Magnetospheric and Plasma Science with Cassini-huygens

نویسندگان

  • M. BLANC
  • S. BOLTON
  • J. BRADLEY
  • M. BURTON
  • T. E. CRAVENS
  • I. DANDOURAS
  • M. K. DOUGHERTY
  • M. C. FESTOU
  • J. FEYNMAN
  • R. E. JOHNSON
  • T. G. GOMBOSI
  • W. S. KURTH
  • P. C. LIEWER
  • B. H. MAUK
  • S. MAURICE
  • D. MITCHELL
  • F. M. NEUBAUER
  • J. D. RICHARDSON
  • D. E. SHEMANSKY
  • E. C. SITTLER
  • B. T. TSURUTANI
  • Ph. ZARKA
  • L. W. ESPOSITO
  • E. GRÜN
  • D. A. GURNETT
  • A. J. KLIORE
  • S. M. KRIMIGIS
  • D. SOUTHWOOD
  • J. H. WAITE
چکیده

Magnetospheric and plasma science studies at Saturn offer a unique opportunity to explore in-depth two types of magnetospheres. These are an ‘induced’ magnetosphere generated by the interaction of Titan with the surrounding plasma flow and Saturn’s ‘intrinsic’ magnetosphere, the magnetic cavity Saturn’s planetary magnetic field creates inside the solar wind flow. These two objects will be explored using the most advanced and diverse package of instruments for the analysis of plasmas, energetic particles and fields ever flown to a planet. These instruments will make it possible to address and solve a series of key scientific questions concerning the interaction of these two magnetospheres with their environment. The flow of magnetospheric plasma around the obstacle, caused by Titan’s atmosphere/ionosphere, produces an elongated cavity and wake, which we call an ‘induced magnetosphere’. The Mach number characteristics of this interaction make it unique in the solar system. We first describe Titan’s ionosphere, which is the obstacle to the external plasma flow. We then study Titan’s induced magnetosphere, its structure, dynamics and variability, and discuss the possible existence of a small intrinsic magnetic field of Titan. Saturn’s magnetosphere, which is dynamically and chemically coupled to all other components of Saturn’s environment in addition to Titan, is then described. We start with a summary of the morphology of magnetospheric plasma and fields. Then we discuss what we know of the magnetospheric interactions in each region. Beginning with the innermost regions and moving outwards, we first describe the region of the main rings and their connection to the low-latitude ionosphere. Next the icy satellites, which develop specific magnetospheric interactions, are imbedded in a relatively dense neutral gas cloud which also overlaps the spatial extent of the diffuse E ring. This region constitutes a Space Science Reviews 104: 253–346, 2002. © 2003 Kluwer Academic Publishers. Printed in the Netherlands.

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تاریخ انتشار 2003