Magnetic field observations of the jovian magnetosphere suggest an extended magnetic tail, which has been formed by solar wind interaction with the planetary field.
References
Van Allen, J. A. et al. Science 188, 459–462 (1974).
Smith, E. J. et al. J. geophys. Res. 79, 3501–3513, 1974.
Goertz, C. K. Space Sci. Rev. 23, 319–344 (1979).
Northrop, T. G., Goertz, C. K. & Thomsen, M. F. J. geophys. Res. 79, 3579–3583 (1974).
Kivelson, M. G., Coleman, P. J., Froidevanx, L. & Rosenberg, R. L. J. geophys. Res. 83, 4823–4841, 1978.
Smith, E. J., Davis, L. Jr & Jones, D. E. Jupiter (ed. Gehrels, T. 788–829 (University of Arizona Press, 1976).
Dessler, A. J. & Vasyliunas, V. Geophys. Res. Lett. 6, 37–40 (1979).
Acuna, M. & Ness, N. F. J. geophys. Res. 81, 2917–2922 (1976).
Ness, N. F. et al. Science 204, 982–987 (1979).
Ness, N. F. J. geophys. Res. 70, 2989–3005 (1965).
Ness, N. F., Behannon, K. W., Lepping, R. P. & Whang, Y. C. J. geophys. Res. 80, 2708–2716, 1975.
Carr, T. D. & Desch, M. D. in Jupiter (ed. Gehrels, T.) 693–737 (University of Arizona Press, 1976).
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Ness, N., Acuna, M., Lepping, R. et al. Jupiter's magnetic tail. Nature 280, 799–802 (1979). https://doi.org/10.1038/280799a0
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DOI: https://doi.org/10.1038/280799a0
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