File:Ganymede field.svg

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Description Magnetic field of Ganymede. Calculated using data from Gallileo's second encounter to the moon at September 6th 1996 (superposition model with 120nT homogenous field and equatorial field strength of 720nT for the moon's own dipole field). The co-rotating Ganymede-centered reference system is such that the x-axis points towards Jupiter, the z-axis is the common spin axes of Jupiter, Ganymede and its orbit. The y-axis is suppressed and shows in direction of Ganymede's orbital motion. The green line - the separatrix - seperates regions of magnetic field lines which a) go from moon to moon, b) from moon to planet or c) from planet to planet.
Date 4 August 2007 (upload date)
Source Own work
Author CWitte

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I, the copyright holder of this work, hereby publish it under the following licenses:
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attribution share alike
This file is licensed under the Creative Commons Attribution-Share Alike 2.5 Generic, 2.0 Generic and 1.0 Generic license.
You are free:
  • to share – to copy, distribute and transmit the work
  • to remix – to adapt the work
Under the following conditions:
  • attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
  • share alike – If you remix, transform, or build upon the material, you must distribute your contributions under the same or compatible license as the original.
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Date/TimeThumbnailDimensionsUserComment
current12:45, 4 August 2007Thumbnail for version as of 12:45, 4 August 20071,200 × 800 (47 KB)CWitte (talk | contribs)better arrows
12:19, 4 August 2007Thumbnail for version as of 12:19, 4 August 20071,800 × 1,200 (144 KB)CWitte (talk | contribs)minor things and license
11:46, 4 August 2007Thumbnail for version as of 11:46, 4 August 20072,400 × 3,600 (41 KB)CWitte (talk | contribs){{Information |Description=Magnetic field of Ganymede. Calculated using data from Gallileo's second encounter to the moon at September 6th 1996 (superposition model with 120nT homogenous field and equatorial field strength of 720nT for the moon's own dipo

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