Mechanisms and predictability of sudden stratospheric warming in winter 2018

In the beginning of February 2018 a rapid deceleration of the westerly circulation in the polar Northern Hemisphere stratosphere took place, and on 12 February the zonal-mean zonal wind at 60 ∘ N and 10 hPa reversed to easterly in a sudden stratospheric warming (SSW) event. We investigate the role o...

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Published in:Weather and Climate Dynamics
Main Authors: Statnaia, Irina A., Karpechko, Alexey Y., Järvinen, Heikki J.
Format: Text
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.5194/wcd-1-657-2020
https://wcd.copernicus.org/articles/1/657/2020/
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spelling ftcopernicus:oai:publications.copernicus.org:wcd85272 2023-05-15T18:41:27+02:00 Mechanisms and predictability of sudden stratospheric warming in winter 2018 Statnaia, Irina A. Karpechko, Alexey Y. Järvinen, Heikki J. 2020-10-27 application/pdf https://doi.org/10.5194/wcd-1-657-2020 https://wcd.copernicus.org/articles/1/657/2020/ eng eng doi:10.5194/wcd-1-657-2020 https://wcd.copernicus.org/articles/1/657/2020/ eISSN: 2698-4016 Text 2020 ftcopernicus https://doi.org/10.5194/wcd-1-657-2020 2020-11-02T17:22:14Z In the beginning of February 2018 a rapid deceleration of the westerly circulation in the polar Northern Hemisphere stratosphere took place, and on 12 February the zonal-mean zonal wind at 60 ∘ N and 10 hPa reversed to easterly in a sudden stratospheric warming (SSW) event. We investigate the role of the tropospheric forcing in the occurrence of the SSW, its predictability and teleconnection with the Madden–Julian oscillation (MJO) by analysing the European Centre for Medium-Range Weather Forecasts (ECMWF) ensemble forecast. The SSW was preceded by significant synoptic wave activity over the Pacific and Atlantic basins, which led to the upward propagation of wave packets and resulted in the amplification of a stratospheric wavenumber 2 planetary wave. The dynamical and statistical analyses indicate that the main tropospheric forcing resulted from an anticyclonic Rossby wave breaking, subsequent blocking and upward wave propagation in the Ural Mountains region, in agreement with some previous studies. The ensemble members which predicted the wind reversal also reasonably reproduced this chain of events, from the horizontal propagation of individual wave packets to upward wave-activity fluxes and the amplification of wavenumber 2. On the other hand, the ensemble members which failed to predict the wind reversal also failed to properly capture the blocking event in the key region of the Urals and the associated intensification of upward-propagating wave activity. Finally, a composite analysis suggests that teleconnections associated with the record-breaking MJO phase 6 observed in late January 2018 likely played a role in triggering this SSW event. Text ural mountains ural mountains Copernicus Publications: E-Journals Pacific Weather and Climate Dynamics 1 2 657 674
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description In the beginning of February 2018 a rapid deceleration of the westerly circulation in the polar Northern Hemisphere stratosphere took place, and on 12 February the zonal-mean zonal wind at 60 ∘ N and 10 hPa reversed to easterly in a sudden stratospheric warming (SSW) event. We investigate the role of the tropospheric forcing in the occurrence of the SSW, its predictability and teleconnection with the Madden–Julian oscillation (MJO) by analysing the European Centre for Medium-Range Weather Forecasts (ECMWF) ensemble forecast. The SSW was preceded by significant synoptic wave activity over the Pacific and Atlantic basins, which led to the upward propagation of wave packets and resulted in the amplification of a stratospheric wavenumber 2 planetary wave. The dynamical and statistical analyses indicate that the main tropospheric forcing resulted from an anticyclonic Rossby wave breaking, subsequent blocking and upward wave propagation in the Ural Mountains region, in agreement with some previous studies. The ensemble members which predicted the wind reversal also reasonably reproduced this chain of events, from the horizontal propagation of individual wave packets to upward wave-activity fluxes and the amplification of wavenumber 2. On the other hand, the ensemble members which failed to predict the wind reversal also failed to properly capture the blocking event in the key region of the Urals and the associated intensification of upward-propagating wave activity. Finally, a composite analysis suggests that teleconnections associated with the record-breaking MJO phase 6 observed in late January 2018 likely played a role in triggering this SSW event.
format Text
author Statnaia, Irina A.
Karpechko, Alexey Y.
Järvinen, Heikki J.
spellingShingle Statnaia, Irina A.
Karpechko, Alexey Y.
Järvinen, Heikki J.
Mechanisms and predictability of sudden stratospheric warming in winter 2018
author_facet Statnaia, Irina A.
Karpechko, Alexey Y.
Järvinen, Heikki J.
author_sort Statnaia, Irina A.
title Mechanisms and predictability of sudden stratospheric warming in winter 2018
title_short Mechanisms and predictability of sudden stratospheric warming in winter 2018
title_full Mechanisms and predictability of sudden stratospheric warming in winter 2018
title_fullStr Mechanisms and predictability of sudden stratospheric warming in winter 2018
title_full_unstemmed Mechanisms and predictability of sudden stratospheric warming in winter 2018
title_sort mechanisms and predictability of sudden stratospheric warming in winter 2018
publishDate 2020
url https://doi.org/10.5194/wcd-1-657-2020
https://wcd.copernicus.org/articles/1/657/2020/
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ural mountains
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op_source eISSN: 2698-4016
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https://wcd.copernicus.org/articles/1/657/2020/
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