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...
Published in: | Deep Sea Research Part I: Oceanographic Research Papers |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
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Elsevier
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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 |
id | ftconicet:oai:ri.conicet.gov.ar:11336/17208 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-63.567,-63.567,-65.083,-65.083) |
op_collection_id | ftconicet |
op_container_end_page | 69 |
op_doi | https://doi.org/10.1016/j.dsr.2012.07.005 |
op_relation | 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 |
op_rights | info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-nd/2.5/ar/ |
publisher | Elsevier |
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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 |