The bottomside mid-latitude ionospheric troughLockwood, M. ORCID: https://orcid.org/0000-0002-7397-2172 (1980) The bottomside mid-latitude ionospheric trough. Journal of Atmospheric and Terrestrial Physics, 42 (7). pp. 605-615. ISSN 00219169 Full text not archived in this repository. It is advisable to refer to the publisher's version if you intend to cite from this work. See Guidance on citing. To link to this item DOI: 10.1016/0021-9169(80)90095-1 Abstract/SummaryThe measured power losses and Doppler shifts of h.f. radio waves propagated over a long, west-east, sub-auroral path are found to exhibit features which cannot be explained by simple predictions and models. Both theory and the limited available data indicate that a bottomside F2-layer depletion should be present below the topside mid-latitude trough. Introducing this into the models (using the mean statistical positions of the trough deduced from Alouette I and II soundings) is shown to explain many of these features. From the Doppler shifts and a simple ray-tracing model the height of the depleted F2-peak inside the trough is deduced to be greater than its value outside the trough by an amount of the order of only 30–80 km.
Altmetric Deposit Details University Staff: Request a correction | Centaur Editors: Update this record |