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A large Vertical Wind in the thermosphere at the Auroral Oval/Polar Cap Boundary seen simultaneously from Mawson and Davis, Antarctica. Journal of Atmospheric and Solar-Terrestial Physics, 1999 (Ref: 8819)
Category 1: Peer-reviewed literature

Ground-based Fabry-Perot spectrometer observations from the Australian Antarctic stations of Davis and Mawson show an upward wind ~100 m s-1 in the thermosphere at ~240 km altitude on the night of Day of Year 159 in 1997.

Thermospheric wind field over Mawson and Davis, Antarctica; simultaneous observations by two Fabry-Perot spectrometers of l630 nm emission. Journal of Atmospheric and Solar-Terrestrial Physics., 1999 (Ref: 8818)
Category 1: Peer-reviewed literature

The thermopheric oxygen l630 nm emission has been observed using high-resolution Fabry-Perot spectrometers at Mawson (67.6°S, 62.9°E) and Davis (68.6°S, 78.0°E), Antarctica. A new technique, combining the results from the two instruments, is used to derive vector wind fields.

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