Limited single-spacecraft observations of Jupiter's magnetopause have been used to infer that the boundary moves inward or outward in response to variations in the dynamic pressure of the solar wind1,2,3,4,5,6,7,8. At Earth, multiple-spacecraft observations have been implemented to understand the physics of how this motion occurs, because they can provide a snapshot of a transient event in progress. Here we present a set of nearly simultaneous two-point measurements of the jovian magnetopause at a time when the jovian magnetopause was in a state of transition from a relatively larger to a relatively smaller size in response to an increase in solar-wind pressure. The response of Jupiter's magnetopause is very similar to that of the Earth, confirming that the understanding built on studies of the Earth's magnetosphere is valid. The data also reveal evidence for a well-developed boundary layer just inside the magnetopause.
The measurements shown here are primarily from the radio and plasma wave science instruments on Cassini9 and Galileo10; they make use of Cassini's fly-by of Jupiter centred on 30 December 2000 coupled with the extended Galileo orbital mission. Figure 1 shows the trajectories of Cassini and Galileo near Jupiter during the time interval surrounding the Cassini closest approach. Cassini first encountered the jovian bow shock at about 0419 spacecraft event time (SCET; HHMM ut at the spacecraft) on 28 December (day 363) 2000. As shown in Fig. 2, the shock is identified in the plasma wave data as a broadband burst of noise extending to about 1.5 kHz. The shock was preceded by about 3 h of Langmuir wave activity11 at the electron plasma frequency fpe near 2 kHz, giving an upstream solar-wind electron density ne of 0.05 cm-3 using ne = (fpe/8,980)2, where fpe is measured in Hz. For several hours preceding the Langmuir wave activity, lower frequency, broadband, ion acoustic wave activity12 in bursts was observed. We note that the Langmuir waves and ion acoustic waves are mutually exclusive. This would be consistent with Cassini's traversal of the ion foreshock into the electron foreshock. Cassini encountered the bow shock numerous times between 28 December 2000 and the end of the plotted interval. The bow shock was detected as late as early March 2001 to a distance of approximately 800 jovian radii (RJ).
On 9 January 2001 between 1250 and 2115 SCET, and again on 10 January between 0655 and 2035 SCET the Cassini radio and plasma wave instrument observed trapped continuum radiation13,14, which is a clear indication that the spacecraft was within the jovian magnetosphere. Data from the Cassini plasma and magnetometer instruments confirmed the timing of the magnetopause crossings. A portion of the 10 January wave observations through the magnetopause crossing is shown in the upper panel of Fig. 3. The intense waves between about 300 Hz and 3 kHz are the trapped continuum radiation with the low-frequency cutoff being the electron plasma frequency, corresponding to an electron density of about 1 × 10-3 cm-3. The cutoff frequency (electron density) increased to about 2 kHz (0.05 cm-3) before the continuum radiation disappeared at the magnetopause. The Cassini magnetometer and plasma data confirmed the time of the magnetopause crossing.
At nearly the same time, Galileo was outbound on its 29th orbit (see Fig. 1) and observed a very similar pattern of continuum radiation as that observed by Cassini, as shown in the bottom panel of Fig. 3. Here, the minimum cutoff frequency of the continuum radiation was somewhat higher, 500 Hz, corresponding to a plasma density of 3 × 10-3 cm-3, and the cutoff increased to a frequency of about 3 kHz before disappearing at 2052 SCET at the magnetopause. The time of the magnetopause crossing was confirmed by the Galileo magnetometer. Galileo was well sunward of Cassini; the difference in the x position of the two spacecraft was more than 100 jovian radii (RJ).
The nearly simultaneous magnetopause crossings initially suggest that the magnetopause shape might be approximated by a simple curve connecting the two spacecraft. However, steady-state magnetohydrodynamic models of the interaction of the solar wind with the jovian magnetosphere15 are inconsistent with this interpretation. Superposed on the trajectories in Fig. 1 are four magnetopause models16 representing contours on which an observer would have a 10, 25, 75 or 90% chance of being within the magnetosphere, where the 10% contour is farthest from Jupiter. The lower probability curves require smaller solar wind dynamic pressures. Galileo's crossing lies almost directly on the 25% model but the Cassini crossing is significantly more distant than even the 10% (outermost) model16. The model magnetopause shapes clearly do not allow a curve representative of a steady-state boundary to intersect both spacecraft. We conclude that the magnetopause was in a state of transition from a significantly inflated size at Cassini, to a large but nominal size at Galileo, and that there must have been a kink or wave in the boundary somewhere between the two as suggested in the qualitative model in Fig. 1. We have assumed that a solar-wind pressure increase is directly transmitted through the magnetosheath at a nominal speed of ∼400 km s-1 and have modelled the reconfiguration of the magnetopause by smoothly connecting the 25% Joy et al. contour to one parallel to the Joy et al. 10% model16, but at a distance consistent with the Cassini crossing. On the basis of magnetohydrodynamic modelling, the radius of curvature of this transition is not extreme. The pressure front would take some five hours to propagate from the position of Galileo to that of Cassini. The Cassini plasma science investigation26 observed rapidly rising magnetosheath densities over the several hours following this outbound magnetopause crossing, by as much as a factor of ten by 0600 SCET on the following day. Hence, there is clear evidence of a region of increasing pressure moving from Galileo to Cassini's position on timescales similar to what might be expected for a region of increased pressure in the solar wind. Furthermore, after a few short periods of northward magnetosheath fields, Galileo observed continuous southward-directed magnetic fields for approximately a day. Simulations show17 that southward-directed fields would cause the magnetopause to move outward, so the inward motion observed by both spacecraft could not have resulted from changes of the interplanetary magnetic field orientation. That each spacecraft observed only one outbound crossing on this day rules out a Kelvin–Helmholtz instability, which would have appeared as rather small-amplitude periodic motions of the boundary. Therefore, provided there were no internal variations, we conclude that the magnetosphere was compressed by increasing solar-wind dynamic pressure.
Variations in the size of the terrestrial magnetosphere have been reported for decades, for example, by Fairfield18, with Sibeck et al.19 giving a compendium of some 1,821 observations. At Jupiter, fewer, but similar observations have been reported on the basis of Pioneer1 and Voyager2,3,4,5 data and modelled with conic sections6,7,8. It is well recognized that the magnetopause distance should be controlled, in part, by the solar-wind dynamic pressure18 and the consequences of these motions have been discussed at length20,21,22. Lepping et al.23 suggested that the extended jovian magnetotail would assume a sausage-like shape owing to recurring pressure variations in the solar wind, suggesting that transients reported herein become a part of the magnetotail structure as they propagate downstream. Kivelson and Southwood24 argued that in response to changes in pressure at the magnetopause, field-aligned currents would be driven into the auroral ionosphere and suggest that some auroral signatures at high latitudes could result. Although we have found no optical auroral observations concurrent with the observations presented here, Hubble observations25 taken on 13 January 2001 revealed an auroral oval that was smaller and brighter (upon preliminary analysis) than observed during December 2000 (D. Grodent, personal communication) which might be expected for a compressed magnetosphere.
The gradual increase in electron density inferred from the continuum radiation cutoff from both sets of observations in Fig. 3 is suggestive of a boundary layer just inside the magnetopause where the plasma density changes from that in the magnetosphere to that in the magnetosheath. Galileo showed additional evidence for such a boundary layer during its orbit 28 outbound trajectory. Figure 4 shows a 4-h spectrogram illustrating a rather abrupt decrease in density (decrease in the lower frequency cutoff of the continuum radiation) at about 1645 SCET on 30 May 2000, preceded by a much more gradual decline. The actual magnetopause crossing, determined by a rotation of the field and a decrease in ultra-low-frequency wave activity observed by the magnetometer, occurred at about 1545 SCET. There was a slight decrease in plasma density at this time, but the spacecraft spent nearly an hour in an intermediate density regime, which is also suggestive of a boundary layer.
Smith, E. J., Fillius, R. W. & Wolfe, J. H. Compression of Jupiter's magnetosphere by the solar wind. J. Geophys. Res. 83, 4733–4742 (1978).
Ness, N. F. et al. Magnetic field studies at Jupiter by Voyager 1: Preliminary results. Science 204, 982–987 (1979).
Ness, N. F. et al. Magnetic field studies at Jupiter by Voyager 2: Preliminary results. Science 206, 966–972 (1979).
Bridge, H. S. et al. Plasma observations near Jupiter: Initial results from Voyager 1. Science 204, 987–991 (1979).
Bridge, H. S. et al. Plasma observations near Jupiter: Initial results from Voyager 2. Science 206, 972–976 (1979).
Lepping, R. P., Burlaga, L. F. & Klein, L. W. Jupiter's magnetopause, bow shock, and 10-hour modulated magnetosheath: Voyagers 1 and 2. Geophys. Res. Lett. 8, 99–102 (1981).
Acuña, M. H., Behannon, K. H. & Connerney, J. E. P. in Physics of the Jovian Magnetosphere (ed. Dessler, A. J.) 1–50 (Cambridge Univ. Press, Cambridge, 1983).
Slavin, J. A., Smith, E. J., Spreiter, J. R. & Stahara, S. S. Solar wind flow about the outer planets: Gas dynamic modeling of the Jupiter and Saturn bow shocks. J. Geophys. Res. 90, 6275–6286 (1985).
Gurnett, D. A. et al. The Cassini radio and plasma wave science investigation. Space Sci. Rev. (in the press).
Gurnett, D. A. et al. The Galileo plasma wave investigation. Space Sci. Rev. 60, 341–355 (1992).
Gurnett, D. A., Maggs, J. E., Gallagher, D. L., Kurth, W. S. & Scarf, F. L. Parametric interaction and spatial collapse of beam-driven Langmuir waves in the solar wind. J. Geophys. Res. 86, 8833–8841 (1981).
Kurth, W. S., Gurnett, D. A. & Scarf, F. L. High resolution spectrograms of ion-acoustic waves in the solar wind. J. Geophys. Res. 84, 3413–3419 (1979).
Scarf, F. L., Gurnett, D. A. & Kurth, W. S. Jupiter plasma wave observations: An initial Voyager 1 overview. Science 204, 991–995 (1979).
Gurnett, D. A., Kurth, W. S. & Scarf, F. L. The structure of the Jovian magnetotail from plasma wave observations. Geophys. Res. Lett. 7, 53–56 (1980).
Ogino, T., Walker, R. J. & Kivelson, M. G. A global magnetohydrodynamic simulation of the Jovian magnetosphere. J. Geophys. Res. 103, 225–235 (1998).
Joy, S. P., Kivelson, M. G., Walker, R. J., Khurana, K. & Russell, C. T. Probabilistic models of the Jovian magnetopause and bowshock locations. J. Geophys. Res. (in the press).
Walker, R. J., Ogino, T. & Kivelson, M. G. Magnetohydrodynamic simulations of the effects of the solar wind on the Jovian magnetosphere. Planet. Space Sci. 49, 237–245 (2001).
Fairfield, D. H. Average and unusual locations of the Earth's magnetopause and bow shock. J. Geophys. Res. 76, 6700–6716 (1971).
Sibeck, D. G., Lopez, R. E. & Roelof, E. C. Solar wind control of the magnetopause shape, location and motion. J. Geophys. Res. 96, 5489–5495 (1991).
Elphic, R. C. Multipoint observations of the magnetopause: Results from ISEE and AMPTE. Adv. Space Res. 8(9), 223–228 (1988).
Southwood, D. J. & Kivelson, M. G. The magnetohydrodynamic response of the magnetospheric cavity to changes in solar wind pressure. J. Geophys. Res. 95, 2301–2309 (1990).
Kivelson, M. G. & Southwood, D. J. Ionospheric traveling vortex generation by solar wind buffeting of the magnetosphere. J. Geophys. Res. 96, 1661–1667 (1991).
Lepping, R. P. et al. Structure and other properties of Jupiter's distant magnetotail. J. Geophys. Res. 88, 8801–8816 (1983).
Kivelson, M. G. & Southwood, D. J. in AGU Monograph 58, Physics of Magnetic Flux Ropes (eds Russell, C. T., Priest, E. R. & Lee, L. C.) 619–625 (AGU, Washington DC, 1990).
Grodent, D., Clarke, J. T., Kim, J. & Waite, J. H. Jr HST-STIS observations of Jupiter's far-ultraviolet aurora during the Millennium Campaign. Icarus (submitted).
Young, D. T. et al. Cassini plasma spectrometer investigation. Space Sci. Rev. (in the press).
This research was supported by NASA through contracts with the Jet Propulsion Laboratory.
About this article
Cite this article
Kurth, W., Gurnett, D., Hospodarsky, G. et al. The dusk flank of Jupiter's magnetosphere. Nature 415, 991–994 (2002). https://doi.org/10.1038/415991a
A K ‐Means Clustering Analysis of the Jovian and Terrestrial Magnetopauses: A Technique to Classify Global Magnetospheric Behavior
Journal of Geophysical Research: Planets (2020)
Suprathermal Magnetospheric Atomic and Molecular Heavy Ions at and Near Earth, Jupiter, and Saturn: Observations and Identification
Journal of Geophysical Research: Space Physics (2020)
Energetic Oxygen and Sulfur Charge States in the Outer Jovian Magnetosphere: Insights From the Cassini Jupiter Flyby
Geophysical Research Letters (2019)
Journal of Geophysical Research: Space Physics (2019)
Geophysical Research Letters (2018)