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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Published in:Weather and Climate Dynamics
Main Authors: Kretschmer, M., Zappa, G., Shepherd, T. G.
Format: Article in Journal/Newspaper
Language:English
Published: EGU 2020
Subjects:
Online Access: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
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spelling 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
collection 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>
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container_title Weather and Climate Dynamics
container_volume 1
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