Lagged response of Tropical Atlantic Ocean to cold and fresh water pulse from Antarctic sea ice melting

Abstract The formation of dense water masses at polar regions has been largely influenced by climate changes arising from global warming. In this context, based on ensemble simulations with a coupled model we evaluate the meridional shift of a climate signal (i.e., a cold and fresh water input pulse...

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Published in:Anais da Academia Brasileira de Ciências
Main Authors: ANA LAURA R. TORRES, CLAUDIA K. PARISE, LUCIANO P. PEZZI, MICHELLY G. DOS SANTOS QUEIROZ, ADILSON M.B. MACHADO, GABRIEL S. CERVEIRA, GUSTAVO S. CORREIA, WESLEY L. BARBOSA, LEONARDO G. DE LIMA, UESLEI A. SUTIL
Format: Article in Journal/Newspaper
Language:English
Published: Academia Brasileira de Ciências 2021
Subjects:
Q
Online Access:https://doi.org/10.1590/0001-3765202220210800
https://doaj.org/article/2485439c2886417fa371aeab81847a66
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spelling ftdoajarticles:oai:doaj.org/article:2485439c2886417fa371aeab81847a66 2023-05-15T14:06:28+02:00 Lagged response of Tropical Atlantic Ocean to cold and fresh water pulse from Antarctic sea ice melting ANA LAURA R. TORRES CLAUDIA K. PARISE LUCIANO P. PEZZI MICHELLY G. DOS SANTOS QUEIROZ ADILSON M.B. MACHADO GABRIEL S. CERVEIRA GUSTAVO S. CORREIA WESLEY L. BARBOSA LEONARDO G. DE LIMA UESLEI A. SUTIL 2021-04-01T00:00:00Z https://doi.org/10.1590/0001-3765202220210800 https://doaj.org/article/2485439c2886417fa371aeab81847a66 EN eng Academia Brasileira de Ciências http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652022000201110&tlng=en https://doaj.org/toc/1678-2690 1678-2690 doi:10.1590/0001-3765202220210800 https://doaj.org/article/2485439c2886417fa371aeab81847a66 Anais da Academia Brasileira de Ciências, Vol 94, Iss suppl 1 (2021) Sea Ice Melting Freshwater Input Teleconnections Oceanic Bridge Oceanography Science Q article 2021 ftdoajarticles https://doi.org/10.1590/0001-3765202220210800 2022-12-31T12:11:29Z Abstract The formation of dense water masses at polar regions has been largely influenced by climate changes arising from global warming. In this context, based on ensemble simulations with a coupled model we evaluate the meridional shift of a climate signal (i.e., a cold and fresh water input pulse generated from melting of positive Antarctic sea ice (ASI) extremes) towards the Tropical Atlantic Ocean (TAO). This oceanic signal propagated from Southern Ocean towards the equator through the upper layers due to an increase in its buoyance. Its northward shift has given by the Subantarctic Mode Water (SAMW) and Antarctic Intermediate Water (AAIW) flows, that inject cold and fresh mode/intermediate waters from into subtropical basin. The signal has reached low latitudes through the equatorial upwelling and spreads out southwards, through the upper branch of southern subtropical gyre. We concluded that 10 years of coupled simulations was enough time to propagate the climate signal generated by ASI positive extremes melting, which reached TOA around 2 year later. The oceanic connection between Southern Ocean and TAO is indeed established within the timescale analyzed in the study (10 years). Nonetheless, the period needed to completely dissipate the disturbance generated from ASI seems to be longer. Article in Journal/Newspaper Antarc* Antarctic Sea ice Southern Ocean Directory of Open Access Journals: DOAJ Articles Antarctic Southern Ocean Anais da Academia Brasileira de Ciências 94 suppl 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Sea Ice Melting
Freshwater Input
Teleconnections
Oceanic Bridge
Oceanography
Science
Q
spellingShingle Sea Ice Melting
Freshwater Input
Teleconnections
Oceanic Bridge
Oceanography
Science
Q
ANA LAURA R. TORRES
CLAUDIA K. PARISE
LUCIANO P. PEZZI
MICHELLY G. DOS SANTOS QUEIROZ
ADILSON M.B. MACHADO
GABRIEL S. CERVEIRA
GUSTAVO S. CORREIA
WESLEY L. BARBOSA
LEONARDO G. DE LIMA
UESLEI A. SUTIL
Lagged response of Tropical Atlantic Ocean to cold and fresh water pulse from Antarctic sea ice melting
topic_facet Sea Ice Melting
Freshwater Input
Teleconnections
Oceanic Bridge
Oceanography
Science
Q
description Abstract The formation of dense water masses at polar regions has been largely influenced by climate changes arising from global warming. In this context, based on ensemble simulations with a coupled model we evaluate the meridional shift of a climate signal (i.e., a cold and fresh water input pulse generated from melting of positive Antarctic sea ice (ASI) extremes) towards the Tropical Atlantic Ocean (TAO). This oceanic signal propagated from Southern Ocean towards the equator through the upper layers due to an increase in its buoyance. Its northward shift has given by the Subantarctic Mode Water (SAMW) and Antarctic Intermediate Water (AAIW) flows, that inject cold and fresh mode/intermediate waters from into subtropical basin. The signal has reached low latitudes through the equatorial upwelling and spreads out southwards, through the upper branch of southern subtropical gyre. We concluded that 10 years of coupled simulations was enough time to propagate the climate signal generated by ASI positive extremes melting, which reached TOA around 2 year later. The oceanic connection between Southern Ocean and TAO is indeed established within the timescale analyzed in the study (10 years). Nonetheless, the period needed to completely dissipate the disturbance generated from ASI seems to be longer.
format Article in Journal/Newspaper
author ANA LAURA R. TORRES
CLAUDIA K. PARISE
LUCIANO P. PEZZI
MICHELLY G. DOS SANTOS QUEIROZ
ADILSON M.B. MACHADO
GABRIEL S. CERVEIRA
GUSTAVO S. CORREIA
WESLEY L. BARBOSA
LEONARDO G. DE LIMA
UESLEI A. SUTIL
author_facet ANA LAURA R. TORRES
CLAUDIA K. PARISE
LUCIANO P. PEZZI
MICHELLY G. DOS SANTOS QUEIROZ
ADILSON M.B. MACHADO
GABRIEL S. CERVEIRA
GUSTAVO S. CORREIA
WESLEY L. BARBOSA
LEONARDO G. DE LIMA
UESLEI A. SUTIL
author_sort ANA LAURA R. TORRES
title Lagged response of Tropical Atlantic Ocean to cold and fresh water pulse from Antarctic sea ice melting
title_short Lagged response of Tropical Atlantic Ocean to cold and fresh water pulse from Antarctic sea ice melting
title_full Lagged response of Tropical Atlantic Ocean to cold and fresh water pulse from Antarctic sea ice melting
title_fullStr Lagged response of Tropical Atlantic Ocean to cold and fresh water pulse from Antarctic sea ice melting
title_full_unstemmed Lagged response of Tropical Atlantic Ocean to cold and fresh water pulse from Antarctic sea ice melting
title_sort lagged response of tropical atlantic ocean to cold and fresh water pulse from antarctic sea ice melting
publisher Academia Brasileira de Ciências
publishDate 2021
url https://doi.org/10.1590/0001-3765202220210800
https://doaj.org/article/2485439c2886417fa371aeab81847a66
geographic Antarctic
Southern Ocean
geographic_facet Antarctic
Southern Ocean
genre Antarc*
Antarctic
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Sea ice
Southern Ocean
op_source Anais da Academia Brasileira de Ciências, Vol 94, Iss suppl 1 (2021)
op_relation http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652022000201110&tlng=en
https://doaj.org/toc/1678-2690
1678-2690
doi:10.1590/0001-3765202220210800
https://doaj.org/article/2485439c2886417fa371aeab81847a66
op_doi https://doi.org/10.1590/0001-3765202220210800
container_title Anais da Academia Brasileira de Ciências
container_volume 94
container_issue suppl 1
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