Physics
Scientific paper
Jul 1979
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1979jgr....84.3283c&link_type=abstract
Journal of Geophysical Research, vol. 84, July 1, 1979, p. 3283-3290. Research sponsored by the Aerospace Corp.;
Physics
1
Equatorial Atmosphere, F Region, Ionospheric Drift, Night Sky, Perturbation Theory, Taylor Instability, Wind Effects, E Region, Graphs (Charts), Ion Recombination, Ionospheric Disturbances, Molecular Ions, Positive Ions
Scientific paper
A thorough re-examination has been made of the Rayleigh-Taylor instability in the nighttime equatorial ionosphere from approximately 100 km to the bottomside F region. The following effects have been taken into account explicitly in various combinations: (1) the eastward drift of the ionosphere caused by the nighttime polarization electric field, (2) the eastward nighttime neutral wind, and (3) recombination in the F and E regions. It was found that, well below the bottomside F region, the Rayleigh-Taylor mode can be unstable and is driven by an eastward neutral wind rather than by gravitational drift. Formation of ionospheric bubbles below the bottomside F region is consistent with the observation of lower ionospheric ions in F region ionospheric holes; furthermore, seasonal and shorter term variations in spread-F occurrence may be associated with variations in the neutral wind and polarization electric field.
Chiu Yam T.
Straus J. M.
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