Physics
Scientific paper
Dec 2003
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30wssc9z&link_type=abstract
Geophysical Research Letters, Volume 30, Issue 23, pp. SSC 9-1, CiteID 2225, DOI 10.1029/2003GL018521
Physics
1
Atmospheric Composition And Structure: Thermosphere-Energy Deposition, Magnetospheric Physics: Storms And Substorms, Magnetospheric Physics: Polar Cap Phenomena, Meteorology And Atmospheric Dynamics: Mesospheric Dynamics, Meteorology And Atmospheric Dynamics: Remote Sensing
Scientific paper
An intense space storm occurred on 17-20 April, 2002. The effects of this storm on the mesospheric wind system were observed by two meteor wind radars at Andenes (69N, 16E) and Esrange (68N, 21E). At those locations, neutral winds showed a pattern similar to the ion convection pattern on 17 April for several hours at altitudes of 94-97 km. It is the first time that this kind of wind pattern is detected at such low altitudes. In contrast, winds by a medium frequency radar at Poker Flat (65N, 213E) showed no obvious storm effect, reflecting different responses of the dayside atmosphere and the nightside atmosphere. The ion convection wind pattern at Andenes and Esrange only appeared on the first day of the storm. We hypothesize that this behaviour may be related to a short-lived but prominent electron density enhancement in the local thermosphere on the same day observed by an incoherent scatter radar at Svalbard (78N, 16E).
Clark Rebecca
Mitchell N.
Murayama Yuko
Salah Joseph E.
Singer Wolfgang
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