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- W2080641311 abstract "Abstract Long duration incoherent-scatter data from the Chatanika radar have been analyzed to obtain the meridional component of the neutral wind in the sunlit F -layer thermosphere. In the cases examined, the meridional wind exhibits a southward surge of 150 to 500 m/s around local midnight. Joule heating does not account for the surge because the surge occurs close to local midnight in each of the cases examined, whereas the onset time of appreciable local heating varies from 3 to 6 h earlier. The magnitude of the surge correlates highly with planetary magnetic activity. It has been proposed by others that the ionospheric electric field sets up two great counter-rotating convection vortices in the polar cap thermosphere at altitudes near the sunlit F -layer maximum. The surge is concluded to be the result of the passage over the radar of the narrow region of southward wind dividing the vortices. The midnight surge may be a daily source of thermospheric waves as the Earth rotates beneath it." @default.
- W2080641311 created "2016-06-24" @default.
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- W2080641311 date "1977-01-01" @default.
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- W2080641311 title "The southward midnight surge in F-layer wind observed with the Chatanika incoherent scatter radar" @default.
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- W2080641311 doi "https://doi.org/10.1016/0021-9169(77)90047-2" @default.
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