Modulation of the El Niño teleconnection to the North Atlantic by the tropical North Atlantic during boreal spring and summer

Equatorial Pacific sea surface temperature anomalies (SSTAs) associated with El Niño–Southern Oscillation (ENSO) can influence the North Atlantic European (NAE) region. ENSO tends to be negatively correlated with the North Atlantic Oscillation in winter, while this connection is less clear in boreal...

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Published in:Weather and Climate Dynamics
Main Authors: J. W. Casselman, B. Jiménez-Esteve, D. I. V. Domeisen
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
Online Access:https://doi.org/10.5194/wcd-3-1077-2022
https://doaj.org/article/536340e9db6b4ce1a818f4ffff539623
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spelling ftdoajarticles:oai:doaj.org/article:536340e9db6b4ce1a818f4ffff539623 2023-05-15T17:27:22+02:00 Modulation of the El Niño teleconnection to the North Atlantic by the tropical North Atlantic during boreal spring and summer J. W. Casselman B. Jiménez-Esteve D. I. V. Domeisen 2022-09-01T00:00:00Z https://doi.org/10.5194/wcd-3-1077-2022 https://doaj.org/article/536340e9db6b4ce1a818f4ffff539623 EN eng Copernicus Publications https://wcd.copernicus.org/articles/3/1077/2022/wcd-3-1077-2022.pdf https://doaj.org/toc/2698-4016 doi:10.5194/wcd-3-1077-2022 2698-4016 https://doaj.org/article/536340e9db6b4ce1a818f4ffff539623 Weather and Climate Dynamics, Vol 3, Pp 1077-1096 (2022) Meteorology. Climatology QC851-999 article 2022 ftdoajarticles https://doi.org/10.5194/wcd-3-1077-2022 2022-12-30T20:35:49Z Equatorial Pacific sea surface temperature anomalies (SSTAs) associated with El Niño–Southern Oscillation (ENSO) can influence the North Atlantic European (NAE) region. ENSO tends to be negatively correlated with the North Atlantic Oscillation in winter, while this connection is less clear in boreal spring and summer when the ENSO teleconnection encounters altered background conditions (i.e., a weaker subtropical jet), which can modulate the signal on the way to the NAE region. One such region that modulates the ENSO teleconnection to the NAE region is the tropical North Atlantic (TNA). While several mechanisms exist for this modulation, we center our analysis on the Caribbean region and the Walker cells. In order to isolate the relevant mechanism, we force an idealized atmospheric circulation model with three different seasonally varying sea surface temperature patterns that represent an ENSO event with or without the influence of the TNA, focusing on the decaying phase of ENSO in boreal spring and summer. We find that in boreal spring, the TNA modulates the ENSO teleconnection to the NAE primarily through a propagating Rossby wave train, while in summer, the TNA's influence tends to strengthen the ENSO influence over the NAE sector. Overall, this study offers a deeper understanding of the inter-basin interactions through the Walker cell following an ENSO event and the central role of tropical Atlantic SSTAs in modulating the teleconnection to the NAE region in boreal spring and summer. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Directory of Open Access Journals: DOAJ Articles Pacific Weather and Climate Dynamics 3 3 1077 1096
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Meteorology. Climatology
QC851-999
spellingShingle Meteorology. Climatology
QC851-999
J. W. Casselman
B. Jiménez-Esteve
D. I. V. Domeisen
Modulation of the El Niño teleconnection to the North Atlantic by the tropical North Atlantic during boreal spring and summer
topic_facet Meteorology. Climatology
QC851-999
description Equatorial Pacific sea surface temperature anomalies (SSTAs) associated with El Niño–Southern Oscillation (ENSO) can influence the North Atlantic European (NAE) region. ENSO tends to be negatively correlated with the North Atlantic Oscillation in winter, while this connection is less clear in boreal spring and summer when the ENSO teleconnection encounters altered background conditions (i.e., a weaker subtropical jet), which can modulate the signal on the way to the NAE region. One such region that modulates the ENSO teleconnection to the NAE region is the tropical North Atlantic (TNA). While several mechanisms exist for this modulation, we center our analysis on the Caribbean region and the Walker cells. In order to isolate the relevant mechanism, we force an idealized atmospheric circulation model with three different seasonally varying sea surface temperature patterns that represent an ENSO event with or without the influence of the TNA, focusing on the decaying phase of ENSO in boreal spring and summer. We find that in boreal spring, the TNA modulates the ENSO teleconnection to the NAE primarily through a propagating Rossby wave train, while in summer, the TNA's influence tends to strengthen the ENSO influence over the NAE sector. Overall, this study offers a deeper understanding of the inter-basin interactions through the Walker cell following an ENSO event and the central role of tropical Atlantic SSTAs in modulating the teleconnection to the NAE region in boreal spring and summer.
format Article in Journal/Newspaper
author J. W. Casselman
B. Jiménez-Esteve
D. I. V. Domeisen
author_facet J. W. Casselman
B. Jiménez-Esteve
D. I. V. Domeisen
author_sort J. W. Casselman
title Modulation of the El Niño teleconnection to the North Atlantic by the tropical North Atlantic during boreal spring and summer
title_short Modulation of the El Niño teleconnection to the North Atlantic by the tropical North Atlantic during boreal spring and summer
title_full Modulation of the El Niño teleconnection to the North Atlantic by the tropical North Atlantic during boreal spring and summer
title_fullStr Modulation of the El Niño teleconnection to the North Atlantic by the tropical North Atlantic during boreal spring and summer
title_full_unstemmed Modulation of the El Niño teleconnection to the North Atlantic by the tropical North Atlantic during boreal spring and summer
title_sort modulation of the el niño teleconnection to the north atlantic by the tropical north atlantic during boreal spring and summer
publisher Copernicus Publications
publishDate 2022
url https://doi.org/10.5194/wcd-3-1077-2022
https://doaj.org/article/536340e9db6b4ce1a818f4ffff539623
geographic Pacific
geographic_facet Pacific
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Weather and Climate Dynamics, Vol 3, Pp 1077-1096 (2022)
op_relation https://wcd.copernicus.org/articles/3/1077/2022/wcd-3-1077-2022.pdf
https://doaj.org/toc/2698-4016
doi:10.5194/wcd-3-1077-2022
2698-4016
https://doaj.org/article/536340e9db6b4ce1a818f4ffff539623
op_doi https://doi.org/10.5194/wcd-3-1077-2022
container_title Weather and Climate Dynamics
container_volume 3
container_issue 3
container_start_page 1077
op_container_end_page 1096
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