Seasonal and interannual variations of the upper ocean energetics between Tasmania and Antarctica
International audience Nine years of Topex/Poseidon and ERS satellite altimetry and XBT data from the SURVOSTRAL program were used to analyze the seasonal and interannual variations of the eddy energetics in terms of its spatial distribution and relation with the upper ocean heat content. Eddy kinet...
Published in: | Deep Sea Research Part I: Oceanographic Research Papers |
---|---|
Main Authors: | , , |
Other Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2003
|
Subjects: | |
Online Access: | https://hal.science/hal-00765431 https://doi.org/10.1016/S0967-0637(03)00015-3 |
id |
ftmeteofrance:oai:HAL:hal-00765431v1 |
---|---|
record_format |
openpolar |
institution |
Open Polar |
collection |
Météo-France: HAL |
op_collection_id |
ftmeteofrance |
language |
English |
topic |
XBT COURANT MARIN FLUX THERMIQUE ANOMALIE DE TEMPERATURE VARIATION SAISONNIERE VARIATION INTERANNUELLE ALTIMETRIE DONNEES SATELLITE [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
spellingShingle |
XBT COURANT MARIN FLUX THERMIQUE ANOMALIE DE TEMPERATURE VARIATION SAISONNIERE VARIATION INTERANNUELLE ALTIMETRIE DONNEES SATELLITE [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography Morrow, Rosemary Brut, Aurore Chaigneau, Alexis Seasonal and interannual variations of the upper ocean energetics between Tasmania and Antarctica |
topic_facet |
XBT COURANT MARIN FLUX THERMIQUE ANOMALIE DE TEMPERATURE VARIATION SAISONNIERE VARIATION INTERANNUELLE ALTIMETRIE DONNEES SATELLITE [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
description |
International audience Nine years of Topex/Poseidon and ERS satellite altimetry and XBT data from the SURVOSTRAL program were used to analyze the seasonal and interannual variations of the eddy energetics in terms of its spatial distribution and relation with the upper ocean heat content. Eddy kinetic energy is calculated in two frequency bands one associated with transient and the other with low-frequency variability. The two eddy components have distinct geographical distribution. At the SURVOSTRAL line, the transient eddy energy is twice the low-frequency energy, with maximum transient energy occurring during the austral summer period and maximum low-frequency energy in winter. The site is one of growing eddy energy. Eddy momentum flux is northward over the SURVOSTRAL line, and the summertime eddy heat flux is poleward across the Subantarctic and Subtropical Fronts, and equatorward either side of the fronts. Eddy fluxes are strongly influenced by their position relative to the bathymetry and the mean current. |
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) Centre d'études spatiales de la biosphère (CESBIO) 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 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 National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) Echanges Côte-Large (ECOLA) |
format |
Article in Journal/Newspaper |
author |
Morrow, Rosemary Brut, Aurore Chaigneau, Alexis |
author_facet |
Morrow, Rosemary Brut, Aurore Chaigneau, Alexis |
author_sort |
Morrow, Rosemary |
title |
Seasonal and interannual variations of the upper ocean energetics between Tasmania and Antarctica |
title_short |
Seasonal and interannual variations of the upper ocean energetics between Tasmania and Antarctica |
title_full |
Seasonal and interannual variations of the upper ocean energetics between Tasmania and Antarctica |
title_fullStr |
Seasonal and interannual variations of the upper ocean energetics between Tasmania and Antarctica |
title_full_unstemmed |
Seasonal and interannual variations of the upper ocean energetics between Tasmania and Antarctica |
title_sort |
seasonal and interannual variations of the upper ocean energetics between tasmania and antarctica |
publisher |
HAL CCSD |
publishDate |
2003 |
url |
https://hal.science/hal-00765431 https://doi.org/10.1016/S0967-0637(03)00015-3 |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
ISSN: 0967-0637 Deep Sea Research Part I: Oceanographic Research Papers https://hal.science/hal-00765431 Deep Sea Research Part I: Oceanographic Research Papers, 2003, 50, p. 339-356; ISSN 0967-0637. ⟨10.1016/S0967-0637(03)00015-3⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/S0967-0637(03)00015-3 hal-00765431 https://hal.science/hal-00765431 doi:10.1016/S0967-0637(03)00015-3 |
op_doi |
https://doi.org/10.1016/S0967-0637(03)00015-3 |
container_title |
Deep Sea Research Part I: Oceanographic Research Papers |
container_volume |
50 |
container_issue |
3 |
container_start_page |
339 |
op_container_end_page |
356 |
_version_ |
1799485349771083776 |
spelling |
ftmeteofrance:oai:HAL:hal-00765431v1 2024-05-19T07:30:19+00:00 Seasonal and interannual variations of the upper ocean energetics between Tasmania and Antarctica Morrow, Rosemary Brut, Aurore Chaigneau, Alexis 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) Centre d'études spatiales de la biosphère (CESBIO) 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 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 National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) Echanges Côte-Large (ECOLA) 2003 https://hal.science/hal-00765431 https://doi.org/10.1016/S0967-0637(03)00015-3 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/S0967-0637(03)00015-3 hal-00765431 https://hal.science/hal-00765431 doi:10.1016/S0967-0637(03)00015-3 ISSN: 0967-0637 Deep Sea Research Part I: Oceanographic Research Papers https://hal.science/hal-00765431 Deep Sea Research Part I: Oceanographic Research Papers, 2003, 50, p. 339-356; ISSN 0967-0637. ⟨10.1016/S0967-0637(03)00015-3⟩ XBT COURANT MARIN FLUX THERMIQUE ANOMALIE DE TEMPERATURE VARIATION SAISONNIERE VARIATION INTERANNUELLE ALTIMETRIE DONNEES SATELLITE [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography info:eu-repo/semantics/article Journal articles 2003 ftmeteofrance https://doi.org/10.1016/S0967-0637(03)00015-3 2024-04-25T00:45:50Z International audience Nine years of Topex/Poseidon and ERS satellite altimetry and XBT data from the SURVOSTRAL program were used to analyze the seasonal and interannual variations of the eddy energetics in terms of its spatial distribution and relation with the upper ocean heat content. Eddy kinetic energy is calculated in two frequency bands one associated with transient and the other with low-frequency variability. The two eddy components have distinct geographical distribution. At the SURVOSTRAL line, the transient eddy energy is twice the low-frequency energy, with maximum transient energy occurring during the austral summer period and maximum low-frequency energy in winter. The site is one of growing eddy energy. Eddy momentum flux is northward over the SURVOSTRAL line, and the summertime eddy heat flux is poleward across the Subantarctic and Subtropical Fronts, and equatorward either side of the fronts. Eddy fluxes are strongly influenced by their position relative to the bathymetry and the mean current. Article in Journal/Newspaper Antarc* Antarctica Météo-France: HAL Deep Sea Research Part I: Oceanographic Research Papers 50 3 339 356 |