Comparison of the Jovian north and south pole aurorae using the IUE observatory
- 1 November 1984
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 11 (11) , 1107-1110
- https://doi.org/10.1029/gl011i011p01107
Abstract
New results on the spatial and temporal variability of the auroral emissions from Jupiter have been obtained from three IUE observations of the south pole made during the period July 1983 to March 1984. The current observations, together with previous IUE studies of the north pole aurora, provide convincing evidence for persistent longitudinal asymmetries in the Jovian auroral emissions. The strongest emissions appear to originate from regions centered near λIII ∼ 0° at the south pole and λIII ∼ 185° at the north pole. Differences in surface magnetic field strength seem inadequate to explain the extent to which particles precipitating along field lines into a given longitude sector in one hemisphere are inhibited from precipitating along the same field lines into the opposite hemisphere. Thus, the IUE auroral results present a challenge to existing models of auroral production.This publication has 7 references indexed in Scilit:
- Jovian magnetospheric neutral wind and auroral precipitation fluxJournal of Geophysical Research, 1984
- IUE observations of longitudinal and temporal variations in the Jovian auroral emissionThe Astrophysical Journal, 1984
- Energetic oxygen and sulfur ions in the Jovian magnetosphere and their contribution to the auroral excitationJournal of Geophysical Research, 1983
- Magnetospheric modelsPublished by Cambridge University Press (CUP) ,1983
- H2 fluorescence spectrum from 1200 to 1700 A by electron impact - Laboratory study and application to Jovian auroraThe Astrophysical Journal, 1982
- Modeling the Jovian current sheet and inner magnetosphereJournal of Geophysical Research, 1981
- Composition and thermal profiles of the Jovian upper atmosphere determined by the Voyager Ultraviolet Stellar Occultation ExperimentJournal of Geophysical Research, 1981