DOI QR코드

DOI QR Code

TEMPORAL VARIATIONS OF IO'S MAGNETIC FOOTPRINT BRIGHTNESS

  • WANNAWICHIAN, SUWICHA (Department of Physics and Materials Science, Faculty of Science, Chiang Mai University) ;
  • PROMFU, TATPHICHA (Department of Physics and Materials Science, Faculty of Science, Chiang Mai University)
  • Received : 2014.11.30
  • Accepted : 2015.06.30
  • Published : 2015.09.30

Abstract

The brightness of Io's magnetic footprint, an indicator of electromagnetic interaction at the satellite, appears to be strongly connected to the satellite's distance from the plasma equator. As a result, the brightest footprints were detected when Io is near the interception location between the satellite's orbital plane and the plasma equator. However, volcanic activities on Io show strong correlation with the equatorward shift of Jupiter's main auroral oval, consequently causing the disappearance of Io's footprint. The same conclusion was suggested via the observation of Jupiter's hectometric radio emission, called HOM, which closely corresponds to Jupiter's auroral activity. The plasma environment near the Jovian satellites was found to vary significantly at different observational epochs. The electron density increased by approximately a factor of three from the Voyager epoch (1979) to the Galileo epoch (1995), while the electron density was found to be significantly higher (~ 5 times) in the Cassini epoch (2001). In this current study, the magnetic footprints were clearly brighter ten years ago (from peak brightness in 1998-2001) than the footprints detected in 2007. For volcanic activities on Io in 2007, there are two clear activities in February and late May. The magnetic footprint appeared to be dimmer in March 2007, expected to be the result of volcano activities in Feb 2007. However, the magnetic footprint brightness in June appeared to be slightly brighter than the footprints observed in May. The reason could be the time delay between the brightening of the sodium nebula on approximately May 31st and, a while later, the enhancement of flux tube content peaking on approximately June 5th. On the other hand, Io's magnetic footprints were observed during June 1st - 10th when they may not yet have been affected by the increase in mass outflow due to the increase of plasma density.

Keywords

References

  1. Bonfond, B., Grodent, D., & Gerard,J.-C., et al., 2012, Auroral Evidence of Lo's Control over the Magnetosphere of Jupiter, GRL,39, L01105
  2. Clarke, J. T., Ben Jaffel, L., & Gerard, J. -C., 1998, Hubble Space Telescope Imaging of Jupiter's UV Aurora during the Galileo Orbiter Mission, JGR, 103, 20217 https://doi.org/10.1029/98JE01130
  3. Connerney, J. E. P., Acuna, M. H., & Ness, N. F., 1983, Currents in Saturn's Magnetosphere, JGR, 88, 8779 https://doi.org/10.1029/JA088iA11p08779
  4. Connerney, J. E. P., Acuna, M. H., Ness, N. F., & Satoh, T., 1998, New Models of Jupiter's Magnetic Field Constrained by the Lo Flux Tube Footprint, JGR, 103, 11929 https://doi.org/10.1029/97JA03726
  5. Grodent, D., Bonfond, B., & Gerard, J. -C., et al., 2008, Auroral Evidence of a Localized Magnetic Anomaly in Jupiter's Northern Hemisphere, JGR, 113, A09201
  6. Hill, T. W. & Michel, F. C., 1976, Heavy Lons from the Galilean Satellites and the Centrifugal Distortion of the Jovian Magnetosphere, JGR, 81, 4561 https://doi.org/10.1029/JA081i025p04561
  7. Serio, A. W. & Clarke, J. T., 2008, The Variation of Lo's Auroral Footprint Brightness with the Location of Lo in the Plasma Torus, Icarus, 197, 368 https://doi.org/10.1016/j.icarus.2008.03.026
  8. Schneider, N. M. & Trauger, J. T., 1995, The Structure of the IL Torus, ApJ, 450, 450 https://doi.org/10.1086/176155
  9. Steffl, A. J., Delamere, P. A., & Bagenal, F., 2006, Cassini UVIS Observations of the Lo Plasma Torus. III. Observations of Temporal and Azimuthal Variability, Icarus, 180,124 https://doi.org/10.1016/j.icarus.2005.07.013
  10. Steffl, A. J., Delamere, P. A., & Bagena, F., 2008, Cassini UVIS Observations of the Lo Plasma Torus. IV. Modeling Temporal and Azimuthal Variability, Icarus, 194,153 https://doi.org/10.1016/j.icarus.2007.09.019
  11. Vincent, M. B., Clarke, J. T., & Ballester, G. E., et al., 2000, Jupiter's Polar Regions in the Ultraviolet as Imaged by HST/WFPC2: Auroral-Aligned Features and Zonal Motions, Icarus, 143, 205 https://doi.org/10.1006/icar.1999.6233
  12. Wannawichian, S., Clarke, J. T., & Pontius, D. H., 2008, Interaction Evidence between Enceladus's Atmosphere and Saturn's Magnetosphere, JGR, 113, A07217
  13. Wannawichian, S., Clarke, J. T., & Nichols, J. D., 2010, Ten Years of Hubble Space Telescope Observations of the Variation of the Jovian Satellites's Auroral Footprint Brightness, JGR, 115, A02206
  14. Yoneda, M., Tsuchiya, F., Misawa, H., Bonfond, B., Tao, C., Kagitani, & Okano, S., 2013, Lo's Volcanism Controls Jupiter's Radio Emissions, GRL, 40, 671 https://doi.org/10.1002/grl.50095