On eddy polarity distribution in the southwestern Atlantic

Eddies in the southwestern Atlantic were detected from more than 18 years of satellite altimetry data using a modified version of the Okubo–Weiss method. The spatial distribution and polarity of eddies were examined. A larger concentration of cyclonic (anticyclonic) eddies was found on the left (rig...

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Published in:Deep Sea Research Part I: Oceanographic Research Papers
Main Authors: Saraceno, Martin, Provost, Christine
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier
Subjects:
Online Access:http://hdl.handle.net/11336/17208
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author Saraceno, Martin
Provost, Christine
author_facet Saraceno, Martin
Provost, Christine
author_sort Saraceno, Martin
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_start_page 62
container_title Deep Sea Research Part I: Oceanographic Research Papers
container_volume 69
description Eddies in the southwestern Atlantic were detected from more than 18 years of satellite altimetry data using a modified version of the Okubo–Weiss method. The spatial distribution and polarity of eddies were examined. A larger concentration of cyclonic (anticyclonic) eddies was found on the left (right) side when looking downstream on some of the largest current systems in the region, such as the South Atlantic Current, the anticyclonic circulation associated with the Zapiola Drift (ZD) and the northern branch of the Antarctic Circumpolar Current. In the region isolated by the anticyclonic Zapiola Current, 91% of eddies were cyclonic. The observed distribution of eddies is in agreement with the generation of eddies from meanders of the above-mentioned currents: cyclonic (anticyclonic) eddies might detach from a meander of the current on the left (right) side when looking downstream on the current. Furthermore, in the ZD area, the bottom topography plays a key role in determining the trajectory of eddies: the anticyclonic current associated with the ZD meanders and eventually generates a cyclonic eddy that enters the ZD region only across the northeastern border, where the gradient of potential vorticity is lower. Finally, average surface chlorophyll-a concentration inside cyclonic and anticyclonic eddies shows that the former have higher chlorophyll-a values. Thus, on average, the classical eddy-pumping theory explains the difference in chlorophyll-a concentration within eddies in the southwestern Atlantic. Fil: Saraceno, Martin. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmosfera. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Centro de Investigaciones del Mar y la Atmosfera; Argentina Fil: Provost, Christine. Universite Pierre et Marie Curie; Francia
format Article in Journal/Newspaper
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
geographic Antarctic
The Antarctic
Argentina
Zapiola
geographic_facet Antarctic
The Antarctic
Argentina
Zapiola
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op_doi https://doi.org/10.1016/j.dsr.2012.07.005
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/17208 2025-01-16T19:42:03+00:00 On eddy polarity distribution in the southwestern Atlantic Saraceno, Martin Provost, Christine application/pdf http://hdl.handle.net/11336/17208 eng eng Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.dsr.2012.07.005 info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0967063712001537 http://hdl.handle.net/11336/17208 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-nd/2.5/ar/ EDDIES SOUTHWESTERN ATLANTIC ZAPIOLA DRIFT https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1016/j.dsr.2012.07.005 2024-10-04T09:34:04Z Eddies in the southwestern Atlantic were detected from more than 18 years of satellite altimetry data using a modified version of the Okubo–Weiss method. The spatial distribution and polarity of eddies were examined. A larger concentration of cyclonic (anticyclonic) eddies was found on the left (right) side when looking downstream on some of the largest current systems in the region, such as the South Atlantic Current, the anticyclonic circulation associated with the Zapiola Drift (ZD) and the northern branch of the Antarctic Circumpolar Current. In the region isolated by the anticyclonic Zapiola Current, 91% of eddies were cyclonic. The observed distribution of eddies is in agreement with the generation of eddies from meanders of the above-mentioned currents: cyclonic (anticyclonic) eddies might detach from a meander of the current on the left (right) side when looking downstream on the current. Furthermore, in the ZD area, the bottom topography plays a key role in determining the trajectory of eddies: the anticyclonic current associated with the ZD meanders and eventually generates a cyclonic eddy that enters the ZD region only across the northeastern border, where the gradient of potential vorticity is lower. Finally, average surface chlorophyll-a concentration inside cyclonic and anticyclonic eddies shows that the former have higher chlorophyll-a values. Thus, on average, the classical eddy-pumping theory explains the difference in chlorophyll-a concentration within eddies in the southwestern Atlantic. Fil: Saraceno, Martin. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmosfera. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Centro de Investigaciones del Mar y la Atmosfera; Argentina Fil: Provost, Christine. Universite Pierre et Marie Curie; Francia Article in Journal/Newspaper Antarc* Antarctic CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Antarctic The Antarctic Argentina Zapiola ENVELOPE(-63.567,-63.567,-65.083,-65.083) Deep Sea Research Part I: Oceanographic Research Papers 69 62 69
spellingShingle EDDIES
SOUTHWESTERN ATLANTIC
ZAPIOLA DRIFT
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Saraceno, Martin
Provost, Christine
On eddy polarity distribution in the southwestern Atlantic
title On eddy polarity distribution in the southwestern Atlantic
title_full On eddy polarity distribution in the southwestern Atlantic
title_fullStr On eddy polarity distribution in the southwestern Atlantic
title_full_unstemmed On eddy polarity distribution in the southwestern Atlantic
title_short On eddy polarity distribution in the southwestern Atlantic
title_sort on eddy polarity distribution in the southwestern atlantic
topic EDDIES
SOUTHWESTERN ATLANTIC
ZAPIOLA DRIFT
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet EDDIES
SOUTHWESTERN ATLANTIC
ZAPIOLA DRIFT
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/17208