Other
Scientific paper
Oct 1992
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992adspr..12..107n&link_type=abstract
(The earth's middle and upper atmosphere; Proceedings of the Topical Meeting of the Interdisciplinary Scientific Commission C /M
Other
1
Atmospheric Tides, Eiscat Radar System (Europe), Gravity Waves, Incoherent Scatter Radar, Thermosphere, Electron Density (Concentration), F Region, Field Aligned Currents, Vertical Distribution, Wind (Meteorology)
Scientific paper
Studies of the atmospheric tides and gravity waves at 70 deg N were made with the EISCAT incoherent scatter radar on 3, 4 and 8 Aug. 1988. This paper discusses measurements of the electron density and the field-aligned velocity, which is related to the horizontal meridional neutral-air wind. The phase of the 12 h oscillation in the neutral wind behaves smoothly with height on 3 Aug., but abrupt phase changes at 120 and 130 km are observed on 4 and 8 Aug., respectively. At lower heights the vertical wavelength of the 12 h oscillation is about 45 km, which corresponds to the (2, 4) component of the semidiurnal tide. On 4 Aug. the vertical wavelength above 120 km altitude is about 200 km, which most probably indicates the dominance of the (2, 2) mode. On the other hand, the phase above 130 km on 8 Aug. and in the F-region on 4 Aug. is nearly constant. The amplitude of the 12 h oscillation is quite variable from day to day, but it has a maximum at 100-110 km, which also speaks for the dominance of the (2, 4) mode. In the F-region above 150 km, complex patterns of gravity waves are observed on all three days, which break up into discrete frequency ranges when subjected to filtering. The day-to-day variability of the 12 h oscillation may be due to interaction between the semidiurnal tide and the gravity waves.
Huuskonen Asko
Lanchester B. S.
Nygrén T.
Rishbeth Henry
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