Tropospheric Role in the Predictability of the Surface Impact of the 2018 Sudden Stratospheric Warming Event
Abstract Sudden stratospheric warmings (SSWs) can have a strong impact on the troposphere. Their fingerprint is often associated with the negative phase of the Northern Annular Mode (NAM) and the North Atlantic Oscillation (NAO), and extreme weather with high societal impact. However, the mechanisms...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Zenodo
2023
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Subjects: | |
Online Access: | https://doi.org/10.1029/2021GL095464 |
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author | González-Alemán, Juan J. Grams, Christian M. Ayarzagüena, Blanca Zurita-Gotor, Pablo Domeisen, Daniela I. V. Gómara, Iñigo Rodríguez-Fonseca, Belén Vitart, Frédéric |
author_facet | González-Alemán, Juan J. Grams, Christian M. Ayarzagüena, Blanca Zurita-Gotor, Pablo Domeisen, Daniela I. V. Gómara, Iñigo Rodríguez-Fonseca, Belén Vitart, Frédéric |
author_sort | González-Alemán, Juan J. |
collection | Zenodo |
container_issue | 1 |
container_title | Geophysical Research Letters |
container_volume | 49 |
description | Abstract Sudden stratospheric warmings (SSWs) can have a strong impact on the troposphere. Their fingerprint is often associated with the negative phase of the Northern Annular Mode (NAM) and the North Atlantic Oscillation (NAO), and extreme weather with high societal impact. However, the mechanisms behind this downward impact are not well understood. We investigate this surface impact through its associated predictability limits, by studying the 2018 SSW event. We search for predictability barriers that occurred after the onset of the SSW and before its surface impact. It is found that dynamical tropospheric events consisting of two cyclogenesis events were the main reasons for these predictability barriers in the prediction of negative NAM/NAO anomalies reaching the surface. This work corroborates that individual synoptic events might constitute predictability barriers during the downward impact of SSW events, and thereby sheds light on stratosphere-troposphere coupling. Plain Language Summary Sudden stratospheric warmings (SSWs) can have a strong impact on near-surface weather. They have the potential to alter the atmospheric circulation and associated extreme events, thus affecting society. However, the way the stratosphere couples with surface weather is not fully understood. In this work, we investigate this relationship by analyzing the predictability of the surface impact of a stratospheric warming event that occurred in 2018, and which left widespread societal impacts over Europe due to a severe cold spell and extraordinary rainy and windy conditions. We find that the impact of this SSW event on the surface was regulated by two low-pressure systems that developed over the North Atlantic. Even though the SSW event was well developed, alternative behavior of these systems could have led to drastically different weather conditions over Europe. Thus, this study highlights the role of the tropospheric circulation in the effectiveness of the stratospheric impact on surface weather. Acknowledgments JJGA is ... |
format | Article in Journal/Newspaper |
genre | North Atlantic North Atlantic oscillation |
genre_facet | North Atlantic North Atlantic oscillation |
id | ftzenodo:oai:zenodo.org:8220976 |
institution | Open Polar |
language | English |
op_collection_id | ftzenodo |
op_doi | https://doi.org/10.1029/2021GL095464 |
op_relation | https://zenodo.org/communities/nextgems-publications https://zenodo.org/communities/eu https://doi.org/10.1029/2021GL095464 oai:zenodo.org:8220976 |
op_rights | info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode |
op_source | Geophysical Research Letters, 49(1), (2023-08-07) |
publishDate | 2023 |
publisher | Zenodo |
record_format | openpolar |
spelling | ftzenodo:oai:zenodo.org:8220976 2025-01-16T23:38:39+00:00 Tropospheric Role in the Predictability of the Surface Impact of the 2018 Sudden Stratospheric Warming Event González-Alemán, Juan J. Grams, Christian M. Ayarzagüena, Blanca Zurita-Gotor, Pablo Domeisen, Daniela I. V. Gómara, Iñigo Rodríguez-Fonseca, Belén Vitart, Frédéric 2023-08-07 https://doi.org/10.1029/2021GL095464 eng eng Zenodo https://zenodo.org/communities/nextgems-publications https://zenodo.org/communities/eu https://doi.org/10.1029/2021GL095464 oai:zenodo.org:8220976 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Geophysical Research Letters, 49(1), (2023-08-07) Troposphere Medium-range Uncertainties Stratospheric Warming info:eu-repo/semantics/article 2023 ftzenodo https://doi.org/10.1029/2021GL095464 2024-07-25T19:29:32Z Abstract Sudden stratospheric warmings (SSWs) can have a strong impact on the troposphere. Their fingerprint is often associated with the negative phase of the Northern Annular Mode (NAM) and the North Atlantic Oscillation (NAO), and extreme weather with high societal impact. However, the mechanisms behind this downward impact are not well understood. We investigate this surface impact through its associated predictability limits, by studying the 2018 SSW event. We search for predictability barriers that occurred after the onset of the SSW and before its surface impact. It is found that dynamical tropospheric events consisting of two cyclogenesis events were the main reasons for these predictability barriers in the prediction of negative NAM/NAO anomalies reaching the surface. This work corroborates that individual synoptic events might constitute predictability barriers during the downward impact of SSW events, and thereby sheds light on stratosphere-troposphere coupling. Plain Language Summary Sudden stratospheric warmings (SSWs) can have a strong impact on near-surface weather. They have the potential to alter the atmospheric circulation and associated extreme events, thus affecting society. However, the way the stratosphere couples with surface weather is not fully understood. In this work, we investigate this relationship by analyzing the predictability of the surface impact of a stratospheric warming event that occurred in 2018, and which left widespread societal impacts over Europe due to a severe cold spell and extraordinary rainy and windy conditions. We find that the impact of this SSW event on the surface was regulated by two low-pressure systems that developed over the North Atlantic. Even though the SSW event was well developed, alternative behavior of these systems could have led to drastically different weather conditions over Europe. Thus, this study highlights the role of the tropospheric circulation in the effectiveness of the stratospheric impact on surface weather. Acknowledgments JJGA is ... Article in Journal/Newspaper North Atlantic North Atlantic oscillation Zenodo Geophysical Research Letters 49 1 |
spellingShingle | Troposphere Medium-range Uncertainties Stratospheric Warming González-Alemán, Juan J. Grams, Christian M. Ayarzagüena, Blanca Zurita-Gotor, Pablo Domeisen, Daniela I. V. Gómara, Iñigo Rodríguez-Fonseca, Belén Vitart, Frédéric Tropospheric Role in the Predictability of the Surface Impact of the 2018 Sudden Stratospheric Warming Event |
title | Tropospheric Role in the Predictability of the Surface Impact of the 2018 Sudden Stratospheric Warming Event |
title_full | Tropospheric Role in the Predictability of the Surface Impact of the 2018 Sudden Stratospheric Warming Event |
title_fullStr | Tropospheric Role in the Predictability of the Surface Impact of the 2018 Sudden Stratospheric Warming Event |
title_full_unstemmed | Tropospheric Role in the Predictability of the Surface Impact of the 2018 Sudden Stratospheric Warming Event |
title_short | Tropospheric Role in the Predictability of the Surface Impact of the 2018 Sudden Stratospheric Warming Event |
title_sort | tropospheric role in the predictability of the surface impact of the 2018 sudden stratospheric warming event |
topic | Troposphere Medium-range Uncertainties Stratospheric Warming |
topic_facet | Troposphere Medium-range Uncertainties Stratospheric Warming |
url | https://doi.org/10.1029/2021GL095464 |