS Paris)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS Paris)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS), Institute of Geophysics and Planetary Physics [Los Angeles] (IGPP), University of California [Los Angeles] (UCLA), University of California-University of California, University of the Basque Country [Bizkaia] (UPV/EHU), Institute of Atmospheric Physics, Institut für Geophysik und Meteorologie [Köln], Universität zu Köln, Institute of Atmospheric Physics [Prague] (IAP), Czech Academy of Sciences [Prague] (ASCR), Lunar and Planetary Institute [Houston] (LPI), Department of Earth Sciences [USC Los Angeles], University of Southern California (USC), Office for Space Research and Applications [Athens], Academy of Athens, University of Potsdam, Max Planck Institute for Nuclear Physics (MPIK), International Space Science Institute [Bern] (ISSI), Cornelle University, Laboratoire de Planétologie et Géodynamique UMR6112 (LPG), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Nantes - Faculté des Sciences et des Techniques, Université de Nantes (UN)-Université de Nantes (UN)-Université d'Angers (UA), Agence Spatiale Européenne = European Space Agency (ESA), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Japan Aerospace Exploration Agency [Sagamihara] (JAXA), NASA-California Institute of Technology (CALTECH), Cornell University [New York], Institut de Planétologie et d'Astrophysique de Grenoble (IPAG ), Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS), Technische Universität Braunschweig = Technical University of Braunschweig [Braunschweig], National University of Ireland Maynooth (Maynooth University), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université Paris Diderot - Paris 7 (UPD7)-Centre National de la Recherche Scientifique (CNRS), Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS), Max-Planck-Institut für Sonnensystemforschung = Max Planck Institute for Solar System Research (MPS), DPHY, ONERA, Université Paris Saclay (COmUE) [Châtillon], ONERA-Université Paris Saclay (COmUE), National and Kapodistrian University of Athens (NKUA), University of Oxford, University of California [Santa Cruz] (UC Santa Cruz), University of California (UC), Tel Aviv University (TAU), HELIOS - LATMOS, Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Universität Heidelberg [Heidelberg] = Heidelberg University, Royal Observatory of Belgium [Brussels] (ROB), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Lille-Centre National de la Recherche Scientifique (CNRS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS), Université Bourgogne Franche-Comté [COMUE] (UBFC)-Université Bourgogne Franche-Comté [COMUE] (UBFC), Université de Namur [Namur] (UNamur), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS), University of California (UC)-University of California (UC), University of the Basque Country/Euskal Herriko Unibertsitatea (UPV/EHU), Universität zu Köln = University of Cologne, Czech Academy of Sciences [Prague] (CAS), University of Potsdam = Universität Potsdam, Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Toulouse III - Paul Sabatier (UT3), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS), Centre National de la Recherche Scientifique (CNRS)-Université de Lille-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC), Université Pierre et Marie Curie - Paris 6 (UPMC)-Fédération de recherche du Département de physique de l'Ecole Normale Supérieure - ENS Paris (FRDPENS), École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS), Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS), Mullard Space Science Laboratory ( MSSL ), University College of London [London] ( UCL ), Centre for Planetary Sciences [UCL/Birkbeck] ( CPS ), European Space Research and Technology Centre ( ESTEC ), European Space Agency ( ESA ), Queen Mary University of London ( QMUL ), Institut de recherche en astrophysique et planétologie ( IRAP ), Université Paul Sabatier - Toulouse 3 ( UPS ) -Observatoire Midi-Pyrénées ( OMP ) -Centre National de la Recherche Scientifique ( CNRS ), Institute of Space and Astronautical Science ( ISAS ), Jet Propulsion Laboratory ( JPL ), NASA-California Institute of Technology ( CALTECH ), University of Wisconsin-Madison [Madison], Institut de Planétologie et d'Astrophysique de Grenoble ( IPAG ), Observatoire des Sciences de l'Univers de Grenoble ( OSUG ), Université Joseph Fourier - Grenoble 1 ( UJF ) -Institut national des sciences de l'Univers ( INSU - CNRS ) -Centre National de la Recherche Scientifique ( CNRS ) -Université Grenoble Alpes ( UGA ) -Université Joseph Fourier - Grenoble 1 ( UJF ) -Institut national des sciences de l'Univers ( INSU - CNRS ) -Centre National de la Recherche Scientifique ( CNRS ) -Université Grenoble Alpes ( UGA ) -Centre National de la Recherche Scientifique ( CNRS ), STFC Rutherford Appleton Laboratory ( RAL ), Science and Technology Facilities Council ( STFC ), Delft University of Technology ( TU Delft ), Laboratoire de Physique Atmosphérique et Planétaire ( LPAP ), National University of Ireland Maynooth ( NUIM ), Johns Hopkins University Applied Physics Laboratory [Laurel, MD] ( APL ), Laboratoire d'études spatiales et d'instrumentation en astrophysique ( LESIA ), Université Pierre et Marie Curie - Paris 6 ( UPMC ) -Institut national des sciences de l'Univers ( INSU - CNRS ) -Observatoire de Paris-Université Paris Diderot - Paris 7 ( UPD7 ) -Centre National de la Recherche Scientifique ( CNRS ), Laboratoire de physique et chimie de l'environnement ( LPCE ), Institut national des sciences de l'Univers ( INSU - CNRS ) -Université d'Orléans ( UO ) -Centre National de la Recherche Scientifique ( CNRS ), Max-Planck-Institut für Sonnensystemforschung ( MPS ), ONERA - The French Aerospace Lab ( Toulouse ), ONERA, NASA Goddard Space Flight Center ( GSFC ), European Space Astronomy Center ( ESAC ), National and Kapodistrian University of Athens, University of California [Berkeley], Southwest Research Institute [San Antonio] ( SwRI ), Istituto di Astrofisica e Planetologia Spaziali ( IAPS ), Istituto Nazionale di Astrofisica ( INAF ), Department of Atmospheric, Oceanic and Planetary Physics [Oxford] ( AOPP ), University of California [Santa Cruz] ( UCSC ), Max-Planck-Institut für Kernphysik ( MPIK ), Laboratory for Atmospheric and Space Physics [Boulder] ( LASP ), University of Colorado Boulder [Boulder], Laboratoire Atmosphères, Milieux, Observations Spatiales ( LATMOS ), Université de Versailles Saint-Quentin-en-Yvelines ( UVSQ ) -Université Pierre et Marie Curie - Paris 6 ( UPMC ) -Institut national des sciences de l'Univers ( INSU - CNRS ) -Centre National de la Recherche Scientifique ( CNRS ) -Université de Versailles Saint-Quentin-en-Yvelines ( UVSQ ) -Université Pierre et Marie Curie - Paris 6 ( UPMC ) -Institut national des sciences de l'Univers ( INSU - CNRS ) -Centre National de la Recherche Scientifique ( CNRS ), Institut de Mécanique Céleste et de Calcul des Ephémérides ( IMCCE ), Université Pierre et Marie Curie - Paris 6 ( UPMC ) -Institut national des sciences de l'Univers ( INSU - CNRS ) -Observatoire de Paris-Université de Lille-Centre National de la Recherche Scientifique ( CNRS ), University of Iowa [Iowa], University of Southampton [Southampton], Institut de Physique du Globe de Paris ( IPGP ), Université Pierre et Marie Curie - Paris 6 ( UPMC ) -Institut national des sciences de l'Univers ( INSU - CNRS ) -IPG PARIS-Université Paris Diderot - Paris 7 ( UPD7 ) -Université de la Réunion ( UR ) -Centre National de la Recherche Scientifique ( CNRS ), Space Research Institute of Austrian Academy of Sciences ( IWF ), Austrian Academy of Sciences ( OeAW ), Institut für Raumfahrtsysteme ( IRS ), Deutsches Zentrum für Luft- und Raumfahrt ( DLR ), Space Science Institute [Boulder] ( SSI ), Univers, Transport, Interfaces, Nanostructures, Atmosphère et environnement, Molécules ( UTINAM ), Institut national des sciences de l'Univers ( INSU - CNRS ) -Centre National de la Recherche Scientifique ( CNRS ) -Université de Franche-Comté ( UFC ), Institute for Geophysics and Meteorology [Köln] ( IGM ), University of Reading ( UOR ), Université Pierre et Marie Curie - Paris 6 - UFR de Médecine Pierre et Marie Curie ( UPMC ), Université Pierre et Marie Curie - Paris 6 ( UPMC ), Laboratoire Kastler Brossel ( LKB (Jussieu) ), Fédération de recherche du Département de physique de l'Ecole Normale Supérieure - ENS Paris ( FRDPENS ), Centre National de la Recherche Scientifique ( CNRS ) -École normale supérieure - Paris ( ENS Paris ) -Centre National de la Recherche Scientifique ( CNRS ) -École normale supérieure - Paris ( ENS Paris ) -Université Pierre et Marie Curie - Paris 6 ( UPMC ) -Centre National de la Recherche Scientifique ( CNRS ), Institute of Geophysics and Planetary Physics [Los Angeles] ( IGPP ), University of California at Los Angeles [Los Angeles] ( UCLA ), University of the Basque Country [Bizkaia] ( UPV/EHU ), Institute of Atmospheric Physics [Prague] ( IAP ), Czech Academy of Sciences [Prague] ( ASCR ), Lunar and Planetary Institute [Houston] ( LPI ), Department of Earth Sciences [Los Angeles], University of Southern California ( USC ), Laboratoire de Planétologie et Géodynamique de Nantes ( LPGN ), Université de Nantes ( UN ) -Institut national des sciences de l'Univers ( INSU - CNRS ) -Centre National de la Recherche Scientifique ( CNRS ), and International Space Science Institute ( ISSI )
Subjects: Outer planets, Gas giant, [PHYS.ASTR.EP]Physics [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP], Uranus, [SDU.ASTR.EP]Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP], Natural satellites, Astrobiology, ice giant planets, Neptune, Rings, Physics, Naturalsatellites, Atmosphere, Nice model, Institut für Physik und Astronomie, Astronomy, Astronomy and Astrophysics, orbital mission, [ SDU.ASTR.EP ] Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP], science case, [ PHYS.ASTR.EP ] Physics [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP], Rings of Uranus, Space and Planetary Science, Exploration of Uranus, Magnetosphere, Physics::Space Physics, Astrophysics::Earth and Planetary Astrophysics, Planetary interior, [PHYS.ASTR]Physics [physics]/Astrophysics [astro-ph], Ice giant
Abstract: 著者人数: 114名, Accepted: 2014-08-07, 資料番号: SA1005021000
Published: 2014

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