Surface hazards in North-west Europe following sudden stratospheric warming events

Sudden stratospheric warmings (SSWs) have been linked to surface temperature anomalies, but how these connect to changes in the likelihood of specific weather extremes and their associated weather patterns remains uncertain. While, on average, it is true that cold surface temperatures follow SSW eve...

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Main Authors: Richard J Hall, Dann M Mitchell, William J M Seviour, Corwin J Wright
Format: Article
Language:English
Published: IOP Publishing 2023-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/acd0c3
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author Richard J Hall
Dann M Mitchell
William J M Seviour
Corwin J Wright
author_facet Richard J Hall
Dann M Mitchell
William J M Seviour
Corwin J Wright
author_sort Richard J Hall
collection DOAJ
description Sudden stratospheric warmings (SSWs) have been linked to surface temperature anomalies, but how these connect to changes in the likelihood of specific weather extremes and their associated weather patterns remains uncertain. While, on average, it is true that cold surface temperatures follow SSW events, particularly in Northern Europe, there is considerable event-to-event variability. Over the British Isles and Central Europe, only around 45% of SSWs are followed by a colder than average period and a negative phase of the North Atlantic Oscillation, cautioning against an over-generalised approach to surface anomalies associated with SSWs. Focussing on more hazardous weather, which in winter is associated with cold extremes, we use reanalysis data to consider how SSWs impact temperature-related hazards; namely the frequency of snowy days, frost days and spells of extreme cold weather in 12 major European cities. In general, SSWs are associated with an increased risk of snow across most of western Europe, and that this is particularly significant in milder, more maritime locations such as London where in reanalysis, snowfall days are 40% more likely after an SSW. However, there is considerable variation in surface temperature anomalies between SSW events; the third of SSWs with the warmest surface anomalies are statistically more likely to have a decreased risk of snow, frost and persistent cold spells compared with non-SSW time periods. These warmer events are associated with a different temperature anomaly pattern, which is consistent in both reanalysis data and large ensemble CMIP6 models. We further show that these warm surface temperature anomaly SSWs are becoming more frequent, a trend which is consistent with background global warming. The varied surface anomalies associated with SSWs highlights the need to study their impacts in a probabilistic sense, and motivates further work to enable better prediction of the impacts of a given event.
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spelling doaj.art-dc3464e1da574259acca62d9fbeeb28c2023-08-09T15:15:41ZengIOP PublishingEnvironmental Research Letters1748-93262023-01-0118606400210.1088/1748-9326/acd0c3Surface hazards in North-west Europe following sudden stratospheric warming eventsRichard J Hall0https://orcid.org/0000-0003-4840-383XDann M Mitchell1William J M Seviour2Corwin J Wright3School of Geographical Sciences, University of Bristol , Bristol, United Kingdom; Cabot Institute for the Environment, University of Bristol , Bristol, United KingdomSchool of Geographical Sciences, University of Bristol , Bristol, United Kingdom; Cabot Institute for the Environment, University of Bristol , Bristol, United KingdomGlobal Systems Institute and Department of Mathematics, University of Exeter , Exeter, United KingdomCentre for Space, Atmospheric and Oceanic Science, University of Bath , Bath, United KingdomSudden stratospheric warmings (SSWs) have been linked to surface temperature anomalies, but how these connect to changes in the likelihood of specific weather extremes and their associated weather patterns remains uncertain. While, on average, it is true that cold surface temperatures follow SSW events, particularly in Northern Europe, there is considerable event-to-event variability. Over the British Isles and Central Europe, only around 45% of SSWs are followed by a colder than average period and a negative phase of the North Atlantic Oscillation, cautioning against an over-generalised approach to surface anomalies associated with SSWs. Focussing on more hazardous weather, which in winter is associated with cold extremes, we use reanalysis data to consider how SSWs impact temperature-related hazards; namely the frequency of snowy days, frost days and spells of extreme cold weather in 12 major European cities. In general, SSWs are associated with an increased risk of snow across most of western Europe, and that this is particularly significant in milder, more maritime locations such as London where in reanalysis, snowfall days are 40% more likely after an SSW. However, there is considerable variation in surface temperature anomalies between SSW events; the third of SSWs with the warmest surface anomalies are statistically more likely to have a decreased risk of snow, frost and persistent cold spells compared with non-SSW time periods. These warmer events are associated with a different temperature anomaly pattern, which is consistent in both reanalysis data and large ensemble CMIP6 models. We further show that these warm surface temperature anomaly SSWs are becoming more frequent, a trend which is consistent with background global warming. The varied surface anomalies associated with SSWs highlights the need to study their impacts in a probabilistic sense, and motivates further work to enable better prediction of the impacts of a given event.https://doi.org/10.1088/1748-9326/acd0c3hazardssudden stratospheric warmingssurface weather impactsweather patterns
spellingShingle Richard J Hall
Dann M Mitchell
William J M Seviour
Corwin J Wright
Surface hazards in North-west Europe following sudden stratospheric warming events
Environmental Research Letters
hazards
sudden stratospheric warmings
surface weather impacts
weather patterns
title Surface hazards in North-west Europe following sudden stratospheric warming events
title_full Surface hazards in North-west Europe following sudden stratospheric warming events
title_fullStr Surface hazards in North-west Europe following sudden stratospheric warming events
title_full_unstemmed Surface hazards in North-west Europe following sudden stratospheric warming events
title_short Surface hazards in North-west Europe following sudden stratospheric warming events
title_sort surface hazards in north west europe following sudden stratospheric warming events
topic hazards
sudden stratospheric warmings
surface weather impacts
weather patterns
url https://doi.org/10.1088/1748-9326/acd0c3
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AT corwinjwright surfacehazardsinnorthwesteuropefollowingsuddenstratosphericwarmingevents