The Dynamics of the Mesosphere and Lower Thermosphere at Saskatoon (52°N)
Open Access
- 1 February 1986
- journal article
- Published by American Meteorological Society in Journal of the Atmospheric Sciences
- Vol. 43 (3) , 276-284
- https://doi.org/10.1175/1520-0469(1986)043<0276:tdotma>2.0.co;2
Abstract
The dynamics of the upper Middle Atmosphere (60–110 km) over Saskatoon (52°N, 107°W) are described, using wind data from a medium frequency radar (2.2 MHz). Seasonal variations of gravity wave intensities (8 h-10 min) and tidal amplitudes and wavelengths (24 h-8 h) are considered. Below ∼80 km, gravity wave amplitudes are larger (≲100%) in winter than in summer months and there are equinoctial minima especially for short periods: tidal amplitudes are also slightly larger (∼40%) in winter, but wavelengths are comparable with season. Between 80 and 95 km seasonal variations of gravity wave amplitudes are small, but above that height winter values are 40–100% greater. The tidal amplitudes vary in similar fashion, mainly due to large semidiurnal tides above ∼90 km. Winter tidal wavelengths also tend to be shorter than in summer above 80 km altitude. These results are compared with recent data from other middle to high-latitude radar observatories: Monpazier (44°N), Christchurch (44°S), Poker Flat (65... Abstract The dynamics of the upper Middle Atmosphere (60–110 km) over Saskatoon (52°N, 107°W) are described, using wind data from a medium frequency radar (2.2 MHz). Seasonal variations of gravity wave intensities (8 h-10 min) and tidal amplitudes and wavelengths (24 h-8 h) are considered. Below ∼80 km, gravity wave amplitudes are larger (≲100%) in winter than in summer months and there are equinoctial minima especially for short periods: tidal amplitudes are also slightly larger (∼40%) in winter, but wavelengths are comparable with season. Between 80 and 95 km seasonal variations of gravity wave amplitudes are small, but above that height winter values are 40–100% greater. The tidal amplitudes vary in similar fashion, mainly due to large semidiurnal tides above ∼90 km. Winter tidal wavelengths also tend to be shorter than in summer above 80 km altitude. These results are compared with recent data from other middle to high-latitude radar observatories: Monpazier (44°N), Christchurch (44°S), Poker Flat (65...Keywords
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