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Concerning Steady State Corotation of the Io Plasma Torus

Concerning Steady State Corotation of the Io Plasma Torus

by B. I. Rabinovich * and V. I. Prokhorenko **

* Moscow State Academy of Control Devices Design and Informatics, Stromynka 20, Moscow 107846, Russia

** Space Research Institute Russian Academy of Sciences, Profsojusnaja 84/32, Moscow 117810, Russia

In recent years, substantial information concerning the Io torus has been published. Much new information has been obtained by the Galileo mission (e.g. http://www.jpl.nasa.gov/galileo). Nevertheless, numerous unanswered questions remain.

Explaining the observed steady state rotation of the torus seems to be difficult. The angular velocity of the torus must be in accordance with the celestial mechanics laws, of the same orders as Io's one. But the radial plane corresponding to the eccentricity and maximum thickness of the torus rotates in the inertial medium with an angular velocity approximately 4.5 times greater then Io's orbital angular velocity, being quite stable relative to Jupiter.

Some attempts have been made to explain the picture being observed by hypothesis of continuous ejection of the mass through the outer border of the torus and replacement via Io's volcano activity. Suitable calculations give the value approximately 1000 kg/s as the estimation of the mass debit [Hill et al. 1991; Schneider et al., 1991]. Experimental results from Galileo place the debit closer to 10 kg/s, two orders of magnitude smaller [Russell et al., 1997]. This makes the conception of strictly non steady torus vulnerable to criticism.

We wish to straighten out the situation describing the main geometric and kinematic features of the Io torus using a steady state model based on some of Alfven's ideas [Alfven, 1981]. Three key aspects of our approach are:

- Noncompressional plasma with infinitesimal viscosity and infinitely high electrical conductivity (an ideal magnetized plasma).
- A geometrical model of the thin torus, with the thickness being very small in comparison with torus radius.
- Inclusion of the Newtonian gravitational field and the dipole magnetic field, the latter slightly inclined from the rotation axis of Jupiter (being parallel to the rotation axis of the torus).

A mathematical model of the plasma ring corresponding to these assumptions has already been presented by Rabinovich at al. [1992; 1996]. We improve the model for undisturbed motion by taking into account the eccentricity of the dipole and using some features of the classical "problem of two immovable centers" which was formulated and solved by Leonard Euler more than two centuries ago.

In our case, the geometrical center of the planet and the dipole play the role of the two centers, whereas the gravitational and the ponderomotive ones related to the midpoint of torus elements play the role of the forces. We propose that the repulsive ponderomotive force is smaller than the attractive gravitational force.

Let us use the following transformations:

- Replace the midpoint of the torus where the resultant of both mentioned forces occurs with a straight line connecting the centers.
- Exchange the force system acting on the torus element for the resultant vector directed toward this point.

It is possible to prove that the position of the last point is stable up to first order relative to the eccentricity of the dipole, and the resultant modulus is stable up to the zeroth order. Nonsteady terms could be included in the equations of disturbed motion of the torus, but this is not the point of this paper.

Let use as a mathematical model for the undisturbed motion of the torus the differential equation of the relative motion of material point projected on the torus- central radius-vector in a coordinate system rotating together with the planet. The absolute angular velocity of the torus and the Alfven waves velocity relative to the middle line of the torus are the main parameters of the problem.

The sum of the following two steady state rotations is the exact solution of the basic equation:

- The torus rotates in its plane around a point displaced relative to the planet's center in a direction opposite to the dipole. The square of the absolute velocity of this rotation is the squares difference (always positive in our case) between the circular (taking into account the magnetic field) and Alfven waves velocities.
- As it rotates together with the planet, the torus' diameter passes through the planet's center.

We may identify the last rotation as a "corotation" of the torus and the sum of two rotations mentioned above as a "partial corotation" [Alfven, 1981].

Table 1 presents the calculated values of some torus' parameters related to its middle line obtained by aforementioned mathematical model.

Table 1. The kinematic parameters of the torus and the plasma density

      1      Circular velocity (km/s)                     17.27

      2      Circular velocity, tacking into account 
             the magnetic field (km/s)                    10.70

      3      Corotation velocity (km/s)                   80.65

      4      Alfven's waves velocity  (km/s)              7.831

      5      Plasma density g/cm3                         4.246 10-17

The basic data for the calculations were taken from [Russel et al., 1997] (for torus geometry) and [Kaufmann, 1979; Whiple, 1981; Burgess, 1977] (for the Jovian systems parameters).

Figure 1 presents the kinematic picture of the partial corotation of the torus corresponding to the described model for the mean values of the torus parameters related to its central line.

Summarizing the results, the steady state model considered here gives a possible explanation for the main natural features of geometry and kinematics of the Io torus without any additional physical hypotheses. Comparison with new experimental data should provide a possibility for checking the improved model. Acknowledgments The authors thank the Russian Foundation for Fundamental Research (grant 97-01- 00536) for support of this investigation.

References

Alfven H., Cosmic Plasma. Reidel, Dordrecht, 1981

Bagenal, F., Empirical Model of the Io Plasma Torus: Voyager Measurements. J. Geophys. Res., 99, 11.043, 1994.

Burgess, Eric. Uranus & Neptune The Distant Giants. Columbia University Press, New York, 1988.

Frank, L. A., W. R. Paterson, K. L. Ackerson, V. M. Vasyliunas, F. V. Coroniti, and S. J. Belton, Plasma observation at Io with the Galileo spacecraft: Passage through the ionosphere, Science, 274, 394, 1996.

Gurnett, D. A., W. S. Kurth, A. Roux, S. J. Bolton, and C. F. Kennel, Galileo plasma wave observations in the Io plasma torus and near Io, Science, 273, 391, 1996.

Hill, T. W. and A. J. Dessler, Plasma Motion in Planetary Magnetospheres, Science, 252, 410, 1991.

Hill, T. W. and A. J. Dessler. Space Physics and Astronomy Converge in Exploration of Jupiter's Magnetosphere, EOS Trans., AGU, 76, 313, 1995.

Kaufmann III , William J., Planets and Moons, W. H. Freemen and Company. San Francisco, 1979.

Rabinovich, B. I., V. G. Lebedev, and A. V. Kalinina, Magnetohydrodynamics of a Rotating Ring of Magnetized Plasma, Sov. Physics - Dokl., 37 (10), 502, 1992.

Rabinovich, B. I., Magnetohydrodynamics of Rotating Vortex Rings of Magnetized Plasma, Sov. Physics - Dokl., 41 (11), 562, 1996.

Russel, C. T., F. Bagenal, A. F. Cheng, W. - H. Ip, A. Roux, W. H. Smyth, S. J. Bolton, and C. A. Polanskey, Io's interaction with the Jovian Magnetosphere, EOS Trans., AGU, 78, 93, 1997.

Schneider, Nick, and John Spencer, Io and Jupiter: The Volcano-Magnetosphere Connection, Geophysics News, 15, 55, 1991.

Torrence, V. Johnson, The Galileo Mission. Scientific American, 44, December, 1995.

Whiple, F. L., Orbiting the Sun: Planets and Satellites of the Solar System. Harvard University Press. Cambridge Massachusetts, London, England 1981.

Figure Captions

Fig. 1.. Five positions of the Io torus, Io and Jupiter in the inertial medium corresponding to one rotation of Jupiter around its axis (the scale is distorted for clarity).

Dated December 1997