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- W1971239969 abstract "Abstract During two 24 h periods of EISCAT observations in the summer of 1982, the F-region ion temperature and density responded differently before and after midnight to large ion convective flows. Such observations were recently reported at Chatanika (Alaska), however, the mechanism invoked to interpret these measurements (large day-to-night variation in electron density affecting the coupling between ions and neutrals) appears insufficient, for summer conditions, to account for the EISCAT observations. Hence, it is proposed, with the support of Fabry-Perot observations and numerical models, that in addition to the electron density asymmetry, the presence of a large southward neutral wind around midnight induces, through Coriolis coupling, a zonal neutral wind of an opposite direction to the convective flow. This enhances considerably the frictional energy and momentum transfer between ions and neutrals in the post-midnight sector." @default.
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- W1971239969 date "1984-06-01" @default.
- W1971239969 modified "2023-09-27" @default.
- W1971239969 title "Dynamical coupling of the auroral F-region ionosphere and thermosphere: case studies" @default.
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- W1971239969 doi "https://doi.org/10.1016/0021-9169(84)90080-1" @default.
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