Vertical thermospheric winds at the equatorward edge of the auroral oval

Crickmore, R.I; Dudeney, J.R; Rodger, Alan S.. 1991 Vertical thermospheric winds at the equatorward edge of the auroral oval. Journal of Atmospheric and Terrestrial Physics, 53 (6-7). 485-492. 10.1016/0021-9169(91)90076-J

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Official URL: http://dx.doi.org/10.1016/0021-9169(91)90076-J

Abstract/Summary

A study has been made of vertical thermospheric winds in the vicinity of Halley, Antarctica (75.5°S, 26.8°W; L = 4.2). Strong downward winds, up to 50 m s−1, are frequently observed when the station is located under the equatorward edge of the oval. Whether there is a net downwards motion throughout the night is discussed, and it is concluded that this is probable. The consequent effects upon thermospheric composition and ionospheric electron concentration are also discussed, and related to observations made at Halley.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1016/0021-9169(91)90076-J
ISSN:	00219169
Date made live:	27 Mar 2018 10:42 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/519695

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1016/0021-9169(91)90076-J

ISSN:

00219169

Date made live:

27 Mar 2018 10:42 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/519695