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...
Published in: | Atmospheric Science Letters |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2020
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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 |
id | ftdoajarticles:oai:doaj.org/article:ed2a58f2c2914f9288b21cba83f761b5 |
institution | Open Polar |
language | English |
op_collection_id | ftdoajarticles |
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) |
publishDate | 2020 |
publisher | Wiley |
record_format | openpolar |
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 |