All Physics Faculty Publications
Document Type
Article
Journal/Book Title/Conference
Journal of Geophysical Research: Space Physics
Volume
91
Issue
A3
Publisher
American Geophysical Union
Publication Date
1986
First Page
3245
Last Page
3253
Abstract
The origins, transport, and decay of large-scale (≳ 10 km) F region density irregularities were theoretically studied using a high-latitude time dependent ionospheric model. Such density irregularities (blobs) have been found both in the polar cap and the auroral zone. The model study, which focuses on blobs being produced by auroral precipitation, shows that the observed energy fluxes can readily account for the blob densities if a plasma flux tube is exposed to the precipitation for 5-10 min. Once the flux tube is transported away from the source, the F region density profile recovers its shape on a time scale of 10-20 min. Hence after this time period it is not possible to determine whether hard or soft precipitation was the source of the blob. Once created a blob will maintain its relative size for many hours, since it decays at the same rate as the background plasma. Blobs are removed by being transported into a region of high production, where the new background density exceeds the old blob density. The high hmF2’s observed with some blobs need not necessarily imply soft precipitation; induced upward plasma drifts from neural winds or E×B convection can readily account for them. Since the high latitude ionosphere contains discrete auroral forms in the oval and polar cap and since plasma is continually convecting through these regions, blobs are the rule rather than the exception.
Recommended Citation
Sojka, J. J., and R. W. Schunk (1986), A Theoretical Study of the Production and Decay of Localized Electron Density Enhancements in the Polar Ionosphere, J. Geophys. Res., 91(A3), 3245–3253, doi:10.1029/JA091iA03p03245.
Comments
Originally published by the American Geophysical Union. Abstract available online through the Journal of Geophysical Research: Space Physics.