Physics
Scientific paper
Jun 1989
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989jgr....94.6517h&link_type=abstract
Journal of Geophysical Research (ISSN 0148-0227), vol. 94, June 1, 1989, p. 6517-6522.
Physics
18
Dynamo Theory, Planetary Ionospheres, Ultraviolet Radiation, Uranus Atmosphere, Elastic Scattering, Electron Acceleration, Field Aligned Currents, Ionization Cross Sections, Photoelectrons, Scattering Cross Sections, Uranus, Ionosphere, Dynamo, Ultraviolet, Wavelengths, Emissions, Origin, Formation, Electroglow, Lyman-Alpha Radiation, Acceleration, Giant Planets, Electrons, Diagrams, Currents, Electrical Properties, Magnetic Fields, Calculations, Homopause, Models, Electrical Fields
Scientific paper
A model is presented to explain diffuse FUV emissions from the outer planets, specifically Uranus, in excess of those diffuse emissions that are currently explainable by scattering of sunlight and/or excitation by photoelectrons. These electroglow emissions in H Ly-alpha and H2 bands, which occur in the sunlit hemisphere slightly above the homopause, appear to require particle excitation in the 10- to 50-eV range. An in situ mechanism for accelerating photoelectrons (and ions is proposed, involving neutral wind dynamo generation of field-aligned currents analogous to what occurs in the earth's equatorial E and F regions. Sufficiently strong field-aligned currents are found in the model calculation for Uranus to produce a potential drop of about 100 eV or greater between the F peak and homopause, concentrated at lower altitudes, and capable in principle of accelerating photoelectrons (and ions) to the 10- to 50-eV energies required to explain the observed emissions. The fact that the excitation and ionization cross sections are larger than elastic scattering cross sections in an H2 atmosphere at these energies makes in situ acceleration feasible for the production of UV on the outer planets.
Clarke John T.
Hudson Mary K.
Warren James A.
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