Recent enhanced high-summer North Atlantic Jet variability emerges from three-century context

A recent increase in mid-latitude extreme weather events has been linked to Northern Hemisphere polar jet stream anomalies. To put recent trends in a historical perspective, long-term records of jet stream variability are needed. Here we combine two tree-ring records from the British Isles and the n...

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Published in:Nature Communications
Main Authors: Trouet, V., Babst, F., Meko, M.
Other Authors: Univ Arizona, Lab Tree Ring Res
Format: Article in Journal/Newspaper
Language:English
Published: NATURE PUBLISHING GROUP 2018
Subjects:
Online Access:http://hdl.handle.net/10150/626571
https://doi.org/10.1038/s41467-017-02699-3
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spelling ftunivarizona:oai:repository.arizona.edu:10150/626571 2023-05-15T15:07:24+02:00 Recent enhanced high-summer North Atlantic Jet variability emerges from three-century context Trouet, V. Babst, F. Meko, M. Univ Arizona, Lab Tree Ring Res 2018-01-12 http://hdl.handle.net/10150/626571 https://doi.org/10.1038/s41467-017-02699-3 en eng NATURE PUBLISHING GROUP http://www.nature.com/articles/s41467-017-02699-3 Recent enhanced high-summer North Atlantic Jet variability emerges from three-century context 2018, 9 (1) Nature Communications 2041-1723 29330475 doi:10.1038/s41467-017-02699-3 http://hdl.handle.net/10150/626571 Nature Communications © The Author(s) 2018. This article is licensed under a Creative Commons Attribution 4.0 International License. CC-BY Article 2018 ftunivarizona https://doi.org/10.1038/s41467-017-02699-3 2020-06-14T08:16:05Z A recent increase in mid-latitude extreme weather events has been linked to Northern Hemisphere polar jet stream anomalies. To put recent trends in a historical perspective, long-term records of jet stream variability are needed. Here we combine two tree-ring records from the British Isles and the northeastern Mediterranean to reconstruct variability in the latitudinal position of the high-summer North Atlantic Jet (NAJ) back to 1725 CE. We find that northward NAJ anomalies have resulted in heatwaves and droughts in northwestern Europe and southward anomalies have promoted wildfires in southeastern Europe. We further find an unprecedented increase in NAJ variance since the 1960s, which co-occurs with enhanced late twentieth century variance in the Central and North Pacific Basin. Our results suggest increased late twentieth century interannual meridional jet stream variability and support more sinuous jet stream patterns and quasi-resonant amplification as potential dynamic pathways for Arctic warming to influence mid-latitude weather. National Science Foundation CAREER grant [AGS-1349942]; Swiss National Science Foundation [P300P2_154543]; EU-H project "BACI" [640176] This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu. Article in Journal/Newspaper Arctic North Atlantic The University of Arizona: UA Campus Repository Arctic Pacific Nature Communications 9 1
institution Open Polar
collection The University of Arizona: UA Campus Repository
op_collection_id ftunivarizona
language English
description A recent increase in mid-latitude extreme weather events has been linked to Northern Hemisphere polar jet stream anomalies. To put recent trends in a historical perspective, long-term records of jet stream variability are needed. Here we combine two tree-ring records from the British Isles and the northeastern Mediterranean to reconstruct variability in the latitudinal position of the high-summer North Atlantic Jet (NAJ) back to 1725 CE. We find that northward NAJ anomalies have resulted in heatwaves and droughts in northwestern Europe and southward anomalies have promoted wildfires in southeastern Europe. We further find an unprecedented increase in NAJ variance since the 1960s, which co-occurs with enhanced late twentieth century variance in the Central and North Pacific Basin. Our results suggest increased late twentieth century interannual meridional jet stream variability and support more sinuous jet stream patterns and quasi-resonant amplification as potential dynamic pathways for Arctic warming to influence mid-latitude weather. National Science Foundation CAREER grant [AGS-1349942]; Swiss National Science Foundation [P300P2_154543]; EU-H project "BACI" [640176] This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.
author2 Univ Arizona, Lab Tree Ring Res
format Article in Journal/Newspaper
author Trouet, V.
Babst, F.
Meko, M.
spellingShingle Trouet, V.
Babst, F.
Meko, M.
Recent enhanced high-summer North Atlantic Jet variability emerges from three-century context
author_facet Trouet, V.
Babst, F.
Meko, M.
author_sort Trouet, V.
title Recent enhanced high-summer North Atlantic Jet variability emerges from three-century context
title_short Recent enhanced high-summer North Atlantic Jet variability emerges from three-century context
title_full Recent enhanced high-summer North Atlantic Jet variability emerges from three-century context
title_fullStr Recent enhanced high-summer North Atlantic Jet variability emerges from three-century context
title_full_unstemmed Recent enhanced high-summer North Atlantic Jet variability emerges from three-century context
title_sort recent enhanced high-summer north atlantic jet variability emerges from three-century context
publisher NATURE PUBLISHING GROUP
publishDate 2018
url http://hdl.handle.net/10150/626571
https://doi.org/10.1038/s41467-017-02699-3
geographic Arctic
Pacific
geographic_facet Arctic
Pacific
genre Arctic
North Atlantic
genre_facet Arctic
North Atlantic
op_relation http://www.nature.com/articles/s41467-017-02699-3
Recent enhanced high-summer North Atlantic Jet variability emerges from three-century context 2018, 9 (1) Nature Communications
2041-1723
29330475
doi:10.1038/s41467-017-02699-3
http://hdl.handle.net/10150/626571
Nature Communications
op_rights © The Author(s) 2018. This article is licensed under a Creative Commons Attribution 4.0 International License.
op_rightsnorm CC-BY
op_doi https://doi.org/10.1038/s41467-017-02699-3
container_title Nature Communications
container_volume 9
container_issue 1
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