Recent weakening in the winter ENSO teleconnection over the North Atlantic‑European region

New observational evidence for variability of the atmospheric response to wintertime El Niño-Southern Oscillation (ENSO) is found. Using different approaches and datasets, a weakening in the recent ENSO teleconnection over the North Atlantic-European (NAE) region is demonstrated. Changes in both pat...

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Published in:Climate Dynamics
Main Authors: Ivasic, Sara, Herceg-Bulic, Ivana, King, Martin Peter
Format: Article in Journal/Newspaper
Language:English
Published: Springer 2021
Subjects:
Online Access:https://hdl.handle.net/11250/2986591
https://doi.org/10.1007/s00382-021-05783-z
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spelling ftunivbergen:oai:bora.uib.no:11250/2986591 2023-05-15T15:05:21+02:00 Recent weakening in the winter ENSO teleconnection over the North Atlantic‑European region Ivasic, Sara Herceg-Bulic, Ivana King, Martin Peter 2021 application/pdf https://hdl.handle.net/11250/2986591 https://doi.org/10.1007/s00382-021-05783-z eng eng Springer https://link.springer.com/article/10.1007%2Fs00382-021-05783-z Norges forskningsråd: 275268 Notur/NorStore: NS9039K Norges forskningsråd: 255027 Notur/NorStore: NS9001K urn:issn:0930-7575 https://hdl.handle.net/11250/2986591 https://doi.org/10.1007/s00382-021-05783-z cristin:1908204 Climate Dynamics. 2021, 57, 1953-1972. Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no Copyright The Author(s) 2021 Climate Dynamics 1953-1972 57 Journal article Peer reviewed 2021 ftunivbergen https://doi.org/10.1007/s00382-021-05783-z 2023-03-14T17:39:40Z New observational evidence for variability of the atmospheric response to wintertime El Niño-Southern Oscillation (ENSO) is found. Using different approaches and datasets, a weakening in the recent ENSO teleconnection over the North Atlantic-European (NAE) region is demonstrated. Changes in both pattern and strength of the teleconnection indicate a turning point in the 1970s with a shift from a response resembling the North Atlantic Oscillation (NAO) to an anomaly pattern orthogonal to NAO with very weak or statistically non-significant values; and to nearly non-existent teleconnection in the most recent decades. Results shows the importance of the background sea surface temperature (SST) state and sea-ice climatology having opposite effects in modulating the ENSO-NAE teleconnection. As indicated with targeted simulations, the recent change in the SST climatology in the Atlantic and Arctic has contributed to the weakening of the ENSO effect. The findings of this study can have implications on our understanding of modulations of ENSO teleconnections and ENSO as a source of predictability in the NAE sector. publishedVersion Article in Journal/Newspaper Arctic North Atlantic North Atlantic oscillation Sea ice University of Bergen: Bergen Open Research Archive (BORA-UiB) Arctic Climate Dynamics 57 7-8 1953 1972
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
description New observational evidence for variability of the atmospheric response to wintertime El Niño-Southern Oscillation (ENSO) is found. Using different approaches and datasets, a weakening in the recent ENSO teleconnection over the North Atlantic-European (NAE) region is demonstrated. Changes in both pattern and strength of the teleconnection indicate a turning point in the 1970s with a shift from a response resembling the North Atlantic Oscillation (NAO) to an anomaly pattern orthogonal to NAO with very weak or statistically non-significant values; and to nearly non-existent teleconnection in the most recent decades. Results shows the importance of the background sea surface temperature (SST) state and sea-ice climatology having opposite effects in modulating the ENSO-NAE teleconnection. As indicated with targeted simulations, the recent change in the SST climatology in the Atlantic and Arctic has contributed to the weakening of the ENSO effect. The findings of this study can have implications on our understanding of modulations of ENSO teleconnections and ENSO as a source of predictability in the NAE sector. publishedVersion
format Article in Journal/Newspaper
author Ivasic, Sara
Herceg-Bulic, Ivana
King, Martin Peter
spellingShingle Ivasic, Sara
Herceg-Bulic, Ivana
King, Martin Peter
Recent weakening in the winter ENSO teleconnection over the North Atlantic‑European region
author_facet Ivasic, Sara
Herceg-Bulic, Ivana
King, Martin Peter
author_sort Ivasic, Sara
title Recent weakening in the winter ENSO teleconnection over the North Atlantic‑European region
title_short Recent weakening in the winter ENSO teleconnection over the North Atlantic‑European region
title_full Recent weakening in the winter ENSO teleconnection over the North Atlantic‑European region
title_fullStr Recent weakening in the winter ENSO teleconnection over the North Atlantic‑European region
title_full_unstemmed Recent weakening in the winter ENSO teleconnection over the North Atlantic‑European region
title_sort recent weakening in the winter enso teleconnection over the north atlantic‑european region
publisher Springer
publishDate 2021
url https://hdl.handle.net/11250/2986591
https://doi.org/10.1007/s00382-021-05783-z
geographic Arctic
geographic_facet Arctic
genre Arctic
North Atlantic
North Atlantic oscillation
Sea ice
genre_facet Arctic
North Atlantic
North Atlantic oscillation
Sea ice
op_source Climate Dynamics
1953-1972
57
op_relation https://link.springer.com/article/10.1007%2Fs00382-021-05783-z
Norges forskningsråd: 275268
Notur/NorStore: NS9039K
Norges forskningsråd: 255027
Notur/NorStore: NS9001K
urn:issn:0930-7575
https://hdl.handle.net/11250/2986591
https://doi.org/10.1007/s00382-021-05783-z
cristin:1908204
Climate Dynamics. 2021, 57, 1953-1972.
op_rights Navngivelse 4.0 Internasjonal
http://creativecommons.org/licenses/by/4.0/deed.no
Copyright The Author(s) 2021
op_doi https://doi.org/10.1007/s00382-021-05783-z
container_title Climate Dynamics
container_volume 57
container_issue 7-8
container_start_page 1953
op_container_end_page 1972
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