Driving mechanisms of the variability and long-term trend of the Brazil–Malvinas confluence during the 21st century

Over the last decade, several studies have identified a southward drift of the mean meridional position of the Brazil–Malvinas confluence (BMC). Although this trend has been ascribed to different mechanisms, the most recent study found a reduction of the Malvinas current (MC) as the main reason behi...

Full description

Bibliographic Details
Published in:Climate Dynamics
Main Authors: de Souza, M., Mathis, M., Pohlmann, T.
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:http://hdl.handle.net/21.11116/0000-0004-9AF4-B
http://hdl.handle.net/21.11116/0000-0005-6163-E
id ftpubman:oai:pure.mpg.de:item_3158699
record_format openpolar
spelling ftpubman:oai:pure.mpg.de:item_3158699 2023-08-27T04:04:44+02:00 Driving mechanisms of the variability and long-term trend of the Brazil–Malvinas confluence during the 21st century de Souza, M. Mathis, M. Pohlmann, T. 2019-11 application/pdf http://hdl.handle.net/21.11116/0000-0004-9AF4-B http://hdl.handle.net/21.11116/0000-0005-6163-E eng eng info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-019-04942-7 http://hdl.handle.net/21.11116/0000-0004-9AF4-B http://hdl.handle.net/21.11116/0000-0005-6163-E Climate Dynamics info:eu-repo/semantics/article 2019 ftpubman https://doi.org/10.1007/s00382-019-04942-7 2023-08-02T00:04:07Z Over the last decade, several studies have identified a southward drift of the mean meridional position of the Brazil–Malvinas confluence (BMC). Although this trend has been ascribed to different mechanisms, the most recent study found a reduction of the Malvinas current (MC) as the main reason behind it. It is unclear, however, how this mechanism would persist in the face of global warming and under projected increased winds over the Southern Ocean, as the response of the Antarctic Circumpolar Current (ACC) varies within different Earth System Models (ESM), ultimately impacting the MC. We ran a high-resolution (1 / 12 ∘) ocean model driven with results from the Max-Planck-Institute–ESM to verify how the confluence will respond to anthropogenic climate change, by downscaling results from the pre-industrial control and RCP8.5 scenarios. Our results show that the southward confluence shift is only persistent under anthropogenic forcing and is led by a reduction of the MC volume transport. This reduction of the Malvinas transport is induced by a shift of the main ACC flow closer to Antarctica’s shelf, in response to a southward movement of the westerlies band, even if no long-term changes on the total ACC transport can be found. Our results corroborate previous evidence regarding the MC as the main responsible behind the observed BMC southward shift in the recent past but points toward anthropogenic climate change as the triggering mechanism, with various effects cascading from its impact on the Southern Ocean. This also has consequences for the BMC variability, whose amplitude reduces as we approach the end of the 21st century. © 2019, Springer-Verlag GmbH Germany, part of Springer Nature. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean Max Planck Society: MPG.PuRe Antarctic Southern Ocean The Antarctic Climate Dynamics 53 9-10 6453 6468
institution Open Polar
collection Max Planck Society: MPG.PuRe
op_collection_id ftpubman
language English
description Over the last decade, several studies have identified a southward drift of the mean meridional position of the Brazil–Malvinas confluence (BMC). Although this trend has been ascribed to different mechanisms, the most recent study found a reduction of the Malvinas current (MC) as the main reason behind it. It is unclear, however, how this mechanism would persist in the face of global warming and under projected increased winds over the Southern Ocean, as the response of the Antarctic Circumpolar Current (ACC) varies within different Earth System Models (ESM), ultimately impacting the MC. We ran a high-resolution (1 / 12 ∘) ocean model driven with results from the Max-Planck-Institute–ESM to verify how the confluence will respond to anthropogenic climate change, by downscaling results from the pre-industrial control and RCP8.5 scenarios. Our results show that the southward confluence shift is only persistent under anthropogenic forcing and is led by a reduction of the MC volume transport. This reduction of the Malvinas transport is induced by a shift of the main ACC flow closer to Antarctica’s shelf, in response to a southward movement of the westerlies band, even if no long-term changes on the total ACC transport can be found. Our results corroborate previous evidence regarding the MC as the main responsible behind the observed BMC southward shift in the recent past but points toward anthropogenic climate change as the triggering mechanism, with various effects cascading from its impact on the Southern Ocean. This also has consequences for the BMC variability, whose amplitude reduces as we approach the end of the 21st century. © 2019, Springer-Verlag GmbH Germany, part of Springer Nature.
format Article in Journal/Newspaper
author de Souza, M.
Mathis, M.
Pohlmann, T.
spellingShingle de Souza, M.
Mathis, M.
Pohlmann, T.
Driving mechanisms of the variability and long-term trend of the Brazil–Malvinas confluence during the 21st century
author_facet de Souza, M.
Mathis, M.
Pohlmann, T.
author_sort de Souza, M.
title Driving mechanisms of the variability and long-term trend of the Brazil–Malvinas confluence during the 21st century
title_short Driving mechanisms of the variability and long-term trend of the Brazil–Malvinas confluence during the 21st century
title_full Driving mechanisms of the variability and long-term trend of the Brazil–Malvinas confluence during the 21st century
title_fullStr Driving mechanisms of the variability and long-term trend of the Brazil–Malvinas confluence during the 21st century
title_full_unstemmed Driving mechanisms of the variability and long-term trend of the Brazil–Malvinas confluence during the 21st century
title_sort driving mechanisms of the variability and long-term trend of the brazil–malvinas confluence during the 21st century
publishDate 2019
url http://hdl.handle.net/21.11116/0000-0004-9AF4-B
http://hdl.handle.net/21.11116/0000-0005-6163-E
geographic Antarctic
Southern Ocean
The Antarctic
geographic_facet Antarctic
Southern Ocean
The Antarctic
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
op_source Climate Dynamics
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-019-04942-7
http://hdl.handle.net/21.11116/0000-0004-9AF4-B
http://hdl.handle.net/21.11116/0000-0005-6163-E
op_doi https://doi.org/10.1007/s00382-019-04942-7
container_title Climate Dynamics
container_volume 53
container_issue 9-10
container_start_page 6453
op_container_end_page 6468
_version_ 1775353128171864064