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Composition and dynamics of plasma in Saturn's magnetosphere

  • D.T. Young*
  • , J.-J. Berthelier
  • , M. Blanc
  • , J.L. Burch
  • , S. Bolton
  • , A.J. Coates
  • , F.J. Crary
  • , R. Goldstein
  • , M. Grande
  • , T.W. Hill
  • , R.E. Johnson
  • , R.A. Baragiola
  • , Väinö Kelhä
  • , D.J. McComas
  • , K. Mursula
  • , E.C. Sittler
  • , K.R. Svenes
  • , K. Szegö
  • , P. Tanskanen
  • , M.F. Thomsen
  • S. Bakshi, B.L. Barraclough, Z. Bebesi, D. Delapp, M.W. Dunlop, J.T. Gosling, J.D. Furman, L.K. Gilbert, D. Glenn, Christer Holmlund, J.-M.. Illiano, G.R. Lewis, D.R. Linder, S. Maurice, H.J. McAndrews, B.T. Narheim, E. Pallier, D. Reisenfeld, A.M. Rymer, H.T. Smith, R.L. Tokar, J. Vilppola, C. Zinsmeyer
*Corresponding author for this work
    • California Institute of Technology
    • University of Montana
    • Southwest Research Institute (SWRI)
    • CETP - Centre d'Etudes des Environnements Terrestre et Planetaires
    • Observatoire Midi-Pyrénées
    • Jet Propulsion Laboratory (JPL)
    • University College London
    • Rutherford Appleton Laboratory (RAL)
    • Rice University
    • University of Virginia
    • VTT (former employee or external)
    • University of Oulu
    • National Aeronautics and Space Administration (NASA)
    • Norwegian Defense Research Institute
    • Hungarian Academy of Sciences Centre for Energy Research (mtaEK)
    • Los Alamos National Laboratory

    Research output: Contribution to journalArticleScientificpeer-review

    Abstract

    During Cassini's initial orbit, we observed a dynamic magnetosphere composed primarily of a complex mixture of water-derived atomic and molecular ions. We have identified four distinct regions characterized by differences in both bulk plasma properties and ion composition. Protons are the dominant species outside about 9 RS (where RS is the radial distance from the center of Saturn), whereas inside, the plasma consists primarily of a corotating comet-like mix of water-derived ions with ∼3% N+. Over the A and B rings, we found an ionosphere in which O2+ and O+ are dominant, which suggests the possible existence of a layer of O2 gas similar to the atmospheres of Europa and Ganymede.
    Original languageEnglish
    Pages (from-to)1262-1266
    JournalScience
    Volume307
    Issue number5713
    DOIs
    Publication statusPublished - 2005
    MoE publication typeA1 Journal article-refereed

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