Modeling the Jovian Magnetospheric System


About the Models:

A 3-D Multi-fluid simulation was used to examine both large and small scale features in the Jovian magnetospheric system.  A nested grid system was used to get the finest resolution and least amount of numerical diffusion near Jupiter and Io.  Multi-fluid simulations have a plethora of benefits, especially with respect to a complicated system like Jupiter's where there are several high mass ion species dominating the energy and momentum transport of the inner and most likely outer magnetosphere.  This phenomenon is due to the rapid rotation of Jupiter and its magnetosphere, which preferentially accelerates more massive ion species.  It allows one to examine the differential acceleration and heating between the heavy and light ion species, and  follow their flow trajectories.  Below are a few examples of what can be examined with the multi-fluid simulation.    




Side view of the magnetic field lines
around Jupiter with highlighted flux tubes
representative of those mapping to
the Galilean satellites.

A figure looking at the pole of Jupiter,
showing the bulk fluid flow with
co-rotation and the Parker spiral.
A 3-D density and flow plot for O +
complete with resolved Io plasma
torus, corotion out to ~16RJ and
a distinct shear between inner and
outer torus flows at about 5RJ.

A 3-D density and flow plot for  H+.  
Note similar coration features to the O+
and a similar polar jet.

A 3-D density and flow plot for
the solar wind, note that the cusp flow
does not actually reach Jupiter, but is
turned around well above the planet.

A 2-D density contour for O +
with Io (Io not to scale), demonstrating
the initialized torus did not drift after
running the simulation.

A 2-D density contour for H + shows
centrifugal forces at work due to
Jupiter's rapid rotation and corotation
of its magnetosphere out to ~16RJ.



Who's Doing It:


Geophysics Main Page | Program InformationSolid EarthNear-Surface | Space Physics

Modeling the Jovian Magnetospheric System / 28 Aug 2002 / winglee@geophys.washington.edu