Dependence of sudden stratospheric warming type‐transition on preceding North Atlantic Oscillation conditions

Abstract Most sudden stratospheric warming (SSW) events initiate with their centers being displaced from the pole. Some retain their displaced form until termination but some split into two vortices during their course. Here, we show that existence of a transition during the course of the SSW life c...

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Published in:Atmospheric Science Letters
Main Authors: Hyesun Choi, Wookap Choi, Seong‐Joong Kim, Baek‐Min Kim
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2020
Subjects:
Online Access:https://doi.org/10.1002/asl.953
https://doaj.org/article/ed2a58f2c2914f9288b21cba83f761b5
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author Hyesun Choi
Wookap Choi
Seong‐Joong Kim
Baek‐Min Kim
author_facet Hyesun Choi
Wookap Choi
Seong‐Joong Kim
Baek‐Min Kim
author_sort Hyesun Choi
collection Directory of Open Access Journals: DOAJ Articles
container_issue 3
container_title Atmospheric Science Letters
container_volume 21
description Abstract Most sudden stratospheric warming (SSW) events initiate with their centers being displaced from the pole. Some retain their displaced form until termination but some split into two vortices during their course. Here, we show that existence of a transition during the course of the SSW life cycle can be attributable to the condition of North Atlantic Oscillation (NAO) preceding before onset: Positive NAO favors SSW of displacement type with no transition while negative NAO favors the displacement–split type. We show that, in positive NAO precondition, vertical flux of wave activity immediately before onset is mostly contributed only by wavenumber 1 component, which contrasts with the relatively stronger contribution of wavenumber 2 in negative NAO precondition. Whole Atmosphere Community Climate Model (WACCM) simulation results are also consistent with the observational findings. Therefore, NAO can be regarded as a useful precursor for determining the type of forthcoming SSW events.
format Article in Journal/Newspaper
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
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institution Open Polar
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op_doi https://doi.org/10.1002/asl.953
op_relation https://doi.org/10.1002/asl.953
https://doaj.org/toc/1530-261X
1530-261X
doi:10.1002/asl.953
https://doaj.org/article/ed2a58f2c2914f9288b21cba83f761b5
op_source Atmospheric Science Letters, Vol 21, Iss 3, Pp n/a-n/a (2020)
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spelling ftdoajarticles:oai:doaj.org/article:ed2a58f2c2914f9288b21cba83f761b5 2025-01-16T23:32:35+00:00 Dependence of sudden stratospheric warming type‐transition on preceding North Atlantic Oscillation conditions Hyesun Choi Wookap Choi Seong‐Joong Kim Baek‐Min Kim 2020-03-01T00:00:00Z https://doi.org/10.1002/asl.953 https://doaj.org/article/ed2a58f2c2914f9288b21cba83f761b5 EN eng Wiley https://doi.org/10.1002/asl.953 https://doaj.org/toc/1530-261X 1530-261X doi:10.1002/asl.953 https://doaj.org/article/ed2a58f2c2914f9288b21cba83f761b5 Atmospheric Science Letters, Vol 21, Iss 3, Pp n/a-n/a (2020) North Atlantic oscillation precursor sudden stratospheric warming tropospheric‐stratospheric dynamical processes type‐transition Meteorology. Climatology QC851-999 article 2020 ftdoajarticles https://doi.org/10.1002/asl.953 2022-12-31T08:56:20Z Abstract Most sudden stratospheric warming (SSW) events initiate with their centers being displaced from the pole. Some retain their displaced form until termination but some split into two vortices during their course. Here, we show that existence of a transition during the course of the SSW life cycle can be attributable to the condition of North Atlantic Oscillation (NAO) preceding before onset: Positive NAO favors SSW of displacement type with no transition while negative NAO favors the displacement–split type. We show that, in positive NAO precondition, vertical flux of wave activity immediately before onset is mostly contributed only by wavenumber 1 component, which contrasts with the relatively stronger contribution of wavenumber 2 in negative NAO precondition. Whole Atmosphere Community Climate Model (WACCM) simulation results are also consistent with the observational findings. Therefore, NAO can be regarded as a useful precursor for determining the type of forthcoming SSW events. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Directory of Open Access Journals: DOAJ Articles Atmospheric Science Letters 21 3
spellingShingle North Atlantic oscillation
precursor
sudden stratospheric warming
tropospheric‐stratospheric dynamical processes
type‐transition
Meteorology. Climatology
QC851-999
Hyesun Choi
Wookap Choi
Seong‐Joong Kim
Baek‐Min Kim
Dependence of sudden stratospheric warming type‐transition on preceding North Atlantic Oscillation conditions
title Dependence of sudden stratospheric warming type‐transition on preceding North Atlantic Oscillation conditions
title_full Dependence of sudden stratospheric warming type‐transition on preceding North Atlantic Oscillation conditions
title_fullStr Dependence of sudden stratospheric warming type‐transition on preceding North Atlantic Oscillation conditions
title_full_unstemmed Dependence of sudden stratospheric warming type‐transition on preceding North Atlantic Oscillation conditions
title_short Dependence of sudden stratospheric warming type‐transition on preceding North Atlantic Oscillation conditions
title_sort dependence of sudden stratospheric warming type‐transition on preceding north atlantic oscillation conditions
topic North Atlantic oscillation
precursor
sudden stratospheric warming
tropospheric‐stratospheric dynamical processes
type‐transition
Meteorology. Climatology
QC851-999
topic_facet North Atlantic oscillation
precursor
sudden stratospheric warming
tropospheric‐stratospheric dynamical processes
type‐transition
Meteorology. Climatology
QC851-999
url https://doi.org/10.1002/asl.953
https://doaj.org/article/ed2a58f2c2914f9288b21cba83f761b5