Consistent picture of the horizontal circulation of the Atlantic Ocean over three decades
The circulation in the Atlantic Ocean is marked by the complex system of pathways of the Atlantic Meridional Overturning Circulation (AMOC). These currents change meridionally due to the interaction with nearby water masses. Hydrographic data provide the opportunity to characterize these currents fo...
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ftcopernicus:oai:publications.copernicus.org:egusphere109286 2023-07-30T03:59:20+02:00 Consistent picture of the horizontal circulation of the Atlantic Ocean over three decades Caínzos, Verónica Pérez-Hernández, M. Dolores Santana-Toscano, Daniel Arumí-Planas, Cristina Hernández-Guerra, Alonso 2023-07-06 application/pdf https://doi.org/10.5194/egusphere-2023-136 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-136/ eng eng doi:10.5194/egusphere-2023-136 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-136/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2023-136 2023-07-10T16:24:18Z The circulation in the Atlantic Ocean is marked by the complex system of pathways of the Atlantic Meridional Overturning Circulation (AMOC). These currents change meridionally due to the interaction with nearby water masses. Hydrographic data provide the opportunity to characterize these currents for the whole water column with high-resolution data over the last 30 years. Moreover, inverse methods enable the quantification of absolute zonal transports across these sections, determining the strength of each current at a certain latitude in terms of mass, heat, and freshwater, as well as their transport-weighted temperature and salinity. Generally, no changes can be found among decades for each of the currents in terms of transport or their properties. In the South Atlantic, the circulation describes the subtropical gyre affected by several recirculations. There are nearly 61 Sv entering from the Southern and Indian oceans at 45 ∘ S. The South Atlantic subtropical gyre exports 17.0 ± 1.2 Sv and around 1 PW northward via the North Brazil Current, as well as − 55 Sv southward at 45 ∘ S into the Antarctic Circumpolar Current. In the North Atlantic, most of the transport is advected northward via the western boundary currents, which reduce their strength as they take part in convection processes in the subpolar North Atlantic, also reflected in the northward progress of mass and heat transport. Deep layers carry waters southward along the western boundary, maintaining similar values of mass and heat transport until the separation into an eastern branch crossing the mid-Atlantic Ridge in the South Atlantic. Abyssal waters originating in the Southern Ocean are distributed along the South Atlantic mainly through its western subbasin, flowing northward up to 24.5 ∘ N, subjected to an increasing trend in their temperature with time. Text Antarc* Antarctic North Atlantic Southern Ocean Copernicus Publications: E-Journals Antarctic Southern Ocean The Antarctic Indian Mid-Atlantic Ridge |
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Copernicus Publications: E-Journals |
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English |
description |
The circulation in the Atlantic Ocean is marked by the complex system of pathways of the Atlantic Meridional Overturning Circulation (AMOC). These currents change meridionally due to the interaction with nearby water masses. Hydrographic data provide the opportunity to characterize these currents for the whole water column with high-resolution data over the last 30 years. Moreover, inverse methods enable the quantification of absolute zonal transports across these sections, determining the strength of each current at a certain latitude in terms of mass, heat, and freshwater, as well as their transport-weighted temperature and salinity. Generally, no changes can be found among decades for each of the currents in terms of transport or their properties. In the South Atlantic, the circulation describes the subtropical gyre affected by several recirculations. There are nearly 61 Sv entering from the Southern and Indian oceans at 45 ∘ S. The South Atlantic subtropical gyre exports 17.0 ± 1.2 Sv and around 1 PW northward via the North Brazil Current, as well as − 55 Sv southward at 45 ∘ S into the Antarctic Circumpolar Current. In the North Atlantic, most of the transport is advected northward via the western boundary currents, which reduce their strength as they take part in convection processes in the subpolar North Atlantic, also reflected in the northward progress of mass and heat transport. Deep layers carry waters southward along the western boundary, maintaining similar values of mass and heat transport until the separation into an eastern branch crossing the mid-Atlantic Ridge in the South Atlantic. Abyssal waters originating in the Southern Ocean are distributed along the South Atlantic mainly through its western subbasin, flowing northward up to 24.5 ∘ N, subjected to an increasing trend in their temperature with time. |
format |
Text |
author |
Caínzos, Verónica Pérez-Hernández, M. Dolores Santana-Toscano, Daniel Arumí-Planas, Cristina Hernández-Guerra, Alonso |
spellingShingle |
Caínzos, Verónica Pérez-Hernández, M. Dolores Santana-Toscano, Daniel Arumí-Planas, Cristina Hernández-Guerra, Alonso Consistent picture of the horizontal circulation of the Atlantic Ocean over three decades |
author_facet |
Caínzos, Verónica Pérez-Hernández, M. Dolores Santana-Toscano, Daniel Arumí-Planas, Cristina Hernández-Guerra, Alonso |
author_sort |
Caínzos, Verónica |
title |
Consistent picture of the horizontal circulation of the Atlantic Ocean over three decades |
title_short |
Consistent picture of the horizontal circulation of the Atlantic Ocean over three decades |
title_full |
Consistent picture of the horizontal circulation of the Atlantic Ocean over three decades |
title_fullStr |
Consistent picture of the horizontal circulation of the Atlantic Ocean over three decades |
title_full_unstemmed |
Consistent picture of the horizontal circulation of the Atlantic Ocean over three decades |
title_sort |
consistent picture of the horizontal circulation of the atlantic ocean over three decades |
publishDate |
2023 |
url |
https://doi.org/10.5194/egusphere-2023-136 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-136/ |
geographic |
Antarctic Southern Ocean The Antarctic Indian Mid-Atlantic Ridge |
geographic_facet |
Antarctic Southern Ocean The Antarctic Indian Mid-Atlantic Ridge |
genre |
Antarc* Antarctic North Atlantic Southern Ocean |
genre_facet |
Antarc* Antarctic North Atlantic Southern Ocean |
op_source |
eISSN: |
op_relation |
doi:10.5194/egusphere-2023-136 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-136/ |
op_doi |
https://doi.org/10.5194/egusphere-2023-136 |
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1772810113533345792 |