El Niño teleconnection to the Euro-Mediterranean late-winter: the role of extratropical Pacific modulation

International audience Abstract El Niño Southern Oscillation (ENSO) represents the major driver of interannual climate variability at global scale. Observational and model-based studies have fostered a long-standing debate on the shape and intensity of the ENSO influence over the Euro-Mediterranean...

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Published in:Climate Dynamics
Main Authors: Benassi, Marianna, Conti, Giovanni, Gualdi, Silvio, Ruggieri, Paolo, Materia, Stefano, García-Serrano, Javier, Palmeiro, Froila, Batté, Lauriane, Ardilouze, Constantin
Other Authors: Euro-Mediterranean Center on Climate Change (CMCC), Centro Euro-Mediterraneo per i Cambiamenti Climatici Bologna (CMCC), University of Bologna/Università di Bologna, Universitat de Barcelona (UB), Barcelona Supercomputing Center - Centro Nacional de Supercomputacion (BSC - CNS), Centre national de recherches météorologiques (CNRM), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2021
Subjects:
Online Access:https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096
https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096/document
https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096/file/2021_Article_-2.pdf
https://doi.org/10.1007/s00382-021-05768-y
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collection Université de Nantes: HAL-UNIV-NANTES
op_collection_id ftunivnantes
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
Benassi, Marianna
Conti, Giovanni
Gualdi, Silvio
Ruggieri, Paolo
Materia, Stefano
García-Serrano, Javier
Palmeiro, Froila
Batté, Lauriane
Ardilouze, Constantin
El Niño teleconnection to the Euro-Mediterranean late-winter: the role of extratropical Pacific modulation
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
description International audience Abstract El Niño Southern Oscillation (ENSO) represents the major driver of interannual climate variability at global scale. Observational and model-based studies have fostered a long-standing debate on the shape and intensity of the ENSO influence over the Euro-Mediterranean sector. Indeed, the detection of this signal is strongly affected by the large internal variability that characterizes the atmospheric circulation in the North Atlantic–European (NAE) region. This study explores if and how the low-frequency variability of North Pacific sea surface temperature (SST) may impact the El Niño-NAE teleconnection in late winter, which consists of a dipolar pattern between middle and high latitudes. A set of idealized atmosphere-only experiments, prescribing different phases of the anomalous SST linked to the Pacific Decadal Oscillation (PDO) superimposed onto an El Niño-like forcing in the tropical Pacific, has been performed in a multi-model framework, in order to assess the potential modulation of the positive ENSO signal. The modelling results suggest, in agreement with observational estimates, that the PDO negative phase (PDO − ) may enhance the amplitude of the El Niño-NAE teleconnection, while the dynamics involved appear to be unaltered. On the other hand, the modulating role of the PDO positive phase (PDO + ) is not reliable across models. This finding is consistent with the atmospheric response to the PDO itself, which is robust and statistically significant only for PDO − . Its modulation seems to rely on the enhanced meridional SST gradient and the related turbulent heat-flux released along the Kuroshio–Oyashio extension. PDO − weakens the North Pacific jet, whereby favoring more poleward propagation of wave activity, strengthening the El Niño-forced Rossby wave-train. These results imply that there might be conditional predictability for the interannual Euro-Mediterranean climate variability depending on the background state.
author2 Euro-Mediterranean Center on Climate Change (CMCC)
Centro Euro-Mediterraneo per i Cambiamenti Climatici Bologna (CMCC)
University of Bologna/Università di Bologna
Universitat de Barcelona (UB)
Barcelona Supercomputing Center - Centro Nacional de Supercomputacion (BSC - CNS)
Centre national de recherches météorologiques (CNRM)
Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Benassi, Marianna
Conti, Giovanni
Gualdi, Silvio
Ruggieri, Paolo
Materia, Stefano
García-Serrano, Javier
Palmeiro, Froila
Batté, Lauriane
Ardilouze, Constantin
author_facet Benassi, Marianna
Conti, Giovanni
Gualdi, Silvio
Ruggieri, Paolo
Materia, Stefano
García-Serrano, Javier
Palmeiro, Froila
Batté, Lauriane
Ardilouze, Constantin
author_sort Benassi, Marianna
title El Niño teleconnection to the Euro-Mediterranean late-winter: the role of extratropical Pacific modulation
title_short El Niño teleconnection to the Euro-Mediterranean late-winter: the role of extratropical Pacific modulation
title_full El Niño teleconnection to the Euro-Mediterranean late-winter: the role of extratropical Pacific modulation
title_fullStr El Niño teleconnection to the Euro-Mediterranean late-winter: the role of extratropical Pacific modulation
title_full_unstemmed El Niño teleconnection to the Euro-Mediterranean late-winter: the role of extratropical Pacific modulation
title_sort el niño teleconnection to the euro-mediterranean late-winter: the role of extratropical pacific modulation
publisher HAL CCSD
publishDate 2021
url https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096
https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096/document
https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096/file/2021_Article_-2.pdf
https://doi.org/10.1007/s00382-021-05768-y
long_lat ENVELOPE(157.000,157.000,50.000,50.000)
geographic Pacific
Oyashio
geographic_facet Pacific
Oyashio
genre North Atlantic
genre_facet North Atlantic
op_source ISSN: 0930-7575
EISSN: 1432-0894
Climate Dynamics
https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096
Climate Dynamics, 2021, ⟨10.1007/s00382-021-05768-y⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-021-05768-y
meteo-03478096
https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096
https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096/document
https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096/file/2021_Article_-2.pdf
doi:10.1007/s00382-021-05768-y
op_rights http://creativecommons.org/licenses/by/
info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1007/s00382-021-05768-y
container_title Climate Dynamics
container_volume 58
container_issue 7-8
container_start_page 2009
op_container_end_page 2029
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spelling ftunivnantes:oai:HAL:meteo-03478096v1 2023-05-15T17:36:27+02:00 El Niño teleconnection to the Euro-Mediterranean late-winter: the role of extratropical Pacific modulation Benassi, Marianna Conti, Giovanni Gualdi, Silvio Ruggieri, Paolo Materia, Stefano García-Serrano, Javier Palmeiro, Froila Batté, Lauriane Ardilouze, Constantin Euro-Mediterranean Center on Climate Change (CMCC) Centro Euro-Mediterraneo per i Cambiamenti Climatici Bologna (CMCC) University of Bologna/Università di Bologna Universitat de Barcelona (UB) Barcelona Supercomputing Center - Centro Nacional de Supercomputacion (BSC - CNS) Centre national de recherches météorologiques (CNRM) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS) 2021-05-03 https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096 https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096/document https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096/file/2021_Article_-2.pdf https://doi.org/10.1007/s00382-021-05768-y en eng HAL CCSD Springer Verlag info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-021-05768-y meteo-03478096 https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096 https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096/document https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096/file/2021_Article_-2.pdf doi:10.1007/s00382-021-05768-y http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0930-7575 EISSN: 1432-0894 Climate Dynamics https://hal-meteofrance.archives-ouvertes.fr/meteo-03478096 Climate Dynamics, 2021, ⟨10.1007/s00382-021-05768-y⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2021 ftunivnantes https://doi.org/10.1007/s00382-021-05768-y 2023-02-22T02:33:16Z International audience Abstract El Niño Southern Oscillation (ENSO) represents the major driver of interannual climate variability at global scale. Observational and model-based studies have fostered a long-standing debate on the shape and intensity of the ENSO influence over the Euro-Mediterranean sector. Indeed, the detection of this signal is strongly affected by the large internal variability that characterizes the atmospheric circulation in the North Atlantic–European (NAE) region. This study explores if and how the low-frequency variability of North Pacific sea surface temperature (SST) may impact the El Niño-NAE teleconnection in late winter, which consists of a dipolar pattern between middle and high latitudes. A set of idealized atmosphere-only experiments, prescribing different phases of the anomalous SST linked to the Pacific Decadal Oscillation (PDO) superimposed onto an El Niño-like forcing in the tropical Pacific, has been performed in a multi-model framework, in order to assess the potential modulation of the positive ENSO signal. The modelling results suggest, in agreement with observational estimates, that the PDO negative phase (PDO − ) may enhance the amplitude of the El Niño-NAE teleconnection, while the dynamics involved appear to be unaltered. On the other hand, the modulating role of the PDO positive phase (PDO + ) is not reliable across models. This finding is consistent with the atmospheric response to the PDO itself, which is robust and statistically significant only for PDO − . Its modulation seems to rely on the enhanced meridional SST gradient and the related turbulent heat-flux released along the Kuroshio–Oyashio extension. PDO − weakens the North Pacific jet, whereby favoring more poleward propagation of wave activity, strengthening the El Niño-forced Rossby wave-train. These results imply that there might be conditional predictability for the interannual Euro-Mediterranean climate variability depending on the background state. Article in Journal/Newspaper North Atlantic Université de Nantes: HAL-UNIV-NANTES Pacific Oyashio ENVELOPE(157.000,157.000,50.000,50.000) Climate Dynamics 58 7-8 2009 2029