The influence of Antarctic sea‐ice loss on Northern Hemisphere cold surges and associated compound events
Abstract The synoptic cold surge is a weather event that frequently occurs in the Northern Hemisphere, often causing severe damage accompanied with intense winds and precipitation. It is reported that the Arctic Oscillation and the North Atlantic Oscillation can affect the cold surge. However, on in...
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crwiley:10.1002/joc.8354 2024-06-02T07:58:22+00:00 The influence of Antarctic sea‐ice loss on Northern Hemisphere cold surges and associated compound events Su, Tianhua Chen, Jie Li, Lu Toniazzo, Thomas Mooney, Priscilla National Natural Science Foundation of China Norges Forskningsråd 2024 http://dx.doi.org/10.1002/joc.8354 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.8354 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 44, issue 3, page 759-774 ISSN 0899-8418 1097-0088 journal-article 2024 crwiley https://doi.org/10.1002/joc.8354 2024-05-03T11:40:21Z Abstract The synoptic cold surge is a weather event that frequently occurs in the Northern Hemisphere, often causing severe damage accompanied with intense winds and precipitation. It is reported that the Arctic Oscillation and the North Atlantic Oscillation can affect the cold surge. However, on interacting with tropical circulation, the cold surge potentially links to the Antarctic sea‐ice loss with influence extending to Tropics. Therefore, this research aims to investigate the potential link between Antarctic sea‐ice loss and Northern Hemisphere cold surges and corresponding wind–precipitation compound events. To study this link, twin numerical experiments using a physically based atmosphere model with a prescribed 30% Antarctic sea‐ice loss scenario were used. The results show that the cold surge occurs more frequently in most regions of the world, except for central North America and central Eurasia. In Europe, the cold surges occur closer to the lower latitudes in the Antarctic sea‐ice loss scenario. Additionally, the Antarctic sea‐ice loss can result in intensified wind and precipitation extremes within compound events. The intensified precipitation extremes are caused by increased moisture transportation by tropical easterlies and higher local temperature after the cold surge occurrence, providing more moisture available for precipitation in East Asia and East North America, respectively. Overall, the results of the numerical experiments provide evidence that Antarctic sea‐ice loss influences cold surges in Northern Hemisphere through atmospheric teleconnections. It is important to continue investigating the link between Antarctic sea‐ice loss and weather events like cold surges, as this research can help improve our understanding of the impacts of polar climate change on lower latitudes. Article in Journal/Newspaper Antarc* Antarctic Arctic Climate change North Atlantic North Atlantic oscillation Sea ice Wiley Online Library Antarctic Arctic The Antarctic International Journal of Climatology 44 3 759 774 |
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Wiley Online Library |
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English |
description |
Abstract The synoptic cold surge is a weather event that frequently occurs in the Northern Hemisphere, often causing severe damage accompanied with intense winds and precipitation. It is reported that the Arctic Oscillation and the North Atlantic Oscillation can affect the cold surge. However, on interacting with tropical circulation, the cold surge potentially links to the Antarctic sea‐ice loss with influence extending to Tropics. Therefore, this research aims to investigate the potential link between Antarctic sea‐ice loss and Northern Hemisphere cold surges and corresponding wind–precipitation compound events. To study this link, twin numerical experiments using a physically based atmosphere model with a prescribed 30% Antarctic sea‐ice loss scenario were used. The results show that the cold surge occurs more frequently in most regions of the world, except for central North America and central Eurasia. In Europe, the cold surges occur closer to the lower latitudes in the Antarctic sea‐ice loss scenario. Additionally, the Antarctic sea‐ice loss can result in intensified wind and precipitation extremes within compound events. The intensified precipitation extremes are caused by increased moisture transportation by tropical easterlies and higher local temperature after the cold surge occurrence, providing more moisture available for precipitation in East Asia and East North America, respectively. Overall, the results of the numerical experiments provide evidence that Antarctic sea‐ice loss influences cold surges in Northern Hemisphere through atmospheric teleconnections. It is important to continue investigating the link between Antarctic sea‐ice loss and weather events like cold surges, as this research can help improve our understanding of the impacts of polar climate change on lower latitudes. |
author2 |
National Natural Science Foundation of China Norges Forskningsråd |
format |
Article in Journal/Newspaper |
author |
Su, Tianhua Chen, Jie Li, Lu Toniazzo, Thomas Mooney, Priscilla |
spellingShingle |
Su, Tianhua Chen, Jie Li, Lu Toniazzo, Thomas Mooney, Priscilla The influence of Antarctic sea‐ice loss on Northern Hemisphere cold surges and associated compound events |
author_facet |
Su, Tianhua Chen, Jie Li, Lu Toniazzo, Thomas Mooney, Priscilla |
author_sort |
Su, Tianhua |
title |
The influence of Antarctic sea‐ice loss on Northern Hemisphere cold surges and associated compound events |
title_short |
The influence of Antarctic sea‐ice loss on Northern Hemisphere cold surges and associated compound events |
title_full |
The influence of Antarctic sea‐ice loss on Northern Hemisphere cold surges and associated compound events |
title_fullStr |
The influence of Antarctic sea‐ice loss on Northern Hemisphere cold surges and associated compound events |
title_full_unstemmed |
The influence of Antarctic sea‐ice loss on Northern Hemisphere cold surges and associated compound events |
title_sort |
influence of antarctic sea‐ice loss on northern hemisphere cold surges and associated compound events |
publisher |
Wiley |
publishDate |
2024 |
url |
http://dx.doi.org/10.1002/joc.8354 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.8354 |
geographic |
Antarctic Arctic The Antarctic |
geographic_facet |
Antarctic Arctic The Antarctic |
genre |
Antarc* Antarctic Arctic Climate change North Atlantic North Atlantic oscillation Sea ice |
genre_facet |
Antarc* Antarctic Arctic Climate change North Atlantic North Atlantic oscillation Sea ice |
op_source |
International Journal of Climatology volume 44, issue 3, page 759-774 ISSN 0899-8418 1097-0088 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/joc.8354 |
container_title |
International Journal of Climatology |
container_volume |
44 |
container_issue |
3 |
container_start_page |
759 |
op_container_end_page |
774 |
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1800741687172005888 |