Variability of the thermohaline circulation of the North Atlantic: Sensitivity to overflows of dense water masses
A numerical model of the Atlantic Ocean was used to study the low-frequency variability of meridi-onal transports in the North Atlantic. The model shows a behaviour similar to those used in previous studies, and the temporal variability of certain variables compares favourably to observed time serie...
Published in: | Ocean Dynamics |
---|---|
Main Authors: | , |
Other Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2004
|
Subjects: | |
Online Access: | https://hal.archives-ouvertes.fr/hal-00182980 https://hal.archives-ouvertes.fr/hal-00182980/document https://hal.archives-ouvertes.fr/hal-00182980/file/Beismann2004.pdf https://doi.org/10.1007/s10236-003-0088-x |
id |
ftccsdartic:oai:HAL:hal-00182980v1 |
---|---|
record_format |
openpolar |
spelling |
ftccsdartic:oai:HAL:hal-00182980v1 2023-05-15T17:24:22+02:00 Variability of the thermohaline circulation of the North Atlantic: Sensitivity to overflows of dense water masses Beismann, Jens-Olaf Barnier, Bernard Technische Fakultät der Universität Kiel, Kiel Laboratoire des Écoulements Géophysiques et Industriels Grenoble (LEGI) Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF) 2004 https://hal.archives-ouvertes.fr/hal-00182980 https://hal.archives-ouvertes.fr/hal-00182980/document https://hal.archives-ouvertes.fr/hal-00182980/file/Beismann2004.pdf https://doi.org/10.1007/s10236-003-0088-x en eng HAL CCSD Springer Verlag info:eu-repo/semantics/altIdentifier/doi/10.1007/s10236-003-0088-x hal-00182980 https://hal.archives-ouvertes.fr/hal-00182980 https://hal.archives-ouvertes.fr/hal-00182980/document https://hal.archives-ouvertes.fr/hal-00182980/file/Beismann2004.pdf doi:10.1007/s10236-003-0088-x http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 1616-7341 EISSN: 1616-7228 Ocean Dynamics https://hal.archives-ouvertes.fr/hal-00182980 Ocean Dynamics, Springer Verlag, 2004, 54, pp.92-106. ⟨10.1007/s10236-003-0088-x⟩ [PHYS.MECA.MEFL]Physics [physics]/Mechanics [physics]/Fluid mechanics [physics.class-ph] [SPI.MECA.MEFL]Engineering Sciences [physics]/Mechanics [physics.med-ph]/Fluids mechanics [physics.class-ph] info:eu-repo/semantics/article Journal articles 2004 ftccsdartic https://doi.org/10.1007/s10236-003-0088-x 2021-10-24T00:24:23Z A numerical model of the Atlantic Ocean was used to study the low-frequency variability of meridi-onal transports in the North Atlantic. The model shows a behaviour similar to those used in previous studies, and the temporal variability of certain variables compares favourably to observed time series. By changing the depth and width of the sills between the subpolar North Atlantic and the Nordic Seas, the mean horizontal and overturning circulation as well as some water mass properties are modified significantly. The reaction of meridional oceanic transports to atmospheric forcing fluctuations remains, however, unchanged. The critical role of the surface heat flux retroaction term for the meridional heat transport in stand-alone ocean models is discussed. The experiments underline the role of atmospheric variability for fluctuations of the large-scale ocean circulation on time scales from years to decades, and they support the hypothesis that the mean overturning strength is controlled by the model representation of the density of the overflow water masses. Article in Journal/Newspaper Nordic Seas North Atlantic Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Ocean Dynamics 54 5 537 537 |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
[PHYS.MECA.MEFL]Physics [physics]/Mechanics [physics]/Fluid mechanics [physics.class-ph] [SPI.MECA.MEFL]Engineering Sciences [physics]/Mechanics [physics.med-ph]/Fluids mechanics [physics.class-ph] |
spellingShingle |
[PHYS.MECA.MEFL]Physics [physics]/Mechanics [physics]/Fluid mechanics [physics.class-ph] [SPI.MECA.MEFL]Engineering Sciences [physics]/Mechanics [physics.med-ph]/Fluids mechanics [physics.class-ph] Beismann, Jens-Olaf Barnier, Bernard Variability of the thermohaline circulation of the North Atlantic: Sensitivity to overflows of dense water masses |
topic_facet |
[PHYS.MECA.MEFL]Physics [physics]/Mechanics [physics]/Fluid mechanics [physics.class-ph] [SPI.MECA.MEFL]Engineering Sciences [physics]/Mechanics [physics.med-ph]/Fluids mechanics [physics.class-ph] |
description |
A numerical model of the Atlantic Ocean was used to study the low-frequency variability of meridi-onal transports in the North Atlantic. The model shows a behaviour similar to those used in previous studies, and the temporal variability of certain variables compares favourably to observed time series. By changing the depth and width of the sills between the subpolar North Atlantic and the Nordic Seas, the mean horizontal and overturning circulation as well as some water mass properties are modified significantly. The reaction of meridional oceanic transports to atmospheric forcing fluctuations remains, however, unchanged. The critical role of the surface heat flux retroaction term for the meridional heat transport in stand-alone ocean models is discussed. The experiments underline the role of atmospheric variability for fluctuations of the large-scale ocean circulation on time scales from years to decades, and they support the hypothesis that the mean overturning strength is controlled by the model representation of the density of the overflow water masses. |
author2 |
Technische Fakultät der Universität Kiel, Kiel Laboratoire des Écoulements Géophysiques et Industriels Grenoble (LEGI) Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF) |
format |
Article in Journal/Newspaper |
author |
Beismann, Jens-Olaf Barnier, Bernard |
author_facet |
Beismann, Jens-Olaf Barnier, Bernard |
author_sort |
Beismann, Jens-Olaf |
title |
Variability of the thermohaline circulation of the North Atlantic: Sensitivity to overflows of dense water masses |
title_short |
Variability of the thermohaline circulation of the North Atlantic: Sensitivity to overflows of dense water masses |
title_full |
Variability of the thermohaline circulation of the North Atlantic: Sensitivity to overflows of dense water masses |
title_fullStr |
Variability of the thermohaline circulation of the North Atlantic: Sensitivity to overflows of dense water masses |
title_full_unstemmed |
Variability of the thermohaline circulation of the North Atlantic: Sensitivity to overflows of dense water masses |
title_sort |
variability of the thermohaline circulation of the north atlantic: sensitivity to overflows of dense water masses |
publisher |
HAL CCSD |
publishDate |
2004 |
url |
https://hal.archives-ouvertes.fr/hal-00182980 https://hal.archives-ouvertes.fr/hal-00182980/document https://hal.archives-ouvertes.fr/hal-00182980/file/Beismann2004.pdf https://doi.org/10.1007/s10236-003-0088-x |
genre |
Nordic Seas North Atlantic |
genre_facet |
Nordic Seas North Atlantic |
op_source |
ISSN: 1616-7341 EISSN: 1616-7228 Ocean Dynamics https://hal.archives-ouvertes.fr/hal-00182980 Ocean Dynamics, Springer Verlag, 2004, 54, pp.92-106. ⟨10.1007/s10236-003-0088-x⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1007/s10236-003-0088-x hal-00182980 https://hal.archives-ouvertes.fr/hal-00182980 https://hal.archives-ouvertes.fr/hal-00182980/document https://hal.archives-ouvertes.fr/hal-00182980/file/Beismann2004.pdf doi:10.1007/s10236-003-0088-x |
op_rights |
http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1007/s10236-003-0088-x |
container_title |
Ocean Dynamics |
container_volume |
54 |
container_issue |
5 |
container_start_page |
537 |
op_container_end_page |
537 |
_version_ |
1766115333116002304 |