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The Dust Halo of Saturn's largest Icy moon, Rhea

  • G. H. Jones
  • , E. Roussos
  • , N. Krupp
  • , U. Beckmann
  • , A. J. Coates
  • , F. Crary
  • , I. Dandouras
  • , V. Dikarev
  • , M. K. Dougherty
  • , P. Garnier
  • , C. J. Hansen
  • , A. R. Hendrix
  • , G. B. Hospodarsky
  • , R. E. Johnson
  • , S. Kempf
  • , K. K. Khurana
  • , S. M. Krimigis
  • , H. Krüger
  • , W. S. Kurth
  • , A. Lagg
  • H. J. McAndrews, D. G. Mitchell, C. Paranicas, F. Postberg, C. T. Russell, J. Saur, M. Seiß, F. Spahn, R. Srama, D. F. Strobel, R. Tokar, J. E. Wahlund, R. J. Wilson, J. Woch, D. Young
  • Max Planck Inst Solar Syst Res, Max Planck Society
  • UCL
  • Max Planck Institute for Nuclear Physics
  • Southwest Research Institute
  • Université Paul Sabatier
  • St. Petersburg State University
  • Imperial College London
  • Swedish Institute of Space Physics
  • Jet Propulsion Laboratory, California Institute of Technology
  • University of Iowa
  • University of Virginia
  • University of California at Los Angeles
  • Johns Hopkins Applied Physics Laboratory
  • Los Alamos Natl Lab, Los Alamos National Laboratory, United States Department of Energy (DOE)
  • University of Cologne
  • University of Potsdam
  • Johns Hopkins University

Tutkimustuotos: Lehtiartikkeli › Article › Scientific › vertaisarvioitu

57 Sitaatiot (Scopus)

Abstrakti

Saturn's moon Rhea had been considered massive enough to retain a thin, externally generated atmosphere capable of locally affecting Saturn's magnetosphere. The Cassini spacecraft's in situ observations reveal that energetic electrons are depleted in the moon's vicinity. The absence of a substantial exosphere implies that Rhea's magnetospheric interaction region, rather than being exclusively induced by sputtered gas and its products, likely contains solid material that can absorb magnetospheric particles. Combined observations from several instruments suggest that this material is in the form of grains and boulders up to several decimetres in size and orbits Rhea as an equatorial debris disk. Within this disk may reside denser, discrete rings or arcs of material.

AlkuperäiskieliEnglanti
Sivut1380-1384
Sivumäärä5
JulkaisuScience
Vuosikerta319
Numero5868
DOI - pysyväislinkit
TilaJulkaistu - 7 maalisk. 2008
OKM-julkaisutyyppiA1 Alkuperäisartikkeli tieteellisessä aikakauslehdessä

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