Coupled stratosphere-troposphere-Atlantic multidecadal oscillation and its importance for near-future climate projection

Northern Hemisphere (NH) climate has experienced various coherent wintertime multidecadal climate trends in stratosphere, troposphere, ocean, and cryosphere. However, the overall mechanistic framework linking these trends is not well established. Here we show, using long-term transient forced couple...

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Published in:npj Climate and Atmospheric Science
Main Authors: Nour-Eddine Omrani, Noel Keenlyside, Katja Matthes, Lina Boljka, Davide Zanchettin, Johann H. Jungclaus, Sandro W. Lubis
Other Authors: Omrani, Nour-Eddine, Keenlyside, Noel, Matthes, Katja, Boljka, Lina, Zanchettin, Davide, Jungclaus, Johann H., Lubis, Sandro W.
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:https://hdl.handle.net/10278/5007460
https://doi.org/10.1038/s41612-022-00275-1
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author Nour-Eddine Omrani
Noel Keenlyside
Katja Matthes
Lina Boljka
Davide Zanchettin
Johann H. Jungclaus
Sandro W. Lubis
author2 Omrani, Nour-Eddine
Keenlyside, Noel
Matthes, Katja
Boljka, Lina
Zanchettin, Davide
Jungclaus, Johann H.
Lubis, Sandro W.
author_facet Nour-Eddine Omrani
Noel Keenlyside
Katja Matthes
Lina Boljka
Davide Zanchettin
Johann H. Jungclaus
Sandro W. Lubis
author_sort Nour-Eddine Omrani
collection Università Ca’ Foscari Venezia: ARCA (Archivio Istituzionale della Ricerca)
container_issue 1
container_title npj Climate and Atmospheric Science
container_volume 5
description Northern Hemisphere (NH) climate has experienced various coherent wintertime multidecadal climate trends in stratosphere, troposphere, ocean, and cryosphere. However, the overall mechanistic framework linking these trends is not well established. Here we show, using long-term transient forced coupled climate simulation, that large parts of the coherent NH-multidecadal changes can be understood within a damped coupled stratosphere/troposphere/ocean-oscillation framework. Wave-induced downward propagating positive stratosphere/troposphere-coupled Northern Annular Mode (NAM) and associated stratospheric cooling initiate delayed thermohaline strengthening of Atlantic overturning circulation and extratropical Atlantic-gyres. These increase the poleward oceanic heat transport leading to Arctic sea-ice melting, Arctic warming amplification, and large-scale Atlantic warming, which in turn initiates wave-induced downward propagating negative NAM and stratospheric warming and therefore reverse the oscillation phase. This coupled variability improves the performance of statistical models, which project further weakening of North Atlantic Oscillation, North Atlantic cooling and hiatus in wintertime North Atlantic-Arctic sea-ice and global surface temperature just like the 1950s-1970s.
format Article in Journal/Newspaper
genre Arctic
Atlantic Arctic
Atlantic-Arctic
North Atlantic
North Atlantic oscillation
Sea ice
genre_facet Arctic
Atlantic Arctic
Atlantic-Arctic
North Atlantic
North Atlantic oscillation
Sea ice
geographic Arctic
geographic_facet Arctic
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institution Open Polar
language English
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op_doi https://doi.org/10.1038/s41612-022-00275-1
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volume:5
issue:1
journal:NPJ CLIMATE AND ATMOSPHERIC SCIENCE
https://hdl.handle.net/10278/5007460
doi:10.1038/s41612-022-00275-1
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85134268822
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spelling ftuniveneziairis:oai:iris.unive.it:10278/5007460 2025-01-16T20:20:41+00:00 Coupled stratosphere-troposphere-Atlantic multidecadal oscillation and its importance for near-future climate projection Nour-Eddine Omrani Noel Keenlyside Katja Matthes Lina Boljka Davide Zanchettin Johann H. Jungclaus Sandro W. Lubis Omrani, Nour-Eddine Keenlyside, Noel Matthes, Katja Boljka, Lina Zanchettin, Davide Jungclaus, Johann H. Lubis, Sandro W. 2022 https://hdl.handle.net/10278/5007460 https://doi.org/10.1038/s41612-022-00275-1 eng eng info:eu-repo/semantics/altIdentifier/wos/WOS:000824621300001 volume:5 issue:1 journal:NPJ CLIMATE AND ATMOSPHERIC SCIENCE https://hdl.handle.net/10278/5007460 doi:10.1038/s41612-022-00275-1 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85134268822 info:eu-repo/semantics/openAccess Settore GEO/12 - Oceanografia e Fisica dell'Atmosfera info:eu-repo/semantics/article 2022 ftuniveneziairis https://doi.org/10.1038/s41612-022-00275-1 2024-03-21T17:59:54Z Northern Hemisphere (NH) climate has experienced various coherent wintertime multidecadal climate trends in stratosphere, troposphere, ocean, and cryosphere. However, the overall mechanistic framework linking these trends is not well established. Here we show, using long-term transient forced coupled climate simulation, that large parts of the coherent NH-multidecadal changes can be understood within a damped coupled stratosphere/troposphere/ocean-oscillation framework. Wave-induced downward propagating positive stratosphere/troposphere-coupled Northern Annular Mode (NAM) and associated stratospheric cooling initiate delayed thermohaline strengthening of Atlantic overturning circulation and extratropical Atlantic-gyres. These increase the poleward oceanic heat transport leading to Arctic sea-ice melting, Arctic warming amplification, and large-scale Atlantic warming, which in turn initiates wave-induced downward propagating negative NAM and stratospheric warming and therefore reverse the oscillation phase. This coupled variability improves the performance of statistical models, which project further weakening of North Atlantic Oscillation, North Atlantic cooling and hiatus in wintertime North Atlantic-Arctic sea-ice and global surface temperature just like the 1950s-1970s. Article in Journal/Newspaper Arctic Atlantic Arctic Atlantic-Arctic North Atlantic North Atlantic oscillation Sea ice Università Ca’ Foscari Venezia: ARCA (Archivio Istituzionale della Ricerca) Arctic npj Climate and Atmospheric Science 5 1
spellingShingle Settore GEO/12 - Oceanografia e Fisica dell'Atmosfera
Nour-Eddine Omrani
Noel Keenlyside
Katja Matthes
Lina Boljka
Davide Zanchettin
Johann H. Jungclaus
Sandro W. Lubis
Coupled stratosphere-troposphere-Atlantic multidecadal oscillation and its importance for near-future climate projection
title Coupled stratosphere-troposphere-Atlantic multidecadal oscillation and its importance for near-future climate projection
title_full Coupled stratosphere-troposphere-Atlantic multidecadal oscillation and its importance for near-future climate projection
title_fullStr Coupled stratosphere-troposphere-Atlantic multidecadal oscillation and its importance for near-future climate projection
title_full_unstemmed Coupled stratosphere-troposphere-Atlantic multidecadal oscillation and its importance for near-future climate projection
title_short Coupled stratosphere-troposphere-Atlantic multidecadal oscillation and its importance for near-future climate projection
title_sort coupled stratosphere-troposphere-atlantic multidecadal oscillation and its importance for near-future climate projection
topic Settore GEO/12 - Oceanografia e Fisica dell'Atmosfera
topic_facet Settore GEO/12 - Oceanografia e Fisica dell'Atmosfera
url https://hdl.handle.net/10278/5007460
https://doi.org/10.1038/s41612-022-00275-1