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Annales Geophysicae An open-access journal of the European Geosciences Union
Ann. Geophys., 35, 711-720, 2017
https://doi.org/10.5194/angeo-35-711-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Regular paper
12 Jun 2017
Exceptionally strong summer-like zonal wind reversal in the upper mesosphere during winter 2015/16
Gunter Stober1, Vivien Matthias1, Christoph Jacobi2, Sven Wilhelm1, Josef Höffner1, and Jorge L. Chau1 1Leibniz Institute of Atmospheric Physics at the University of Rostock, Schlossstr. 6, 18225 Kuehlungsborn, Germany
2Institute for Meteorology, University of Leipzig, Stephanstr. 3, 04103 Leipzig, Germany
Abstract. The 2015/16 Northern Hemisphere winter season was marked by peculiarities in the circulation pattern in the high-latitude mesopause region. Wind measurements from the Andenes (69° N, 13° E) meteor radar show westward winds below 84 km and eastward winds above. This wind pattern in the zonal wind was observable between the end of December 2015 and the end of January 2016, i.e., conditions that are typical for the summer were found during winter. Additional meteor radar measurements at midlatitude stations did not show such a zonal wind reversal but indicate, together with the polar latitude stations, a reversal of the horizontal temperature gradient. This is confirmed by global satellite measurements. Therefore, it is plausible that the polar latitude summer-like zonal wind reversal in December–January is in accordance with the reversed horizontal temperature gradient assuming a thermal wind balance between mid- and polar latitudes. The reversed horizontal temperature gradient itself is induced by stationary planetary waves at lower and midlatitudes in the mesosphere, leading to a weakening of the residual circulation above the European sector.

Citation: Stober, G., Matthias, V., Jacobi, C., Wilhelm, S., Höffner, J., and Chau, J. L.: Exceptionally strong summer-like zonal wind reversal in the upper mesosphere during winter 2015/16, Ann. Geophys., 35, 711-720, https://doi.org/10.5194/angeo-35-711-2017, 2017.
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