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AGU: Geophysical Research Letters

 

Keywords

  • Saturn's E-ring
  • Enceladus plumes
  • dust dynamics

Index Terms

  • Planetary Sciences: Fluid Planets: Rings and dust
  • Space Plasma Physics: Plasma interactions with dust and aerosols
  • Magnetospheric Physics: Planetary magnetospheres

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L04203, 5 PP., 2008
doi:10.1029/2007GL032726

Large-scale structure of Saturn's E-ring

Mihály Horányi

Max-Planck-Institute for Extraterrestrial Physics, Garching, Germany

Antal Juhász

Department of Space Physics, KFKI Research Institute for Particle and Nuclear Physics, Budapest, Hungary

Gregor E. Morfill

Geysers on the recently discovered, geologically active south-polar region of the moon Enceladus are now recognized as the dominant source of material in Saturn's E ring. The ring was traditionally thought to span the region between 3 to 8 R S , where R S is the radius of Saturn. However, new in situ dust measurements indicate that the density of small grains might continuously extend far beyond these boundaries, and the E ring could reach even beyond the orbit of Titan (20.3 R S ). We report on the modeling results of the long-term evolution of dust particles comprising the E ring to show that grains from Enceladus could indeed reach the outskirts of Saturn's magnetosphere.

Received 26 November 2007; accepted 25 January 2008; published 28 February 2008.

Citation: Horányi, M., A. Juhász, and G. E. Morfill (2008), Large-scale structure of Saturn's E-ring, Geophys. Res. Lett., 35, L04203, doi:10.1029/2007GL032726.

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