Role of transport from the auroral zone in the formation of the winter anomaly at midlatitudes of the Northern Hemisphere

Details Role of transport from the auroral zone in the formation of the winter anomaly at midlatitudes of the Northern Hemisphere Role of transport from the auroral zone in the formation of the winter anomaly at midlatitudes of the Northern Hemisphere

Aug 1984

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1984ge%26ae..24..586p&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 24, July-Aug. 1984, p. 586-591. In Russian.

Physics

Atmospheric Circulation, Auroral Zones, Ionospheric Electron Density, Northern Hemisphere, Winter, Anomalies, Arctic Regions, D Region

Scientific paper

An analysis of radio-meteor wind data indicates that the mechanism of
active-admixture transport from auroral latitudes to midlatitudes is
significant in the formation of the winter anomaly in the D-region. The
analysis of this mechanism employs actual parameters of the wind field
characteristic for winter-anomaly heights.

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