Scotia Sea pathways as deduced from Argo floats
7th Euro-Argo Science Meeting, 22-23 October 2019, Athens, Greece We use the Argo floats database to quantify the water transports of the Antarctic Circumpolar Current (ACC) through the Scotia Sea in the upper 2000 m of the water column. The reference velocities are calculated from the speed of the...
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ftcsic:oai:digital.csic.es:10261/199714 2024-02-11T09:58:00+01:00 Scotia Sea pathways as deduced from Argo floats Olivé Abelló, Anna Pelegrí, Josep Lluís Olivé Abelló, Anna 2019-10-22 http://hdl.handle.net/10261/199714 en eng https://www.euro-argo.eu/News-Meetings/Meetings/Euro-Argo-Users-Meetings/7th-Euro-Argo-Science-Meeting/PRESENTATIONS Sí 7th Euro-Argo Science Meeting (2019) http://hdl.handle.net/10261/199714 open Argo floats Scotia Sea Antarctic Circumpolar Current comunicación de congreso http://purl.org/coar/resource_type/c_5794 2019 ftcsic 2024-01-16T10:47:13Z 7th Euro-Argo Science Meeting, 22-23 October 2019, Athens, Greece We use the Argo floats database to quantify the water transports of the Antarctic Circumpolar Current (ACC) through the Scotia Sea in the upper 2000 m of the water column. The reference velocities are calculated from the speed of the floats at the 1000-m parking depth and the relative geostrophic velocities are calculated from the float profiles nearby the selected sections. After removal of all floats deployed too close to the Drake Passage, the number of floats crossing each passage correlates well with the transports, and the individual trajectories allow identifying the preferred pathways. Considering the entire database till October 2018, we identify a total of 253 floats drifting through the Drake Passage with 214 of them following through the North Scotia Ridge passages. This allows reconstructing the vertical hydrographic structure at 25-km resolution from the sea surface to 2000 m. Our results indicate a geostrophic transport of 174.0 Sv in the Drake Passage, with a barotropic component of 114.1 Sv and a baroclinic component of 59.9 Sv, while in the North Scotia Ridge passages the total transport is 192.8 Sv, with a barotropic component of 107.9 Sv and a baroclinic component of 84.9 Sv. Most transport through the Drake and North Scotia Ridge Passages comes from jets associated with the Subantarctic and Polar Fronts, and to a lesser degree the Southern ACC Front. The amount of data is enough to explore the inter-annual variations (through a 5-yr running filter), which illustrates the existence of substantial changes, up to 45.5 Sv through the Drake Passage Peer reviewed Conference Object Antarc* Antarctic Drake Passage Scotia Sea Digital.CSIC (Spanish National Research Council) Antarctic Drake Passage North Scotia Ridge ENVELOPE(-51.431,-51.431,-53.581,-53.581) Scotia Sea The Antarctic |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
English |
topic |
Argo floats Scotia Sea Antarctic Circumpolar Current |
spellingShingle |
Argo floats Scotia Sea Antarctic Circumpolar Current Olivé Abelló, Anna Pelegrí, Josep Lluís Scotia Sea pathways as deduced from Argo floats |
topic_facet |
Argo floats Scotia Sea Antarctic Circumpolar Current |
description |
7th Euro-Argo Science Meeting, 22-23 October 2019, Athens, Greece We use the Argo floats database to quantify the water transports of the Antarctic Circumpolar Current (ACC) through the Scotia Sea in the upper 2000 m of the water column. The reference velocities are calculated from the speed of the floats at the 1000-m parking depth and the relative geostrophic velocities are calculated from the float profiles nearby the selected sections. After removal of all floats deployed too close to the Drake Passage, the number of floats crossing each passage correlates well with the transports, and the individual trajectories allow identifying the preferred pathways. Considering the entire database till October 2018, we identify a total of 253 floats drifting through the Drake Passage with 214 of them following through the North Scotia Ridge passages. This allows reconstructing the vertical hydrographic structure at 25-km resolution from the sea surface to 2000 m. Our results indicate a geostrophic transport of 174.0 Sv in the Drake Passage, with a barotropic component of 114.1 Sv and a baroclinic component of 59.9 Sv, while in the North Scotia Ridge passages the total transport is 192.8 Sv, with a barotropic component of 107.9 Sv and a baroclinic component of 84.9 Sv. Most transport through the Drake and North Scotia Ridge Passages comes from jets associated with the Subantarctic and Polar Fronts, and to a lesser degree the Southern ACC Front. The amount of data is enough to explore the inter-annual variations (through a 5-yr running filter), which illustrates the existence of substantial changes, up to 45.5 Sv through the Drake Passage Peer reviewed |
author2 |
Olivé Abelló, Anna |
format |
Conference Object |
author |
Olivé Abelló, Anna Pelegrí, Josep Lluís |
author_facet |
Olivé Abelló, Anna Pelegrí, Josep Lluís |
author_sort |
Olivé Abelló, Anna |
title |
Scotia Sea pathways as deduced from Argo floats |
title_short |
Scotia Sea pathways as deduced from Argo floats |
title_full |
Scotia Sea pathways as deduced from Argo floats |
title_fullStr |
Scotia Sea pathways as deduced from Argo floats |
title_full_unstemmed |
Scotia Sea pathways as deduced from Argo floats |
title_sort |
scotia sea pathways as deduced from argo floats |
publishDate |
2019 |
url |
http://hdl.handle.net/10261/199714 |
long_lat |
ENVELOPE(-51.431,-51.431,-53.581,-53.581) |
geographic |
Antarctic Drake Passage North Scotia Ridge Scotia Sea The Antarctic |
geographic_facet |
Antarctic Drake Passage North Scotia Ridge Scotia Sea The Antarctic |
genre |
Antarc* Antarctic Drake Passage Scotia Sea |
genre_facet |
Antarc* Antarctic Drake Passage Scotia Sea |
op_relation |
https://www.euro-argo.eu/News-Meetings/Meetings/Euro-Argo-Users-Meetings/7th-Euro-Argo-Science-Meeting/PRESENTATIONS Sí 7th Euro-Argo Science Meeting (2019) http://hdl.handle.net/10261/199714 |
op_rights |
open |
_version_ |
1790593546303045632 |