Mean Antarctic Circumpolar Current Transport Measured in Drake Passage
- Autores
- Donohue, K. A.; Tracey, K. L.; Watts, D. R.; Chidichimo, María Paz; Chereskin, T. K.
- Año de publicación
- 2016
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The Antarctic Circumpolar Current is an important component of the global climate system connecting the major ocean basins as it flows eastward around Antarctica, yet due to the paucity of data it remains unclear how much water is transported by the current. Between 2007 and 2011 flow through Drake Passage was continuously monitored with a line of moored instrumentation with unprecedented horizontal and temporal resolution. Annual mean near-bottom currents are remarkably stable from year to year. The mean depth-independent, or barotropic transport, determined from the near-bottom current meter records was 45.6 Sv with an uncertainty of 8.9 Sv. Summing the mean barotropic transport with the mean baroclinic transport relative to zero at the seafloor of 127.7 Sv gives a total transport through Drake Passage of 173.3 Sv. This new measurement is 30% larger than the canonical value often used as the benchmark for global circulation and climate models.
Fil: Donohue, K. A.. University Of Rhode Island; Estados Unidos
Fil: Tracey, K. L.. University Of Rhode Island; Estados Unidos
Fil: Watts, D. R.. University Of Rhode Island; Estados Unidos
Fil: Chidichimo, María Paz. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Ministerio de Defensa. Armada Argentina. Servicio de Hidrografía Naval; Argentina. Universidad de Buenos Aires; Argentina
Fil: Chereskin, T. K.. University of California at San Diego. Scripps Institution of Oceanography; Estados Unidos - Materia
-
ANTARCTIC CIRCUMPOLAR CURRENT
OBSERVATIONS WITH UNPRECEDENTED RESOLUTION
MEAN TRANSPORT 30% HIGHER THAN HISTORICAL ESTIMATE - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/47067
Ver los metadatos del registro completo
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Mean Antarctic Circumpolar Current Transport Measured in Drake PassageDonohue, K. A.Tracey, K. L.Watts, D. R.Chidichimo, María PazChereskin, T. K.ANTARCTIC CIRCUMPOLAR CURRENTOBSERVATIONS WITH UNPRECEDENTED RESOLUTIONMEAN TRANSPORT 30% HIGHER THAN HISTORICAL ESTIMATEhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Antarctic Circumpolar Current is an important component of the global climate system connecting the major ocean basins as it flows eastward around Antarctica, yet due to the paucity of data it remains unclear how much water is transported by the current. Between 2007 and 2011 flow through Drake Passage was continuously monitored with a line of moored instrumentation with unprecedented horizontal and temporal resolution. Annual mean near-bottom currents are remarkably stable from year to year. The mean depth-independent, or barotropic transport, determined from the near-bottom current meter records was 45.6 Sv with an uncertainty of 8.9 Sv. Summing the mean barotropic transport with the mean baroclinic transport relative to zero at the seafloor of 127.7 Sv gives a total transport through Drake Passage of 173.3 Sv. This new measurement is 30% larger than the canonical value often used as the benchmark for global circulation and climate models.Fil: Donohue, K. A.. University Of Rhode Island; Estados UnidosFil: Tracey, K. L.. University Of Rhode Island; Estados UnidosFil: Watts, D. R.. University Of Rhode Island; Estados UnidosFil: Chidichimo, María Paz. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Ministerio de Defensa. Armada Argentina. Servicio de Hidrografía Naval; Argentina. Universidad de Buenos Aires; ArgentinaFil: Chereskin, T. K.. University of California at San Diego. Scripps Institution of Oceanography; Estados UnidosAmerican Geophysical Union2016-11info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/47067Donohue, K. A.; Tracey, K. L.; Watts, D. R.; Chidichimo, María Paz; Chereskin, T. K.; Mean Antarctic Circumpolar Current Transport Measured in Drake Passage; American Geophysical Union; Geophysical Research Letters; 43; 11-2016; 1-80094-8276CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1002/2016GL070319/abstractinfo:eu-repo/semantics/altIdentifier/doi/10.1002/2016GL070319info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T10:00:19Zoai:ri.conicet.gov.ar:11336/47067instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 10:00:19.652CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Mean Antarctic Circumpolar Current Transport Measured in Drake Passage |
title |
Mean Antarctic Circumpolar Current Transport Measured in Drake Passage |
spellingShingle |
Mean Antarctic Circumpolar Current Transport Measured in Drake Passage Donohue, K. A. ANTARCTIC CIRCUMPOLAR CURRENT OBSERVATIONS WITH UNPRECEDENTED RESOLUTION MEAN TRANSPORT 30% HIGHER THAN HISTORICAL ESTIMATE |
title_short |
Mean Antarctic Circumpolar Current Transport Measured in Drake Passage |
title_full |
Mean Antarctic Circumpolar Current Transport Measured in Drake Passage |
title_fullStr |
Mean Antarctic Circumpolar Current Transport Measured in Drake Passage |
title_full_unstemmed |
Mean Antarctic Circumpolar Current Transport Measured in Drake Passage |
title_sort |
Mean Antarctic Circumpolar Current Transport Measured in Drake Passage |
dc.creator.none.fl_str_mv |
Donohue, K. A. Tracey, K. L. Watts, D. R. Chidichimo, María Paz Chereskin, T. K. |
author |
Donohue, K. A. |
author_facet |
Donohue, K. A. Tracey, K. L. Watts, D. R. Chidichimo, María Paz Chereskin, T. K. |
author_role |
author |
author2 |
Tracey, K. L. Watts, D. R. Chidichimo, María Paz Chereskin, T. K. |
author2_role |
author author author author |
dc.subject.none.fl_str_mv |
ANTARCTIC CIRCUMPOLAR CURRENT OBSERVATIONS WITH UNPRECEDENTED RESOLUTION MEAN TRANSPORT 30% HIGHER THAN HISTORICAL ESTIMATE |
topic |
ANTARCTIC CIRCUMPOLAR CURRENT OBSERVATIONS WITH UNPRECEDENTED RESOLUTION MEAN TRANSPORT 30% HIGHER THAN HISTORICAL ESTIMATE |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
The Antarctic Circumpolar Current is an important component of the global climate system connecting the major ocean basins as it flows eastward around Antarctica, yet due to the paucity of data it remains unclear how much water is transported by the current. Between 2007 and 2011 flow through Drake Passage was continuously monitored with a line of moored instrumentation with unprecedented horizontal and temporal resolution. Annual mean near-bottom currents are remarkably stable from year to year. The mean depth-independent, or barotropic transport, determined from the near-bottom current meter records was 45.6 Sv with an uncertainty of 8.9 Sv. Summing the mean barotropic transport with the mean baroclinic transport relative to zero at the seafloor of 127.7 Sv gives a total transport through Drake Passage of 173.3 Sv. This new measurement is 30% larger than the canonical value often used as the benchmark for global circulation and climate models. Fil: Donohue, K. A.. University Of Rhode Island; Estados Unidos Fil: Tracey, K. L.. University Of Rhode Island; Estados Unidos Fil: Watts, D. R.. University Of Rhode Island; Estados Unidos Fil: Chidichimo, María Paz. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Ministerio de Defensa. Armada Argentina. Servicio de Hidrografía Naval; Argentina. Universidad de Buenos Aires; Argentina Fil: Chereskin, T. K.. University of California at San Diego. Scripps Institution of Oceanography; Estados Unidos |
description |
The Antarctic Circumpolar Current is an important component of the global climate system connecting the major ocean basins as it flows eastward around Antarctica, yet due to the paucity of data it remains unclear how much water is transported by the current. Between 2007 and 2011 flow through Drake Passage was continuously monitored with a line of moored instrumentation with unprecedented horizontal and temporal resolution. Annual mean near-bottom currents are remarkably stable from year to year. The mean depth-independent, or barotropic transport, determined from the near-bottom current meter records was 45.6 Sv with an uncertainty of 8.9 Sv. Summing the mean barotropic transport with the mean baroclinic transport relative to zero at the seafloor of 127.7 Sv gives a total transport through Drake Passage of 173.3 Sv. This new measurement is 30% larger than the canonical value often used as the benchmark for global circulation and climate models. |
publishDate |
2016 |
dc.date.none.fl_str_mv |
2016-11 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/47067 Donohue, K. A.; Tracey, K. L.; Watts, D. R.; Chidichimo, María Paz; Chereskin, T. K.; Mean Antarctic Circumpolar Current Transport Measured in Drake Passage; American Geophysical Union; Geophysical Research Letters; 43; 11-2016; 1-8 0094-8276 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/47067 |
identifier_str_mv |
Donohue, K. A.; Tracey, K. L.; Watts, D. R.; Chidichimo, María Paz; Chereskin, T. K.; Mean Antarctic Circumpolar Current Transport Measured in Drake Passage; American Geophysical Union; Geophysical Research Letters; 43; 11-2016; 1-8 0094-8276 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1002/2016GL070319/abstract info:eu-repo/semantics/altIdentifier/doi/10.1002/2016GL070319 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
American Geophysical Union |
publisher.none.fl_str_mv |
American Geophysical Union |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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13.13397 |