Coupled Feedbacks From the Tropical Pacific to the Atlantic Meridional Overturning Circulation

Abstract The tropical Pacific Ocean is a key regulator of Earth's climate, with teleconnections that influence remote locations all around the world. Here we use partially coupled climate model experiments to show that tropical Pacific cooling related to an abrupt Atlantic Meridional Overturnin...

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Published in:Geophysical Research Letters
Main Authors: Bryam Orihuela‐Pinto, Agus Santoso, Matthew H. England, Andréa S. Taschetto
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2023GL103250
https://doaj.org/article/0cb622ec156b494bb6d5811e51828334
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spelling ftdoajarticles:oai:doaj.org/article:0cb622ec156b494bb6d5811e51828334 2024-09-15T18:22:11+00:00 Coupled Feedbacks From the Tropical Pacific to the Atlantic Meridional Overturning Circulation Bryam Orihuela‐Pinto Agus Santoso Matthew H. England Andréa S. Taschetto 2023-10-01T00:00:00Z https://doi.org/10.1029/2023GL103250 https://doaj.org/article/0cb622ec156b494bb6d5811e51828334 EN eng Wiley https://doi.org/10.1029/2023GL103250 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL103250 https://doaj.org/article/0cb622ec156b494bb6d5811e51828334 Geophysical Research Letters, Vol 50, Iss 20, Pp n/a-n/a (2023) Atlantic meridional overturning circulation (AMOC) tropical Pacific Pacific‐North Atlantic teleconnection tropical‐extratropical teleconnection interbasin interactions multidecadal timescale Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2023GL103250 2024-08-05T17:49:23Z Abstract The tropical Pacific Ocean is a key regulator of Earth's climate, with teleconnections that influence remote locations all around the world. Here we use partially coupled climate model experiments to show that tropical Pacific cooling related to an abrupt Atlantic Meridional Overturning Circulation (AMOC) slowdown can strengthen the AMOC by ∼25%. This tropical‐extratropical teleconnection occurs initially via atmospheric Rossby waves propagating from the tropical Pacific to the North Atlantic which alter surface climate conditions locally. These changes facilitate ocean heat loss from the subpolar gyre, favoring enhanced oceanic convection. The AMOC strengthening is subsequently enhanced by anomalous northward salt advection in the Atlantic, with a potential contribution from oceanic wave adjustment triggered by increased Southern Ocean westerly winds. These results highlight the influence of the tropical Pacific on the AMOC on multidecadal timescales and suggest that cold phases of tropical Pacific decadal variability could drive temporary strengthening of the AMOC. Article in Journal/Newspaper North Atlantic Southern Ocean Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 20
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Atlantic meridional overturning circulation (AMOC)
tropical Pacific
Pacific‐North Atlantic teleconnection
tropical‐extratropical teleconnection
interbasin interactions
multidecadal timescale
Geophysics. Cosmic physics
QC801-809
spellingShingle Atlantic meridional overturning circulation (AMOC)
tropical Pacific
Pacific‐North Atlantic teleconnection
tropical‐extratropical teleconnection
interbasin interactions
multidecadal timescale
Geophysics. Cosmic physics
QC801-809
Bryam Orihuela‐Pinto
Agus Santoso
Matthew H. England
Andréa S. Taschetto
Coupled Feedbacks From the Tropical Pacific to the Atlantic Meridional Overturning Circulation
topic_facet Atlantic meridional overturning circulation (AMOC)
tropical Pacific
Pacific‐North Atlantic teleconnection
tropical‐extratropical teleconnection
interbasin interactions
multidecadal timescale
Geophysics. Cosmic physics
QC801-809
description Abstract The tropical Pacific Ocean is a key regulator of Earth's climate, with teleconnections that influence remote locations all around the world. Here we use partially coupled climate model experiments to show that tropical Pacific cooling related to an abrupt Atlantic Meridional Overturning Circulation (AMOC) slowdown can strengthen the AMOC by ∼25%. This tropical‐extratropical teleconnection occurs initially via atmospheric Rossby waves propagating from the tropical Pacific to the North Atlantic which alter surface climate conditions locally. These changes facilitate ocean heat loss from the subpolar gyre, favoring enhanced oceanic convection. The AMOC strengthening is subsequently enhanced by anomalous northward salt advection in the Atlantic, with a potential contribution from oceanic wave adjustment triggered by increased Southern Ocean westerly winds. These results highlight the influence of the tropical Pacific on the AMOC on multidecadal timescales and suggest that cold phases of tropical Pacific decadal variability could drive temporary strengthening of the AMOC.
format Article in Journal/Newspaper
author Bryam Orihuela‐Pinto
Agus Santoso
Matthew H. England
Andréa S. Taschetto
author_facet Bryam Orihuela‐Pinto
Agus Santoso
Matthew H. England
Andréa S. Taschetto
author_sort Bryam Orihuela‐Pinto
title Coupled Feedbacks From the Tropical Pacific to the Atlantic Meridional Overturning Circulation
title_short Coupled Feedbacks From the Tropical Pacific to the Atlantic Meridional Overturning Circulation
title_full Coupled Feedbacks From the Tropical Pacific to the Atlantic Meridional Overturning Circulation
title_fullStr Coupled Feedbacks From the Tropical Pacific to the Atlantic Meridional Overturning Circulation
title_full_unstemmed Coupled Feedbacks From the Tropical Pacific to the Atlantic Meridional Overturning Circulation
title_sort coupled feedbacks from the tropical pacific to the atlantic meridional overturning circulation
publisher Wiley
publishDate 2023
url https://doi.org/10.1029/2023GL103250
https://doaj.org/article/0cb622ec156b494bb6d5811e51828334
genre North Atlantic
Southern Ocean
genre_facet North Atlantic
Southern Ocean
op_source Geophysical Research Letters, Vol 50, Iss 20, Pp n/a-n/a (2023)
op_relation https://doi.org/10.1029/2023GL103250
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2023GL103250
https://doaj.org/article/0cb622ec156b494bb6d5811e51828334
op_doi https://doi.org/10.1029/2023GL103250
container_title Geophysical Research Letters
container_volume 50
container_issue 20
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