Low-Energy Charged Particles in Saturn's Magnetosphere: Results from Voyager 1
- 10 April 1981
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 212 (4491) , 225-231
- https://doi.org/10.1126/science.212.4491.225
Abstract
The low-energy charged particle instrument on Voyager 1 measured low-energy electrons and ions (energies ≥ 26 and ≥ 40 kiloelectron volts, respectively) in Saturn's magnetosphere. The first-order ion anisotropies on the dayside are generally in the corotation direction with the amplitude decreasing with decreasing distance to the planet. The ion pitch-angle distributions generally peak at 90°, whereas the electron distributions tend to have field-aligned bidirectional maxima outside the L shell of Rhea. A large decrease in particle fluxes is seen near the L shell of Titan, while selective particle absorption (least affecting the lowest energy ions) is observed at the L shells of Rhea, Dione, and Tethys. The phase space density of ions with values of the first invariant in the range ∼ 300 to 1000 million electron volts per gauss is consistent with a source in the outer magnetosphere. The ion population at higher energies (≥ 200 kiloelectron volts per nucleon) consists primarily of protons, molecular hydrogen, and helium. Spectra of all ion species exhibit an energy cutoff at energies ≥ 2 million electron volts. The proton-to-helium ratio at equal energy per nucleon is larger (up to ∼ 5 x 103) than seen in other magnetospheres and is consistent with a local (nonsolar wind) proton source. In contrast to the magnetospheres of Jupiter and Earth, there are no lobe regions essentially devoid of particles in Saturn's nighttime magnetosphere. Electron pitch-angle distributions are generally bidirectional andfield-aligned, indicating closed field lines at high latitudes. Ions in this region are generally moving toward Saturn, while in the magnetosheath they exhibit strong antisunward streaming which is inconsistent with purely convective flows. Fluxes of magnetospheric ions downstream from the bow shock are present over distances ≥ 200 Saturn radii from the planet. Novel features identified in the Saturnian magnetosphere include a mantle of low-energy particles extending inward from the dayside magnetopause to ∼ 17 Saturn radii, at least two intensity dropouts occurring ∼ 11 hours apart in the nighttime magnetosphere, and a pervasive population of energetic molecular hydrogen.Keywords
This publication has 18 references indexed in Scilit:
- Composition of nonthermal ions in the Jovian magnetosphereJournal of Geophysical Research, 1981
- Magnetic Field Studies by Voyager 1: Preliminary Results at SaturnScience, 1981
- Extreme Ultraviolet Observations from Voyager 1 Encounter with SaturnScience, 1981
- Plasmas in Saturn's magnetosphereJournal of Geophysical Research, 1980
- Sources and sinks of energetic electrons and protons in Saturn's magnetosphereJournal of Geophysical Research, 1980
- Saturn's magnetosphere and its interaction with the solar windJournal of Geophysical Research, 1980
- Detection of energetic hydrogen molecules in Jupiter's magnetosphere by Voyager 2: Evidence for an ionospheric plasma sourceGeophysical Research Letters, 1980
- Preliminary Results on the Plasma Environment of Saturn from the Pioneer 11 Plasma Analyzer ExperimentScience, 1980
- The magnetic anomaly model of the Jovian magnetosphere: Predictions for VoyagerGeophysical Research Letters, 1979
- The clouds of VenusSpace Science Reviews, 1977