The 2018-19 Arctic stratospheric polar vortex

The stratospheric polar vortex is a westerly circulation that forms over the winter pole around 10-50 km above the surface, which is known to influence mid-latitude weather patterns. During 2018-19, the Arctic polar vortex demonstrated an unusually large amount of variability, including a strong and...

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Published in:Weather
Main Authors: Lee, Simon H., Butler, Amy H.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2020
Subjects:
Online Access:https://centaur.reading.ac.uk/87110/
https://centaur.reading.ac.uk/87110/1/lee_butler_weather_accepted.pdf
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spelling ftunivreading:oai:centaur.reading.ac.uk:87110 2024-05-19T07:33:04+00:00 The 2018-19 Arctic stratospheric polar vortex Lee, Simon H. Butler, Amy H. 2020-02 text https://centaur.reading.ac.uk/87110/ https://centaur.reading.ac.uk/87110/1/lee_butler_weather_accepted.pdf en eng Wiley https://centaur.reading.ac.uk/87110/1/lee_butler_weather_accepted.pdf Lee, S. H. and Butler, A. H. (2020) The 2018-19 Arctic stratospheric polar vortex. Weather, 75 (2). pp. 52-57. ISSN 0043-1656 doi: https://doi.org/10.1002/wea.3643 <https://doi.org/10.1002/wea.3643> Article PeerReviewed 2020 ftunivreading https://doi.org/10.1002/wea.3643 2024-05-01T00:23:28Z The stratospheric polar vortex is a westerly circulation that forms over the winter pole around 10-50 km above the surface, which is known to influence mid-latitude weather patterns. During 2018-19, the Arctic polar vortex demonstrated an unusually large amount of variability, including a strong and persistent sudden stratospheric warming (SSW) event, a strong vortex event, and a dynamic final stratospheric warming (FSW). In this article we discuss the evolution of the vortex, placing it in the context of wider observed climatology, and comment on its apparent impacts on tropospheric weather patterns – notably, the lack of a surface climate response to the SSW of similar magnitude to the February-March 2018 “Beast from the East” cold-wave. Article in Journal/Newspaper Arctic Arctic CentAUR: Central Archive at the University of Reading Weather 75 2 52 57
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collection CentAUR: Central Archive at the University of Reading
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language English
description The stratospheric polar vortex is a westerly circulation that forms over the winter pole around 10-50 km above the surface, which is known to influence mid-latitude weather patterns. During 2018-19, the Arctic polar vortex demonstrated an unusually large amount of variability, including a strong and persistent sudden stratospheric warming (SSW) event, a strong vortex event, and a dynamic final stratospheric warming (FSW). In this article we discuss the evolution of the vortex, placing it in the context of wider observed climatology, and comment on its apparent impacts on tropospheric weather patterns – notably, the lack of a surface climate response to the SSW of similar magnitude to the February-March 2018 “Beast from the East” cold-wave.
format Article in Journal/Newspaper
author Lee, Simon H.
Butler, Amy H.
spellingShingle Lee, Simon H.
Butler, Amy H.
The 2018-19 Arctic stratospheric polar vortex
author_facet Lee, Simon H.
Butler, Amy H.
author_sort Lee, Simon H.
title The 2018-19 Arctic stratospheric polar vortex
title_short The 2018-19 Arctic stratospheric polar vortex
title_full The 2018-19 Arctic stratospheric polar vortex
title_fullStr The 2018-19 Arctic stratospheric polar vortex
title_full_unstemmed The 2018-19 Arctic stratospheric polar vortex
title_sort 2018-19 arctic stratospheric polar vortex
publisher Wiley
publishDate 2020
url https://centaur.reading.ac.uk/87110/
https://centaur.reading.ac.uk/87110/1/lee_butler_weather_accepted.pdf
genre Arctic
Arctic
genre_facet Arctic
Arctic
op_relation https://centaur.reading.ac.uk/87110/1/lee_butler_weather_accepted.pdf
Lee, S. H. and Butler, A. H. (2020) The 2018-19 Arctic stratospheric polar vortex. Weather, 75 (2). pp. 52-57. ISSN 0043-1656 doi: https://doi.org/10.1002/wea.3643 <https://doi.org/10.1002/wea.3643>
op_doi https://doi.org/10.1002/wea.3643
container_title Weather
container_volume 75
container_issue 2
container_start_page 52
op_container_end_page 57
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