Astron. Astrophys. 347, 1029-1038 (1999)

Jupiter's magnetic field as revealed by the synchrotron radiation belts

I. Comparison of a 3-D reconstruction with models of the field

G.A. Dulk ¹, Y. Leblanc ¹, R.J. Sault ², S.J. Bolton ³, J.H. Waite ⁴ and J.E.P. Connerney <sup>5

1</sup> CNRS-URA 264, Departement de Recherche Spatiale, Observatoire de Paris, F-92195 Meudon, France
² Australia Telescope National Facility, CSIRO, Epping, NSW 1710, Australia
³ Jet Propulsion Laboratory, Pasadena, CA, USA
⁴ Southwest Research Institute, San Antonio, TX, USA
⁵ NASA/Goddard Space Flight Center, Greenbelt, MD, USA

Received 29 March 1999 / Accepted 30 April 1999

Abstract

We use tomographic techniques to make a 3-D reconstruction of Jupiter's synchrotron radiation belts from Very Large Array observations at 20 cm. As in earlier observations with the Australia Telescope Compact Array, this reconstruction shows that the equatorial belt is not symmetric or planar, but is warped. The warp is related to the component of the magnetic field, or equivalently the magnetic declination at Jupiter's magnetic equator: . We show that there is a well defined maximum of intensity at a radius that ranges from about 1.4 to 1.7 , and that the brightness variation with longitude is anticorrelated with at the magnetic equator. The observed magnetic equatorial radius, jovicentric latitude and brightness are compared with calculations of radius, jovicentric latitude and magnetic declination at the magnetic equator on a locus of constant  G in two field models: H4 and VIP4. The agreement between the observed and model quantities is generally good. However, there are discrepancies that suggest inadequacies in the models, particularly at longitudes where the non-dipolar field elements are pronounced.

Until now, observations have provided very few constraints at small radii and low latitudes () for the generation of magnetic field models. Therefore it is not surprising that they are accurate at high latitudes but not at low. The observations of this paper should provide useful constraints for improved models.

Key words: magnetic fields plasmas radiation mechanisms: non-thermal planets and satellites: individual: Jupiter radio continuum: solar system

This article contains no SIMBAD objects.

Contents

• 1. Introduction
• 2. Review of Jupiter's synchrotron radiation
• 3. Observations and reconstructions
  • 3.1. 3-D reconstructions: method and assumptions
  • 3.2. The 3-D reconstruction of the VLA observations
• 4. Reconstructions and models of the magnetic field
  • 4.1. 3-D reconstructions and simulations
    • 4.1.1. Radius and latitude of the magnetic equator
    • 4.1.2. The relationship between brightness and
• 5. Comparison of observations and magnetic field models
  • 5.1. Comparison of radius and latitude
  • 5.2. Comparison of brightness with
  • 5.3. Brightness distribution and at the magnetic dipolar equator
  • 5.4. The sign of
  • 5.5. Constraints for a new model of the magnetic field
• 6. Summary and conclusions
• Acknowledgements
• Appendix
• References

© European Southern Observatory (ESO) 1999

Online publication: June 6, 1999
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