The role of Barents-Kara sea ice loss in projected polar vortex changes
The Northern Hemisphere stratospheric polar vortex (SPV) plays a key role for mid-latitude weather and climate. However, in what way the SPV will respond to global warming is not clear, with climate models disagreeing on the sign and magnitude of projected SPV strength change. Here we address the po...
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ftunivreading:oai:centaur.reading.ac.uk:93799 2024-09-15T18:08:09+00:00 The role of Barents-Kara sea ice loss in projected polar vortex changes Kretschmer, M. Zappa, G. Shepherd, T. G. 2020 text https://centaur.reading.ac.uk/93799/ https://centaur.reading.ac.uk/93799/16/wcd-1-715-2020.pdf https://centaur.reading.ac.uk/93799/1/SUB3_FINAL.pdf https://centaur.reading.ac.uk/93799/2/SI.pdf en eng EGU https://centaur.reading.ac.uk/93799/16/wcd-1-715-2020.pdf https://centaur.reading.ac.uk/93799/1/SUB3_FINAL.pdf https://centaur.reading.ac.uk/93799/2/SI.pdf Kretschmer, M. <https://centaur.reading.ac.uk/view/creators/90010232.html> orcid:0000-0002-2756-9526 , Zappa, G. <https://centaur.reading.ac.uk/view/creators/90003969.html> and Shepherd, T. G. <https://centaur.reading.ac.uk/view/creators/90004685.html> orcid:0000-0002-6631-9968 (2020) The role of Barents-Kara sea ice loss in projected polar vortex changes. Weather and Climate Dynamics, 1 (2). pp. 715-730. ISSN 2698-4024 doi: https://doi.org/10.5194/wcd-1-715-2020 <https://doi.org/10.5194/wcd-1-715-2020> cc_by_4 Article PeerReviewed 2020 ftunivreading https://doi.org/10.5194/wcd-1-715-2020 2024-07-30T14:08:25Z The Northern Hemisphere stratospheric polar vortex (SPV) plays a key role for mid-latitude weather and climate. However, in what way the SPV will respond to global warming is not clear, with climate models disagreeing on the sign and magnitude of projected SPV strength change. Here we address the potential role of Barents and Kara (BK) sea ice loss in this. We provide evidence for a non-linear response of the SPV to global mean temperature change, coincident with the time the BK Seas become ice-free. Using a causal network approach, we demonstrate that climate models show some partial support for the previously proposed link between low BK sea ice in autumn and a weakened winter SPV, but that this effect is plausibly very small relative to internal variability. Yet, given the expected dramatic decrease of sea ice in the future, even a small causal effect can explain all of the projected ensemble-mean SPV weakening, approximately one-half of the ensemble spread at the middle of the 21st century, and one-third of the spread at the end of the century. Finally, we note that most models have unrealistic amounts of BK sea ice, meaning that their SPV response to ice loss is unrealistic. Bias-adjusting for this effect leads to pronounced differences in SPV response of individual models at both ends of the spectrum, but has no strong consequences for the overall ensemble mean and spread. Overall, our results indicate the importance of exploring all plausible implications of a changing Arctic for regional climate risk assessments. Article in Journal/Newspaper Global warming Kara Sea Sea ice CentAUR: Central Archive at the University of Reading Weather and Climate Dynamics 1 2 715 730 |
institution |
Open Polar |
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CentAUR: Central Archive at the University of Reading |
op_collection_id |
ftunivreading |
language |
English |
description |
The Northern Hemisphere stratospheric polar vortex (SPV) plays a key role for mid-latitude weather and climate. However, in what way the SPV will respond to global warming is not clear, with climate models disagreeing on the sign and magnitude of projected SPV strength change. Here we address the potential role of Barents and Kara (BK) sea ice loss in this. We provide evidence for a non-linear response of the SPV to global mean temperature change, coincident with the time the BK Seas become ice-free. Using a causal network approach, we demonstrate that climate models show some partial support for the previously proposed link between low BK sea ice in autumn and a weakened winter SPV, but that this effect is plausibly very small relative to internal variability. Yet, given the expected dramatic decrease of sea ice in the future, even a small causal effect can explain all of the projected ensemble-mean SPV weakening, approximately one-half of the ensemble spread at the middle of the 21st century, and one-third of the spread at the end of the century. Finally, we note that most models have unrealistic amounts of BK sea ice, meaning that their SPV response to ice loss is unrealistic. Bias-adjusting for this effect leads to pronounced differences in SPV response of individual models at both ends of the spectrum, but has no strong consequences for the overall ensemble mean and spread. Overall, our results indicate the importance of exploring all plausible implications of a changing Arctic for regional climate risk assessments. |
format |
Article in Journal/Newspaper |
author |
Kretschmer, M. Zappa, G. Shepherd, T. G. |
spellingShingle |
Kretschmer, M. Zappa, G. Shepherd, T. G. The role of Barents-Kara sea ice loss in projected polar vortex changes |
author_facet |
Kretschmer, M. Zappa, G. Shepherd, T. G. |
author_sort |
Kretschmer, M. |
title |
The role of Barents-Kara sea ice loss in projected polar vortex changes |
title_short |
The role of Barents-Kara sea ice loss in projected polar vortex changes |
title_full |
The role of Barents-Kara sea ice loss in projected polar vortex changes |
title_fullStr |
The role of Barents-Kara sea ice loss in projected polar vortex changes |
title_full_unstemmed |
The role of Barents-Kara sea ice loss in projected polar vortex changes |
title_sort |
role of barents-kara sea ice loss in projected polar vortex changes |
publisher |
EGU |
publishDate |
2020 |
url |
https://centaur.reading.ac.uk/93799/ https://centaur.reading.ac.uk/93799/16/wcd-1-715-2020.pdf https://centaur.reading.ac.uk/93799/1/SUB3_FINAL.pdf https://centaur.reading.ac.uk/93799/2/SI.pdf |
genre |
Global warming Kara Sea Sea ice |
genre_facet |
Global warming Kara Sea Sea ice |
op_relation |
https://centaur.reading.ac.uk/93799/16/wcd-1-715-2020.pdf https://centaur.reading.ac.uk/93799/1/SUB3_FINAL.pdf https://centaur.reading.ac.uk/93799/2/SI.pdf Kretschmer, M. <https://centaur.reading.ac.uk/view/creators/90010232.html> orcid:0000-0002-2756-9526 , Zappa, G. <https://centaur.reading.ac.uk/view/creators/90003969.html> and Shepherd, T. G. <https://centaur.reading.ac.uk/view/creators/90004685.html> orcid:0000-0002-6631-9968 (2020) The role of Barents-Kara sea ice loss in projected polar vortex changes. Weather and Climate Dynamics, 1 (2). pp. 715-730. ISSN 2698-4024 doi: https://doi.org/10.5194/wcd-1-715-2020 <https://doi.org/10.5194/wcd-1-715-2020> |
op_rights |
cc_by_4 |
op_doi |
https://doi.org/10.5194/wcd-1-715-2020 |
container_title |
Weather and Climate Dynamics |
container_volume |
1 |
container_issue |
2 |
container_start_page |
715 |
op_container_end_page |
730 |
_version_ |
1810445488530391040 |