Paper
18 December 2019 Influence of the upward wave activity flux in the winter 2012/2013 on the Arctic polar vortex
Vladimir V. Zuev, Ekaterina S. Savelieva
Author Affiliations +
Proceedings Volume 11208, 25th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics; 112088M (2019) https://doi.org/10.1117/12.2535587
Event: XXV International Symposium, Atmospheric and Ocean Optics, Atmospheric Physics, 2019, Novosibirsk, Russian Federation
Abstract
One of the most prominent features of the Arctic polar vortex is its large interannual variability associated with a high frequency of occurrence of sudden stratospheric warmings (SSWs). SSWs appear due to the breaking and dissipation of planetary Rossby waves, propagating from the troposphere into the stratosphere, as a result of interaction with the westerly zonal flow (i.e. the stratospheric polar vortex). In this study, we analyze the dynamics of the Arctic polar vortex under the influence of the anomalous upward wave activity flux in the winter 2012/2013.
© (2019) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
Vladimir V. Zuev and Ekaterina S. Savelieva "Influence of the upward wave activity flux in the winter 2012/2013 on the Arctic polar vortex", Proc. SPIE 11208, 25th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics, 112088M (18 December 2019); https://doi.org/10.1117/12.2535587
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KEYWORDS
Stratosphere

Climatology

Heat flux

Wave propagation

Ozone

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