Polar Vortex Disruptions by High Latitude Ocean Warming
Mid-latitude extreme cold outbreaks are associated with disruptions of the Polar Vortex, which often happen abruptly in connection to a Sudden Stratospheric Warming. Understanding Global Warming (particularly Arctic Amplification) impacts on forecasting such events is challenging for the scientific...
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Authorea, Inc.
2024
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Online Access: | http://dx.doi.org/10.22541/au.170602922.21514713/v1 |
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crwinnower:10.22541/au.170602922.21514713/v1 2024-06-02T08:02:00+00:00 Polar Vortex Disruptions by High Latitude Ocean Warming Hamouda, Mostafa E Portal, Alice Pasquero, Claudia 2024 http://dx.doi.org/10.22541/au.170602922.21514713/v1 unknown Authorea, Inc. https://creativecommons.org/licenses/by-sa/4.0/ posted-content 2024 crwinnower https://doi.org/10.22541/au.170602922.21514713/v1 2024-05-07T14:19:22Z Mid-latitude extreme cold outbreaks are associated with disruptions of the Polar Vortex, which often happen abruptly in connection to a Sudden Stratospheric Warming. Understanding Global Warming (particularly Arctic Amplification) impacts on forecasting such events is challenging for the scientific community. Here we apply clustering analysis on the Northern Annular Mode to identify surface precursors and the governing mechanisms causing polar vortex disruption events. Two clusters of breakdown emerge; 65% of the events are associated with high latitude ocean warming, expressed as North Pacific anomalies and Barents-Kara sea ice loss. Such warming causes large scale modifications of the tropospheric flow that favors a slowdown of the stratospheric vortex. The persistence of ocean surface temperature patterns allows forecasting polar vortex disruptions, and potentially improves prediction skills at the sub-seasonal to seasonal time scales. Other/Unknown Material Arctic Global warming Kara Sea Sea ice The Winnower Arctic Kara Sea Pacific |
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Open Polar |
collection |
The Winnower |
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crwinnower |
language |
unknown |
description |
Mid-latitude extreme cold outbreaks are associated with disruptions of the Polar Vortex, which often happen abruptly in connection to a Sudden Stratospheric Warming. Understanding Global Warming (particularly Arctic Amplification) impacts on forecasting such events is challenging for the scientific community. Here we apply clustering analysis on the Northern Annular Mode to identify surface precursors and the governing mechanisms causing polar vortex disruption events. Two clusters of breakdown emerge; 65% of the events are associated with high latitude ocean warming, expressed as North Pacific anomalies and Barents-Kara sea ice loss. Such warming causes large scale modifications of the tropospheric flow that favors a slowdown of the stratospheric vortex. The persistence of ocean surface temperature patterns allows forecasting polar vortex disruptions, and potentially improves prediction skills at the sub-seasonal to seasonal time scales. |
format |
Other/Unknown Material |
author |
Hamouda, Mostafa E Portal, Alice Pasquero, Claudia |
spellingShingle |
Hamouda, Mostafa E Portal, Alice Pasquero, Claudia Polar Vortex Disruptions by High Latitude Ocean Warming |
author_facet |
Hamouda, Mostafa E Portal, Alice Pasquero, Claudia |
author_sort |
Hamouda, Mostafa E |
title |
Polar Vortex Disruptions by High Latitude Ocean Warming |
title_short |
Polar Vortex Disruptions by High Latitude Ocean Warming |
title_full |
Polar Vortex Disruptions by High Latitude Ocean Warming |
title_fullStr |
Polar Vortex Disruptions by High Latitude Ocean Warming |
title_full_unstemmed |
Polar Vortex Disruptions by High Latitude Ocean Warming |
title_sort |
polar vortex disruptions by high latitude ocean warming |
publisher |
Authorea, Inc. |
publishDate |
2024 |
url |
http://dx.doi.org/10.22541/au.170602922.21514713/v1 |
geographic |
Arctic Kara Sea Pacific |
geographic_facet |
Arctic Kara Sea Pacific |
genre |
Arctic Global warming Kara Sea Sea ice |
genre_facet |
Arctic Global warming Kara Sea Sea ice |
op_rights |
https://creativecommons.org/licenses/by-sa/4.0/ |
op_doi |
https://doi.org/10.22541/au.170602922.21514713/v1 |
_version_ |
1800746513807179776 |