An observational study of the D-region winter anomaly and sudden stratospheric warmings

Physics

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Atmospheric Temperature, D Region, Electromagnetic Absorption, Ionospheric Disturbances, Stratosphere, Stratospheric Warming, Anomalies, Ionospheric Electron Density, Mesosphere, Nitric Oxide, Planetary Waves, Radio Waves, Temperature Effects, Winter

Scientific paper

An observational study of the link between the winter anomaly in ionospheric absorption and sudden stratospheric warmings for the 1967/1968 winter has been made. On the basis of the daily large-scale distributions of the absorption index, it is found that the winter anomaly during sudden warming could result from a NO increase induced by southward transport from the polar region, where NO is most abundant, associated with a well-developed vortex in the D-region (large amplitude planetary wave).

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