Abstract
The Arctic stratosphere winter season of 2020–2021 was characterized by a weakened stratospheric polar vortex as a result of a major sudden stratospheric warming (SSW) in early January. After the SSW, which persisted for about 3 weeks, and until the end of the winter season, the lower stratosphere temperature inside the stratospheric polar vortex remained higher than required for the formation of polar stratospheric clouds.
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Funding
This study was supported by the Russian Foundation for Basic Research, grants nos. 19–05-00370 (P.N. Vargin and A.N. Lukyanov) and 20-55-00014 Bel_a (V.V. Guryanov).
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Translated by N. Tretyakova
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Vargin, P.N., Guryanov, V.V., Lukyanov, A.N. et al. Dynamic Processes of the Arctic Stratosphere in the 2020–2021 Winter. Izv. Atmos. Ocean. Phys. 57, 568–580 (2021). https://doi.org/10.1134/S0001433821060098
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DOI: https://doi.org/10.1134/S0001433821060098