Nineteen-year changes in surface salinity in the Southern Ocean south of Australia

International audience A 19-year time series of underway sea surface salinity (SSS) data from the SURVOSTRAL line between Hobart, Australia and Adelie Land, Antarctica has revealed the distinct patterns of seasonal and interannual variability in two key zones of the Southern Ocean: in the Subantarct...

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Published in:Journal of Marine Systems
Main Authors: Morrow, R., Kestenare, E.
Other Authors: Océan du Large et Variabilité Climatique (OLVAC), Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2014
Subjects:
Online Access:https://hal.science/hal-01021088
https://doi.org/10.1016/j.jmarsys.2013.09.011
id ftinsu:oai:HAL:hal-01021088v1
record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic Surface salinity
Seasonal variations
Interannual variations
Sea ice
cover
GLOBAL PRECIPITATION
MIXED-LAYER
VARIABILITY
TASMANIA
PROJECT
MISSION
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
spellingShingle Surface salinity
Seasonal variations
Interannual variations
Sea ice
cover
GLOBAL PRECIPITATION
MIXED-LAYER
VARIABILITY
TASMANIA
PROJECT
MISSION
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
Morrow, R.
Kestenare, E.
Nineteen-year changes in surface salinity in the Southern Ocean south of Australia
topic_facet Surface salinity
Seasonal variations
Interannual variations
Sea ice
cover
GLOBAL PRECIPITATION
MIXED-LAYER
VARIABILITY
TASMANIA
PROJECT
MISSION
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
description International audience A 19-year time series of underway sea surface salinity (SSS) data from the SURVOSTRAL line between Hobart, Australia and Adelie Land, Antarctica has revealed the distinct patterns of seasonal and interannual variability in two key zones of the Southern Ocean: in the Subantarctic Zone and in the Antarctic Zone. Both regions show a weak seasonal freshening of the surface waters over the summer months, with surface waters becoming shallower, warmer and fresher during the summer heating cycle. In the region north of the Subantarctic Front, interannual variations in the summer SSS signature are linked to the latitudinal movements of the Subtropical Front. When this front shifts southward, more high salinity subtropical waters are brought into the domain. Rather than responding to local wind stress forcing, the interannual SSS variability is strongly linked to southward flow from eastern Tasmania (the Tasman outflow), whose decadal variability responds with a 2-3 year delay to remote wind forcing in the South Pacific (Hill et al., 2008). Over this period, variations in the local surface freshwater forcing make a minor contribution to the SURVOSTRAL SSS signature. There appears to be a regime shift in the surface forcing and the SSS response, before and after the large perturbation in 2001-2002. In the Antarctic Zone, the summer SSS signature shows distinct biannual variations that are correlated with upstream sea-ice coverage in the preceding spring. There is no significant correlation between local precipitation changes and the SURVOSTRAL SSS time series. Rather, the integrated effects of upstream sea-ice melt dominate the interannual variations in SSS at the SURVOSTRAL line. Finally, a simple 2D Lagrangian particle analysis shows that in some years the surface waters circulate for a longer time in the northern part of the domain, where their freshwater content may be reduced by mixing with the surrounding waters. (C) 2013 Elsevier B.V. All rights reserved.
author2 Océan du Large et Variabilité Climatique (OLVAC)
Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Morrow, R.
Kestenare, E.
author_facet Morrow, R.
Kestenare, E.
author_sort Morrow, R.
title Nineteen-year changes in surface salinity in the Southern Ocean south of Australia
title_short Nineteen-year changes in surface salinity in the Southern Ocean south of Australia
title_full Nineteen-year changes in surface salinity in the Southern Ocean south of Australia
title_fullStr Nineteen-year changes in surface salinity in the Southern Ocean south of Australia
title_full_unstemmed Nineteen-year changes in surface salinity in the Southern Ocean south of Australia
title_sort nineteen-year changes in surface salinity in the southern ocean south of australia
publisher HAL CCSD
publishDate 2014
url https://hal.science/hal-01021088
https://doi.org/10.1016/j.jmarsys.2013.09.011
geographic Antarctic
Pacific
Southern Ocean
The Antarctic
geographic_facet Antarctic
Pacific
Southern Ocean
The Antarctic
genre Adelie Land
Antarc*
Antarctic
Antarctica
Sea ice
Southern Ocean
genre_facet Adelie Land
Antarc*
Antarctic
Antarctica
Sea ice
Southern Ocean
op_source ISSN: 0924-7963
Journal of Marine Systems
https://hal.science/hal-01021088
Journal of Marine Systems, 2014, 129, pp.472-483. ⟨10.1016/j.jmarsys.2013.09.011⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jmarsys.2013.09.011
hal-01021088
https://hal.science/hal-01021088
doi:10.1016/j.jmarsys.2013.09.011
op_doi https://doi.org/10.1016/j.jmarsys.2013.09.011
container_title Journal of Marine Systems
container_volume 129
container_start_page 472
op_container_end_page 483
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spelling ftinsu:oai:HAL:hal-01021088v1 2023-12-17T10:17:40+01:00 Nineteen-year changes in surface salinity in the Southern Ocean south of Australia Morrow, R. Kestenare, E. Océan du Large et Variabilité Climatique (OLVAC) Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) 2014 https://hal.science/hal-01021088 https://doi.org/10.1016/j.jmarsys.2013.09.011 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jmarsys.2013.09.011 hal-01021088 https://hal.science/hal-01021088 doi:10.1016/j.jmarsys.2013.09.011 ISSN: 0924-7963 Journal of Marine Systems https://hal.science/hal-01021088 Journal of Marine Systems, 2014, 129, pp.472-483. ⟨10.1016/j.jmarsys.2013.09.011⟩ Surface salinity Seasonal variations Interannual variations Sea ice cover GLOBAL PRECIPITATION MIXED-LAYER VARIABILITY TASMANIA PROJECT MISSION [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2014 ftinsu https://doi.org/10.1016/j.jmarsys.2013.09.011 2023-11-22T17:52:07Z International audience A 19-year time series of underway sea surface salinity (SSS) data from the SURVOSTRAL line between Hobart, Australia and Adelie Land, Antarctica has revealed the distinct patterns of seasonal and interannual variability in two key zones of the Southern Ocean: in the Subantarctic Zone and in the Antarctic Zone. Both regions show a weak seasonal freshening of the surface waters over the summer months, with surface waters becoming shallower, warmer and fresher during the summer heating cycle. In the region north of the Subantarctic Front, interannual variations in the summer SSS signature are linked to the latitudinal movements of the Subtropical Front. When this front shifts southward, more high salinity subtropical waters are brought into the domain. Rather than responding to local wind stress forcing, the interannual SSS variability is strongly linked to southward flow from eastern Tasmania (the Tasman outflow), whose decadal variability responds with a 2-3 year delay to remote wind forcing in the South Pacific (Hill et al., 2008). Over this period, variations in the local surface freshwater forcing make a minor contribution to the SURVOSTRAL SSS signature. There appears to be a regime shift in the surface forcing and the SSS response, before and after the large perturbation in 2001-2002. In the Antarctic Zone, the summer SSS signature shows distinct biannual variations that are correlated with upstream sea-ice coverage in the preceding spring. There is no significant correlation between local precipitation changes and the SURVOSTRAL SSS time series. Rather, the integrated effects of upstream sea-ice melt dominate the interannual variations in SSS at the SURVOSTRAL line. Finally, a simple 2D Lagrangian particle analysis shows that in some years the surface waters circulate for a longer time in the northern part of the domain, where their freshwater content may be reduced by mixing with the surrounding waters. (C) 2013 Elsevier B.V. All rights reserved. Article in Journal/Newspaper Adelie Land Antarc* Antarctic Antarctica Sea ice Southern Ocean Institut national des sciences de l'Univers: HAL-INSU Antarctic Pacific Southern Ocean The Antarctic Journal of Marine Systems 129 472 483