On the temporal variability of the Weddell Sea Deep Water masses

The Weddell Sea is one of the key regions of the Southern Ocean with respect to climate as most of the Antarctic Bottom Water (AABW) that occupies the world ocean deepest layers is likely to originate from this region. This study applies the Optimum Multiparameter water mass analysis to the Weddell...

Full description

Bibliographic Details
Published in:Antarctic Science
Main Authors: Kerr, Rodrigo, Mata, Mauricio Magalhães, Garcia, Carlos Alberto Eiras
Format: Article in Journal/Newspaper
Language:English
Published: 2009
Subjects:
Online Access:http://repositorio.furg.br/handle/1/1961
https://doi.org/10.1017/S0954102009001990
id ftunivfurg:oai:repositorio.furg.br:1/1961
record_format openpolar
spelling ftunivfurg:oai:repositorio.furg.br:1/1961 2023-11-12T04:04:45+01:00 On the temporal variability of the Weddell Sea Deep Water masses Kerr, Rodrigo Mata, Mauricio Magalhães Garcia, Carlos Alberto Eiras 2009 application/pdf http://repositorio.furg.br/handle/1/1961 https://doi.org/10.1017/S0954102009001990 eng eng KERR, Rodrigo; MATA, Mauricio Magalhães; GARCIA, Carlos Alberto Eiras. On the temporal variability of the Weddell Sea Deep Water masses. Antarctic Science, v.21, n.4, p. 383–400, 2009. Disponível em:<http://journals.cambridge.org/download.php?file=%2FANS%2FANS21_04%2FS0954102009001990a.pdf&code=e60ac8642decea7914e1b68b258da7cd>. Acesso em: 19 mar. 2012. http://repositorio.furg.br/handle/1/1961 doi:10.1017/S0954102009001990 restrict access Antartica OMP analysis Southern Annular Mode Southern Ocean article 2009 ftunivfurg https://doi.org/10.1017/S0954102009001990 2023-10-24T21:01:48Z The Weddell Sea is one of the key regions of the Southern Ocean with respect to climate as most of the Antarctic Bottom Water (AABW) that occupies the world ocean deepest layers is likely to originate from this region. This study applies the Optimum Multiparameter water mass analysis to the Weddell deep waters in order to investigate their distribution and variability. The dataset used is based on the WOCE repeat sections in the area (SR04 and A12) from 1984 to 1998. The mean water mass distribution is consistent with previous knowledge of the region, along with high interannual variability. Regarding the temporal variability, it seems that the years of maximum Weddell Sea Deep Water (WSDW) contribution correspond to the lowest levels of Weddell Sea Bottom Water (WSBW), and vice versa. In order to identify possible forcing mechanisms for such variability, the water mass temporal anomalies were compared with oceanic and atmospheric modes of variability in that region such as the Southern Annular Mode (SAM). An apparent correlation between the SAM index temporal gradients and WSBW anomalies indicate that the Weddell Sea export of dense waters to the world ocean may be linked to that index on several time scales. Article in Journal/Newspaper Antarc* Antarctic Antarctic Science antartic* Southern Ocean Weddell Sea RI FURG (Repositório da Universidade Federal do Rio Grande) Antarctic Southern Ocean The Antarctic Weddell Weddell Sea Antarctic Science 21 04 383
institution Open Polar
collection RI FURG (Repositório da Universidade Federal do Rio Grande)
op_collection_id ftunivfurg
language English
topic Antartica
OMP analysis
Southern Annular Mode
Southern Ocean
spellingShingle Antartica
OMP analysis
Southern Annular Mode
Southern Ocean
Kerr, Rodrigo
Mata, Mauricio Magalhães
Garcia, Carlos Alberto Eiras
On the temporal variability of the Weddell Sea Deep Water masses
topic_facet Antartica
OMP analysis
Southern Annular Mode
Southern Ocean
description The Weddell Sea is one of the key regions of the Southern Ocean with respect to climate as most of the Antarctic Bottom Water (AABW) that occupies the world ocean deepest layers is likely to originate from this region. This study applies the Optimum Multiparameter water mass analysis to the Weddell deep waters in order to investigate their distribution and variability. The dataset used is based on the WOCE repeat sections in the area (SR04 and A12) from 1984 to 1998. The mean water mass distribution is consistent with previous knowledge of the region, along with high interannual variability. Regarding the temporal variability, it seems that the years of maximum Weddell Sea Deep Water (WSDW) contribution correspond to the lowest levels of Weddell Sea Bottom Water (WSBW), and vice versa. In order to identify possible forcing mechanisms for such variability, the water mass temporal anomalies were compared with oceanic and atmospheric modes of variability in that region such as the Southern Annular Mode (SAM). An apparent correlation between the SAM index temporal gradients and WSBW anomalies indicate that the Weddell Sea export of dense waters to the world ocean may be linked to that index on several time scales.
format Article in Journal/Newspaper
author Kerr, Rodrigo
Mata, Mauricio Magalhães
Garcia, Carlos Alberto Eiras
author_facet Kerr, Rodrigo
Mata, Mauricio Magalhães
Garcia, Carlos Alberto Eiras
author_sort Kerr, Rodrigo
title On the temporal variability of the Weddell Sea Deep Water masses
title_short On the temporal variability of the Weddell Sea Deep Water masses
title_full On the temporal variability of the Weddell Sea Deep Water masses
title_fullStr On the temporal variability of the Weddell Sea Deep Water masses
title_full_unstemmed On the temporal variability of the Weddell Sea Deep Water masses
title_sort on the temporal variability of the weddell sea deep water masses
publishDate 2009
url http://repositorio.furg.br/handle/1/1961
https://doi.org/10.1017/S0954102009001990
geographic Antarctic
Southern Ocean
The Antarctic
Weddell
Weddell Sea
geographic_facet Antarctic
Southern Ocean
The Antarctic
Weddell
Weddell Sea
genre Antarc*
Antarctic
Antarctic Science
antartic*
Southern Ocean
Weddell Sea
genre_facet Antarc*
Antarctic
Antarctic Science
antartic*
Southern Ocean
Weddell Sea
op_relation KERR, Rodrigo; MATA, Mauricio Magalhães; GARCIA, Carlos Alberto Eiras. On the temporal variability of the Weddell Sea Deep Water masses. Antarctic Science, v.21, n.4, p. 383–400, 2009. Disponível em:<http://journals.cambridge.org/download.php?file=%2FANS%2FANS21_04%2FS0954102009001990a.pdf&code=e60ac8642decea7914e1b68b258da7cd>. Acesso em: 19 mar. 2012.
http://repositorio.furg.br/handle/1/1961
doi:10.1017/S0954102009001990
op_rights restrict access
op_doi https://doi.org/10.1017/S0954102009001990
container_title Antarctic Science
container_volume 21
container_issue 04
container_start_page 383
_version_ 1782341757438001152