Effects of Arctic ozone on the stratospheric spring onset and its surface impact
Ozone in the Arctic stratosphere is subject to large interannual variability, driven by both chemical ozone depletion and dynamical variability. Anomalies in Arctic stratospheric ozone become particularly important in spring, when returning sunlight allows them to alter stratospheric temperatures vi...
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00063293 2023-05-15T14:50:08+02:00 Effects of Arctic ozone on the stratospheric spring onset and its surface impact Friedel, Marina Chiodo, Gabriel Stenke, Andrea Domeisen, Daniela I. V. Peter, Thomas 2022-11 electronic https://doi.org/10.5194/acp-22-13997-2022 https://noa.gwlb.de/receive/cop_mods_00063293 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00062379/acp-22-13997-2022.pdf https://acp.copernicus.org/articles/22/13997/2022/acp-22-13997-2022.pdf eng eng Copernicus Publications Atmospheric Chemistry and Physics -- http://www.atmos-chem-phys.net/volumes_and_issues.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2069847 -- 1680-7324 https://doi.org/10.5194/acp-22-13997-2022 https://noa.gwlb.de/receive/cop_mods_00063293 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00062379/acp-22-13997-2022.pdf https://acp.copernicus.org/articles/22/13997/2022/acp-22-13997-2022.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess CC-BY article Verlagsveröffentlichung article Text doc-type:article 2022 ftnonlinearchiv https://doi.org/10.5194/acp-22-13997-2022 2022-11-07T00:12:05Z Ozone in the Arctic stratosphere is subject to large interannual variability, driven by both chemical ozone depletion and dynamical variability. Anomalies in Arctic stratospheric ozone become particularly important in spring, when returning sunlight allows them to alter stratospheric temperatures via shortwave heating, thus modifying atmospheric dynamics. At the same time, the stratospheric circulation undergoes a transition in spring with the final stratospheric warming (FSW), which marks the end of winter. A causal link between stratospheric ozone anomalies and FSWs is plausible and might increase the predictability of stratospheric and tropospheric responses on sub-seasonal to seasonal timescales. However, it remains to be fully understood how ozone influences the timing and evolution of the springtime vortex breakdown. Here, we contrast results from chemistry climate models with and without interactive ozone chemistry to quantify the impact of ozone anomalies on the timing of the FSW and its effects on surface climate. We find that ozone feedbacks increase the variability in the timing of the FSW, especially in the lower stratosphere. In ozone-deficient springs, a persistent strong polar vortex and a delayed FSW in the lower stratosphere are partly due to the lack of heating by ozone in that region. High-ozone anomalies, on the other hand, result in additional shortwave heating in the lower stratosphere, where the FSW therefore occurs earlier. We further show that FSWs in high-ozone springs are predominantly followed by a negative phase of the Arctic Oscillation (AO) with positive sea level pressure anomalies over the Arctic and cold anomalies over Eurasia and Europe. These conditions are to a significant extent (at least 50 %) driven by ozone. In contrast, FSWs in low-ozone springs are not associated with a discernible surface climate response. These results highlight the importance of ozone–circulation coupling in the climate system and the potential value of interactive ozone chemistry for sub-seasonal to ... Article in Journal/Newspaper Arctic Niedersächsisches Online-Archiv NOA Arctic Atmospheric Chemistry and Physics 22 21 13997 14017 |
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article Verlagsveröffentlichung Friedel, Marina Chiodo, Gabriel Stenke, Andrea Domeisen, Daniela I. V. Peter, Thomas Effects of Arctic ozone on the stratospheric spring onset and its surface impact |
topic_facet |
article Verlagsveröffentlichung |
description |
Ozone in the Arctic stratosphere is subject to large interannual variability, driven by both chemical ozone depletion and dynamical variability. Anomalies in Arctic stratospheric ozone become particularly important in spring, when returning sunlight allows them to alter stratospheric temperatures via shortwave heating, thus modifying atmospheric dynamics. At the same time, the stratospheric circulation undergoes a transition in spring with the final stratospheric warming (FSW), which marks the end of winter. A causal link between stratospheric ozone anomalies and FSWs is plausible and might increase the predictability of stratospheric and tropospheric responses on sub-seasonal to seasonal timescales. However, it remains to be fully understood how ozone influences the timing and evolution of the springtime vortex breakdown. Here, we contrast results from chemistry climate models with and without interactive ozone chemistry to quantify the impact of ozone anomalies on the timing of the FSW and its effects on surface climate. We find that ozone feedbacks increase the variability in the timing of the FSW, especially in the lower stratosphere. In ozone-deficient springs, a persistent strong polar vortex and a delayed FSW in the lower stratosphere are partly due to the lack of heating by ozone in that region. High-ozone anomalies, on the other hand, result in additional shortwave heating in the lower stratosphere, where the FSW therefore occurs earlier. We further show that FSWs in high-ozone springs are predominantly followed by a negative phase of the Arctic Oscillation (AO) with positive sea level pressure anomalies over the Arctic and cold anomalies over Eurasia and Europe. These conditions are to a significant extent (at least 50 %) driven by ozone. In contrast, FSWs in low-ozone springs are not associated with a discernible surface climate response. These results highlight the importance of ozone–circulation coupling in the climate system and the potential value of interactive ozone chemistry for sub-seasonal to ... |
format |
Article in Journal/Newspaper |
author |
Friedel, Marina Chiodo, Gabriel Stenke, Andrea Domeisen, Daniela I. V. Peter, Thomas |
author_facet |
Friedel, Marina Chiodo, Gabriel Stenke, Andrea Domeisen, Daniela I. V. Peter, Thomas |
author_sort |
Friedel, Marina |
title |
Effects of Arctic ozone on the stratospheric spring onset and its surface impact |
title_short |
Effects of Arctic ozone on the stratospheric spring onset and its surface impact |
title_full |
Effects of Arctic ozone on the stratospheric spring onset and its surface impact |
title_fullStr |
Effects of Arctic ozone on the stratospheric spring onset and its surface impact |
title_full_unstemmed |
Effects of Arctic ozone on the stratospheric spring onset and its surface impact |
title_sort |
effects of arctic ozone on the stratospheric spring onset and its surface impact |
publisher |
Copernicus Publications |
publishDate |
2022 |
url |
https://doi.org/10.5194/acp-22-13997-2022 https://noa.gwlb.de/receive/cop_mods_00063293 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00062379/acp-22-13997-2022.pdf https://acp.copernicus.org/articles/22/13997/2022/acp-22-13997-2022.pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_relation |
Atmospheric Chemistry and Physics -- http://www.atmos-chem-phys.net/volumes_and_issues.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2069847 -- 1680-7324 https://doi.org/10.5194/acp-22-13997-2022 https://noa.gwlb.de/receive/cop_mods_00063293 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00062379/acp-22-13997-2022.pdf https://acp.copernicus.org/articles/22/13997/2022/acp-22-13997-2022.pdf |
op_rights |
https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5194/acp-22-13997-2022 |
container_title |
Atmospheric Chemistry and Physics |
container_volume |
22 |
container_issue |
21 |
container_start_page |
13997 |
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14017 |
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1766321200187834368 |