Preprints
https://doi.org/10.5194/egusphere-2025-976
https://doi.org/10.5194/egusphere-2025-976
07 Mar 2025
 | 07 Mar 2025

The impact of tropospheric blockings on duration of the sudden stratospheric warmings in boreal winter 2023/24

Ekaterina Vorobeva and Yvan Orsolini

Abstract. The winter 2023/24 exhibited remarkable stratospheric dynamics with multiple sudden stratospheric warmings (SSWs). Based on the fifth generation European Centre for Medium-Range Weather Forecasts (ECMWF) reanalysis (ERA5) polar-cap averaged 10 hPa zonal wind, three major SSWs are identified – an extremely rare occurrence in a single winter. Two of three SSWs were short-lived, lasting under 7 days. In this study, we give an overview of the three SSWs that occurred in winter 2023/24 and focus on the impact of tropospheric forcing on their duration. Blocking high-pressure systems are shown to modulate wave activity flux into the stratosphere through interactions with tropospheric planetary waves, depending on their location. The rapid termination of the first SSW (14–19 January 2024) is linked to a developing high-pressure system over the North Pacific. The second SSW (16–22 February 2024) terminated quickly due to more contributing factors, one of which was a high-pressure system developed over the Far East. The third SSW (3–28 March 2024) was a long-duration canonical event extending to levels below 100 hPa. In contrast to two short-lived SSWs in winter 2023/24, the tropospheric forcing was sustained around the SSW onset in March 2024, allowing a long event to develop. We also note that conditions for these SSWs were particularly favorable due to external factors, including an Easterly Quasi-Biennial Oscillation (QBO), the presence of El Niño conditions of the ENSO cycle, and the proximity to the solar maximum.

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Journal article(s) based on this preprint

26 Sep 2025
The impact of tropospheric blocking on the duration of the sudden stratospheric warmings in boreal winter 2023/24
Ekaterina Vorobeva and Yvan Orsolini
Weather Clim. Dynam., 6, 1015–1026, https://doi.org/10.5194/wcd-6-1015-2025,https://doi.org/10.5194/wcd-6-1015-2025, 2025
Short summary
Ekaterina Vorobeva and Yvan Orsolini

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-976', Anonymous Referee #1, 05 Apr 2025
  • RC2: 'Comment on egusphere-2025-976', Anonymous Referee #2, 20 Apr 2025
  • EC1: 'Comment on egusphere-2025-976', Amy Butler, 09 Jun 2025

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-976', Anonymous Referee #1, 05 Apr 2025
  • RC2: 'Comment on egusphere-2025-976', Anonymous Referee #2, 20 Apr 2025
  • EC1: 'Comment on egusphere-2025-976', Amy Butler, 09 Jun 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Ekaterina Vorobeva on behalf of the Authors (16 Jun 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (17 Jun 2025) by Amy Butler
RR by Anonymous Referee #2 (19 Jun 2025)
RR by Anonymous Referee #1 (04 Jul 2025)
ED: Publish subject to technical corrections (07 Jul 2025) by Amy Butler
AR by Ekaterina Vorobeva on behalf of the Authors (14 Jul 2025)  Author's response   Manuscript 

Journal article(s) based on this preprint

26 Sep 2025
The impact of tropospheric blocking on the duration of the sudden stratospheric warmings in boreal winter 2023/24
Ekaterina Vorobeva and Yvan Orsolini
Weather Clim. Dynam., 6, 1015–1026, https://doi.org/10.5194/wcd-6-1015-2025,https://doi.org/10.5194/wcd-6-1015-2025, 2025
Short summary
Ekaterina Vorobeva and Yvan Orsolini
Ekaterina Vorobeva and Yvan Orsolini

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Short summary
The factors behind why some polar stratospheric wind disturbances persist while others remain short are unclear. This study examines the impact of tropospheric high-pressure systems on the duration of three recent polar stratospheric wind disturbances in winter 2023/24. Two were short-lived, lasting under seven days. Findings in this study show that two short disturbances could not develop into long-lasting events due to developing high-pressure systems over the planetary waves troughs.
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