Sea Level Trend and Fronts in the South Atlantic Ocean

The understanding of the physical drivers of sea level trend is crucial on global and regional scales. In particular, little is known about the sea level trend in the South Atlantic Ocean in comparison with other parts of the world. In this work, we computed the South Atlantic mean sea level (SAMSL)...

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Published in:Geosciences
Main Authors: Laura A. Ruiz-Etcheverry, Martin Saraceno
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
Online Access:https://doi.org/10.3390/geosciences10060218
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spelling ftmdpi:oai:mdpi.com:/2076-3263/10/6/218/ 2023-08-20T04:09:49+02:00 Sea Level Trend and Fronts in the South Atlantic Ocean Laura A. Ruiz-Etcheverry Martin Saraceno agris 2020-06-03 application/pdf https://doi.org/10.3390/geosciences10060218 EN eng Multidisciplinary Digital Publishing Institute Geophysics https://dx.doi.org/10.3390/geosciences10060218 https://creativecommons.org/licenses/by/4.0/ Geosciences; Volume 10; Issue 6; Pages: 218 sea level trend South Atlantic ocean mass steric height satellite altimetry Text 2020 ftmdpi https://doi.org/10.3390/geosciences10060218 2023-07-31T23:35:22Z The understanding of the physical drivers of sea level trend is crucial on global and regional scales. In particular, little is known about the sea level trend in the South Atlantic Ocean in comparison with other parts of the world. In this work, we computed the South Atlantic mean sea level (SAMSL) trend from 25 years of satellite altimetry data, and we analyzed the contributions of steric height (thermosteric and halosteric components) and ocean mass changes for the period 2005–2016 when all the source data used (Argo, GRACE and satellite altimetry) overlap. The SAMSL trend is 2.65 ± 0.24 mm/yr and is mostly explained by ocean mass trend, which is 2.22 ± 0.21 mm/yr. However, between 50° S–33° S, the steric height component constitutes the main contribution in comparison with the ocean mass component. Within that latitudinal band, three regions with trend values higher than the SAMSL trend are observed when considering 25 years of satellite SLA. In the three regions, a southward displacement of the Subtropical, Subantarctic, and Polar Fronts is observed. The southward shift of the fronts is associated with the strengthening and polar shift of westerly winds and contributes to a clear thermosteric trend that translates to the SLA trend observed in those regions. Text South Atlantic Ocean MDPI Open Access Publishing Geosciences 10 6 218
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic sea level trend
South Atlantic
ocean mass
steric height
satellite altimetry
spellingShingle sea level trend
South Atlantic
ocean mass
steric height
satellite altimetry
Laura A. Ruiz-Etcheverry
Martin Saraceno
Sea Level Trend and Fronts in the South Atlantic Ocean
topic_facet sea level trend
South Atlantic
ocean mass
steric height
satellite altimetry
description The understanding of the physical drivers of sea level trend is crucial on global and regional scales. In particular, little is known about the sea level trend in the South Atlantic Ocean in comparison with other parts of the world. In this work, we computed the South Atlantic mean sea level (SAMSL) trend from 25 years of satellite altimetry data, and we analyzed the contributions of steric height (thermosteric and halosteric components) and ocean mass changes for the period 2005–2016 when all the source data used (Argo, GRACE and satellite altimetry) overlap. The SAMSL trend is 2.65 ± 0.24 mm/yr and is mostly explained by ocean mass trend, which is 2.22 ± 0.21 mm/yr. However, between 50° S–33° S, the steric height component constitutes the main contribution in comparison with the ocean mass component. Within that latitudinal band, three regions with trend values higher than the SAMSL trend are observed when considering 25 years of satellite SLA. In the three regions, a southward displacement of the Subtropical, Subantarctic, and Polar Fronts is observed. The southward shift of the fronts is associated with the strengthening and polar shift of westerly winds and contributes to a clear thermosteric trend that translates to the SLA trend observed in those regions.
format Text
author Laura A. Ruiz-Etcheverry
Martin Saraceno
author_facet Laura A. Ruiz-Etcheverry
Martin Saraceno
author_sort Laura A. Ruiz-Etcheverry
title Sea Level Trend and Fronts in the South Atlantic Ocean
title_short Sea Level Trend and Fronts in the South Atlantic Ocean
title_full Sea Level Trend and Fronts in the South Atlantic Ocean
title_fullStr Sea Level Trend and Fronts in the South Atlantic Ocean
title_full_unstemmed Sea Level Trend and Fronts in the South Atlantic Ocean
title_sort sea level trend and fronts in the south atlantic ocean
publisher Multidisciplinary Digital Publishing Institute
publishDate 2020
url https://doi.org/10.3390/geosciences10060218
op_coverage agris
genre South Atlantic Ocean
genre_facet South Atlantic Ocean
op_source Geosciences; Volume 10; Issue 6; Pages: 218
op_relation Geophysics
https://dx.doi.org/10.3390/geosciences10060218
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/geosciences10060218
container_title Geosciences
container_volume 10
container_issue 6
container_start_page 218
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