The Structure of the warped Io Plasma Torus constrained by the Io Footprint
Stephan Schlegel, Joachim Saur

TL;DR
This study uses Hubble observations and magnetic field models to refine the understanding of the Io plasma torus's structure, demonstrating that a warped multipole magnetic field model better explains the data than a simple dipole model.
Contribution
The paper introduces a method to constrain the Io plasma torus structure using Hubble data and a multipole magnetic field model, improving the fit over traditional dipole assumptions.
Findings
Warped multipole model improves fit by 25% over dipole model.
Peak plasma densities are between 1830 and 2032 particles/cm³.
Multipole moments significantly affect Io's plasma environment.
Abstract
Standard models of force balance along Jovian field lines predict the location of the Io plasma torus to be the centrifugal equator of Jupiter's magnetosphere, i.e. the position along the magnetic field lines farthest away from Jupiter's rotational axis. In many models, the centrifugal equator is assumed to lay on a plane, calculated from a (shifted) dipole magnetic field, rather than on a warped surface which incorporates Jupiter's higher magnetic field moments. In this work, we use Hubble Space Telescope observations of the Io Main Footprint to constrain density, scale height and lateral position of the Io Plasma Torus. Therefore, we employ the leading angle of the footprints to calculate expected travel times of Alfven waves and carry out an inversion of the observations. For the magnetic field we use the JRM33 magnetic field model. The inversion results show peak densities between…
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Taxonomy
TopicsAstro and Planetary Science · Ionosphere and magnetosphere dynamics · Geomagnetism and Paleomagnetism Studies
