Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Ion cyclotron waves in the Io plasma torus: polarization reversal of whistler mode noise. Revision. Progess report

Technical Report ·
OSTI ID:5811789
Because of the presence of multiple ion species in the Io plasma torus whistler mode noise can be converted to ion cyclotron waves via a polarization reversal process at the local crossover frequency. Using whistler mode intensity measurements in the Jovian magnetosphere from Voyager 1 we estimate the pitch-angle diffusion rates that would occur if the noise is converted to ion cyclotron waves. Typical pitch-angle diffusion coefficients range from D sub alpha alpha approx. = 1/1000000 sec for protons resonating near the equator to D sub alpha alpha approx = 1/10000 sec for 10 keV 0(+) ions resonating at high latitudes. Although complete bounce averaged diffusion coefficients have not yet been computed, preliminary estimates indicate that the energetic ion precipitation caused by these wave may be able to account for the EUV auroral emissions at the foot of the torus field lines.
Research Organization:
Iowa Univ., Iowa City (USA). Dept. of Physics and Astronomy
OSTI ID:
5811789
Report Number(s):
AD-A-129873/6
Country of Publication:
United States
Language:
English

Similar Records

Detection of Jovian whistler mode chorus; implications for the Io torus aurora
Journal Article · Mon Dec 31 23:00:00 EST 1979 · Geophys. Res. Lett.; (United States) · OSTI ID:5391650

Diffuse Jovian aurora influenced by plasma injection from IO
Journal Article · Wed Aug 01 00:00:00 EDT 1979 · Geophys. Res. Lett.; (United States) · OSTI ID:5939281

Pitch-angle diffusion by whistler mode waves near the Io plasma torus
Journal Article · Wed Aug 01 00:00:00 EDT 1979 · Geophys. Res. Lett.; (United States) · OSTI ID:5939269